A Halo of Storms and Heatwaves — New Study Confirms that Global Warming is Wrecking the Northern Hemisphere Jet Stream

“We came as close as one can to demonstrating a direct link between climate change and a large family of extreme recent weather events.”Michael Mann

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The Earth is warming, the weather is growing more extreme, and from the observational perspective, it appears that the Northern Hemisphere Jet Stream has undergone some seriously disturbing changes. Over the past five years, this subject has been one that’s spurred heated debate among scientists, meteorologists, and global climate and weather watchers. Now, a new model study finds that it’s likely that the Jet Stream is being significantly altered by human-forced climate change and that this alteration is helping to drive extreme weather events like the 2003 European heat wave, the 2010 Pakistan flood and Russian heat wave, the 2011 Texas heat wave and recent floods in Europe.

(More extreme variation in upper level wind speeds is an upshot of polar warming during boreal summer. The result is that risks of severe heatwaves, droughts, wildfires and floods increases as the Earth warms. Image source: Michael Mann, Penn State.)

From the study:

… our analysis of both historical model simulations and observational surface temperature data, strongly suggests that anthropogenic warming is impacting the zonal mean temperature profile in a manner conducive to wave resonance and a consequent increase in persistent weather extremes in the boreal summer.

What this means is that the new study provides still more evidence that the Jet Stream’s north to south variance is increasing during summer. As a result, it is enabling powerful heat domes to form in regions where winds run from south to north. In regions where the upper level winds run from north to south, it creates cooler zones in which powerful storms can flood large swaths of countryside. In other words, increasingly juxtapposed zones of extreme temperature anomalies and higher atmospheric instability and moisture loading tend to form more and more often. And this results in weather patterns that we have never really seen before.

(An Inconvenient Sequel is a call for action on climate change like we’ve never seen before. And the imperative to act on climate is now stronger than it ever was.)

The fact that the Mann study uses observational and model assessments to find that such changes are likely to very likely now being caused by human-forced warming and related polar amplification is a highly significant scientific finding. It adds one more attribution tie to the extreme weather events that we’ve been seeing with increasing frequency. A tie directly to global warming. And it does so through model studies that identify the underlying physical mechanisms at work. It’s a pivotal moment in the atmospheric sciences. And everyone needs to sit up and pay attention.

Credits: 

Hat tip to Colorado Bob

Hat tip to Cate

Scientific hat tip to Dr Michael Mann

(Please support publicly-funded, non-special interest based science that is now under assault by the climate change denying Trump Administration)

Powerful Cyclone to Blow Hole in Thinning Arctic Sea Ice

Back in 2012, a powerful Arctic cyclone smashed the sea ice with days of wind and waves. This year, a storm that’s nearly as strong threatens to make a similar mark on late-season melt. With a very unstable Arctic weather pattern in play, there’s an outlier possibility the dynamic is setting up for something even more dramatic by late August.

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Earlier today, a strong gale roared up out of the Laptev Sea north of central Siberia. Feeding on the abnormally warm, moist air over the Barents Sea and the hot air over northwestern Siberia, the storm collided with comparatively cold air over the central Arctic. The differences between hot/cold and damp/dry air can really bomb out a storm system.

Arctic Cyclone

(Storms, heat and moisture feed up through a high-amplitude wave in the Jet Stream over northern Europe and Siberia and into a developing Arctic cyclone over the Laptev Sea during the early hours of August 15, 2016. Image source: LANCE MODIS.)

Central pressures in the storm fell to 969 millibars and the winds whipping out over the Laptev, East Siberian, and central Arctic waters gusted at 45 to 55 miles per hour. Waves of 6 to 10 feet or higher roared through the newly-opened waters filled with increasingly dispersed ice floes.

The Great Arctic Cyclone of 2016?

This powerful storm is pulling these strong winds over some of the weakest and thinnest sections of Arctic sea ice. During July and August a huge section of ice running along the 80° North Latitude line and stretching from the Laptev, through the East Siberian Sea, and into the Beaufort Sea grew ever more thin and eventually dispersed. Now 25 to 60 percent ice concentrations in this region abound — a tongue of thinning which stretches nearly to the North Pole itself.

Powerful Arctic Cyclone

(A powerful storm running out of the Laptev Sea and into the central Arctic is threatening sea ice with strong winds, large waves, and the motion of abnormally warm surface waters. Image source: Earth Nullschool.)

The storm is generating waves, mixing warmer-than-normal surface waters with even higher temperature waters just below. These sea surfaces are between 1 and 2 degrees Celsius above average over much of the area, with pockets of 3 or even 4 C above normal surface water temperatures interspersed. The storm’s Coriolis Effect will spin chunks of ice out from the pack to float lonely in these warmer-than-normal waters as they are churned by the raging swells.

Storm Raging Over Warm Waters, Thin Ice

Currently, the storm’s strongest winds and waves are running through a big melt wedge that extends from the Laptev and East Siberian Seas toward the 85th parallel. The motion and force produced by the storm’s winds and waves will eject the ice currently located over the northern East Siberian and Chukchi Seas even as waves eat into it. Upwelling of warm water in the seas beneath the center of the storm will open and disperse the ice, generating holes and polynya as it tracks north of the 85th parallel and toward the Pole.

Thin Arctic Sea Ice

(Very low concentrations of ice, like those seen in this Uni Bremen image, are vulnerable to disruption and melting by storms during August and early September. Current ice thinning and dispersal are among the worst seen for any year. With a powerful storm now raging over the ice, impacts to end-season totals could be significant. Image source: Universität Bremen.)

Compared to the Great Arctic Cyclone (GAC) of 2012 — an event that helped to tip that year into the strongest late-season melt on record — this storm is a bit weaker. The GAC bottomed out at 963 mb and carried on for about four days. The current storm, by comparison, is expected to remain in place for quite some time even as it slowly weakens over the coming days.

Arctic sea-ice extent values are now tracking at around third lowest on record, or just above the 2007 line. Such a strong storm certainly has the potential to knock a big hole in the ice, possibly propelling 2016 closer to 2007 ranges or even beyond them. Surface waters in the Laptev, East Siberian, Chukchi, and Beaufort Seas aren’t quite as warm as they were in 2012, but there’s still a lot of potential here for storm-associated melt. Meanwhile, the very warm waters over the Kara and Barents Seas remain a disturbing feature.

Arctic in hot water

(Above-average sea-surface temperatures during late summer have more potential to rapidly melt sea ice when they are churned up and put into motion by powerful storms. Image source: NOAA NCEP.)

Models predict that lows will continue to feed in from the Atlantic and northeastern Siberia along various high-amplitude waves in the Jet Stream to combine in a triangular bite between the East Siberian Sea, the Laptev Sea and the Pole. Such continued reinvigoration will tend to enforce a generally stormy and unstable atmosphere. And there’s some risk (small, but worth considering) that the current storm could refire into something more powerful on the fuel provided by one of these lows.

Troubling Atmospheric Instability Loads the Dice for Future Bombification

Already, a few of the long-range models are popping with amazing predictions of storm-center intensity in the range of 950 to 960 mb. Both the GFS model and CMC models separately produced these results for the nine to 12 day timeframe. GFS had backed off its own high-intensity forecast when this odd CMC run popped up (see below).

CMC Arctic Megacyclone

(CMC 10-day forecast model run showing an extremely powerful 955-mb low just north of Svalbard on August 25th. Such a storm is low-probability at this time, but its formation would likely result in serious impacts to sea ice. Image source: Tropical Tidbits.)

Though these are long-range outliers, there is quite a lot of fuel for strong storms in the region this year due to conditions related to human-caused climate change. In particular, ocean surfaces in the Barents and Kara Seas are in record-hot ranges. And the heat and moisture coming off those waters is fuel for some serious atmospheric instability as the Polar region attempts to cool. Any significant cooling in the 80-90° North Latitude region would help to generate a strong dipole between this zone and the Kara-Barents. Such a dipole would create strong instability for storm generation.

A low bombing out at 953 to 955 mb in ten days, as the CMC model currently indicates, would represent an Arctic megacyclone with serious potential to wreck sea ice. The location predicted would generate a strong push of warm water from the Barents and Laptev and on toward the ice-clogged polar waters. The resulting Ekman pumping and powerful swell generation would have the potential to generate severe ice losses in the late August timeframe.

Probabilities for such a storm this far out are low, but given the underlying conditions, it’s worth putting a marker out. This is, therefore, a situation to watch. We’ve already got one strong storm blowing away at the ice. A one-two punch would hurt even more. In other words, the situation in the Arctic just got really interesting. Let’s just hope it doesn’t tilt into scary…

Links:

Big Cyclone

LANCE MODIS

Earth Nullschool

Universität Bremen

Ice vs. Storm

NOAA NCEP

Tropical Tidbits

Early Warning Signs for James Hansen’s Superstorms Visible — North Atlantic Cool Pool As Harbinger to “All Hell Breaking Loose”

Extreme weather. It’s something that’s tough to predict 2 weeks out, much less 2 decades. But for more than twenty years Dr James Hansen has been warning that the out-flush of cold water from glaciers in Greenland and Canada into the North Atlantic could set up a storm-producing weather pattern the likes of which human civilization has never seen. An atmospheric wrecking ball in the form of an intense cold-hot dipole that, once firmly established over Atlantic Ocean waters between North American and Europe, would carry on in brutally destructive fashion for decades and decades. In other words, as Dr. Hansen says in the below video, “all hell would break loose.”

His recent and, what might well be called, earth-shattering paper on the subject — Ice Melt, Sea Level Rise, and Superstorms — takes a good, hard look at both the potential for exponentially ramping rates of ice melt and sea level rise over the coming decades and the impact those thousands of cubic kilometers of fresh water ramming out into the North Atlantic would have in producing a barrage of increasingly intense superstorms.

(Hansen addresses his concerns about the potential for increasingly severe storms and rapid sea level rise if human fossil fuel emissions do not stop soon in the above video.)

Early Evidence That All Hell is Starting to Break Loose

How could this happen? And what might it look like?

These are questions Hansen valiantly attempts to tackle. And according to him, in addition to a growing number of top climate researchers like Dr. Jason Box and Dr. Stephan Ramhstorf (please see Dr. Jason Box’s very salient take on the new Hansen study here), we may already be starting to witness signs of the wrenching oceanic and atmospheric shift that would produce these terrible weather systems.

For what we see now is the visible formation of a large cool pool in the North Atlantic. One that appears to be developing due to an increasingly rapid rate of Greenland melt. One that may be setting up atmospheric conditions for the age of storms that Hansen has feared could arise. An event resulting from a rampant human fossil fuel emission and a related very rapid injection of heat into the Earth System.

North Atlantic Cool Pool

(Composite global temperature anomaly data from NOAA for 2013 through 2015 provides evidence of the early start to the formation of a possible superstorm-producing North Atlantic cool pool. Image source: Climate Crocks.)

How might this cool pool become such a powerful storm generator? It could well be thought of as an ironic matter of atmospheric and ocean physics. Ironic in the sense that overall global heating produces a severe weather hazard in the form of a large area of cool ocean surface water.

Increased warming of the Earth results in more rapid warming at the poles, especially in the Northern Hemisphere. In turn, this polar amplification sets off a number of feedback loops in which ice in Greenland and West Antarctica begin to melt faster and faster. The ironic atmospheric relationship to large slabs of ice sliding off the great ice sheets and into the ocean begins to come into play. For a thin veil of fresh water from these increasingly massive volumes of melting ice begin to lock more and more heat into the local ocean system.

Over hundreds of thousands of square kilometers, the fresh water begins to cut off the ocean’s ability to ventilate heat into the airs above. As a result, the surface of the ocean and the local atmosphere cools. More heat is shoved into the deeper waters — where it can melt the sea facing glaciers ever more rapidly even as it gets to doing the dangerous work destabilizing carbon stores on the sea bed. Dangerous — not only for its potential to add more greenhouse gasses to the world atmosphere, but also for its ability to develop anoxic dead zones in the ocean depths and to expand those life-killing layers toward the sea surface.

Climate Change’s War Between Hot and Cold — Understanding the Warning Signs

In scientific terms, we call this a stratified ocean state. But in plainer words, we could think of it as a big mechanism for heat exchange and ocean and atmospheric chemistry change.

Where Hot and Cold Collide

(Anyone who knows anything about ocean and atmospheric physics should be concerned about this picture. Here we see the April 8, 2016 ocean surface temperature anomaly reanalysis provided by Earth Nullschool and developed from data collected by NCEP and the National Weather Service. Here we see a large swath of Gulf Stream waters ranging from 5-8 C above average temperatures coming into collision with waters in a North Atlantic cool pool ranging from 1-10 C below average. It is the increasing difference in temperature, or thermal gradient, between these two ocean zones that Hansen and others identify as having a high potential for very severe storm generation.)

Changing the ocean’s heat relationship with the atmosphere is bound to alter the weather. And Hansen’s paper points toward a serious risk that this fundamentally altered relationship will result in much more powerful storms. A cooler North Atlantic will collide with all kinds of expanding heat from various regions. A backed up Gulf Stream will warm up — it already has. The tropics will begin to heat up, increasing the temperature gradient between the lower Latitudes and the cool pool in the North Atlantic. Such conditions amp up the atmospheric storm potential by producing an abundance of what storms feed on — very extreme differences in temperatures, related strong winds and atmospheric vortexes, strong south to north and north to south air flows that link the tropics to the pole, and an ever-growing abundance of moisture bleeding off the record warm waters that come into increasing collision with the expanding pool of cold to the north. Such conditions risk the development of extraordinarily powerful storms in this region. Storms the likes of which our civilizations have never seen before. Storms that may leap the boundaries of their formation zones to have far broader impacts.

Hansen, in his paper found evidence that such conditions may well have existed during the last warm period between ice ages around 115,000 years ago. Back then, a huge flush of ice bergs running out from a melting Greenland during the peak period of warmth appears to have produced terrible storms in the North Atlantic. Storms powerful enough to pluck 2,000 ton boulders up out of the sea bed and hurl them 100 feet above sea level before depositing them onto the hills of places like Bermuda and the Bahama islands.

During that period, the rate of warming was slower. So the pace of melt was likely also slower than what we would see due to human warming. The atmospheric changes were thus milder than those we are likely to experience if human warming continues along its current path and sets the dramatic melt and related atmospheric wrenching into motion. Already, we see storms the likes of which history has never seen running into the UK and Ireland, aiming their increasingly powerful winds and rains at Western Europe. Already we see climate change enhanced superstorms. New forms of severe weather. Hellacious mergings of devastating hurricanes with extraordinary nor’easters.

But what we see now is nothing compared to what we will see if Hansen’s research is anywhere near the mark and if human fossil fuel burning continues unabated. What we risk, and what Hansen has warned us about in what he considers to be his most important work of science, is setting off a severe chain of events that includes rapid sea level rise and powerful, powerful storms. In addition, the ocean stratification that is the cause of all this atmospheric and oceanic trouble would set off further consequences not touched on in Hansen’s work — hitting ocean health hard and, likely, liberating more carbon stores from the Earth System to add to the troubles that humans (and particularly the fossil fuel special interests) are already rapidly bringing to the fore.

One final point — the Hansen paper has and will continue to generate a huge controversy in the science. But from the point of view of this threat analyst, there is a high potential for dangerous outcomes similar to those the Hansen paper warns of together with a number of additional troubles so long as the human-forced warming continues. And we already see visible evidence of those kinds of dangerous atmospheric and ocean changes starting to happen now.

Links:

Ice Melt, Sea Level Rise, Superstorms

The Storms of My Grandchildren

Human Warming Pushing Seas to Exponentially Rise

Dr Jason Box’s Take on the New Hansen Study

Earth Nullschool

NCEP

National Weather Service

Hurricane Sandy — the Storm that Climate Change Wrought

 

Dr James Hansen — Human Warming Pushing Seas Toward Exponential Rise of Several Meters This Century

Continued high fossil fuel emissions this century are predicted to yield … nonlinearly growing sea level rise, reaching several meters over a timescale of 50–150 years. Statement from a new scientific study led by Dr James Hansen entitled Ice Melt, Sea Level Rise, and Superstorms.

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This week, Dr James Hansen and colleagues published one hell of a groundbreaking bit of scientific research. It’s a multi-disciplinary study incorporating the work of 19 top climate scientists, glaciologists, paleoclimatologists, and other Earth Systems researchers. Scientists from NASA, GEOMAR, JPL, and other top research agencies including recognized names like Dr Eric Rignot and Dr Makiko Sato all appear on the contributors list.

Global mean sea level change

(Rates of sea level rise since 1900 and associated with a 1.1 C jump in global temperatures have already shown a non-linear progression. Ice Melt, Sea Level Rise, and Superstorms attempts to pin down just how fast glacial melt rates will increase over the coming decades.)

The paper covers three topics related to the rapid accumulation of fossil fuel driven greenhouse gasses in the atmosphere and related rapid warming — Ice Melt, Sea Level Rise, and Superstorms. In other words, the paper looks into what will likely be the initiation of a Heinrich Event during the 21st Century so long as high levels of human greenhouse gas emissions continue.

A Heinrich Event for the 21st Century

For those not familiar with a Heinrich Event — it’s one of those disastrous climate change related incidents that you really don’t want to see emerge. One that drives rapid sea level rise, wrenching climate dislocations, and is likely also a trigger for regional and possibly hemispheric superstorms. Something that’s occurred numerous times in the geological past when the great Greenland and West Antarctic ice sheets warmed enough to disgorge armadas of ice bergs into the North Atlantic and/or Southern Ocean. The kind of thing that scientist Steve Pacala called a Climate Monster in the Closet. And Dr. James Hansen and colleagues’ new study is the first of its kind to scientifically explore the potential occurrence of just such a freak and dangerous event during the 21st Century.

Because the paper covers such a broad range of topics related to Heinrich Events, I’ve decided to write a two-blog post covering it. This post will focus on the ice melt and sea level rise issues. The superstorm-generating aspect of Heinrich Events — which Dr Hansen and colleagues found was capable of producing waves powerful enough to pluck 1,000 ton boulders from the sea floor and deposit them upon hillsides in the Bahamas 130 feet above sea level 115,000 years ago — is something we’ll cover in a second related post over the next few days.

Warm Ocean Waters Attacking Weak Glacial Underbellies

The chief driver of Heinrich Events is spiking rates of glacial melt issuing from the Greenland and West Antarctic ice sheets and related outflow of ice bergs and fresh water into the North Atlantic or the Southern Ocean. Hansen and colleagues’ paper builds on recent work by Eric Rignot and others who’ve found that the contact of warming ocean waters with the submerged sea faces of glacial cliffs and undersides of floating ice shelves is a primary driver for melt and ice berg release during periods of local and global temperature increase.

Heinrich Event Amplifying Feedbacks

(Illustration from Ice Melt, Sea Level Rise, and Superstorms shows how ocean stratification acts as an amplifying feedback to glacial melt. Cool, fresh surface waters generated by the initial ice release set up a kind of ocean heat conveyor belt that delivers more and more warm water to the submerged underbellies of the great ice sheets. In Greenland, prograde beds limit the amount of ice that can be released in sudden events. In Antarctica, retrograde beds below sea level set up a situation where the amplifying melt feedback is further enhanced.)

Grounding glaciers and ice shelves are, at first, weakened by slow but ramping melt rates. Eventually, the glaciers and shelves collapse due to the weakening process of melt which leads to a surge of previously buttressed ice sliding out into the oceans. As more fresh melt water expands over the ocean surface, it traps heat into deeper layers of the water column near the submerged glacial faces. So initial melt produces an amplifying feedback that delivers more ocean heat to the ice and, in turn, results in more ice rushing out into the North Atlantic or the Southern Ocean.

Exponential Rates of Glacial Melt and Sea Level Rise

It is this mechanism that Hansen and colleagues fear will come into play over the course of the 21st Century. Their paper identifies a risk that such a mechanism could set up 5, 10, or 20 year melt doubling times for Greenland, West Antarctica or both this Century. A new perspective from some of the world’s top scientists that assumes the risk of non linear melt is high enough to present a major concern. As an example, under a 10 year doubling time, the current approximate 3 mm per year sea level rise would double to 6 mm per year by 2026, 12 mm per year by 2036, 2.4 cm per year by 2046, and nearly 5 cm per year by 2056.

Doubling times in non linear events often don’t fit a pure exponential curve — instead tending to follow a series of spikes and recessions with major transitional events coming at the end of any ‘curve.’ But Hansen’s particular perspective is useful given the fact that current rates of sea level rise do not appear to be following a linear pattern and due to the fact that the mechanism for large, Heinrich Event type glacial melt spikes is becoming more supported in the observational science.

Rate of Greenland Antarctica Mass Change

(It’s still early days for Greenland and Antarctic melt. However, current trend lines do point toward a potential for multi-meter sea level rise this Century. Image source: Ice Melt, Sea Level Rise, and Superstorms.)

Early measures of Greenland and Antarctica ice mass loss imply 8-19 year melt doubling times for Greenland and 5-10 year melt doubling times for Antarctica. For reference, if both these ice systems continued to double mass loss on a roughly 10 year basis, total sea level rise by the 2090s would equal 5 meters or 16.4 feet. By contrast, a 5 year doubling time would result in 5 meters of sea level rise by the late 2050s and a 20 year doubling time would result in nearly a meter of sea level rise by the end of this Century and 5 meters worth of sea level rise by 2160.

Hansen notes that these are still early days and it is unlikely that ice sheet response trends have become clear at this stage. However, initial trend lines, though likely to be less accurate, appear to pose some cause for concern. In addition, Hansen points out that rates of sea level rise are less likely to be constrained by ice sheet inertia during periods when global temperatures are rapidly rising. Projected rates of global temperature increase in the range of 1-5 C this Century is on the order 20-100 times faster than during the end of the last ice age — at the upper end covering all of the 10,000 years worth of ice age warming in just one Century. And Hansen notes that this potentially extreme rate of temperature increase poses a much greater risk of rapid glacial destabilization than is indicated by current IPCC glacial melt models.

Hansen’s research also points to the likelihood that rapid glacial melt would temporarily put a break on rates of global atmospheric warming by cooling local ocean surfaces and increasing the rate of heat transfer into middle ocean layers. And it’s this energy flip-flop and related heightened imbalance that provides a pretty severe potential storm set-up as rates of glacial melt ramp up.

Links:

Ice Melt, Sea Level Rise, and Superstorms

Climate Guru James Hansen Warns of Much Worse Than Expected Sea Level Rise

Dr James Hansen

Dr Eric Rignot

Dr Makiko Sato

Heinrich Event

Climate Monsters We Want to Keep in the Closet

Melting in West Antarctica Could Raise Seas By 3 Meters

Hat Tip to DT Lange

Hat Tip to Colorado Bob

Hat Tip to TodaysGuestIs

Gale After Gale After Gale Dumped Two and a Half Feet of Rain Upon Scotland and Wales This Winter

Reports from the UK Met Office are in. And we can say now with confidence that the UK have never seen weather like what they experienced this Winter. It looks like a storm track super-charged by climate change really socked it to the region this year. That we’ve just passed a winter worse than the then record years of 2013 and 2014 — only two years on.

A Stormy New Climate State for the North Atlantic

For the UK and for North Atlantic weather stability in general, the sea surface temperature anomaly signature in the graphic below is bad news. The cool pool just south of Greenland (indicated by the swatch of pale blue) is a new climate feature. One that appears to be related to glacial ice melt outflow from Greenland.

North Atlantic Sea Surface Temperatures

(10 degree Celsius above average sea surface temperatures off North America in today’s ensemble sea surface temperature model graphic are just insanely warm. Ocean surface anomalies used to rarely exceed 2 degrees Celsius warmer than average. These spikes off North America are an indication that the Gulf Stream is backing up and that overturning circulation off Greenland is slowing down. Image source: RTG-SST/NCEP /US National Weather Service/Earth Nullschool.)

Such melt outflow tends to slightly freshen sea surface waters. Freshening waters keep more heat locked into the ocean’s depths. They tend to cool the surface waters. And they slow down an ocean overturning circulation that, in the North Atlantic, drives the flow of the Gulf Stream.

A slowing Gulf Stream delivers less heat to this zone even as it piles more heat up off the North American Coast. As a result, a warm west, cool east dipole tends to develop. In the cool region south of Greenland, unusually strong storms have developed more and more frequently — with a dramatic impact on UK weather. The storms feed on this temperature differential even as they have gorged on heat and moisture streaming northward in a meridional flow over Western Europe. The results this year were nothing short of record-shattering.

Hottest and Wettest

For England and Wales, with temperatures ranging about 2 degrees Celsius above average for December, January and February, 2015-2016 probably beat out 2007 and 1989 as the hottest Winter on record. Meanwhile, Wales and Scotland saw the most rainfall ever recorded — with totals for both regions hitting around 756 millimeters or about two and one half feet. That’s even more rainfall than the previous record stormy Winter of 2013 and 2014.

Yet one more Gale

(Yet one more gale sets up to hammer Ireland, the UK and Scotland by Thursday. Four months of ongoing stormy conditions appears set to continue through to at least mid-March. Image source: NOAA’s Ocean Prediction Center.)

These heavy rains set off severe floods and damaged homes, roads, and bridges throughout the UK with the worst damage focusing in on regions to the North. One heavy precipitation hot spot — Argyll — saw an extraordinary 1035 mm or 3.5 feet of rainfall over the three month period. The Met Office is quick to point out that though December, January and February were the wettest on record since 1910, heavy rainfall events began in November — resulting in what amounts to a relentless four month pounding as storm followed storm and flood followed flood.

And, it appears, this persistent and ongoing storm pattern has not yet changed. For the North Atlantic remains riled — setting up to hurl a new gale-force low at Ireland and the UK this week. With the weather pattern essentially stuck in stormy since November, folks from these regions have got to be asking — when’s it going to end? As storms continue to fire off in the dipole zone above, it appears it will likely last until at least mid-March.

Links:

The UK Met Office

NOAA’s Ocean Prediction Center

World Ocean Heartbeat Fading

RTG-SST/NCEP /US National Weather Service/Earth Nullschool

Winter of 2015/2016 Wettest on Record for Scotland

Mystery Deepens Around Greenland Cold Spot

Hat tip to Colorado Bob

Hat tip to TodaysGuestIs

Hat tip to Dan Combs

 

 

 

 

 

 

A Blizzard Roars Out of Climate Change’s Heart — Polar Warming and A Record Hot Atlantic Ocean Brew Up Nightmare Storm for US East Coast

There’s a historic blizzard in the form of Winter Storm Jonas setting its sights on the US East Coast. The storm is slowly coming together Thursday evening and now appears to be set to paralyze a 1,000 mile swath under 1 to 2.5 feet of snow even as it hurls a substantial storm surge and 40-60 mph winds at waterfront cities from Norfolk to Boston. A monster storm whose predicted formation has made headlines since Tuesday. But what you won’t hear most major news sources mention is the likelihood that this gathering storm has been dramatically impacted by a number of new climate features related to a human-forced warming of the globe.

Jonas Begins its Ocean-heat Fueled Rampage in Southeastern US

(Jonas begins its ocean-heat-fueled rampage on the evening of Thursday, January 21. Image source: NOAA.)

A Warming Arctic Shoves the Cold Air Out

To understand how climate change helped make Jonas so extreme, it’s best if we start our tale in the Arctic. For if we could mark an area on the Earth’s surface that is at the very heart of impacts for human-caused climate change it would be in that zone of the far north above the 66th parallel. It is there that we see the most dramatic, most rapid changes — to ice, to weather, to the thawing lands, to life itself. But unlike what might be said of an American city made famous by its penchant for sin — what happens in the Arctic doesn’t stay in the Arctic.

This is especially true when it comes to weather. If the Arctic cools, it influences the Jet Stream, strengthens the storm track and shuts more cold air away in the Arctic. But if the Arctic warms, as it has more and more frequently during recent years, then the flood-gates open and cold, Arctic air pours outward — filling the deep, inevitable dips in the Jet Stream that then develop.

And it is a massive accumulation of Arctic heat over the past few weeks that has forced Arctic temperatures, in places, to rocket to above 36 degrees Fahrenheit (20 degrees C) warmer than average. A heating up of the entire region to 2-3 degrees Celsius warmer than the already warmer than average 1979- 2000 baseline. An Arctic warm-up that muscled out a howling torrent of cold air that then raged on into a deep trough in the Jet Stream now forming over the eastern half of the United States.

Hot Arctic, Cold, Stormy Eastern USMangled Jet Stream, Raging Storm Track

(An Arctic that is, on average 2.02 C hotter than normal on Friday joins with a high amplitude wave in the Jet Stream and together drives a massive flood of cold air into eastern parts of the US on Friday. Cold air slamming head on into unprecedented heat and moisture bleeding of the Atlantic Ocean to form the historic weather event that is now in the pipe. Image source: Climate Reanalyzer.)

CAPE — Storms Fueled by Cold Colliding With Hot

In weather parlance, a trough, or a big dip in the Jet Stream is a storm generation zone. The reason has to do with the nature of how extreme differences in temperature and moisture can provide fuel for strong storms. It’s this very temperature differential that sits as the cornerstone of our current understanding of how extreme storms are fueled in terms of Convective Available Potential Energy (CAPE).

In the one case, cold air can’t hold as much water in suspension as warm air. So a big flood of cold air can often fuel major precipitation events when coming into collision with hot, moisture-laden air. As hot and cold air are sandwiched closer together, winds — at both the upper and lower levels — tend to increase in velocity. The higher the difference in temperature, the stronger the winds. When these winds run along a big dip in the Jet Stream — like the one now racing over the US East Coast — they can spin off twists and vortexes that can rapidly develop into powerful low pressure systems.

The lows then feed on the difference in temperatures between the two sides of the dividing air-mass — cold on the one side, and hot, wet on the other. The bigger the differential, the more heat and moisture on one side, and the more cold on the other side, the more potential that such low pressure centers will develop into monster storms. The more potential that the storms will develop these crazy atmospheric sandwiches of hot and cold air that really crank out the extreme weather.

Dulles International Airport 5 inch per hour thundersnow potential identified

(“Tremendous Vertical Motion.” Anthony Sagliani tweets about extreme CAPE for a blizzard zeroing in on the US East Coast. What’s important to mention is that human-forced climate change has CAPE written all over it. Image source: Anthony Sagliani.)

In terms of the current storm, some of the CAPE potentials coming in are just off the charts. The above graphic, posted in this recent tweet by Anthony Sagliani, identifies the potential for 5 inch per hour thundersnow at Dulles International Airport (AID) between 2 AM and 2 PM Saturday. To be very clear, a 1 inch per hour snowfall was once considered an extreme event. Now we are looking at possibly 5!

A Record Hot Atlantic Feeds it All

In the context of human-driven climate change, this is one of the reasons why our warming up of the world can generate extreme weather. It warms the Earth unevenly. It puts cold next to hot by driving cold out of the polar zones and by warming up huge areas of land and ocean. And it dumps more moisture into the atmosphere through an amplified evaporation from these greatly warmed Earth surfaces. Mix it all together and you get Anthony Sagliani’s ‘tremendous vertical motion.’

How does this work? In two words — latent heat. More specifically the convective heat energy available in water vapor. And where does most of that latent heat energy come from? It comes, for the most part, in the form of warm waters evaporating into the air above the world’s oceans. More specifically to our current storm it comes in the form of record warm to near record warm temperatures in the waters of the Gulf Stream off the US East Coast (See Dr Jeff Master’s ‘The Future of Intense Winter Storms”).

image

(Sea surface temperatures off the US East Coast are more comparable to those seen during Summer than what would be typical for January. A 76 degree sea surface off Norfolk will provide a massive amount of heat and moisture to fuel the new kind of storm that is Jonas. Image source: Earth Nullschool.)

As Dr. Michael Mann noted in a tweet earlier this week, sea surface temperatures off the US East Coast are extraordinarily warm for this time of year. And Bill McKibben was absolutely astute in saying that these near record temperatures “should turbo-charge this weekend’s blizzard.”

And they’re absolutely ridiculously warm — in the range of 76 degrees Fahrenheit in a region about 150 miles due east of Norfolk, Virginia. A region of ocean over which the developing storm center will directly cross. An area of water that is now in the range of 7 degrees Celsius above average (13 degrees Fahrenheit). For the ocean surface, this is screaming hot — more typical to summer than anything one would expect to see in January, even in the Gulf Stream.

You just don’t see these kinds of temperature departures for the ocean — or at least you didn’t before human-caused climate change started to ramp up. But now we have them — an ocean surface hot enough to support a hurricane but one that will this weekend provide fuel for a blizzard. So the kind of blizzard we will have will not at all be like even the usual blizzards of the 20th Century. This is the new, worse variety that will sadly become more frequent. Destructive, heavy snowfall in the 4-5 inches per hour range, thundersnow and storm surges combined, swaths of hundreds of miles impacted and crippled. The kind for the new age of a human-heated atmosphere — destabilized to produce freak storms of a ferocity and frequency the likes of which we have never seen.

UPDATE — Snowfall Begins With Some Models Showing 4 Feet or More Possible (Average Guidance For Gaithersburg is 24-30 Inches)

Moderate snowfall began at 1:35 PM on Friday in my hometown of Gaithersburg, MD. Model guidance for our area is in the range of 24-30 inches, with as much as 4 feet coming up in some of the GFS ensembles.

Will be posting videos and related updates every 2-3 hours as conditions change.

UPDATE: 1-2 Inches on the Ground at Gaithersburg, MD as of 3:42 PM

(See Video of 3:42 PM snowfall here)

Wind and rates of snowfall have picked up somewhat over the past two hours. As of 3:42 PM, about 1-2 inches had fallen and the wind was visibly swaying some of the tree branches outside. Reports are coming in from regions to the south of a very heavy band of snow that should arrive in our area by later this evening.

Radar captures by the National Weather Service indicate this band setting up over much of Central and Eastern North Carolina — stretching northward through just west of Richmond. GFS model tracking and satellite confirmation indicate a coastal low developing in the region of Northern South Carolina. This low is beginning to transfer Atlantic moisture into the storm — pulling strong winds off that abnormally warm region of ocean just east of Norfolk and into the developing powerful snowfall band.

Jonas 420 PM NWS Radar

(Image source: National Weather Service.)

Sustained winds along the coast are now approaching gale force.  We should expect these winds to rapidly increase over the afternoon and evening hours even as the moisture feed and rate of snowfall intensifies.

UPDATE: Rate of Snowfall Still Picking up at 6:05 PM; Heavy Bands Expected by 10 PM

(See Video of 6:05 PM Snowfall Here)

Rates of snowfall continue to steadily increase for the Gaithersburg Area. As of 6:05 PM EST on Friday, 3-4 inches lay on the ground in Montgomery County Maryland. A heavy band of snow continued to gather to the south as the storm center went ongoing intensification near the border of South Carolina and North Carolina and just off-shore. Guidance provided by that National Weather Service indicates that heaviest rates of snowfall are still about 4 hours away. Radar indicates this band is forming just north of Richmond at this time.

UPDATE: At 10:30 PM, Heavy Snow Settles in with Six Inches Already on the Ground

(See 10:30 PM Video Here)

As of 1030 PM, heavy bands of snow had started to stream into the Gaithersburg area. Winds were picking up — in the range of 15-25 mph with some higher gusts. A healthy covering of about six inches of snowfall already lay on the ground. National weather service radar at this time indicated a series of stronger bands of precipitation just south of DC and moving northward. Meanwhile, atmospheric analysis indicates the center of Jonas now over Eastern North Carolina and strengthening. Over the next 6-12 hours Jonas is expected to intensify as it traverses toward the Chesapeake Bay. This should bring increasingly intense bands of snowfall over the area.

UPDATE: 1:35 AM Intense, Heavy Snow, 10-12 Inches on the Ground, Howling Gusts

By 1:35 AM, conditions again deteriorated for the region of Montgomery County. Snow accumulations had hit between 10 and 12 inches and the winds were really starting to howl and moan.

National Weather Service Radar indicated that the low pressure center had moved out over the Chesapeake Bay even as the wide-ranging storm really started to pull in substantial amounts of heat and moisture off the Atlantic. This kicked the storm into a higher intensity that will likely last, for the DC region, until around 1 PM tomorrow. We are entering the period of most intense storminess and snowfall now. Over the coming hours conditions could get quite extreme with 2-5 inch per hour snowfall rates and thundersnow in some areas. In other words — we’re starting to hit the height of this long-duration event.

Storm Really Starting to Crank Up Severe Snowfall over DC Area

National Weather Service Radar above shows very heavy snowfall bands moving directly over the DC Metro area at this time even as the Atlantic moisture feed grows more intense. Regional snowfall forecasts have remained quite extraordinary with most locations in the area now expecting between 18 and 40 inches. Still one heck of a night ahead!

Links:

NOAA (Please support public, non-special-interest based science, like the fantastic work done by the experts at NOAA)

Dr Jennifer Francis

Dr Michael E Mann

Bill McKibben

Anthony Sagliani

Dr. Jeff Masters: The Future of Intense Winter Storms

Jonas to Wallop 1,000 Mile Swath of US East Coast

Climate Reanalyzer

Convective Available Potential Energy (CAPE)

Earth Nullschool

Hat Tip to DT Lange

Hat tip to Colorado Bob

 

More Signs of Gulf Stream Slowdown as Floods Devastate Cumbria, England

Back in 2009 heavy rains fell over the Northern UK. The rains, abnormally intense, pushed river levels to heights never before measured. A wall of water built-up. Surging over banks, it inundated the town of Carlisle, Cumbria, England — forcing many to flee to higher ground.

At the time, weather forecasters and climatologists wondered if there might have been a global warming link to the freak Cumbria floods. There was certainly risk. Risk that the North Atlantic would become a mess of storms as the Gulf Stream slowed down and cold air masses collided with warm — developing a raging storm track to the west of the UK. A climate situation with the potential to draw in never-before-seen rivers of moisture and set off flooding the likes of which the UK has never known. Flood defenses were shored up. New commitments were made to shift the country away from carbon emissions.

But in just six short years many of those commitments have lagged. Funding for flood defenses was cut by conservatives in the UK parliament even as similar funds for wind and solar energy were targeted in favor of fracking the countryside for natural gas. The usual litany of climate change denial spewed out of the regular conservative mouthpieces in the politics and the media. It was the height of hubris and mismanagement. And again we have a ‘never before seen’ rainstorm roaring up out of a greatly troubled North Atlantic.

*****

Sands Center Carlisle River Level

(On December 6 of 2015 river levels at Sands Centre in Carlisle hit 8 meters above the typical range. The previous record highest level for this river gauge was 4.5 meters — a level the new flood defense systems were designed to contain. But this week’s rainfall simply overwhelmed both flood defenses and previous expectations for the upper limits of extreme weather. Image source: Shoothill Gauge Map.)

On Saturday and Sunday of December 5th and 6th, 2015, Cumbria flooded again. An even higher flood surge than before overwhelmed the new defenses and forced residents to yet again flee. Then, just three days later on Wednesday more than two months worth of rain fell over the Cumbria region. The amount at 341 mm in just 24 hours was a new UK record and compares to average total rainfall for the month of December at 146 mm. The county was again overwhelmed by water. Human chains were formed to help bring those stranded to safety. After the waters began to subside — devastation. More than 6,000 homes were found to have been flooded with perhaps as many as 20,000 people displaced.

This was the flood UK parliamentarians swore they would fight to keep from happening again. The one conservative politicians said would never again happen in our lifetime. A flood that was worse than the terrible event of 2009 happening just six years after the first. And one that was almost certainly made worse by the dreadful alterations wrought by human forced climate change on the environment of the North Atlantic.

The Gulf Stream Slowdown and The Great New Storms of the North Atlantic

One doesn’t have to be a climatologist to see that sea surface temperature patterns in the North Atlantic are all topsy-turvy. The region of ocean to the west of the UK is cooler than normal. It’s a great cool pool once predicted by climate scientists and now made real by a human-forced warming of the world’s airs and waters. The result of an ever-increasing glacial melt outflow coming from Greenland.

image

(Temperature anomaly deltas in the region of the Gulf Stream are in the range of -5 C below average in the northern, Greenland melt-related, cool pool, and +9 C above average in a hot ribbon off the US East Coast. This overall new 14 C temperature variance from south to north is generating new atmospheric instabilities that intensify storm systems firing off in the North Atlantic. Image source: Earth Nullschool.)

Climate scientists have known for a long time that just such a cool pool of fresh glacial melt could play havok with weather across the North Atlantic and on to far-flung regions of the globe. And it’s just such a weather disruptor that we see developing there now. One that was originally dramatized in the film The Day After Tomorrow. But one that will all-too-likely represent centuries of catastrophic weather terminating in a new, much hotter, far more toxic, and far less life-sustaining world — rather than simply a week-long hemisphere-sized superstorm abruptly halted by a nonsensical new ice age (Please see World Ocean Heartbeat Fading).

To the south of our cool pool and on off the US East Coast we find that sea surface temperatures are screaming hot. Hot as in the range of 5-9 degrees Celsius (9-16 degrees Fahrenheit) above normal. Both the cool pool to the north and the hot pool to the south taken together are an ominous sign that the Gulf Stream is slowing down. The cool, fresh water outflow from glaciers near Greenland is interrupting a heat and salt driven over-turning there. The over-turning, which drives the Gulf Stream current, slows down. As a result, heat that would be transported northward instead backs up off the US East Coast.

What results is a kind of dipole temperature pattern that aids in storm generation over the North Atlantic. The cool pool tends to pull cold air southward from Greenland. The hot ribbon off the US East Coast tends to draw warm, moist, tropical air into collision with the trough zone south and east of Greenland. The result is a high potential for storm bombification in the region west of the UK. These storms, in turn, pull rivers of moisture up from the tropical airs to the south and over England, Ireland and Scotland. This confluence of weather sets off unprecedented storms and heavy rainfall for the UK.

Both the new North Atlantic sea surface temperature pattern and the resulting storms are not normal. They are an upshot of only recently emerging weather patterns resulting from a human-forced climate change. And, sadly, we can expect to see them continue to worsen. This year, in particular, could see some extraordinary trans-Atlantic storms as the El Nino-driven tendency for trough development and tropical air injection over the US East Coast comes into play. But overall, El Nino or no, the new dipole temperature anomaly pattern in the North Atlantic fed by Greenland melt and a related Gulf Stream slowdown will tend to keep pushing the region into a stormier and stormier pattern for the foreseeable future. The UK and its politicians should be made well aware of the consequences of their actions. Continuing to plan to burn fossil fuels is simply adding more fuel to an already raging climate fire.

Links:

The Story of the 2009 Cumbria Floods

More Rain and Flooding Expected in Northwest England

Toxic Interests: In Lead-up to Paris Summit, Conservatives Around the World are Fighting to Kill Renewable Energy

The Devastation in Cumbria

Shoothill Gauge Map

Earth Nullschool

World Ocean Heartbeat Fading

Warning From Scientists – Halt Fossil Fuel Burning Fast or Age of Superstorms, 3-20 Foot Sea Level Rise is Coming Soon

Hat Tip to Dr. James Hansen

Hat Tip to Neven, Jeremy, and Miles

We’re Gonna Need a Bigger Graph — Global Sea Level Rise Just Went off the Chart

From end 2014 through Fall of 2015 global sea levels surged. Building heat hitting +1 C above 1880s averages in the atmosphere-ocean system continued to set off a range of what appear to be ramping impacts. Thermal expansion grew more dramatic as oceans continued to heat up during what may be a record El Nino year. Rates of land ice melt continued to increase — providing a greater and greater fraction of overall global sea level rise. And global ocean currents showed signs of a melt-spurred change — which resulted in an uneven distribution of this overall rise.

We’re Going to Need A Bigger Graph

During that less than one year time, seas rose by fully 1 centimeter. That’s three times the ‘normal’ rate that’s been roughly ongoing since the early 1990s. A big bump that’s now part of a three-and-a-half-year, 3-centimeter surge. One more sign that global sea level rise is starting to really ramp up.

AVISO Sea level rise

(Global sea level rise since 1992 hits past the 8 centimeter mark in the AVISO altimetric graph. Image source: AVISO.)

This big, one-centimeter, jump topped the previous AVISO graph, which went up to 8 centimeters, forcing the measure to generate a new graph with a 9 centimeter top like. In other words, ‘we’re gonna need a bigger graph’ (See the old, smaller, graph here). Unfortunately, with some of the world’s top scientists predicting the potential for an exponentially increasing rate of sea level rise through this Century, it appears that ‘we’re gonna need a bigger graph’ may well become the scientific rallying cry of the age.

Possibility of Exponential Increase in Rate of Sea Level Rise

This year’s seemingly-staggering, 1 centimeter and counting, jump in sea level in less than one year, if maintained over the course of a century would result in a more than 1 meter global rise. Sadly, many new studies on the rate of glacier destabilization in Antarctica and Greenland hint that such a significant jump in sea level is not only likely, but may even be significantly exceeded under business as usual or even a moderately curtailed rate of fossil fuel burning.

A new study led by former NASA GISS head Dr. James Hansen points to the possibility of as much as 3 meters of sea level rise by mid Century and 7 meters or more of sea level rise by end Century even if the global economy somewhat steps off its current high trajectory of fossil fuel burning.

hansen-sea-level-rise

(Steadily ramping sea level rise that may be the start of an exponential curve. Image source: Research Conducted by Dr. James Hansen.)

Such massive rates of sea level rise would clearly be catastrophic.

In such cases, we’d start to see these kinds of exponential increases really begin to ramp up over the next 10, 20, and 30 years. And, given the rather large bumps we’re seeing in the AVISO measure for the past 3 and a half years, it’s possible we’re at the start of one of these potential step changes.

Links:

AVISO Sea Level Rise

Halfway to 2 C — World Approaching Dangerous Climate Milestone

Global Sea Level Rise Going Exponential?

Human-Warmed Southern Ocean Takes Aim at East Antarctica

Warning From Scientists: Age of Superstorms, Rapid Sea Level Rise Likely on the Way

Dr. James Hansen Columbia University

 

 

New Study — Risk of Significant Methane Release From East Siberian Arctic Shelf Still Growing

Large plumes of methane bubbling up from the Arctic Ocean sea-bed, saturating the water column, venting into the air, adding significantly more heat forcing to an already dangerous, fossil fuel-based, accumulation of greenhouse gasses in the Earth’s atmosphere. It’s a nightmare scenario. One in which human-forced warming, already at 1 C above 1880s levels, is further amplified through the feedback release of ancient carbon stored over the past 8 million years of Northern Hemisphere glaciation. And a recent study by the now famous Semiletov and Shakhova team provides still more reason for appropriate concern that such an event may be in the works.

ESAS methane release organic carbon store

(Shakhova and Semiletov’s new study produces an increasingly clear picture of a destabilizing organic carbon store beneath thawing permafrost in the East Siberian Arctic Shelf region. The above images show organic carbon concentration [left frame] and rate of release of methane in grams per square meter per day over observed regions. Image source: The Royal Society.)

*  *  *  *  *  *

By now, many of us are familiar with the controversy over the potential risks of significant-to-catastrophic methane release due to human-forced warming of the ArcticAn increasing number of observational specialists are pointing toward a risk that rapid human warming will set off the release of still more carbon in the Arctic. For some, this release is expected to be gradual. Others believe there’s enough risk of a rapid release to warrant an equally rapid emergency response.

But regardless of where you stand on the issue, new research coming to light from some of the Arctic’s top observational scientists more clearly describes what appears to be an increasingly dangerous situation.

Disintegrating Permafrost Cap in ESAS

At issue is the fact that, at the end of the last ice age, a great store of permafrost carbon was submerged as the Arctic Ocean rose. A low lying region containing about 500 billion tons of carbon as methane became inundated by the shallow sea that is the East Siberian Arctic Shelf (ESAS). The waters of this sea remained cold — below the freezing point of non-salt water in its lower reaches for most of the year. But, in some places, warmth invaded, and it is thought that small portions of the permafrost cap deteriorated.

In the near shore zones and in geologically active zones, methane conduits called taliks developed. And from these expanding taliks an increasing amount of methane bubbled to the surface.

Submerged Thermokarst Lake

(Ivashkina Lagoon was once a thermokarst lake. It has since been flooded by the Laptev Sea. For much of the time of inundation, the fresh water lake surface remained frozen. It is now thawing and releasing its organic carbon store as methane. Image source: The Royal Society.)

However, for the most part, the permafrost cap over the methane stores remained in tact — waiting to be rejuvenated by a new ice age. That is, until human industry belched billions of tons of carbon into the atmosphere, removing the possibility of a new ice age and forcing the world ocean and connecting Arctic Ocean to begin to warm in excess of peak Holocene temperatures. This warming, twice as fast in the Arctic as in the rest of the world, added still more heat pressure to the permafrost cap locking methane within the ESAS sea floor.

Now, more and more permafrost beneath the shallow ESAS waters is starting to thaw. And this, much more rapid than normal thaw is resulting in an increasing risk that methane stores beneath the permafrost cap will destabilize.

Shallow Waters, Geothermal Hot Spots, Taliks

Recent observational records by Dr. Natalia Shakhova and Dr. Igor Semiletov have found what they hypothesize to be an expanding array of methane vents in the East Siberian Arctic Shelf sea bed. According to their recent research, the vents appear to be growing more robust — bubbling up greater volumes of methane from a more vigorous and inter-connected network of channel beneath the thawing sea floor.

Atmospheric Methane September 6 2015

(Ever since 2005, atmospheric methane levels have again been on the rise. Much of this increase may be due to human emissions. However, an overburden of atmospheric methane and carbon dioxide in the Arctic zone hints that destabilizing carbon stores may also be adding substantial volumes of greenhouse gasses to the world’s airs. Image source: NOAA OSPO.)

Currently, according to Shakhova and Semiletov, methane emissions are most vigorous in the near-shore region of the ESAS and in the offshore slope region. Shakhova and Semiletov believe that near shore emissions are increasingly active due to rapid warming occurring there. Not only are the regional waters impacted by a rapidly warming Siberian land mass. They also see the flux of hotter waters from rivers issuing from the continent. As a result, the near shore region is most vulnerable to permafrost thaw and destabilization. In the slope zone, however, geological features are more active. These features provide a natural heat for the formation of taliks. And though most of this region was once frozen to the point that even geological activity did not result in methane venting, the now warming permafrost cap is generating weaker regions that natural geological heat can exploit to greater and greater degrees.

Sea Ice Melt, Storms, Heighten Methane Emissions

Ever since the mid 2000s Shakhova and Semiletov have observed what appears to be a generally heightened methane emission coming from the ESAS. Estimates for total release rates have doubled and then doubled again. By 2013, the scientists were estimating that 17 million tons of methane was venting from the ESAS sea surface each year.

The increased rate of methane release is not only due to permafrost thaw on the sea floor. It is also due to an increase in large polynyas in the ESAS during winter time as well as an overall increase in the area of open water that can be impacted by storms. An ice locked ESAS keeps more of its methane in the water column and gives the methane a longer period to be absorbed by the water or consumed by microbes. But as the ice recedes, more of the methane is able to break the surface and reach the airs above. In addition, ice free seas are more susceptible to the action of storms. Storms increase wave heights, increase the rate of breaking waves, and reduces ocean surface stratification. As a result methane moves more rapidly through the upper level water column and encounters a larger surface area from which to transfer from water to air.

An ice free ESAS is not only warmer, generating more destabilization forcing to the permafrost cap which locks in methane, it is also more and more devoid of the surface ice cap which acts as a secondary barrier to methane to air transfer.

Shakhova, Semiletov Recommend Adding ESAS Methane Release to Global Climate Models

Shakhova and Semiletov’s findings continue to compel them to issue warnings over the prospect of continuing increases in methane emissions from the ESAS and nearby seas. They conclude:

The observed range in CH4 emissions associated with different degrees of subsea permafrost disintegration implies substantial and potent emission enhancement in the ESAS as the process of subsea permafrost thawing progresses with time. While it is still unclear how quickly CH4 flux rates will change, the current process of Arctic warming and associated sea ice loss will accelerate this process. The potential for the release of substantial amounts of CH4 from the ESAS region has important implications not only for atmospheric CH4 concentrations but also, given CH4‘s potency as a greenhouse gas, for the global climate. Because the ESAS contains the largest and arguably most vulnerable stores of subsea CH4, inclusion of the ESAS source in global climate models should be considered a high priority.

Links:

The East Siberian Arctic Shelf: Further Assessment of Permafrost Related Fluxes and the Role of Sea Ice

Double the Rate of Methane Release From the Arctic Sea Floor

NOAA OSPO

Concern Over Arctic Methane Release

Threat of Permafrost Destabilization is ‘Real and Imminent’

 

Bermuda High No More — Global Warming Shoves North Atlantic Anticyclone Toward Azores

The semi-permanent weather patterns are all out of whack. The Aleutians Low has been shoved into Alaska and the Beaufort. The Pacific California High has shifted north and west to dominate the region previously claimed by the Aleutians Low. And the Bermuda High — a feature famous for directing tropical cyclones northward along the Atlantic Seaboard has packed its bags and fled north and east.

During the late summers of more stable climates, a strong high pressure system tended to form over the region of Bermuda. The high swept warm, moist air up off the Atlantic Ocean and over the Eastern Seaboard of the United States. The high was also a reliable governor of the movements of tropical cyclones — with the position of the high critical in determining whether these powerful summer storms would make landfall or rocket out to sea.

But this August, the Bermuda High is nowhere to be seen. Instead, it’s shifted more toward mid and north Ocean — closer to the Azores and the Flemish Cap.

image

(The Bermuda High can now also be counted among the growing number of climate change refugees as it emigrates to the Azores and the higher Latitudes of the North Atlantic. Image source: Earth Nullschool.)

In the above image, provided by Earth Nullschool, white denotes areas of high pressure and purple-to-red denotes areas of low pressure. The green circle in the image marks the position of the North Atlantic High in today’s GFS summary map. Note that the high is shifted more than 1,000 miles to the east and north. It sits at the base of a ridge that stretches well north of the Flemish Cap and then extends eastward to just south of Britain, Scotland and Ireland. Near Iceland, a powerful cyclone rages. A fickle storm that alternatively sets its sights along an arc from England to Svalbard.

How Human-Caused Warming Shoves the Bermuda High Northward

A semi-permanent high pressure system north of the Azores and a very stormy North Atlantic in the triangle between Greenland, Svalbard and England is not remotely a normal summer weather pattern. It’s instead a feature of a number of new ocean and atmospheric dynamics that are the upshot of human-caused climate change.

As equatorial heat embodied by the Hadley Cell expands outward from the lower Latitudes, the oceanic highs, including the Bermuda High, are shoved northward. This motion tends to also shift weather tracks into higher Latitude boundaries even as it, at first, enhances waviness in the Jet Stream. Near North America, we can see this dramatic weather alteration in the form of the Ridiculously Resilient Ridge over the Pacific and the Terribly Tenacious Trough over the Eastern Seaboard.

A second feature that influences the displacement of the North Atlantic High is the expansion of a cool pool of water to the south and east of Greenland. This cool pool is an upshot of the ongoing melt of the Great Greenland ice sheet. As fresh water spills out from Greenland’s glaciers it cuts off the northward propagation of the Gulf Stream even as it prevents bottom water formation. This shutting down of ocean circulation causes heat to build further south along the Eastern Seaboard of the United States and in the Caribbean and Gulf of Mexico. The lack of south to north heat transport combines with the expanding fresh water cap to prevent ocean heat ventilation at the surface in the North Atlantic. As a result, we see an expanding pool of cool water in this zone. A signature feature of both human caused climate change and of glacial melt in Greenland.

image

(Earth Nullschool temperature anomaly map focused in on the North Atlantic with near -5 C readings in an uncanny and freakish cool pool there. This is the mirror opposite of the Hot Blob in the Northeast Pacific. And, eerily enough, it is also a feature of overall global warming. Image source: Earth Nullschool.)

During recent years, we have seen more and more of this cool pool formation as both the Gulf Stream and bottom water formation in the North Atlantic slowed down due to fresh water outflows from Greenland. It’s an oceanic cool pool that forms a kind of atmospheric slot for the Bermuda High to slip north through. It also generates an unstable boundary zone between hot and cold waters and airs — a mechanism that generates very high potential energies for powerful storms cycling in a rough arc around Greenland (climate change driven storms of this kind were the subject of a recent paper by Dr. James Hansen.)

As glacial outflows from Greenland expand due to a continued forced economic dependence on fossil fuels and the dumping of their toxic, heat-trapping emissions into the atmosphere, we are likely to see the Bermuda High continue to shift north. It’s the first of many features that will tend to produce powerful atmospheric bomb-type storms in a great zone within the North Atlantic. Storms of an intensity we likely haven’t seen through all the 10,000 year period of the Holocene.

It is for this reason that the shift of the Bermuda High north and east should be viewed as an ominous atmospheric move. One that is preparatory to far worse weather to come — during a time when the old Bermuda High will, perhaps, be viewed with a kind of fond nostalgia. A gentler weather feature of a once far kinder climate.

Links:

Semi-Permanent Weather Patterns

Earth Nullschool

Global Forecast System Model

Hadley Cell

Ridiculously Resilient Ridge

Terribly Tenacious Trough

Warning From Scientists: Stop Fossil Fuel Burning or Age of Storms, Rapid Sea Level Rise is Coming Soon

The Pace of Ocean Rise Yet Quickens — AVISO Shows Record Spike in Sea Level

According to a new paper out by James Hansen, human warming could force glaciers to melt so fast that seas rise by as much as ten feet in as few as fifty years. Ten feet in fifty years of business as usual fossil fuel burning. It’s enough to change the face of human civilization. To render many of our vast cities waterlogged wastelands as a tide of migrants flood inland to flee the all-too-real rise of the waters.

It’s a situation we really need to get a handle on. One we should be monitoring with increasing concern. One we should absolutely be trying to prevent by ramping down fossil fuel burning as swiftly as possible.

Over the past Century, global sea level rise has been following a steadily sloping curve. At the beginning of the 20th Century, rates of global sea level rise were a mere 0.8 millimeters each year. By mid Century, the rate had increased to around 1.9 millimeters. And by the first decade of the 21st Century, the rate had again jumped — hitting 3.3 millimeters. As of 2014, satellites above the Earth had sniffed out another jump in the rate of sea level increase. A surge in the pace of rising water spiking well above the 3.3 millimeter per year trend line. A potential warning sign that basal melt of ice sheets in Antarctica and Greenland was starting to have an ever-greater impact.

Sea leve rise AVISO July

(Largest spike in sea level rise since 1993 is now being observed in the AVISO satellite monitor. Image source: AVISO.)

For as of this past month sea levels had spiked to nearly one centimeter above the annual trend line. A record spike that, as yet, shows little sign of abating.

Other than glacial melt and thermal expansion of the oceans due to a continued accumulation of heat, there are a few other ocean and atmospheric features with the potential to wag the overall trend line. One of these is El Nino. And this year is likely to feature one of the strongest El Ninos on record. But the current spike is also the highest upward variance we’ve seen in the entire satellite record dating back to 1993. It’s a severe wag to the upside that’s worth at least a couple of raised eyebrows.

To hit Hansen’s 10 foot in fifty year mark, what we’d end up seeing is a doubling in the rate of glacial melt from Greenland and West Antarctica every 5-10 years. It’s an extraordinary pace of melting. A signal that should show up in the GRACE satellite sensors measuring gravity loss from the great ice sheets. This signal, however, would also start to show up in the global sea level rise monitors as a continued ramping up of the pace at which oceans are surging. And we can’t entirely rule out that we’re observing some of that quickening in the spike we see now.

Links:

AVISO

Warning From Scientists: Stop Fossil Fuel Burning or Age of Storms, Rapid Sea Level Rise is Coming Soon

Historic Rate of Sea Level Rise

Possible Strongest El Nino on Record

 

Warning From Scientists — Halt Fossil Fuel Burning Fast or Age of Superstorms, 3-20 Foot Sea Level Rise is Coming Soon

First the good news. James Hansen, one of the world’s most recognized climate scientists, along with 13 of his well-decorated fellows believe that there’s a way out of this hothouse mess we’re brewing for ourselves. It’s a point that’s often missed in media reports on their most recent paper — Ice Melt, Sea Level Rise, and Superstorms. A paper that focuses on just two of the very serious troubles we’ll be visiting on ourselves in short order if we don’t heed their advice.

The way out? Reduce global carbon emissions by 6% each year and manage the biosphere such that it draws carbon down to 350 ppm levels or below through the early 22nd Century. To Hansen and colleagues this involves a scaling carbon fee and dividend or a similarly ramping carbon tax to rapidly dis-incentivize carbon use on a global scale. Do that and we might be relatively safe. Safe, at least in the sense of not setting off a catastrophe never before seen on the face of the Earth. That’s pretty good news. Pretty good news when we consider that some of the best climate scientists in the world see an exit window to a hothouse nightmare we’re already starting to visit upon ourselves.

The bad news? According to Hansen and colleagues, even if we just continue to burn fossil fuels and dump carbon into the atmosphere at a ‘moderate’ pace some of the terrifically catastrophic impacts of human caused climate change are not too far off.

A Moderate Pace of Burning

The new Hansen paper takes a look into both our geological past and our climate future in an attempt to give us an idea what may be in store. In this scenario, model, and paleoclimate based study, Hansen and colleagues assume two things about global human civilization. The first assumption is that we don’t follow the worst case, business as usual carbon emissions policies that lead to around 1000 ppm CO2 in the atmosphere by 2100. It is instead assumed that some effort is given to reducing coal, oil, and gas consumption. That some renewable energy, increased efficiency and behavior changes replace a significant portion of future fossil fuel emissions. But the most effective solution — a complete transition away from fossil fuel burning over the next few decades — fails.

A1B1

(A1B is a ‘moderate’ emissions scenario that, according to model essays, is likely to see between 2.5 and 3.5 C warming by the end of this Century and around 700 ppm of CO2 accumulation. That is, without the kind of major ice sheet response indicated in the new Hansen study. Image source: Knutti and Sedlacek.)

As a result, we end up with around 700 parts per million carbon dioxide in the atmosphere by 2100. In such a case we’ve followed what the IPCC community terms as the A1B or ‘moderate’ fossil fuel emissions scenario.

A Question of Melt Rate Doubling Time

It is in this context that the Hansen paper attempts to determine a key factor that will have wide-ranging impacts on ocean health, the continued existence and lifespan of coastal cities, and on the severity of the weather itself. That factor is captured by a single simple question — if we continue a moderate pace of fossil fuel burning, then how rapidly will ice sheet and ice shelf melt double?

To Hansen this is a critical question. One he has already done quite a bit of work to answer over recent years. And according to his findings it looks as if land ice melt rates for both Greenland and West Antarctica could now be doubling every 5-20 years. It’s a doubling rate that may find a historical allegory in the milder yet still intense glacial outflows of times long past. And it’s something that, according to Hansen, is being directly driven by an extreme pace of human-based greenhouse gas accumulation.

The Eemian — Significant Sea Level Rise and Terrible Storms Under Far Lower CO2 Forcing

To this point, Hansen’s new paper takes a dive into the paleoclimate study of an ice age interglacial that bears some stunning similarities to our own, human warmed, time period. He looks at the Eemian, a warm period that occurred 130,000 to 115,000 years ago. A period that featured temperatures in the range of 1-2 C above 1880s values (we’re in the process of hitting 1 C above 1880s values this year). A period in which CO2 levels were in the range of 285 parts per million (about 15 parts per million higher than the Holocene average before humans spiked that level to 400 parts per million during recent years). And a period that, according to Hansen’s broad study of past research, included numerous Heinrich type glacial outburst and melt events.

Back then, at 285 parts per million CO2 levels, seas were as much as 5-9 meters (16 to 30 feet) higher than they are today. The global climate, on the other hand, was much stormier. For two Heinrich type events that Hansen investigated were found to have dramatic impacts on severe storms in the North Atlantic during the Eemian. Hansen found large boulders propelled up onto the islands of Bermuda and the Bahamas by what appear to be powerful storm waves. Hansen also noted chevron shaped wave channels carved into the calcified sand beds in the Bahama Island Chain.

Heinrich Event

(Heinrich events included major glacial outflows like the one seen here at Jacobshavn, Greenland. Note the significant ice volume outflow through the channel at center frame. Also note the white dots in Baffin Bay indicating ice berg discharge. For reference, bottom edge of frame is about 100 miles. In past Heinrich Events outflows like the one seen above hit high gear as glaciers released armadas of ice bergs into the oceans which generated ocean and atmospheric changes. As the ice bergs melted, they deposited rocks on the sea bed. These piles of ice raft debris then became a signature geological feature of Heinrich events in the ancient past. Image source: LANCE MODIS.)

It paints an overall picture of very stormy weather in the North Atlantic as a result of these Heinrich ice sheet melt episodes affecting Greenland and West Antarctica. These melt events drove fresh water out into the North Atlantic and the Southern Ocean at the rate of about 0.5 to 1 meters of sea level rise per century. The expanding cold, fresh water along the surface zones in the upper latitude waters shut off heat exchange between the ocean and the atmosphere by generating a stratified ocean state. This fresh water wedge interrupted the plunging of heavier, salt-laden waters in the North Atlantic and the Southern Ocean. A loss of heat exchange that resulted in the cooling of airs directly over the fresh water outflow pools.

Meanwhile, since heavy, saltier waters were no long diving to the ocean bottom in these regions — broader ocean circulation was interrupted. As a result, heat from the equator was no longer traveling poleward. The equator warmed. The cold, fresh water outflow regions cooled. And this high temperature gradient subsequently became a powerful storm generator — providing extreme baroclinic potential energies for the storms that likely reshaped the ocean bottom and deposited massive boulders upon islands throughout the North Atlantic.

It’s worth noting that the 5-9 meter sea level rise during the Eemian occurred in the context of global temperatures that are now similar to our own (1-2 C above 1880s values). But it’s also worth considering that the underlying CO2 and greenhouse gas conditions for the current age are far, far worse. Peak global CO2 during the Eemian never hit higher that 285 parts per million. For the Anthropocene age we are now leaving the 400 parts per million CO2 level in the dust. Meanwhile, the pace at which we are warming is also more than 10 times faster than the pace of warming to peak Eemian heat values. And it’s these two factors — an extreme greenhouse gas overburden combined with a very rapid pace of warming that has Hansen and colleagues very concerned about our climate situation over the next 10-80 years.

Land Ice Below Sea Level — Amplifying Feedback For Melt

Turning to the current day, there’s a growing number of reasons why we should be concerned that rapid land ice melt, large fresh water outflow to oceans, and resulting superstorms could be in our future. First, we’ve learned that the topography of Greenland and Antarctica include numerous channels that tunnel deep into its great glaciers at depths well below sea level. When oceans warm, and they’re warming as you read this, the submerged, sea-facing slopes of glaciers are confronted with more and more heat gnawing away at their under-bellies. Just a 0.1 C increase in water temperature can melt away a meter of ice over the course of a year. Multiply that by glaciers with faces that are submerged hundreds of feet deep whose sea fronting cliffs extend for many miles and you can end up with quite a lot of melt due to very little warming. As more of the undersides of glaciers melt, more of the water tunnels inland and large masses of ice are rafted away from the central ice exposing still more of the land anchored ice to a warming ocean flood.

image

(Image from Hansen Paper shows how land ice melt generates ocean stratification which is an amplifying feedback that enables ocean bottom warming and more land ice melt. Note — AABW stands for Antarctic bottom water, NADW — North Atlantic down welling. Image source: Ice Melt, Sea Level Rise, and Superstorms)

As bad as this dynamic may sound, the process includes one more wrinkle that makes it even worse. As the undersides of ice shelves erode and more fresh water laden ice bergs are pulled out into the ocean, these ice bergs begin to melt en mass. This massive ice melt develops into an enormous and expanding pool of fresh water at the surface. And its this troublesome demon that traps heat in the deeper ocean levels. So, in other words, as the ice from the land glaciers floats away and melts it traps and focuses more heat at the base of these great glaciers. It’s an amplifying feedback. A very serious kind that doesn’t even require the human forced kick to create severe trouble. One that during the Eemian really wrecked the weather and caused massive surges in ocean height.

It’s a process that Hansen and his colleagues believe make both Greenland and West Antarctica very vulnerable. A process that could, when combined with the high velocity human heat forcing, produce melt rates that double every 20, 10 or even every 5 years. But of the two — Greenland or Antarctica — which is worst off?

Greenland topography

(Topographic map of Greenland sans its great ice sheet. Most of central Greenland’s mass is now below sea level. It’s a basin that now holds a miles high ice mountain. Various channels allow ocean water access to the central ice mass should the channel openings melt due to warming oceans. Such an invasion could set off a rapid sea level rise driven by Greenland melt. Image source: Livescience.)

Greenland, for its part, is little more than a great Archipelago held together by its stunning ice mass. Remove the ice and the interior of Greenland would flood, leaving a ring of islands as a final remnant. Though deep, most of these channels run up slope. And this feature, according to the Hansen study, may be one saving grace for potential Greenland ice melt pace. Up slope channels limit the impact of basal melt by serving to check rates of catastrophic destabilization. So though Greenland is certainly vulnerable to ice melt due to the fact that many channels cut hundreds of feet below sea level and into the island’s glacial heart, it is not as vulnerable as West Antarctica.

There, many channels cut deeper beneath the Antarctic ice mass. But not only are they below sea level by hundreds of feet as with Greenland, they slope down. They slope down and not for just a little ways under the ice sheet — some of these ocean heat skids extend in down-sloping fashion for hundreds of miles beneath the Antarctic ice. The result is a kind of skid, that once unlocked by initial melt, can continue to expose larger and large chunks of bottom ice to the warming ocean. Allowing, ultimately, the creation of new warming seas underneath the ice and floating it away in very rapid fashion.

In West Antarctica, ice shelves facing the Weddell and Ross seas both feature these dangerous retrograde slopes. In East Antarctica, the Totten Glacier is likewise vulnerable as are many other glaciers surrounding the vast periphery of Antarctica.

Retrograde slope Ross ice shelf

(Retrograde slopes behind ice sheet grounding lines are just one reason why Antarctic land ice is so unstable. Image source: Ice Sheet Mass Balance and Climate Change.)

Finally, in addition to being surrounded by the warming, deeper waters of the Southern Ocean, in addition to featuring dangerous retrograde slopes that channel warming sea water further and further inland and beneath the ice sheets, West Antarctica itself sits on a geological hot bed. Though not mentioned in the Hansen study, recent work also highlighted that West Antarctica rests atop a geologically active zone that had formed numerous sub-glacial lakes warmed by geological activity. This added geological heat makes West Antarctica that much less stable — an instability that when given the shove of human heated oceans is leading the Larsen B Ice Shelf to completely collapse by 2020. It makes Antarctic land ice that much more vulnerable to the added heat human beings are forcing into the oceans and opens up the ominous possibility that melt rate doubling times for West Antarctica could become quite extreme indeed.

Modeling Land Ice Melt’s Impact in the 21st Century — Facing A Coming Age of Superstorms

So what does all this mean? In the worst case (5-10 year melt rate doubling times), it’s possibly 3 meters of sea level rise by mid Century, perhaps 7 meters by end Century under business as usual fossil fuel emissions. Even in the more moderate cases (10-20 year melt rate doubling times), 1 meter of sea level rise by mid Century and 3 meters or more of sea level rise by end Century is not entirely out of the question, according to Hansen’s new research. These potentials are markedly different than the more conservative rates outlined by IPCC which is still calling for a less than 1 meter sea level rise under even the worst case human carbon emissions scenarios (1000 parts per million CO2, in the range of 1200 ppm CO2e).

So much fresh water hitting the oceans would cause a rapid stratification. A rapid loss of ocean to atmosphere heat exchange in the regions impacted. A train wreck of heat backing up at the equator. Such a train wreck would result in temperature extremes and gradient differences that would make the Eemian Heinrich events (mentioned above) seem moderate and slow by comparison.

Hansen has been working on global atmospheric models for tracking these events for a number of years now. And this new study is an improvement on his earlier, model-driven “Storms of My Grandchildren” work. Hansen’s new model runs are imperfect simulations of what may happen given large melt pulses from Greenland and Antarctica. The models, according to Hansen, mix the ocean water too much, reducing the overall impacts of stratification through the mechanism of the fresh water wedge. However, even with this imperfection, the temperature gradients displayed by these models are absolutely stunning. A clear warning to anyone who still wants to keep burning fossil fuels that they’re really grabbing the dragon by the tail.

image

(A mid range simulation including 10-20 year melt rate doubling times and 6 feet of sea level rise by 2080 — half Greenland, half Antarctica — shows enormous weather impacts in the form of a severe, superstorm generating, temperature gradient. Image source: Ice Melt, Sea Level Rise, Superstorms.)

In the above image we can see just one of these model runs. The model assumes a 10-20 year doubling time for rate of land ice melt. It contributes equal portions of melt from Greenland in the north and Antarctica in the south. Greenhouse gas accumulation is considered to be along the moderate case A1B track. By 2080 we have about six feet of sea level rise globally and about 600 parts per million CO2 in the atmosphere. The more rapid rate of melt has put a temporary damper on the rate of global atmospheric warming which has dipped to 1.11 C above 1880s values (just slightly higher than today). But much of this cooling is localized to the Southern Ocean and to an extreme cold pool in the North Atlantic between Northwestern Europe and Greenland.

There a massive outflow of fresh water has shut down the ocean’s ability to exchange heat with the atmosphere. AMOC has been vastly weakened. The Gulf Stream is backed up along the US East Coast and into the Gulf of Mexico. Heat is building in the Arctic opposite Greenland and all along the Equator. Temperature anomalies in the range of 17 degrees Celsius below average occur over the ocean fresh water pool. This drop is enough to generate year round winter like conditions in the cold pool region even as other sections of the atmosphere around it continue to warm or retain severe excess heat.

Energy imbalance at the top of the atmosphere rockets to between 2 and 4 Watts per meter squared. What this means is that, in failing to ventilate heat to the atmosphere in the North Atlantic and Southern Ocean, the world ocean system has continued to accumulate a massive amount of heat. Heat that is now going to work warming the ocean bottom and hitting the bases of the already rapidly melting land ice.

Sandy

(More superstorms in our future. If Hansen’s new research is correct storms like Sandy will grow both more powerful and more common as Greenland dumps ever increasing volumes of fresh water into the North Atlantic. Image Source: NASA.)

For the North Atlantic, it is the greatest of understatements to say that an area of perpetual winter surrounded by warming airs and sitting atop a warming deep ocean is a major storm generator. Summer time temperature deltas between the center of the cold pool will range from near zero C to 20s, 30s and 40s C over nearby ocean and continental land masses. It’s like taking the High Arctic and shifting it to Scotland while all the adjacent airs warm. Temperature gradient and baroclinic (pressure gradient) energy for storm generation will be on the order of something that modern humans have never experienced. The potential for superstorms in this model simulation will, notably be quite high.

Final Notes — Superstorm Conditions Could Emerge Sooner than Models Indicate

The point to consider here is that large scale land ice melt sets in place forces that result in a weather wip-lash of epic proportion. It’s been the heart of Hansen’s work for many decades and it’s an issue that we really need to consider as time goes forward. A dwindling time for response that may well be much shorter than even Hansen’s models indicate. First, ice sheet vulnerability may well be higher than IPCC officials imagine and we could well be on a slope of melt rate doublings in the range of 5-20 years now.

global sea level change

(Global sea level rise keeps hitting a steeper and steeper slope. Image source: Dr. James Hansen, Columbia University)

Second, Hansen’s models likely capture the atmospheric impact of such large-scale land ice melt later than would happen in the real world. This later capture is due to the fact that his low resolution models mix the ocean heat more with the atmosphere than would occur under the kinds of ocean stratification events that we are likely to see due to these doubling times. Third, and finally we return again to the paleoclimate time of the Eemian where there is ample evidence that a mere 0.5 to 1 meter per century rate of sea level rise due to melting Greenland and West Antarctic ice during that time set in place conditions to generate superstorms with high enough peak intensity to deposit massive boulders upon islands in the Atlantic and to carve the impression of gigantic, long-period waves into the sea bed.

Anyone reading this work and considering the notion that some of the greatest scientific minds this age has birthed could be right is immediately confronted with the realization that the gargantuan forces we are playing with are not to be trifled with. And yet, the trifling continues despite the wise and well considered scientific warning to relent.

Links:

Hansen Paper: Ice Melt, Sea Level Rise and Superstorms

Dr. James Hansen, Columbia University, Former NASA GISS Lead Scientist

Knutti and Sedlacek: Robustness and Uncertainties in Climate Model Projections

The Eemian

LANCE MODIS

Livescience — Topographic Map of Greenland Sans Ice Sheet

Ice Sheet Mass Balance and Climate Change

NASA: 10,000 Year Old Ice Shelf to Collapse by 2020

IPCC Sea Level Change

NASA Earth Data

Storms of My Grandchildren

 

Climate Refugees — Extreme Weather Displaced 157.8 Million People From 2008 to 2014

Does it seem to you that the weather is getting worse? Rainfall more intense, droughts drier, longer, more prolific, the strongest storms growing ever stronger? Well, in this case, seeming is all-too-real.

Four decades ago our climate was more placid. Global temperatures were about 0.5 C cooler than they are today. There was less available heat energy to pump up storms. The intensity of evaporation and precipitation was about 4 percent less than it is today and the pace of global warming due to an ongoing fossil fuel emission was slower. Our atmosphere has changed. It has become more dangerous. More capable of producing extreme and disrupting weather events.

Scale of displacement

Nearly 158 million people, or a number equivalent to just under half the population of the United States, were forced from their homes as a result of extreme weather over the past 7 years. It’s a number six times greater than those displaced by earthquakes, volcanoes or other geophysical causes. Individuals living on the Earth today are now at a 60 percent greater risk of being displaced — chiefly due to increases in extreme weather — than they were in 1975. Image source: Internal Displacement Monitoring Center.

And it’s for these reasons that you and I are more vulnerable. More likely to become a casualty of worsening weather. For according to the Internal Displacement Monitoring Agency, an agency that tracks the number of displaced persons globally, you and I are 60 percent more likely now to be forced from our homes by a natural disaster than we were in 1975.

The numbers at this point are pretty concerning. On average, over the past 7 years, 26 million people have been displaced by natural disasters in a single year during that period. For 2014, the count was 19.3 million, 17.5 million of which came from extreme weather events — a factor directly related to human-caused climate change. In total, weather disasters resulted in 157.8 million people being forced to flee their homes during the entire period from 2008 to 2014. Extreme weather — not warfare, volcanoes, or tsunami — is now the primary reason human beings are displaced. Droughts, wildfires, floods, powerful hurricanes, superstorms. A litany of self inflicted violence whose impacts we are continuing to worsen.

Displacement by hazard type

From 2008 to 2014, storms and floods resulted in 84% of natural disaster caused displacements. In 2014, storms and floods generated 91% of the total displacement. Image source: Internal Displacement Monitoring Center.

The Impacts of Displacement Linger as Worsening Weather, Sea Level Rise Loom

Displacement caused by natural disasters is not an easy problem to fix. Anyone who suffered the loss of a home due to impacts related to Superstorm Sandy or Hurricane Katrina can attest to the fact that it often takes a long, long time to become re-established under a secure shelter. For this reason millions of people displaced by extreme weather disasters over the last few years have continued to live as a kind of climate refugee — forced to reside in tent villages or other temporary shelters. Reliant on government assistance because much of what they had, the storms destroyed. Often segregated from larger populations these groups suffer greater risk of falling into permanent poverty and contracting disease even as they are even more vulnerable to subsequent displacement from follow-on events.

As global warming intensifies and the risk of extreme weather events continues to increase, there is also an increasing risk that this expanding number of displaced persons will result in nation-destabilizing stresses in various regions of the world. Currently, the greatest number of displaced persons is centered in the high population density countries of Asia and the Caribbean. But as climate change begins to add another flood stress due to global sea level rise, it is likely that displacement will become ever more ubiquitous.

Even more concerning is the fact that the storms we see now are the early, easy outliers. The ‘small’ climate change weather demons that have already displaced more than 150 million people. Hansen’s Storms of our Grandchildren haven’t yet arrived in full force. And rates of sea level rise are just now starting to ramp up. Would that we had the wit, will, and wisdom to help prevent at least some of this unfolding tragedy. If we do not, there’s no fall back. We’re it.

Links:

Internal Displacement Monitoring Center

NOAA Temperature Graph

How Global Warming Wrecks the Jet Stream and Pumps up The Hydrological Cycle to Generate Extreme Weather

The Storms of My Grandchildren

 

 

Arctic Heatwave Forecast to Crush Northern Hemisphere Snow Cover This Week

The Russian side of the Arctic is heating up.

A high amplitude ridge in the Jet Stream is forecast to develop atop the Yamal region of Russia, expand northward over the Kara and Laptev seas, inject a plume of anomalously warm air over the polar region, and then proceed on along the Arctic Ocean shores of Siberia. Beneath this ridge, temperatures over the Arctic Ocean will spike to +1 to +4 C above average while temperatures over land will hit extreme +20 C and higher anomalies.

Arctic Heatwave June 6

(Arctic heatwave invades Siberia in the GFS forecast for later this week as depicted by Climate Reanalyzer.)

Arctic Ocean zones are forecast to see temperatures climb above freezing for much of the 80 degree North Latitude zone. Over Siberia, land-based temperatures are predicted to range from the 40s and 50s along the Arctic Ocean boundary and climb to the 60s to 80s in regions just inland.

As temperatures tend to flatten out over Arctic Ocean waters and as permafrost zones in Siberia are used to far cooler readings during Northern Hemisphere Summer, the predicted heatwave is likely to have some rather strong impacts should it emerge. Most notably, snow cover over remaining land and sea ice is expected to see a rather extreme reduction over the next seven days. In other words, GFS forecast models show Northern Hemisphere snow cover basically getting crushed:

Current snow CoverPredicted Snow Cover

(Massive reduction in Northern Hemisphere [NH] snow cover predicted coincident with Siberian Heatwave later this week. Left frame shows current NH snow cover. Right frame shows predicted NH snow cover for Tuesday, June 9. Image source: Climate Reanalyzer.)

Sparse remaining snow cover in Northeast Siberia along the East Siberian Arctic Shelf coastal zone is expected to be pretty much wiped out. One foot average snow cover along the shores of the Laptev and Kara seas is also expected to melt. And a broad section of remaining snow upon the sea ice is predicted to retreat away from the North Polar region — receding back toward the final haven near Greenland.

Snow is important for spring and summer-time Arctic temperature moderation due to the fact that it provides insulation to sea ice and permafrost as well as serving as a reflective, high-albedo surface that bounces back some of the incoming heat from the 24-hour seasonal Arctic sun. Snow melt, on the other hand, serves to form albedo-reducing melt ponds over the Arctic Ocean sea ice during summer. A critical factor in late season melt forecasting in which more June melt ponds tend to mean lower sea ice totals by end season. In addition, snow melt fills permafrost zone rivers with above-freezing waters that then flow into the Arctic Ocean — providing yet another heat forcing to the sea ice.

Conditions in Context

This weekly trend and forecast is consistent with an ongoing tendency during 2015 for strong ridge formation and warm air slot development over both Alaska and the Yamal region of Russia. The high amplitude ridges also likely have teleconnections with larger weather patterns such as El Nino in the Pacific, the warm water pool (hot blob) in the Northeast Pacific, and record low sea ice extents continuing for most of Northern Hemisphere Spring. Observations that are also consistent with the predictions made by Dr. Jennifer Francis that are a direct upshot of polar amplification set off by human-caused warming of the global climate system.

image

(GFS model forecast as depicted by Earth Nullschool showing ridge Northwest Territory, trough Greenland and North Atlantic, ridge Kara and Laptev region of Siberia. A dynamic that may be the result of teleconnections set off by factors related to human-caused climate change. Image source: Earth Nullschool.)

It’s worth noting that many of these factors are self reinforcing. For example, more sea ice melt results in higher amplitude wave formation in the Jet Stream. Higher amplitude wave formation in the Jet Stream transports more warmth to the Arctic environment, resulting in more sea ice and snow melt which in turn weakens the Jet Stream further. A longer-term amplifying feedback of Arctic carbon release may also be in play (hinted at by an overburden of both CO2 and methane in the local Arctic atmosphere), which would also contribute to the conditions we now observe.

A final feedback, this one somewhat negative, occurs as a result of Greenland Ice Sheet (GIS) melt. Large cold, freshwater outflows from GIS into the North Atlantic result in localized cooling in that region. This feedback (also related to AMO weakening) enhances trough formation throughout the North Atlantic region adjacent to Greenland and the Canadian Archipelago. A final potential teleconnection to the ridges we see forming over both Yamal and the Alaska/Northwest Territory zone.

Links:

Climate Reanalyzer

Earth Nullschool

Heat Wave Forecast for Russia

Rapid Arctic Sea Ice Loss Linked to Extreme Weather

Tracking for Early Season Melt Pond Formation at The Arctic Ice Blog

Climate Change Ratcheting Up: El Nino Strengthens in Equatorial Pacific Increasing Likelihood for Record Warm 2015

A powerful Kelvin Wave continued to ripple through the near-surface waters of the Equatorial Pacific this week — heightening sea surface temperatures, strengthening an ongoing El Nino, and pushing a wave of oceanic heat back into a human-warmed atmosphere that is hotter now than at any time in modern human reckoning.

High temperature anomalies in the Kelvin Wave plug have spread out across the ocean surface. Readings in the range of +1 to +2 C above average stretch along surface waters all the way from the Date Line through 120 West Longitude. East of the 120 line, surface waters have now hit readings of 2 to 4 degrees Celsius above average. And lurking just below the surface along thousands of miles of ocean is a dense zone of 5-6 degree above average water. A zone of extreme heat at the heart of the current intense Kelvin Wave:

NOAA Kelvin Wave April 23

(A strong Kelvin Wave shuts down atmospheric heat transfer into the Equatorial Pacific setting up conditions for an extended El Nino and possible new record heat for 2015. Image Source: NOAA’s Climate Prediction Center.)

Heat that could well make 2015 yet another worsening of the human warming and extreme weather twilight zone we now find ourselves in.

Pushing into Moderate El Nino Range

According to NOAA’s weekly El Nino report, sea surface temperatures in the critical Nino 3.4 region hit a range of 1 degree C above average last week. A jump from the previous week’s measure of +0.7 C and a new push toward moderately strong El Nino levels off the back of the current warm Kelvin Wave. Atmospheric teleconnections that are signatures of a moderate El Nino also began to emerge over past weeks — with a strengthening of the subtropical Jet and related storm track setting off powerful tornadoes, thunderstorms and heavy rain events in states bordering the Gulf of Mexico over the past ten days.

Heat content from the current Kelvin Wave is enough to continue to keep Equatorial Pacific sea surface temperatures in present ranges or to push for further warming over at least the next 1-2 months. A set of factors that will almost certainly lock near moderate El Nino conditions in through Summer and general El Nino conditions through early Autumn. The result is that the extra heat bleed off the Pacific Ocean will combine with the impressive human forcing to generate a high risk that 2015 atmospheric temperatures will beat out all-time record highs set in 2014.

Model Runs Still Showing Potential for Super El Nino

Nino 3.4 Monthly Anomalies

(Unweighted model ensemble runs show the current El Nino peaking out at extreme intensity. Long range model runs can be quite uncertain, but these are very high values. Image source: NOAA Seasonal and Monthly SST Anomalies.)

NOAA model runs also show a potential for El Nino strengthening through the end of 2015. Probability weighted CFS model ensembles (PDF) point toward a seasonal anomaly for Nino 3.4 in the range of 1998 Super El Nino values at 2.1 degrees Celsius above average by the end of 2015. Mean model runs (non-weighted) push the long range forecast heat values even higher at 2.6 C above seasonal averages or 2.75 C above monthly averages.

These unweighted long range forecasts are well outside the strength of even the monster event of nearly two decades ago. A new super El Nino that would have very serious consequences for global temperatures and result in far-reaching climate impacts should it emerge. Atmospheric temperatures that are now in the range of +0.7 C above 20th Century averages and +0.9 C above 1880s values could well push into a new range at +0.8 C and +1 C, or higher, respectively.

Super El Nino Late 2015

(Long range models show Equatorial Pacific has potential to hit near Super El Nino status by late 2015. At this time, such model runs are low certainty. Image source: NOAA Seasonal and Monthly SST Anomalies.)

Cranking up the Human Hothouse

Entering the range of 1-2 C above 1880s values is a zone of heat anomaly that will amplify already apparent ice sheet melt, sea level rise, droughts, wildfires, water stress, and ocean health impacts. At temperatures around +1.5 C we begin to enter a period of strong glacial outflows, weather instability, geophysical changes, and record related storm events in a ‘Storms of My Grandchildren‘ type scenario. At +2 C these very dangerous impacts will likely be in full swing.

It is worth noting that it took 10,000 years to warm the world 4 degrees Celsius at the end of the last ice age. Under current human fossil fuel burning scenarios, it is likely that we reach half that threshold in just 150 to 170 years — from 1880 to 2030-2050. A rapid reduction in fossil fuel emissions along a progression to a net carbon negative human society over the next few decades is absolutely necessary to prevent these outcomes. And while model forecasts indicating the potential for a Super El Nino type event for late 2015 may be somewhat uncertain, there is a much higher certainty that very dangerous climate impacts starting at the current level of human warming will ramp up here on out — with the 1.5 C threshold looking very bad and the 2.0 C threshold looking terrible.

As such, we should do all we can to prevent hitting those marks.

Links:

NOAA’s Climate Prediction Center

NOAA’s Weekly El Nino Report

NOAA Seasonal and Monthly SST Anomalies

The Storms of My Grandchildren

Far Worse than Being Beaten With a Hockey Stick

Climate Change Plays Havoc With World’s Weather as Europe/UK Fear Storms This Fall and Winter

Today, as in recent years, we see ample evidence that extra heat in the atmosphere and oceans can severely alter weather around the world.

We are seeing the impacts in Brazil where Sao Paulo reservoirs are now at 4.5 percent capacity and millions are suffering from inadequate and dwindling water supplies. We see similar stress in California where the worst drought in decades is forcing some communities to truck in water. In Syria the situation is even more dire — on the scale of a humanitarian nightmare — where a multi-year drought has destabilized government and spurred violent extremism to surge through an already troubled region.

Eastern Brazil Oct 15

(Sao Paulo region of Eastern Brazil clearly visible through a mostly cloudless but smoke-filled satellite shot on October 15. Note both the dessicated, browned land of a normally green region together with the steely gray smoke funneling in from wildfires both near Sao Paulo and further north in the drying Amazon rainforest. Intense heat and lack of rainfall combines with fires to create a pallor of smog over much of Brazil also visible here. Image source: LANCE-MODIS.)

In a warming world, drought and deluge are far more common. The added heat increases the rate of evaporation and amplifies the hydrological cycle such that the atmosphere holds 6 to 7.5 percent more moisture per each degree Celsius of heating. This is roughly equal to an increase in the rate of evaporation and precipitation by 6 to 7.5 percent as well. So where droughts occur, they will tend to be more severe and where strong storms develop, they will tend to dump even heavier volumes of rainfall. And a warming of the polar regions coincident with snow and ice loss, plays havoc with both the Jet Stream and traditional storm tracks even as the increased instability generates ever-more-powerful storms.

For a Europe facing off against an Atlantic and Arctic undergoing these wrenching changes, the story is altogether related. Sections of Southern France over a recent six week period received enough rain for an entire year. The Mediterranean waters off this region had heated to between 3 and 4 C above average dumping an intense load of moisture into a hungry upper level low that delivered storm after storm to the beleaguered regions. One spate of deluge dumped a full six months of water from the skies in just three hours.

Meanwhile, the UK may now be staring down a fall and winter season that may bring with it a return to the terrible and historic storms witnessed just last year.

monster storm UK

(Monster storm that bombed out to 952 mb on Wednesday lashes the UK and Ireland with rain and gales on Friday and Hurricane Gonzalo threatens Bermuda. Gonzalo is set to make an eastward turn across the Atlantic and will possibly impact the UK as a tropical storm by Monday or Tuesday of next week. Image source: LANCE-MODIS.)

This week, one such storm swelled to extraordinary intensity in the North Atlantic. On Tuesday and Wednesday it bombed out to a powerful 952 mb monster, filling up most of the Ocean between Newfoundland, Greenland and Europe, casting gales on into the UK and Ireland. It sent storm surges up rivers — forcing them to top their banks, lashed the isles with rainstorms that flooded Belfast, damaged hundreds of homes and sent officials scrambling to assure an already storm-weary public that they were better prepared for such events than last year.

The current storm is expected to rake through the UK and Ireland throughout this weekend before fading off toward the north. As it lifts, hurricane Gonzalo — now packing 125 mph winds and threatening Bermuda — is forecast to surge into the UK with tropical storm intensity come Monday or Tuesday of next week.

Gonzalo path

(Forecast path for Gonzalo shows a tropical storm off Ireland by Monday morning. Image source: NOAA.)

The 1-2 punch is reminiscent of a relentless series of storms that battered the UK this past winter. A sequence spurred by extraordinary and unprecedented changes to the North Atlantic climate including a slowing of the Gulf Stream, a powerful warming of surface waters in the Arctic, major losses to sea ice in almost all Arctic seas, and increasing cold, fresh water outflows from Greenland. The net effect is to enhance storm track intensity across the Atlantic as warmer waters and airs surge northward coming increasingly into contact with cold polar air and generating powerful and intense storms during the winter, fall, and spring seasons.

With global temperatures flirting with new record highs and with El Nino possibly flaring to life in the Pacific, the end of 2014 and the start to 2015 is altogether likely to see a continuation of such intense, extreme weather. Weather that is severe enough to cause damage and disruption in some areas or even powerful enough to throw whole cities and regions into instability.

Just a few of the tragic results of a warming climate as we approach the 1 C above 1880s temperatures mark.

Links:

LANCE-MODIS

NOAA

North Atlantic Ramping up to ‘Storms of My Grandchildren’

How Climate Change Wrecks the Jet Stream and Amps Up the Hydrological Cycle to Cause Dangerous Weather

How Climate Change Helped ISIS

Hat Tip to Colorado Bob

Hat Tip to Bernard

 

Warm Winds Gather to Invade the Arctic: Summer Sea Ice Melt and The Storms of 2014

If there’s an aspect of global warming science that remains unsettled, it’s the general state of prediction and analysis over the fate of Northern Hemisphere sea ice. As is well known by now, model predictions greatly underestimated the pace of sea ice loss as a response to human-caused warming. Big melt years like 2007 and 2012 brought sea ice extent and area, by end 2012, to less than 50% of 1979 values. Sea ice volume for the same period was nearly 80% lower than 1979 measures. Such lows were generally not predicted to appear until the 2060s at the earliest.

Ice response to rapid human warming and polar amplification, in these cases, was, for lack of a better description, outrageously stunning. And the weather impacts of such amazing losses were increasingly dangerous and far-reaching. Climate systems inertia, in the case of sea ice, seemed to be no match at all for the strong and likely unprecedented warming forces we’d already unleashed.

Sifting through the sea ice tea leaves

Though much of what happened was and continues to be unexpected, a few overall patterns emerge in the data. Dynamic melt trends for area and extent were composed of massive melt years (2007 and 2012) followed by pseudo recovery years (2008, 2013) where the ice seemed to bounce back a little before inching again toward previous record lows (2009, 2010) or setting minor new melt records (2011 area) before the next big hit.

Sea ice volume measures were somewhat less messy with massive melt years (2007, 2010), more minor melt years (2011, 2012), one minor pseudo-recovery year (2008) and one major pseudo-recovery year (2013). In this set, one year (2009) stands out as neither showing a new record low volume nor showing pseudo-recovery as end season volume fell off slightly from the previous year. The fact that 2009 followed a pseudo-recovery year (2008) may or may not be instructive for the current melt season.

It is worth noting that in the volume progression, four out of seven years during the 2007 to 2013 period all showed new record lows.

Piomas Minimum Arctic Ice Volume

(Graph of minimum Arctic sea ice volume as measured by PIOMAS since 1979 with various trend line projections. Data source: PIOMAS Image source: Wipneus.)

What one can read from these data points is that strong pseudo-recovery years (like 2013 and 2008) have typically been followed in recent years by a return to the decline trend but not to new record lows. So, statistically, this is what we would expect for 2014.

That said, keep in mind that though it remains extraordinarily difficult to predict end sea ice states for any single year, the overall trend of major and unprecedented melt is most likely to continue and the window for a total sea ice loss by end season before 2020 remains wide open. Further, statistical analysis will, in every case, bow to emerging conditions on and beneath the ice.

Evolution of the early 2014 melt season

For the 2014 melt season, the fickle Arctic does not at all disappoint. By late April and early May of 2014, an extraordinarily warm winter period had wiped out most of the 2013 recovery in sea ice volume measures. By mid April, PIOMAS was showing volume in the range of second or third lowest year on record for the date.

By today, May 12, sea ice area and extent measures were in the range of 4th to 5th lowest on record with both measures approximately mirroring 2007 values for the date.

Given the potential for very rapid melt during June and July, as displayed in recent melt years, these values are within striking distance of new record lows should the weather conditions for rapid melt emerge.

Observed conditions for early to mid May 2014

It is worth noting that May does not generally tend to be a predictive month for sea ice loss. In most cases, it is more a bottleneck period where values tend to crunch together as the sea ice softens up but generally shows few breaks toward the more rapid melt trends typically seen in June or toward a slower melt due to weather that is less favorable for ice degradation.

That said, a few currently ongoing conditions may provide some strong indicators for how the 2014 melt season could progress.

High amplitude Jet Stream waves through Eastern Siberia, the Bering Sea and Alaska. A doggedly persistent weakness in the polar Jet Stream along an arc from East Siberia to Western Canada has resulted in much warmer than usual conditions for the Bering Sea, the Chukchi Sea and regions of the Beaufort adjacent to the Alaskan and Canadian coasts. Warm air originating over a pool of much hotter than normal water in the Northern Pacific just south of Alaska has continued to flow up through the Bering Sea, into the Chukchi, and over Alaska and Western Canada and on into the Beaufort.

Tracking this warm air flow resulted in a bit of incredulity as day after day observation showed the air continuing on through the Beaufort, past the North Pole zone, down over Svalbard and the Fram Strait, into the North Atlantic and finally being swept east in the strong cross-ocean wind pattern toward England and Ireland. In this way, air from 40 North Latitude in the Pacific jumped the pole to end up in the Atlantic near England.

A persistence of this weather pattern would have numerous and potential critical impacts for the Arctic during the summer of 2014. First, it would result in a constant pressure of warmer than usual conditions for sea ice along an arc from the Mackenzie Delta and Adjacent Canadian Arctic Archipelago to the East Siberian Sea. Warm winds would assault the ice from launching pads over warmer land masses in this zone, resulting in increased and early ice erosions.

Already, we can see such conditions emerging in the following MODIS satellite shots provided by NASA:

Mackenzie Delta May 11, 2014

(The Mackenzie Delta [upper left] and adjacent Canadian Archipelago waters. Image source: LANCE-MODIS.)

The above image shows the Mackenzie Delta and the Canadian Arctic Archipelago on May 11 of 2014. In these images, we can seen the result of continued warm winds from the south and near-or-above freezing temperatures. For the Mackenzie Delta, temperatures since early May have ranged between 23 and 42 F, or between 5 and 25 F above average for this time of year. The high temperatures have brought the snow melt line all the way to the coast very early and have resulted in both ice melt and retarded refreeze in the broken ice and large polynyas offshore in the nearby Beaufort. Note that an additional heat influx to these coastal waters will occur once the shallow Mackenzie River fully melts, likely resulting in the early break-up of land-fast ice near the delta.

Chukchi Beaufort Melt May 11, 2014

(The Chukchi and Beaufort Seas on May 11, 2014 from the Bering Strait [upper left] to past Barrow, Alaska [lower center]. Image source: LANCE-MODIS.)

Further along the Canadian and Alaskan coasts, we find a continuation of sea ice weakness and break up in the off-shore regions north of Barrow Alaska and on into the Chukchi Sea. Large polynyas remain open throughout the region and exhibit no refreeze in the open water sections. Past the Bering Strait zone, Chukchi melt is very well advanced for early-to-mid May due to a combination of near constant warm southerly wind influx and an advancing warm water wedge through the Bering Strait.

This warm wind pattern through Eastern Siberia, Alaska and Canada and into the Arctic Ocean is reinforced by a combination of ongoing factors including a weakened polar Jet Stream which has tended to generate high amplitude ridges in this zone, a very warm pool of water in the Northern Pacific south of Alaska, and an emerging El Nino which historically has tended to push a high amplitude split in the Jet Stream up toward Alaska. These self-reinforcing factors make it likely that the overall pattern of warm southerly winds over the region will continue to persist and have an impact well into summer.

Finally, it is worth noting that the current and ongoing warm air influx through this region provides a constant source of energy for Arctic storm genesis, a factor that may well become more significant as melt season progresses. Forecasts for the next 24 hours show a storm pulling warm, above-freezing temperatures deep into the Beaufort as it begins a transition toward the northern polar zone. It is the second system to exhibit such anomalous warm air inflow and progression into the Central Arctic during the month of May.

GFS Warm Storm

(GFS model summary showing warm storm with associated above-freezing temperatures invading deep into the Beaufort Sea during late Monday and early Tuesday of this week. Image source: University of Maine.)

A third warm air invasion, this time from Eastern Siberia, and potential related storm development is also projected for late this week or early next week.

The Arctic dipole: storms over the Arctic Basin, high pressure over Greenland. Today, we track three Arctic low pressure systems — one emerging from the warm air influx over the Beaufort, one over the Laptev and one north and east of Svalbard. Greenland, meanwhile, shows a high pressure system centered almost directly over its large ice sheet. The net effect of these lows and highs is to funnel the warm wind streaming up from the Beaufort over the Northern polar zone near the Canadian Arctic Archipelago and out over the Fram Strait and Svalbard.

It is a dipole of high pressure over Greenland and low pressure over the Arctic Basin on the Central and Eastern Siberian side that has lasted for about two months through Northern Hemisphere Spring. This set-up creates a strong and consistent wind pressure providing transport of sea ice out of the Fram Strait. It is worth noting that Fram Strait export was one of the primary factors involved in the record low sea ice total seen during 2007, so a consistent dipole pattern of storms over the Arctic basin and highs over Greenland promoting ice export could well weigh heavily as melt season progresses.

Warming over Western Russia and Eastern Europe. A second zone showing consistent ridge development, polar Jet Stream weakness and coincident anomalous warming has emerged over western Russia and Eastern Europe. Such warming was seen during the weak El Nino of 2010 and resulted in severe heatwaves and wildfires for the region. A similar pattern has emerged in tandem with the rising and potentially far stronger 2014-2015 El Nino currently developing in the Eastern Pacific. Though it is too early to tell if this emerging hot zone will reach the extremes seen in 2010, this heat pool is likely to contribute warmth to sea ice zones in the Kara and Laptev Sea as the summer melt season progresses.

So far, Kara sea ice retreat has remained within usual boundaries for recent years. However, it is worth considering the potential strength of this developing warm air pool and how it may impact adjacent Arctic zones as May progresses into June. This week’s forecast now shows above-freezing temperatures predicted to progress into the Kara and 50 degree F readings predicted to push into estuaries bordering the Kara over the next few days.

Warm water upwelling, north wind flush, storm suction for Baffin Bay. Finally we come to Baffin Bay, a place many may well consider the Arctic Ocean’s red-headed stepchild. Over recent years, warm water up-welling, possibly driven in part by sea-bed methane release, in Northern Baffin Bay has resulted in an almost constant weakness and erosion of sea ice. This condition creates a bizarre circumstance in which Baffin is often surrounded by warmer waters north and south by late spring. This year is no exception. In addition, a north wind now appears to be flushing Baffin Bay sea ice toward the North Atlantic. The result is an expanding zone of ice-free water along the West Coast of Greenland pushing toward a widening gap in the north of Baffin Bay near the Nares Strait.

To the south, a persistent storm has developed near an anomalous cool zone in the North Atlantic waters off of Newfoundland. This cold pool is likely a residual of the continued dipole, hot-west, cold-east temperature anomaly over North America which has increasingly been squashed toward Newfoundland with the emergence of summer. The cold North Atlantic pool is also likely fed by a rising outflow of fresh, cold water from Greenland glaciers as well as the Baffin Bay ice export already described. A growing Gulf Stream weakening is also well established for the region.

The persistent storm is fed by high temperature differentials in the dipole zone. It is one of the remnant storm systems of this winter’s epic assault on the coasts of Great Britain — a possible precursor to even more vicious storms this coming winter.

But, today, the storm is simply providing added suction to drain ice out of Baffin Bay.

Storm off Greenland and Newfoundland

(Like a drain in a massive bathtub: storm off Greenland and Newfoundland on May 12 reinforces northerly wind flow pulling sea ice out of Baffin Bay. Image source: LANCE-MODIS.)

A final word on Storms and Warm Winds

During late April, we talked a bit about the impact of early season melt ponds on end-season sea ice levels. For recent scientific studies have found that early season melt pond formation has a high correlation with new record lows in sea ice area and extent.

But given the current very thin and broken state of sea ice, it’s worth considering whether the rules for sea ice loss aren’t in the process of changing.

Ever since the 2012 melt season’s close, the Arctic Ocean has exhibited a very battered sea ice state. One featuring widely disassociated packs of broken and brittle ice riddled with a long and pervasive spidering of leeds. For large melt pond systems to develop, the ice pack needs to be relatively contiguous. But the recent ice pack shows very little continuity and could, instead, be said to basically lack integrity. Such a state may well prevent a degree of melt pond formation in areas in which the ice is more and more highly disassociated into floes. And it is this disassociated ice state that may be the current and future norm as sea ice continues to thin and weaken.

In addition, rising temperatures in and around the Arctic have resulted in increased atmospheric water vapor content, increased cloud formation, and increased storm presence during summer periods. This progression toward storminess is consistent with paleoclimate studies showing that ice-free or near-ice-free Arctic states were much stormier than the current one. In the event of an expected stormier Arctic, melt pond formation may well result less from direct solar insolation through clear Arctic skies and more from an increasing number of rainfall and warm fog events over sea ice.

Cyclonic pumping of warmer waters from below the ice pack into surface water zones and the mixing of waters by waves generated by storm winds is also likely to have a far greater impact on sea ice melt than seen in recent years. It is likely we saw a prelude to just such an event during the great, late-season Arctic Cyclone of 2012 which sent waves the size of houses roaring across the Beaufort Sea to batter and disassemble the already weakened sea ice.

In this dynamic and changing system, warm winds are also likely to play a much greater role. Jet Stream erosion, in such a case, unleashes warm southerly winds on the sea ice. The winds, being warmer, hold a higher water vapor content than was typical for the Arctic prior to the human warming insult. Encountering ice and cold water, the water vapor in the winds condenses to form fog. The latent heat in the water vapor is thus released to do work melting the sea ice and warming the sea surface. In such cases, a kind of snow and ice eating mist develops from the warm wind — a blow torch for the sea ice.

Links:

LANCE-MODIS

Dual Ridges Form Sea Ice Achilles Heel for Summer 2014

University of Maine

PIOMAS

Wipneus

Cryosphere Today

NSIDC

Arctic Sea Ice Graphs

The Arctic Sea Ice Blog

The Storms of Arctic Warming

North Atlantic Ramping up to ‘Storms of My Grandchildren’ to set off Major Flood Event for Tempest-Tossed England?

Storms Reshape England's Coastline

(Storms Reshape England’s Coastline during Winter of 2013-2014. Image source: AGU)

Under the ongoing insults of human-caused climate change, the North Atlantic is ground zero for the potential development of the worst storms humankind has ever experienced. And indications are that the ramping up to this dangerous time may well be starting now.

The temperature related weather instabilities between the warming North Atlantic, the melting but still frigid ice packs of Greenland, the retreating polar sea ice, a continental North America enduring a series of polar vortex collapse events flushing cold air south as the Arctic experiences its warmest readings in an age, and an interior Europe and Asia that are also experiencing mass migrations of cold air fleeing the ever-warmer Arctic are just screaming.

A bite of warm air and related warm ocean water has flooded a large region between Scandinavia, Svalbard and Novaya Zemlya, making its home where winter sea ice once resided. The waters near Greenland are now melt-cooled by the 500 gigatons of average annual glacial outflow occurring there. And the never-ending influx and concentration of heat in the Arctic has set the Jet Stream into a fit of wild loops and whirls.

All these changes result in a high degree of weather instability, in a setting off of extreme weather events, of great switches from cool, to extreme hot, from record drought to record deluge. In the past few years we’ve seen these kinds of extreme weather events occur with increasing frequency. But now, a new kind of extreme event is beginning to emerge, a kind of event that may well be prelude to ‘The Storms of My Grandchildren’ Dr James Hansen alluded to in his prescient book examining the ultimate consequences of an ongoing and devastating human greenhouse gas emission.

The Breeder of Storms: Our Warming-Ravaged North Atlantic

Ever since winter began to settle in, and the extreme effects of Northern Hemisphere temperature imbalance and Jet Stream changes began to take hold, the North Atlantic has become a breeder of extraordinarily powerful storms. According to reports from NOAA’s Ocean Prediction Center, the month of December alone featured 14 instances of hurricane wind events, 10 storms that experienced rapid intensification, and 5 storms that featured pressures of 950 mb or lower.

For comparison, a tropical storm that hits 950 mb is usually a category 5 hurricane. And for any ocean basin to show 14 instances of hurricane force winds let alone 5 950 mb and below storms over a one month period is extraordinary indeed. Imagine if the south Atlantic generated 10 hurricanes 5 of which were cat 5 in just one month and then you get a general comparison.

Two of these storms were particularly intense with one reaching 940 mb and another deepening to an exceptionally low 929 mb (the lowest reading ever recorded for the North Atlantic was 916 mb). By comparison, the freakish monster that was Hurricane Sandy bottomed out at 940 mb.

It is worth noting that the storms of the North Atlantic typically spread their energy out over larger areas than a tropical system. So though pressures are low enough to be comparible with the most intense tropical storms, the winds generated typically ranged from 75 to 100 mph while extending outward over hundreds of miles. By comparison, a typical tropical cyclone would have a very intense wind field within 20 to 100 miles of its center with intensity rapidly falling off beyond this zone.

Overall, the North Atlantic sees very few storms of 940 mb or lower, usually at the average rate of less than one every year. So for two to occur in the same month is exceptional indeed.

929 mb low raking the coast of England on Christmas Eve

(929 mb low rakes England with hurricane force winds on Christmas Eve, 2013. Image source: Lance-Modis.)

January also featured an almost endless cavalcade of intense storms rushing across the North Atlantic with numerous lows bottoming out below 950 mb (NOAA will issue a final tally sometime in February). Meanwhile, powerful storms developing in the North Atlantic continually pummeled Europe throughout most of the winter of 2012-2013 resulting in some of the worst rain and snowfall events ever recorded.

This recent climate-change driven shift of the North Atlantic into an increasingly stormy weather pattern may well be a prelude to even more extreme changes to come. Weather models produced by GISS and examined by premier climate scientist James Hansen indicate that very powerful storms arise in conjunction with increasing Greenland melt. Large pulses of fresh, cold water entering the North Atlantic were observed to create climate instabilities that resulted in very powerful storms with frontal systems the size of continents that packed the punch of hurricanes in the physical model runs. It was the likelihood that such storms could emerge by or before mid-century that, in part, spurred Dr. Hansen to write his prescient book — The Storms of My Grandchildren.

As noted above, the current Greenland melt outflow averages about 500 gigatons each year. This outflow is already large enough to weaken the Gulf Stream and set off severe weather instabilities. But with Arctic warming continuing to amplify and Jet Stream patterns bringing more and more warm air over Greenland, melt rates may triple or more over the coming decades, resulting in even more severe weather consequences. So the extreme storm patterns we see emerging in the North Atlantic now are likely just a minor prelude when compared to what we will witness as the years and decades progress.

England in the Firing Line: Windiest December Precedes Wettest January

Currently in the direct firing line of these powerful storms are the main islands of the United Kingdom. Throughout December, England suffered an almost constant assault of storms. In total, five storms, or more than one storm per week brought excessive rains and wind gusts in excess of hurricane force to the British Isles. The results were tens of thousands of power outages, major waves and storm surge events along the coastline resulting in damage to coastal structures and persons being swept out to sea, and increasing instances of flooding over saturated ground.

On record, December 2014 was one of the stormiest ever seen for the British Isles. According to weather data, the month was the windiest since record keeping began in 1969:

Wind Gust Measure Met

(Image source: UK Met Office)

In addition, December also ranked one of the rainiest with many locations seeing 3 times the normal level of rainfall for the month.

As the new year began, the series of severe storms impacting the UK continued unabated through late January. And as of the 28th, South England had experienced its wettest month since record keeping began in 1910. With a month and a half still remaining Southeast England had already experienced its 6th wettest winter season on record.

UK Rainfall

(Southeast UK Rainfall from 1910 to present with 2010 easily setting a new record. Image source: Met Office)

Dr Richard Dixon, director of FES Scotland when commenting in a Guardian interview about the most recent spate of anomalous UK weather noted:

“November and December were record breakers in Scotland, with storm after storm hitting around Christmas. Climate change is bringing chaos to our weather, not just increasing global temperatures but affecting ocean currents and global air currents. Scotland is caught between the changing influences of disappearing Arctic ice, the shifting jet stream and a weakening Gulf Stream. It is no wonder our weather is becoming less and less predictable. The consequences for us are more extreme weather, including more flooding.”

Very Dangerous Flood Situation for Southwesr England: Powerful Storm on the Way

The extreme rainfall, as of today, had resulted in a major flood event for Southeast England focusing on the Midlands and Somerset. The event inundated croplands, homes and farms throughout the rural region and spurred England to put its military on standby as forecasts show more rain and high winds are on the way. The anomalous event also spurred the 15th meeting of COBRA, the UK’s emergency response committee which has, increasingly, been called due to a continuous barrage of weather emergencies.

Somerset Floods

(Aerial photo showing homes, businesses and a vast area of land flooded in Somerset, England. Image Source: David Hedges)

In addition to the clearly visible inundation, numerous villages in the region have been cut off due to flooded roads for more than a week (with some areas being cut off for a month). The constant barrage of storms has resulted in both persistently high tides and almost continuous rainfall. The rainfall, trapped by high sea water, has nowhere to escape and simply pools, continuing to build up in the low-lying lands.

The UK’s conservative government’s response to the situation, thus far, has been anemic, waiting until today to declare the region a disaster area.

Unfortunately, another powerful storm is predicted to arrive by Saturday bringing with it yet one more spate of strong winds, heavy surf and driving rainfall to the already soaked region.

Saturday Forecast Map NOAA

(NOAA forecast map for Saturday. Note a powerful 953 mb storm forecast to impact the UK with 70+ mph winds and heavy rainfall. Image source: NOAA’s Ocean Prediction Center)

So if you’re living in Southeast England please do your best to remain safe, to heed government warnings, and to urge your government officials to provide you with the level of response you deserve during this dangerous time (including policy changes to reduce the rapidly increasing degree of harm coming from human caused climate change).

Early Storms Minor by Comparison

It is worth noting that, though more intense than we’re used to, these storms are the early, weaker outliers of a very dangerous period that is to follow. Our best models and our best climate scientists report the likelihood of far more dangerous storms emerging from this region and from the set of conditions that includes a weakening Gulf Stream, a melting Greenland, an amped up hydrological cycle and rapidly warming zones first at the northern polar region and then in the tropics. The eventual size of these storms could expand to cover continents and involve multiple linked and powerful storm centers. As noted above, Hansen warned of frontal storms large enough to blanket continents and with areas of hurricane strength winds stretching thousands of miles. We haven’t seen anything like that yet. And so the freakish and extraordinary weather we’ve witnessed this winter, and in recent years, is merely prologue for worse events to follow.

Links:

AGU

NASA: Lance-Modis

NOAA’s Ocean Prediction Center

UK Met Office: Winter Storms December 2013 to January 2014

Parts of England See Wettest January Since Records Began

UK Floods: January Rain Breaks Records in Parts of England

Colorado Bob’s Climate Feed

The Storms of My Grandchildren

Beneath the Cracking, Melting Ice, the Arctic Methane Monster Continues its Ominous Rumbling

Methane Concentration

(Large Northern Hemisphere methane overburden points to major Arctic emission. Image source: NASA)

“How am I going to be an optimist about this?” — excerpt from Pompey

*    *    *    *    *

In the high north, deep beneath the sea ice, sequestered within the sea bed, sleeps a monster. A massive store of methane that is the relic of ages past. A beast whose vast body is composed of hundreds of gigatons of this climatologically volatile gas.

Since times immemorial, the monster slumbered. Accumulating vast size and girth through a near constant rain and sequestration of biological material as the long ages passed. Until human time, that is, when an unprecedented warming began to prod the monster to waking. And so, during recent years, the monster has stirred, even as more and more of this gas has been observed escaping into the atmosphere.

What is happening can be compared to the, at this time, slow initial rumblings of a climate volcano. The gas, forced out of its icy traps in the sea bed, escapes into the ocean where it destabilizes the sea bed and wrecks jarring changes on the marine environment. It bubbles up beneath the ice, running along beneath the strong ice to find holes where the ice is weak, or escaping out from under the ice edge. And in these places, it runs out into the atmosphere. There, the gas is between 20 and 100 times as potent a warming agent as CO2 by volume. There, it inevitably adds to the human warming and emissions nightmare now underway.

In other places the tundra thaws, unleashing its own monstrous volumes of methane, adding to the giant emerging from the troubled seas.

We have seen the large and growing escape of methane in the great 1 kilometer plumes in the East Siberian Arctic Shelf and in other large releases off of Svalbard. We have seen them in the 150 kilometer atmospheric plumes observed by NASA’s CARVE study. We have seen them in ‘hot’ melt lakes that bubble with methane dense enough to burn. We have seen them in the explosive Arctic fires that burn the thawing and volatile land itself.

These all-too-obvious hints of steadily increasing emissions are ominous, not only for their current warming contribution, but for the potential of an even more rapid and violent release. For the eruption of the methane monster, though somewhat gradual now, could, in the build-up to an immense disaster rarely witnessed on Earth, evolve into an ever more deadly and rapid release.

There is evidence of such events in the geological past. Events that have left their black fingerprints splattered over most, if not all, of the climate mass extinctions. And there are a handful of leading scientists who are very concerned that such an event may well be in the offing.

The Methane Monster Continues its, For Now Gradual, Emergence

methane-jan21-31

(Image source: Dr. Yurganov)

Unfortunately, 2013-2014 marked the continuation of a dangerous trend where, once again, rates of Arctic methane emission were shown to increase markedly over those seen during previous years. In the above series of enhanced Aqua satellite images, provided by Dr. Leonid Yurganov you can see the steadily increasing volume of atmospheric methane in Arctic regions during a time of typical methane peaks in late January from 2009 to 2013.

A more comprehensive slide-show ensemble displays Arctic methane increases from 2003 through 2012 here. It is is worth noting that top scale values were 1870 ppb in this video series. In the more recent series (images above and below), the scale has been increased to a maximum value of 1920 to account for spiking atmospheric levels. So don’t let the moving goal posts fool you!

Though we are still about two weeks away from the start of 2014 Arctic methane peaks, early data throughout the fall and winter has shown a marked increase in methane values when compared to similar periods last year. The below image, as an example, compares January 1-10 of 2013 with the same period of 2014:

methane 2013 to 2014 January 1 to 10

(Image source: Dr. Yurganov and Sam Carana)

These images, also provided by Dr. Yurganov and composed by Sam Carana, show substantial levels of methane increase for the Arctic during early January of 2014 when compared to the same period in 2013. Especially of note was the significant increase in methane concentrations over the Barents Sea where values were consistently higher than 1920 parts per billion.

It is worth mentioning that during 2009, the same region saw methane levels in the range of 1870 parts per billion and that the jump of +50 ppb or more during this interval is roughly consistent with global average increases. What is more concerning, however, is that these maps clearly show this region of the Arctic as a primary methane hot spot, indicating the likelihood of a very large emission seeping out from under the ice and up from the depths of the ocean.

Overall methane spikes in the Arctic were very significant with, according to observations from Methane Tracker, values exceeding extraordinary levels of 2400 parts per billion in local spikes.

NOAA’s ERSL monitor at Barrow also found large local spikes in the range of 1995 parts per billion during late December:

Barrow Methane 2012 to 2013

(Image source: NOAA ERSL)

Note that local methane levels at Barrow, Alaska on the Arctic Circle have risen from an average of 1895 ppb during early 2012 to about 1920 ppb by early 2014, an increase of more than 12 parts per billion per year.

Globally, methane levels have also been on the rise. The record at the Mauna Loa Observatory is now closing in on 1840 parts per billion and shows a significant upward curve during the past two year interval. Though not rising as fast as regions close to the large Arctic emissions sources, the Mauna Loa measure shows a jump of about 15 parts per billion over the two year interval from early 2012 to early 2014.

Mauna Loa Methane 2001 to 2014

(Image source: NOAA ESRL)

Above we can see the global trend line for methane as measured at the Mauna Loa Observatory. Note that methane increases had slowed during the period of 2001 to 2006. But in 2007, at about the time Arctic sea ice began its rapid retreat, methane levels commenced a rapid rise. Of particular concern is the gradual upturn in the global average methane curve leading into early 2014.

Very High Arctic Temperature Anomalies Coincide With Rising Methane Levels

As methane levels have continued to rise throughout the Arctic, so have winter temperatures. During 2013-2014, abnormal Arctic winter warmth, especially over the Arctic Ocean, the Barents Sea, and the Bering Sea, has played havoc with Northern Hemisphere weather. In early January, a spate of intense Arctic warmth collapsed the polar vortex, shoving a powerful remnant low southward and setting off a 20 year cold snap in the US. The same extreme winter weather pattern that has impacted much of the US also unloaded a fusillade of storms on the coastlines of the British isles, breaking thousand ton rock structures and reshaping seemingly impervious coastlines.

In this case, the added methane release contributes to polar warming amplification and, at this time, is setting in line a series of increasingly violent weather events likely to ramp up over the coming years and decades. In such cases, the methane monster’s contributions to warming cannot be detached from the changing climate as a whole. In fact, it is the kind of amplifying feedback that makes our situation far more dangerous.

Arctic 30 day anomaly a

(30 day Global Temperature Anomaly from 1981 to 2010 base line. Image source: NOAA)

Note the extreme temperature anomalies over the past 30 days throughout much of the high Arctic with extremes ranging from 2-6 degrees Celsius above the, already warmer than normal, 1981 to 2010 average. This is just the kind of heat, in conjunction with rising greenhouse gasses, that we would expect from an Arctic undergoing dangerous, if not yet catastrophic, change.

Is Optimism Rational?

Given the evidence showing an amplifying methane signal coming from the Arctic, a signal that becomes louder with each passing year, it becomes more difficult to cling to the comfort provided by a number of the more conservative scientists on the issue of methane release (hydrates, compost bomb or other). Though we have not yet seen major releases large enough to push global methane levels higher by 50, 100 or more parts per billion per year (as we would see during an exceptionally catastrophic event), what we have seen is a growing Arctic release that remains a serious cause for concern.

In such an instance, we might be wise to compare the Arctic Methane Monster to a massive volcano. One that continues to rumble even as it releases ever greater volumes of its climatologically volatile and heat-contributing gasses. As anyone living in the neighborhood of a volcano can attest, it’s generally not a good idea to ignore such things. In this case, the monstrous volcano is so large as to make all the Earth its neighborhood. So we should all be paying attention.

Links:

NASA

NOAA ESRL

Methane Tracker

Climate Change Driven Storms Reshape Coastlines of the British Isles

Arctic News

Arctic Ice Graphs

Playing with Global Fire

Amplifying Feedbacks

It’s The Collapsing Polar Vortex

Arctic Methane Monster Stirs

Persistent Arctic Cyclone 2013 Churns On, Shattering Central Arctic Sea Ice as Arctic Interior Continues to Warm.

Today, clouds parted enough over the Central Arctic to give us a visual of the ongoing damage inflicted by 2013’s Persistent Arctic Cyclone (PAC). And the damage, as we can see in the images below is extensive.

For comparison, I have provided this shot, taken on May 26th, just as the PAC was beginning to ramp up. Note how pristine and mostly crack-free the ice looks in this satellite shot. Though areas of leads and cracks exist, they are comparatively minor, small, and diffuse.

ArcticCentralBasinBeforeMay26

(Image source: Lance-Modis)

Today’s most recent Lance-Modis shot shows conditions that are radically different. Note the broad, black spider-web of cracks that has come to dominate this large region of the Central Arctic Ocean. The only places where these large, angry cracks aren’t visible is in areas still covered by dense cloud:

ArcticCentralBasinAfterJune13

(Image source: Lance-Modis)

Uni-Bremen sea ice concentration assessments have now been showing confirmation of the storm’s thinning action for more than a week. Today’s concentration graphic provides yet one more validation of central area sea ice losses.

PACBremenarctic_AMSR2_nic

(Image source: Uni-Bremen)

This is the wreckage 18 days of constant pounding has inflicted upon some of the Arctic’s most resilient sea ice. One doesn’t have to think too hard to imagine what another 18 days of such pounding may look like. The Navy CICE/HYCOM model run further on in the post gets us less than half-way there. And weather forecast models show PAC 2013 remaining in the Central Arctic at least until Wednesday of next week.

PAC Positioned Near Warm Air Influx

PAC2013PressureJune13

(Image source: DMI)

The current pressure map shows the cyclone centered near the North Pole. Incorporated in its circulation are two weaker storms — one near the Kara Sea, the other over the East Siberian Sea. Lowest pressures are in the range of 990 mb.

Over the past few days, warmer air has been flowing into the Arctic from the region of Alaska and Kamchatka. This warmer air is embedded throughout the Arctic and is, largely incorporated into the circulation of our cyclone. So a substantial portion of the Central Arctic shows above freezing temperatures at this time:

PACtempsJune13

(Image source: DMI)

Model forecasts show this warm air influx continuing to grow over the next week with above freezing temperatures covering larger portions of the Central Arctic as time moves forward. Above freezing temperatures are rather common this time of year. What is less common is for cold-core Arctic storms to host such temperatures, even during summer time.

A Constant Influx of Storms

One of PAC 2013’s unique features is its ability to consistently gobble up smaller storms. Storm after storm has arisen from the south, only to be subsumed by the Persistent Arctic Cyclone. This constant infusion of energy from the south is, likely, one of the features that has allowed PAC 2013 to last as long as it has.

Model forecasts show this trend continuing until at least June 19th. At that time, the cyclone is shown to transition to the Canadian Archipelago, as weaker storms trail along through the Central Arctic behind it. This projected storm track brings PAC 2013 on a path directly through a region of the Arctic’s thickest ice just north of the Canadian Arctic Archipelago.

Throughout this period, PAC 2013 is expected to maintain a strength between 990 and 1000 mb — about the intensity of a moderately strong tropical cyclone, but diffused over a much larger area. Current projected storm track and strength show that it may pose a risk to fracture, disperse, and thin a section of ice that has been, thus far, left relatively unscathed.

Here is the ECMWF model forecast showing the storm’s predicted position on June 18th:

PAC2013June18

(Image source: ECMWF)

That puts a moderately strong 995 mb storm directly over the thickest part of the ice pack sometime next Tuesday.

Fram Strait Export

The constant counter-clockwise motion of PAC 2013 has also begun to have a substantial impact on the remaining thick ice near Greenland and the Canadian Archipelago. Since late May, this region has shown a thinning at the edges and a consistent motion toward the Fram Strait.

This motion is plainly visible in the US Navy CICE model history and forecast from May 23 to June 20 (posted below). Note the large front of greens and yellows (denoting thicker ice) pushing steadily toward the Fram Strait between Greenland and Svalbard.

It is also worth mentioning that the amount of thinning forecast for a region from the North Pole to the Laptev Sea is astounding. Later days in the model forecast show this large region of thinning starting to wrap around the North Pole in the direction of Svalbard. The US Navy projects this region to include large areas of 0.75 meter thickness or less opening up in this region by June 20th. Bands of thin ice seem to be forming a ring pattern emitting out from the North Pole. A stunning effect more reminiscent of disaster movie graphics than actual weather forecast models. Should this forecast thinning emerge, it will be nothing short of remarkable.

PACforecastJune2013

(Image source: US Navy)

In conclusion, PAC 2013 continues. Though some models show the storm transitioning to the Canadian Archipelago by after June 20th, the storm appears likely to continue to impact one region of the Arctic or another for the time being. At 18 days, this is a very long-lasting storm, especially for early summer. Yet models show the potential for the storm to persist and continue to have impacts, having lasted at least 25 days by the end of some model runs.

Links:

Lance-Modis

Uni-Bremen

DMI

Arctic Ice Graphs

ECMWF

US Navy

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