Warm Winds Take Aim at Chukchi as Arctic Sea Ice Volume Hits Record Lows

Temperatures over the Chukchi Sea are predicted to hit as high as 37 degrees Fahrenheit (2.9 C) on Wednesday and Thursday as a massive high pressure ridge building over Alaska pulls warm, moist Pacific air northward. These temperatures represent staggering warmth for this Arctic Ocean zone during March when temperatures are typically about 54 degrees F (30 degrees C) cooler.

Major Warm Wind Invasion for the Chukchi This Week

(Multi-day above freezing temperatures for the Chukchi sea predicted for later this week is not a normal event for early March. Unfortunately, warm wind invasions like this one have become more common as the globe has warmed up due to human fossil fuel emissions. Image source: Earth Nullschool.)

This recent warm wind invasion is one of many observed over the past five years in which enormous bulges in the Jet Stream have pierced deep into what was once a mostly impenetrable pall of winter chill hanging over the Arctic. It’s a new atmospheric condition associated with rampant fossil fuel burning. One that has produced considerable damage to the Arctic environment by reducing sea ice coverage, threatening key species, melting glaciers and thawing permafrost.

Such incursions of extreme warmth bear the obvious marks of a failing of Arctic cold brought on by human-forced climate change and have tended to generate significant spikes in overall Arctic surface temperatures during fall, winter, and spring. This week’s warm air invasion of the Chukchi is expected to help push readings for the entire region above the 66 degree north latitude line to 4.5 C (8 F) above average for this time of year. That’s a strong departure for this region during the month of March when the typically more uniform advance of warmth in the lower latitudes tends to strengthen the Jet Stream — locking in Polar winter conditions in the far north through about the middle of April.

(The warm wind invasion of the Chukchi Sea is expected to help push overall Arctic temperatures considerably higher. Image source: Climate Reanalyzer.)

Far above average Arctic surface temperatures extending from October of 2016 through March of 2017 have been triggered again and again by these floods of warm air rising up from the south. And the net effect on Arctic sea ice volume has been little short of devastating.

Arctic Sea Ice Volume Lowest Ever Recorded During Winter, Comparable to Summer Volumes of the Early 80s

Arctic sea ice volume for both January and February of 2017 are now far below past record low trend lines for this time of year. Present record low monthly values for this past February are around 17,000 cubic kilometers vs previous record lows for the month during 2013 at around 19,500 cubic kilometers. Last February’s sea ice volume average of 17,000 cubic kilometers is about the same sea ice volume measured at the end of melt season in September of 1981. In other words, sea ice volume in winter now is comparable to sea ice volumes during the summers of the early 1980s.

(Arctic sea ice volume has never been this low during winter time. Image source: PIOMAS.)

All the record warmth flooding into the Arctic during 2016 and 2017 has undoubtedly contributed to these new record lows for sea ice volume. And a cooling of the Arctic surface relative to recent record warmth during March and April could soften this worrying trend somewhat. To this point, it is worth noting that sea ice extent measures are now closer to past record low trend lines. So there has been some slightly more hopeful inching back to slightly less ridiculously abnormal measures. A more positive movement that will likely take a hit as Arctic temperatures are predicted to significantly warm again this week.

Weather is Variable, But the Underlying Trend Looks Pretty Bad

Weather, as we should note, can be quite variable and may bring a more pleasant surprise later in the month. However, despite this potential, sea ice states are looking as bad or worse than they ever have at the end of freeze season. And it is worth noting that less ice coverage and volume leaves more dark water open to absorb the sun’s springtime and summer rays and less ice to reflect it. Furthermore, post La Nina periods, as we are now experiencing, tend to flush more atmospheric and ocean heat into the Arctic. So, despite the variable nature of weather overall, we’re in a bit of a situation where the systemic trend odds of a noteworthy sea ice recovery toward more rational trend lines pre-summer 2017 aren’t looking very good.



Arctic Sea Ice Graphs

Earth Nullschool

Climate Reanalyzer



Tropical Tidbits

Chukchi Sea

January Arctic Sea Ice Volume is Lowest On Record by a Considerable Margin

Almost continuous warm, moist air invasions of the Arctic during fall and winter of 2016 and 2017 have resulted in the lowest sea ice refreeze rates on record. As a result, the amount of ice covering sections of the Northern Hemisphere ocean is now remarkably lower than during past comparable periods. In other words, we’ve never seen a winter in which Northern Hemisphere sea ice was so weak and reduced.

One key measure, sea ice volume, has shown particular losses when compared to past years. And even taking into account a long term trend of ice losses for the northern polar region that has been ongoing since the 20th Century, the 2016-2017 losses stand out like a flashing red indicator light. A trend directly related to the human-forced warming of our world through fossil fuel burning and related greenhouse gas emissions.


(Significant sea ice losses during the winter of 2016-2017 show up clearly in the above PIOMAS graph. PIOMAS is a model measure of sea ice volume. And as you can well see when looking at the red line at the left hand side of the graph, the departure from past years is currently quite large. Image source: PIOMAS.)

In the above PIOMAS graph we find that January sea ice volume averaged around 14,000 cubic kilometers. This reading is roughly comparable to the early July average for the period of 1979 through 2016 — a time when the Arctic saw continuous declines in sea ice. The present reading is also about 1,500 cubic kilometers below the previous record low for the month of January set in 2013. And anyone looking at the above graph can well see that the departure is significantly below the trend line (about 8,000 cubic kilometers below the falling 38 year average for this time of year).

It’s worth reiterating that these are the lowest sea ice volumes ever seen for this time of year in the Arctic. A new record that comes after consistent new record lows occurring throughout the past 38 year period.

Presently, approximate 5 C above average temperatures are dominating the region above the 66 North Latitude. Over the coming days, a pair of warm air invasions of the North Pole region near 90 N are expected to push temperatures to more than 30 degrees Celsius above average and to near the melting point on two separate occasions. This pair of, not at all normal, events will likely produce additional sea ice losses in a polar region that is already seeing very unusual low sea ice concentrations, volumes and extents.


(Warm storm invasions of the northern polar region that inject high heat content, ice-melting moisture and far above average temperatures into the High Arctic have been a frequent occurrence over recent months. By February 10, GFS models predict that another such storm will push temperatures to more than 30 degrees Celsius above average for the North Pole and surrounding regions. This will produce yet one more powerful blow to sea ice attempting to rebuild in the region. Image source: Earth Nullschool.)

After these events roar through, the Jet Stream is predicted to flatten somewhat — allowing cooler air to re-establish over the Central Arctic as warmer air invades the mid-latitudes. As a result, air temperature anomalies in the 66 N and above region are expected to fall back to a range of 1 to 2 C above average in the 7 to 14 day timeframe. Such a return to closer to normal conditions may allow for more short-term bounce-back toward previous record low ranges in the volume measure. But a much longer period of closer to average conditions would be required for a full recovery.

Overall, refreeze season tends to last until April. So some time does remain for a bit of recovery. And we have seen extent measures trend closer to past record lows over recent days. However, considering the massive losses experienced during fall-winter of 2016-2017, two months is unlikely enough time to produce a significant recovery even if cooling to more reasonable above average temperatures were to occur and remain in place for an extended period.



Earth Nullschool

Climate Reanalyzer

Antarctic Sea Ice Likely to Hit New All-Time Record Lows Over Coming Days

Throughout the record global heat of 2016 and on into 2017, the world’s sea ice has taken a merciless pounding.

In the Northern Hemisphere, extreme warming of the polar region pushed Arctic sea ice extents to record low daily ranges throughout the winter, spring and fall of 2016. And even today, after many months of daily record lows, sea ice in the Arctic remains more reduced (in most measures) than it has ever been for this time of year.

On the other side of the world, the story is much the same. For it now appears that the ocean region around Antarctica is about to experience an all-time record annual low for sea ice:


(JAXA Antarctic sea ice measure for all years since 1978 shows a strong challenge to the previous record low for extent set in 1997 [lower left hand corner of the graph]. With 2-4 weeks left in the melt season, the present measure is just about 170,000 square kilometers above the 1997 record low during Southern Hemisphere summer.)

Anomalous warmth, though less intense than in the Arctic zone, did finally begin to invade the austral polar region during Southern Hemisphere spring and summer (2016-2017). And since mid October, sea ice surrounding Antarctica has remained in record low daily ranges (see lower red line on the graph above). Wednesday, February 1st’s, JAXA measure of 2.42 million square kilometers of sea ice extent remaining is now just about 170,000 square kilometers above the previous record low sea ice extent set during mid-to-late February of 1997.

During this time of year, average drops in sea ice extent are around 50,000 square kilometers per day. So if all things were equal, we’d expect melt inertia to push the measure into new record low ranges over the next 3-5 days. Unfortunately, there appears to be an added impetus for melting as another blast of above average temperatures is being drawn into Antarctica underneath strong ridging features in the Southern Hemisphere Jet stream.


(Warmth building into Antarctica over the next two weeks may be the final straw that tips the near ocean region into new all-time record lows for sea ice extent. The above GFS model prediction for February 9th rendered by Climate Reanalyzer shows temperature anomalies predicted for Antarctica and the surrounding regions. Red to orange is warmer than average, blue to purple is colder than average.)

As a result, over the next week, temperatures around Antarctica and in the nearby region of the Southern Ocean are expected to average between 1.2 and 1.8 C above the already warmer than normal 1979 through 2000 average. Meanwhile, parts of West Antarctica’s coastal zone are expected to hit as high as 5-20 C above that average.

With more warmth on the way, with measures already striking nearly half a million square kilometers below previous daily record lows, and with at least two weeks remaining in the melt season, it appears likely that we are in for a new all-time record low for sea ice extent in the ocean region surrounding Antarctica. If the new record does occur, it will happen during a time when the Arctic is also experiencing daily record lows for sea ice during Northern Hemisphere winter and as the world is experiencing global temperatures in the range of 1 to 1.2 degrees Celsius above 1880s averages.


JAXA Sea Ice

Arctic Sea Ice Graphs

Climate Reanalyzer


The Human World Has Never Experienced A Time When Global Sea Ice Was So Weak and Reduced

Neven — one of the world’s most beloved sea ice trackers — has again taken a break from his much-earned sabbatical to issue yet one more warning on the state of global sea ice.

His report, based on this month’s bombshell National Snow and Ice Data Center statement, can best be described as an urgent call for action on the part of the global community to redouble efforts aimed at reducing the wide-ranging and expanding harms caused by the terrible warming trend we have artificially forced upon our world.

Neven is a kind, honest, and open soul. He is also one of the smartest and decent fellow bloggers I have had the good fortune of encountering in my many travels during my last four years of covering the slow motion global train wreck caused by our widespread and vastly irresponsible burning of fossil fuels. In other words, the man, in my view, has the moral and intellectual authority that many lack. We should listen to him.

Before the World Warmed, This Would Have Been a 1 in 30 Billion Probability Event

For, sadly, on the crucial issue of sea ice, a general muting of the subject has tended to continue despite a jaw-dropping plunge in both the coverage and volume of a substance so crucial to maintaining a stable global climate:


(Global sea ice extent fell off a cliff during December of 2016. The measure has now bounced back a little. But the global average remains significantly below past record lows for this time of year. Loss of so much sea ice can be highly disruptive to the climate system and related atmospheric circulation and precipitation patterns. Image source: NSIDC.)

During December, global sea ice extent coverage fell to an amazing 4.4 million square kilometers below average. This is far, far outside the 2 standard deviation range — passing to fully 8 standard deviations beyond the typical yearly average.

Under past expectations of average, the statistical probability of such an event is approximately 1 in 30 billion. Of course, it’s pretty obvious at this time that a normal, natural variability is not the underlying cause of such a great loss of sea ice. That the warmth we added to the system has now greatly tipped the scales beyond anything representing what would have previously been considered a normal range. A range that since the year 2000 had already tended to dip below average more and more frequently. But one that has never seen so much ice lost.

Unprecedented Losses

This area of sea ice removed — enough to change how the face of our Earth looks from space — is approximately the size of two Greenlands (Note that sea ice loss does not directly contribute to sea level rise. But loss of protective sea ice can contribute to land ice melt — which does add to rates of sea level rise.). And it has been roughly split between the Arctic in the north and the Antarctic in the south.

If sea ice extent losses appear bleak, then sea ice volume losses seem even worse. Sea ice extent is a rough measure of the surface of the world covered by ice excluding gaps behind the leading ice edge. Sea ice volume, however, measures both the ice area — including gaps — and the ice thickness.


(Globally, we’ve lost about 1/3 of the total volume of sea ice since the 1980s. 2016’s record fall in the measure coincided with record hot global temperatures and an abnormal period of polar warming that continues on into 2017. Image source: Wipneus.)

Late 2016’s big drop included the approximate removal of 1/3 of the world’s sea ice volume when compared to 1981-2010 averages. In other words, 1/3 of all of the floating portion of the world’s cryosphere beyond the edge of anchored ice shelves had melted away during the period.

Record Global Temperatures as Prime Cause For North and South Pole Sea Ice Melt

In the north, extremely warm temperatures ranging from 2 to up to 7 degrees Celsius above average for the Arctic Ocean region have helped to drive these unprecedented fall and winter sea ice losses. In the south, warmer than normal surface conditions appear to have also helped to drive the amazing coordinate losses there. And overall, 2016 has shown warm to extremely warm conditions for both poles during a year in which global temperatures have spiked to around 1.2 degrees Celsius above 1880s averages.


(Extremely strong polar amplification during 2016 is the likely primary contributor to sea ice loss in both the northern and southern polar regions. Image source: NSIDC.)

Under polar amplification — a condition associated with the human-forced warming of our world — scientists expected that the polar regions would tend to warm faster than the rest of the Earth surface. And during 2016, this global warming related condition presented effects writ large.  The damage to sea ice, so far, has been monumental. And these losses have continued into 2017 — even if they are somewhat less below the record low line than during their period of maximum departure this past December.

Albedo Losses and a Bad Set-up for Arctic Summer

Sea ice loss generates its own form of amplifying feedback — in which already prevalent polar warming can worsen further. Less ice coverage means that during summer more of the dark ocean surface is presented to absorb the sun’s rays. This replacement of a white, reflective surface with a dark blue, absorptive one means that still more heat will tend to be trapped in the polar environment. In addition, during winter, less ice cover means that the warmer ocean beneath will tend ventilate more heat and heat-trapping water vapor into the polar atmospheres. And it’s this kind of self-reinforcing cycle that can tend to lock in the dangerous changes like worsening severe weather, worsening heatwaves in the middle and lower latitudes, and the increasing rates of land glacier melt and sea level rise that scientists have been warning about for so long. And it’s this kind of disruptive longer term climate trend that we are being drawn into at this time.


(Freezing degree days for the crucial 80 N region have significantly departed into record low ranges. The less freezing degree days, the closer this region is to thawing. Image source: Tealight. Data Source: DMI.)

Nearer term, it appears that the polar heat which has already so greatly damaged the Arctic sea ice is set to stay. Over the next few days, the Arctic appears set to experience a powerful series of low pressure systems running in from the Barents side between Svalbard and Siberia. Neven warns that these storms will tend to push a considerable portion of the remaining thick ice out of the Arctic and through the Fram Strait. Over the next couple of weeks, global forecast models indicate that above freezing temperatures will tend to invade regions now covered by sea ice in Hudson Bay, Baffin Bay, and in the Chukchi Sea. Though the ice is trying to grow, such repeated insults will tend to keep ice coverage in record low ranges.

If this trend of warmth, storms and ice export continues through February, March and April — as it has during October, November, December and January — then the set up for the 2017 melt season would be about the worst we have ever seen. And that would tend to increase the likelihood of new record minimums being reached during September all while hastening the day when the Arctic experiences near ice free conditions. Lets hope that doesn’t happen. But, so far, the trends for the winter of 2016-2017, from pole to pole, have followed along the lines of a near worst case scenario.


Global Sea Ice Records Broken Again

National Snow and Ice Data Center Sea Ice News

Wipneus Sea Ice Graphs

NASA GISS Temperature Data

Polar Amplification



Hat tip to Suzanne

Hat tip to Cate

Hat tip to Colorado Bob

From Pole to Pole, Global Sea Ice Values are Plummeting

During the record hot year of 2016, both Arctic and Antarctic sea ice extents took a huge hit.

Extreme warmth in the Arctic helped to produce leading losses there. Values that began during January at 1 million square kilometers below average have steadily declined as the months progressed to near 2 million square kilometers below average. Meanwhile, the Antarctic — which began the year at near average sea ice extent values — saw significant losses as the region grew anomalously warm during austral spring. Today, sea ice extent values surrounding the Antarctic are now also just shy of 2 million square kilometers below average.


(Zachary Labe, one of the most well-recognized up and coming U.S. climate scientists, has produced this graph based on NSIDC recorded global, Arctic, and Antarctic sea ice values. As you can see, global sea ice extent during the hottest year on record has steadily plummeted to near 4 million square kilometers below average as the months progressed. Image source: Zack Labe’s Sea Ice Figures. Data source: NSIDC. You can also follow Zack’s informative twitter feed here.)

In total, global sea ice coverage is now about 3,865,000 square kilometers below average.

If you think that number sounds really big, it’s because it is. It represents a region of lost ice nearly 40 percent the size of the land and water area of the entire United States including Alaska and Hawaii. To visualize it another way, imagine all of the land area of Alaska, California, Texas, Montana, Arizona and New Mexico combined and you begin to get the gist.

Sea Ice Coverage — An Important, But Complex Climate Indicator

Many climate specialists have viewed sea ice as a kind of climate change canary in the coal mine. Sea ice sits upon the warming oceans and beneath a warming atmosphere. And these oceans are now taking up the majority of the heat being trapped in the atmosphere by fossil fuel emissions. Warming ocean surfaces have a higher specific heat value than the air and this greater overall energy capacity in warming regions generates a substantial blow to ice coverage even if the initial water surface temperature swing is only moderate.

Once sea ice is lost for a significant period, a kind of feedback loop comes into play where dark ocean surfaces trap more of the sun’s rays during polar summer than once-white ice coverage — which previously reflected radiation back toward space. This newly absorbed heat is then re-radiated back into the local atmosphere during polar fall and winter — creating an inertial barrier to ice reformation and ultimately generating a big jump in seasonal ocean and atmospheric surface temperatures.


(Highly pronounced ocean surface warming coupled with warm air invasions appears to be generating the extreme losses to sea ice now seen in the Arctic. The Barents Sea, shown above, has seen particularly extreme warming. Note the 11 C above average hot spot near the sea ice edge zone. In the Antarctic, the causes of losses remain uncertain. However, atmospheric warming and shifts in the circumpolar winds appear to be producing this effect even as slightly cooler than average surface waters remain in place — possibly due to storm related Southern Ocean upwelling and increasing fresh water outflows from Antarctic glaciers. Image source: Earth Nullschool.)

This dynamic is particularly pronounced in the Arctic where a thawing ocean surrounded by warming continents tends to readily collect heat even as atmospheric energy transfers from the south, in the form of warm wind events, have grown more pronounced. An effect related to the climate change influence known as Northern Hemisphere Polar Amplification.

In the Antarctic, the stormy Southern Ocean generates up-welling. This dynamic tends to cool the ocean surface even as it transfers heat into the deeper ocean. And increasing stormy conditions surrounding Antarctica related to climate change can intensify this effect. In addition, warm bottom waters melting sea-fronting glaciers in Antarctica produce a lens of fresh water which cools the surface and also traps heat below. So the signal coming from Antarctica with regards to sea ice has tended to be more mixed — with atmospheric warming and changes in wind patterns generating more variable sea ice impacts relative to the Arctic. So this year’s sea ice losses there are more difficult to directly link to climate change even though climate change related influences on the physical system in the Antarctic and among its surrounding waters are becoming more and more apparent.

Zack Labe notes that:

The Arctic sea ice anomaly, however, fits with the ongoing Arctic amplification trend of thinning sea ice and loss of old ice. Additionally, it has been well noted in previous literature (i.e., ) concerning the increasing fall temperatures in the Arctic and possible causes.

Major Volume Losses From 2015 to 2016

Despite big losses to sea ice surrounding the Antarctic this fall, it is the Arctic where the damage and risk of further loss is most pronounced. Particularly, reductions to thicker, multi-year ice in the Arctic during 2015 to 2016 have been exceptionally severe:

image image

In the above images, we see a comparison between late November sea ice coverage and thickness as provided by the U.S. Navy ARCc model. The left frame represents late November of 2015 and the right frame represents projected values for November 20, 2016. Note the greatly reduced coverage in the 2016 image. But even more noteworthy is the substantial loss of thicker ice in the Arctic Ocean north of the Canadian Archipelago and Greenland.

These two images tell a tale of a great loss of sea ice volume. One that the sea ice monitor PIOMAS confirms. According to PIOMAS, ice volume values during October were tracking near lowest levels ever recorded. And continued heat into November generates a concern that a period of new record low volume levels may be on the way.

But it’s not just the record low values that should be a concern. It’s the location of the remaining thick ice that’s a worry as well. For a substantial portion of the remaining thick ice is situated near the Fram Strait. Wind and ocean currents tend to push ice out of the Arctic Ocean and through the Fram. Ice tends to then be funneled down along the coast of Greenland and on into the North Atlantic where it melts. So the fact that a big chunk of the already greatly reduced remaining thick ice now sits on the edge of the sea ice version of Niagra Falls is not a good sign.

La Nina Years Tend to Push More Heat Toward the Poles

It is notoriously difficult to accurately forecast sea ice melt and refreeze trends in the various seasonal measures for any given individual year. And even many of the top sea ice experts have had a devil of a time forecasting the behavior of sea ice during recent years. However, one thing remains quite clear — the long term trend for sea ice in the Arctic is one of rapid decline.


(Arctic sea ice ‘Death Spiral’ by Andy Lee Robinson. Image source: Haveland.)

We are now entering a situation where one very warm winter followed by one warmer than normal summer could push Arctic sea ice values to near the zero mark. A situation that could effectively set off a blue ocean event in the near future. A number of prominent sea ice experts have predicted that it’s likely that such a state will be achieved rather soon — by the early 2030s under current trends. Others point toward nearer-term loss potentials. But there is practically no-one now saying, as was often stated during the early 2010s, that a blue ocean event could hold off until the early 2050s.

All that said, the trajectory going into 2017 for the Arctic at present doesn’t look very good. Both sea ice extent and volume are now at or well below the previous low marks for this time of year. Remaining thick ice positioned near the Fram Strait generates a physical disadvantage to the ice in general. In addition, NOAA has announced that La Nina conditions are now present in the Equatorial Pacific. And La Nina events tend to push more ocean and atmospheric heat toward the poles — particularly toward the Arctic.


Note: This article is written as a follow-on to the previous blog post — For The Arctic Ocean Above 80 North, It’s Still Summer in November — and they should be read together for context.

Disclaimer: I asked PhD student Zachary Labe to make a general comment on sea ice trends, to which he generously provided his particular take on the Arctic. I have also made my own best-shot science and observation-based analysis of the situation given current trends. Because of the fact that the present situation is new and evolving, some of my statements may well pass outside the bounds of currently accepted science. The fact that Labe commented in this post does not, in this case, mean that he agrees fully or in part with my particular initial rough analysis of the subject.

Zack Labe’s Sea Ice Figures


Permafrost and Arctic Sea Ice — Climate Canaries in the Coal Mine

Increasing Fall-Winter Energy Loss From the Arctic Ocean and its Role in Arctic Temperature Amplification

Earth Nullschool

Arctic Sea Ice Graphs


U.S. Navy ARCc Model Sea Ice Thickness



Hat tip to Andy Lee Robinson

Hat tip to Cate

For The Arctic Ocean Above 80 North, It’s Still Summer in November

It’s going to be the hottest year on record — by a long shot. Just ask Gavin Schmidt at a NASA that the climate change denying Trump Administration has now imperiled. But in one region — the Arctic — the rate of heat accumulation has been outrageously extreme. And it is there that this new record warmth could inflict some of the worst damage to an increasingly fragile Earth System.

Summer Heat During Fall Above 80 North

For in the Arctic Ocean above the 80 degree north latitude line which encircles the crest of our world, temperatures today are around 17 degrees Celsius above average. These are the warmest temperatures for this region ever recorded. And they include numerous locations in which temperatures spike to well above 20 C (36 F) warmer than average.


(Temperatures above the 80 degree north latitude line during mid November are about equal to what you would typically expect for late summer. This record warmth in the Arctic is notably severe and could produce serious near term climate and weather impacts. Image source: DMI.)

Taken in total, this region — one that includes the North Pole — is currently experiencing temperatures that it would typically see from September 15 through 21. In other words, it’s about as warm now, on November 14th, in the zone surrounding the North Pole as it typically is during the last week of summer.

It wouldn’t be quite so bad if temperatures had simply rocketed to new highs on this particular day as part of a wild temperature swing. Unfortunately, readings instead have remained consistently high throughout autumn. They have levitated off the baseline 1958-2002 average range for the better part of 80 days. And as temperatures maintained near late summer or early fall averages, the departure from normal (represented by the green line in the graph above) has continued to intensify throughout November. Such long-term maintenance of high temperatures risks producing some severe lasting impacts on both the Arctic and the global environment.

The North Pole’s Big Red Hole

The temperature range we see now is nothing less than astonishing and, to this particular observer, terrifying. A huge hole has been blown in the heart of what should be the building cold of winter. And if it doesn’t reform soon, it will have some serious knock-on climate effects to include worsening atmospheric circulation changes, related increasingly extreme weather, impacts to growing seasons, impacts to sea ice, impacts to Greenland ice, and impacts to life in the Arctic and beyond.


(Today, large swaths of the Arctic Ocean are expected to see temperatures hit 20 C [36 F] + warmer than normal. These temperatures are so high that recently ice-covered sections will, over the next five days, experience temperatures between -2 C and 0 C — or warm enough to produce temporary melt. Such a condition has never been witnessed to the extent that it is now so late in the year. A clear sign that global warming is starting to bite deeper than we had hoped. Image source: Climate Reanalyzer. Note — the map shows temperature departures above [red shift] and below [blue shift] the, already warmer than normal, 1979-2000 baseline average.)

This record fall warmth appears to be part of an ever-more-pervasive ‘death of winter’ type scenario related to human-caused global warming. And unless temperatures in the Arctic revert back toward base-line pretty soon, we are at increasing risk of hitting some state-change tipping points. In particular, these center around a nearer term loss of Arctic Ocean ice than expected. An event that could happen this year if we experience an anomalously warm winter followed by a similarly warm summer — but one that many experts expect to hold off until the 2030s. An alteration that, longer term, under the continued fossil fuel burning presently promoted by the Trump Administration, basically removes winter as a season pretty much altogether (at least as we know it).

I sincerely hope that we see a return to baseline temperature conditions in the Arctic soon. But as the days roll by, this seems less and less likely. Warm winds keep flowing in both from the Barents and the Bering. And the centers of coldest Northern Hemisphere regions are well displaced toward Siberia and Greenland. If this situation continues, implications for summer sea ice during 2017 could be pretty rough (more on this in the follow-on post). And it’s at the point where we hit ice-free summer states in the Arctic Ocean that some very radical regional, hemispheric, and global changes (which produce even worse effects than some of the bad outcomes we’ve already seen) will be well underway.


Climate of Gavin

Cires1 80 North Temperature Anomaly


Jennifer Francis on Jet Stream Changes due to Sea Ice Loss

Climate Reanalyzer

The Trump Administration’s Anti-Climate, Pro-Fossil Fuels Agenda

From the Bering to Maine Hot Oceans are Killing the Puffin


What’s Swimming in the Open Water Near the North Pole These Days?

Globally, it’s been a record-hot year. But nowhere has seen so much anomalous warmth during 2016 as the Arctic. As melt season draws to a close, some dramatic effects are now becoming visible in the NASA satellite shots. Large regions near the North Pole are losing their white covering of sea ice and showing the telltale blue-black of open water:


(Large areas of open water are visible near the North Pole in this LANCE MODIS satellite shot.)

The above image, provided by NASA, shows the Northern Hemisphere polar region on September 5, 2016. To get some sense of the size of this region of low-concentration sea ice, the bottom edge of this capture represents approximately 300 miles. For a point of reference, the North Pole can be seen where the lines of the satellite image frames converge in the lower left-hand side of the capture.

All throughout this satellite shot, we see large expanses of open water. The smaller openings are five to ten miles wide, with very large openings ranging as much as 50 miles long appearing as well. Cloud cover is present throughout the image and blocks some visibility to open regions on the Siberian side of the Pole (upper section of the image) and over the Pole itself (lower left).


(Arctic sea ice area coming uncomfortably close to 2012 record lows in this NORSEX SSM model summary.)

Loss of ice in this region of the central Arctic is similar to and perhaps more extensive than that seen during 2010 and 2013. In 2013, strong storms combined with weakened ice states resulting in severe melt near the North Pole, with ice becoming more dispersed throughout the Arctic. This year, both storms and heat have hit the ice hard. Now, ice edge extent is far lower than in 2013 even as low-concentration ice floes and open water are visible near the Pole. As such, the overall health of sea ice is dramatically worse during 2016.

Unfortunately, sea ice buoy observations near the North Pole have seen cuts to research funding and no camera buoys are operating near the Pole. Otherwise, we’d probably be treated to images like this:


(North Pole Camera 2 goes for a swim during the summer of 2013 as a period of extensive near-polar melt set in. Most indicators show that ice conditions at the North Pole this summer were as bad or worse. Image source: North Pole Environmental Observatory.)

The large, open sections of water near the Pole appeared as sea-ice extent and area in many measures fell to second lowest on record for this time of year. Some measures (shown in the middle image above) have come uncomfortably close to the 2012 record low line.

Overall, 2016 is a very bad year for sea ice. And the weird prospect of polar bears (or anything else) being forced to swim at the North Pole is not at all something to brighten one’s day.





North Pole Environmental Observatory


Warm Arctic Storm Tearing Sea Ice to Shreds amidst Big 2016 Heat Spike

Abnormal. Unprecedented. Remarkable. Extreme. These words are supposed to describe unusual events, but in the weird world we’re now entering, the extreme has become commonplace. Some people call this emerging state of affairs ‘the new normal.’ A more direct descriptor is ‘spiraling into climate chaos.’

Chaos is an apt word to describe the scene in the Arctic this week as one of the most powerful summer cyclones ever to form rages in a place that has just experienced a record-shattering influx of atmospheric heat. This storm is hammering the sea ice, pushing it nearly to the second-lowest extent on record. But worse may be still to come as a very weak and diffuse ice pack is predicted to face off against a storm that’s expected to significantly reintensify on both Friday and Tuesday.

Record Arctic Heat

The Arctic. It’s a place we typically associate with frozen things. Due to the billions and billions of tons of heat-trapping gasses dumped into the atmosphere each year by burning fossil fuels, now it’s a place that’s thawing at a disturbingly fast pace. The region could best be described in these few words — record abnormal warmth in 2016.

(This graphic from University of California, Irvine Ph.D. candidate Zack Labe is a visual measure of a stunning jump in Arctic temperatures for 2016. So much heat in the Arctic has profound implications, not just for the Arctic ice and environment, but for the rest of the world as well. In other words — warming that happens in the Arctic doesn’t stay in the Arctic.)

So far, 2016 has seen temperatures in the Arctic that are well above the warmest previous year ever recorded. This big spike in a decades-long trend includes, for this single year, about 35 percent of all the temperature rise experienced there since the late 1940s. It’s like taking more than a third of all the warming in the Arctic seen over the past 68 years and cramming it into just one year. It’s insane.

The Warm Storm Generator

Heat in the Arctic doesn’t just emerge there. It comes, largely, in the form of energy transfer.

Heat-trapping gasses warm the atmosphere in an uneven fashion. The way these gasses absorb solar radiation results in more heat trapping during the dark of night. And the Arctic experiences a thing called polar night which lasts for months.

As a result, the Arctic already gets a slightly more powerful nudge from global warming than the rest of the world. As the cold begins to fail in the Arctic, a number of amplifying feedbacks come into play that further multiply the warmth.


(A dance of cyclones. GFS model rendering by Earth Nullschool shows a strong influx of heat from the Eurasian Continent and the Barents and Kara Seas feeding into a bombing low-pressure system on Monday at 12:00 UTC. The low is predicted to meet up with the currently raging Arctic cyclone by late Monday or early Tuesday. Combined, these lows are expected to drop into the 960s to 970s mb level, extending the scope of the strong event and possibly resulting in the most powerful cyclone ever to have formed this time of year in the Arctic Basin. Image source: Earth Nullschool.)

As the Arctic heats up, its natural barriers to heat coming up from the ocean or from the south begin to fail. The more evenly-warmed surface of the ocean transfers some of its heat north and pumps this added energy into the Arctic air. The lower sea-ice levels cause this water to warm even more, its dark surface trapping more of the summer sun’s warmth than the white ice ever could.

The polar Jet Stream begins to weaken as the relative difference between Arctic and lower-latitude temperatures drops. In the Jet Stream’s meanders, strong warm winds blow in from the ever-hotter continents and ocean surfaces of the mid and upper latitudes.

It’s a simple physical property of the atmosphere that burgeoning heat often seeks out the cold. It rises as it flows toward the Pole, and when it collides with these chilly pockets, the result can be an atmospheric maelstrom.

The Great Arctic Cyclone of 2016 Smashes Sea Ice

Such was the case earlier this week as a warm tongue of air flowed up into area of the Laptev Sea from Siberia. This warm flow tapped moisture from the Kara and Barents Seas and fed into a developing storm system (see article here). Pressures at the storm’s center rapidly fell and by late Monday, August 15th, had dropped to 966.5 millibars. The result was one of the strongest cyclones ever to form over the Arctic Ocean during August.

(We’ve probably never seen the ice so thin near the Pole during August. Zack Labe‘s rendering of SSMIS sea ice concentration measures from late July to August 17 shows a stunning degree of thinning and loss. Note the large, low-concentration holes opening up near the Pole in the final few frames.)

The storm rampaged through the Arctic. Pulling in strong winds and heavy surf, it smashed the sea ice, driving daily extent losses to 110,000 square kilometers on Tuesday and greatly thinning a vulnerable tongue of ice running out toward the Chukchi Sea. Meanwhile, near the Pole, great gaps 50 to 100 miles wide have opened up, revealing water that is 80 percent clear of ice.

The storm subsequently weakened, with pressures rising today into the 985 mb range. But over the next few days, the system is predicted to reintensify — first on Friday to around 971 to 978 mb as it approaches the Canadian Arctic Archipelago, and then again on Tuesday to around 963 to 976 mb when it loops back toward the Laptev.

Central Arctic Basin Sea Ice lowest Ever Recorded

(AMSR2 and SSMIS sensor reanalysis shows that 2016 Arctic sea ice area [black line] in the Central Arctic Basin — a key region for indicating sea ice health — hit new record lows over recent days. A signal pointing to risk that a challenge to 2012 records may emerge in some measures over the coming days as the 2016 cyclone is expected to re-intensify. Image source: The Great White Con.)

In each case, the storm is predicted to draw on heat, moisture, and low-pressure cells riding up from the south, with the first stream of energy feeding into this low from over the Beaufort and Bering Seas and northeastern Siberia, and the second running up from the Barents and Kara Seas, western Siberia and northeastern Europe (you can see the succession of lows and moisture here in this model run by Climate Reanalyzer).

If this happens, we’ll be coming out of a situation where a warmth-fueled Arctic cyclone will have bombed to record or near-record strength on two to three separate occasions, all the while applying its buzz-saw winds, waves and Coriolis forces to the sea ice — a full-blown nightmare Arctic sea-ice melt scenario in the midst of a record-hot year.

UPDATE (8/19):

A recent report by expert ice observer Neven over at the Arctic Sea Ice Blog (which is very informative) finds that storm impacts thus far have been significant, if not yet quite as extraordinary as the Great Arctic Cyclone of 2012. Overall sea ice area measures (not just those in the Central Arctic Basin indicated above) according to Wipneus have dropped into second lowest on record just below the 2007 line. Extent, meanwhile, in the JAXA measure after falling an average of 90,000 square kilometers per day, is today at third lowest on record — trailing 2007 by just 30,000 kilometers. Tracking for end of year now appears most likely to fall into a range near 2007 in many measures. But the current storm appears to have provided a potential for a stronger downward trend for the ice in which some measures (particularly various regional measures) have the potential to approach or exceed 2012.

Arctic Sea ice Chukchi

(Peering through the clouds on August 19 in this LANCE MODIS satellite shot we find that sea ice in the Chukchi appears to have been greatly reduced and thinned by the current cyclone. Loss and thinning of the ice bridge with the main pack means that this ice may have also suffered separation. Toward the Laptev, sea ice in the pack between that Arctic sea and the Pole is extraordinarily mobile and becoming more diffuse. These observed conditions still present a potential for large daily losses and further reductions in total sea ice coverage. So current tracking comes with a ‘risk of downside’ caveat. Image source: LANCE MODIS.)

One final point is that we are entering La Nina and such events tend to increase heat transport toward the Arctic and particularly into the Arctic Ocean. For this reason El Nino year +1 or El Nino year +2  can tend to present higher risk for greater sea ice melt totals. As such, and dramatic as the heat and melt in the Arctic has been for this year, it’s worth noting that what we may be watching is a set-up for 2017 or 2018 to see worsening conditions. La Nina is currently expected to be weak, so the related North Atlantic influence (NAO) that has been so devastating to the ice during the recent record warm years may be somewhat muted. We’ll have to see.

2016, however, is not entirely out of the woods. Thin ice in the Chukchi and an increasingly thin and diffuse pack extending from the Pole toward the Laptev remain very vulnerable to late season flash melt and compaction. Model runs today indicate the current set of storms tending to restrengthen on one or two occasions back to the 970s or 960s before finally ebbing on Wednesday. After this, some models show a tendency to flip toward a strong high pressure influence which would again wrench the ice (this time toward compaction). So the troubling 2016 Arctic melt drama is still far from over.


Powerful Arctic Cyclone to Blow Hole in Thinning Sea Ice

Arctic Sea Ice Graphs

Arctic Cyclone Update 1

Arctic Cyclone Update 2

NASA: Implications of a Warming Arctic

Zack Labe

Tropical Tidbits

JAXA Sea Ice

Earth Nullschool

The Great White Con

Hat tip to DT Lange

Hat tip to Colorado Bob

Hat tip to Bill h

Siberian Heatwave Wrecks Sea Ice as Greenland High Settles In

We’ve never seen Arctic sea ice extents that are as low as they are now in early June. And with Arctic heatwaves, warm winds, warm storms, and a Greenland High all settling in, something had better change soon or otherwise the ice cap over the northern Polar Ocean is basically screwed.


On the shores of the Arctic Ocean’s East Siberian Sea (ESS), near the town of Logashinko, temperatures today are expected to rise to near 80 degrees Fahrenheit. Readings that are about 40 to 50 degrees (F) above normal for this near-polar region during this time of year.


(Welcome to increasingly ludicrous climates. Temperatures near 80 F at Logashinko, Russia are at least 40 degrees F above average for this time of year. A place well north of the Arctic Circle, but whose temperatures are predicted today to match those of St. Martin Island in the tropics. Image source: Earth Nullschool.)

We would have never expected temperatures to have risen so high near typically frozen Logashinko during early June sans the heating effect of atmospheric CO2 levels that have this year peaked near 407.5 parts per million. The highest levels seen on Earth in about 15 million years. These scorching polar temperatures were driven north by a powerful high amplitude ridge in the Jet Stream that has dominated Eastern Russia for much of 2016 Spring. This expansive ridge enabled extreme wildfires popping up all over the region even as it today drives 80 degree weather all the way to Arctic Ocean shores — enforcing a regime of rapid sea ice melt over the East Siberian Sea.

ESS, Laptev Get Ripped Up

As the warm winds drive northward across ice-clogged Arctic Ocean waters, temperatures rapidly fall into 35 to 41 degree (F) ranges. And though that may sound cool to the casual observer, for the East Siberian Sea zone during early June, that’s scorching hot — topping out at more than 10 degrees above average for some areas. A pretty extreme variation for late Spring when temperatures over the Arctic Ocean only typically depart from average by about 3 or 4 degrees at most.

East Siberian Sea Melting

(The Laptev and East Siberian Sea Ice is getting ripped up by extreme Arctic warmth. The blue tint to ice in the above image indicates melt ponds, while dark blue indicates open water. Zooming in closer reveals the brown flush of warm waters issuing from heated Siberian rivers. Image source: LANCE MODIS.)

All across this Arctic Ocean region, melt ponds and widening polynyas now abound in the ridiculously warm airs. In the satellite shot above, the tell-tale bluish tint of the ice reveals a plethora of these ponds expanding northward through the ESS and on toward the pole. A flush of hot water running into the Arctic Ocean from East Siberia’s rivers is melting the near shore ice. And a giant 80 mile wide gap of open water has now been torn into the ice of the Laptev Sea.

Record Extent Lows Continue to Worsen

The sudden Arctic heatwave and rapid related melt involvement of the ESS and Laptev is just the most recent melt spike in a polar ocean that sees ice extent levels hitting new record lows with each passing day. As of June 2nd, the expanse of Arctic Sea ice only measured 10.37 million square kilometers. This is about 430,000 square kilometers below the previous daily record low set just last year and fully ten days ahead of the record sea ice melt year of 2012.

Arctic sea ice extent new record lows

(Arctic sea ice extent record lows continue for this time of year and threaten to plunge deeply below the 2012 line in coming days. Image source: JAXA.)

A coverage of sea ice that is now 42 days and 2.1 million square kilometers of sea ice loss ahead of an average melt year during the 1980s.

Here Comes the Greenland High

Extreme heat building into the Siberian side of the Arctic and record low sea ice extent measures are today being joined by yet another disturbing Arctic feature. For as of yesterday, a strong ridge of high pressure began to form over Greenland, the Canadian Archipelago and Iceland.

Greenland highs tend to increase temperatures over the enormous glaciers of that frozen island even as the clockwise circulation pattern of an anticyclone tends to shove sea ice out into the Barents and North Atlantic. The dominance of a Greenland High during both 2012 and 2007 is thought to have heavily influenced record end season sea ice melts during those years as well as the extreme Greenland surface melt spike during 2012.


(A high pressure ridge emerging over Greenland, Iceland and the Canadian Archipelago today is expected to strengthen this week — generating a high pressure gradient between warm storms developing over the Arctic Ocean and winds that threaten to increase the rate of ice transport out of the High Arctic and into regions of warmer water. Image source: Earth Nullschool.)

This week’s predicted ridge formation is not expected to bring with it a severe surface melt of Greenland. However, the clockwise winds driving sea ice transport may serve as yet one more heavy blow to the already greatly weakened ocean ice. Pressures later this week are expected to rise to 1040 mb over Greenland. And strong winds running between powerful warm storms expected to form in the Kara and Central Arctic are predicted to rise to near gale force north of Greenland — generating a risk of a very vigorous ice loss from the near polar zone as floes are driven into warm Barents and North Atlantic waters.

In context, the combined severe record sea ice lows and emerging weather conditions represent a seriously bad state for Arctic sea ice. One with a high risk of continued further extreme losses and new daily record lows for at least the next seven days.


Earth Nullschool



Arctic Sea Ice Graphs

The Arctic Ice Blog

Hat tip to Greg

Hat tip to Cate

Hat tip to DT Lange

Arctic Sea Ice is Falling off a Cliff and it May Not Survive The Summer

Near zero sea ice by the end of melt season. The dreaded Blue Ocean Event. Something that appears more and more likely to happen during 2016 with each passing day.

These are the kinds of climate-wrecking phase changes in the Arctic people have been worrying about since sea ice extent, area, and volume achieved gut-wrenching plunges during 2007 and 2012. Plunges that were far faster than sea ice melt rates predicted by model runs and by the then scientific consensus on how the Arctic Ocean ice would respond to human-forced warming this Century. For back during the first decade of the the 21st Century the mainstream scientific view was that Arctic sea ice would be about in the range that it is today by around 2070 or 2080. And that we wouldn’t be contemplating the possibility of zero or near zero sea ice until the end of this Century.

But the amazing ability of an unconscionable fossil fuel emission to rapidly transform our world for the worst appears now to outweigh that cautious science. For during 2016, the Arctic is experiencing a record warm year like never before. Average temperatures over the region have been hitting unprecedented ranges. Temperatures that — when one who understands the sensitive nature of the Arctic looks at them — inspires feelings of dislocation and disbelief. For our Arctic sea ice coverage has been consistently in record low ranges throughout Winter, it has been following a steepening curve of loss since April, and it now appears to have started to fall off a cliff. Severe losses that are likely to both impact the Jet Stream and extreme weather formation in the Northern Hemisphere throughout the Spring and Summer of 2016.

Melting more than Two Weeks Faster than the Early 2000s

Since April 27th, according to a record of sea ice extent provided by JAXA, daily rates of sea ice loss have been in the range of 75,000 square kilometers for every 24 hour period. That’s 300,000 square kilometers of sea ice, or an area the size of New Mexico, lost in just four days. Only during 2015 have we ever seen such similarly rapid rates of loss for this time of year.

Sea Ice Rates of Loss Steepening

(We’ve never seen early season sea ice losses like this before. Severe sea ice losses of this variety can help to generate strong ridges and extreme heatwaves like the one we now see affecting India and Southeast Asia. Image source: JAXA.)

However, this excessive rate of loss is occurring across an Arctic region that features dramatically less ice (exceeding the 2015 mark for the same day by about 360,000 square kilometers) than any other comparable year for the same day. In essence, extent melt is now more than a week ahead of any other previous year. It is two and half weeks ahead of melt rates during the 2000s. And this year’s rate of decline is steepening.

Current melt rates, if maintained throughout summer, would wipe out practically all the ice. And, worryingly, this is a distinct possibility given the severely weakened state of the ice, the large areas of dark, open water available to absorb the sun’s rays as Summer progresses, and given the fact that Arctic heat is continuing in extreme record warm ranges. Furthermore, melt rates tend to seasonally steepen starting by mid June. So rapidly ramping rates of loss seen now, at the end of April and through to the start of May, may see further acceleration as more and more direct sunlight keeps falling on already large exposed areas of dark, heat-absorbing water.

Huge Holes in the Beaufort

All throughout the Arctic Basin, these sunlight-absorbing regions take up far more area than is typical. The Bering has melted very early. Baffin Bay is greatly withdrawn from typical years. Hudson Bay is starting to break up. The Barents and Greenland seas feature far more open water than is typical. However, there is no region showing more dramatic early season losses than the Beaufort.

Beaufort rapid melt 2016

(This Beaufort sea has never looked so bad off so early in the year. High amplitude waves in the Jet Stream continue to deliver record warmth, warm, wet winds, and record sea ice melt to this region of the Arctic. For reference, bottom of frame in this image is around 600 miles. The wispy threads you see in the image is cloud cover, the sections of solid white are snow and ice. And the blue you see is the open waters of the Arctic Ocean. Open water gap size in the widest sections is now more than 150 miles. Image source: LANCE-MODIS.)

There, ice continues to rapidly recede away from the Arctic Ocean shores of the Mackenzie Delta and the Canadian Archipelago — where a large gap has opened up in the sea ice. Now ranging from 70-150 miles in width, this area of open water consistently sees surface temperatures warm enough to melt sea ice (above 28 F or about -2 C).

This great body of open water the size of a sea in itself has now created a new early season edge zone for the ice. A place where a kind of mini-dipole can emerge between the more rapidly warming water surfaces and the cooler, reflective ice. Such a zone will tend to be a magnet for storms. And a low pressure system is expected to ride up an extreme bulge in the Jet Stream over Alaska and Canada and on into this Arctic zone over the next few days. Storms of this kind tend to hasten melt and break up of ice in the edge zones by generating waves, by pulling in warmer airs from the south, or by dropping liquid precipitation along the melting ice edge. And the fact that this kind of dynamic is setting up in the Beaufort in early May is nothing short of extraordinary.

Arctic Heat Like We’ve Never Seen Before

Further to the north, high pressure is expected to continue to dominate over the next seven days. This will generate further compaction of the already weak ice even as it allows more and more sunlight to fall over that greatly thinned white veil.

Freezing Degree Days Cross -1000 threshold

(The Arctic is now so warm that this graph is now too small to capture the excession of extreme heat in the region. Freezing degree days are now more than 1,000 less than during a typical year and the already much warmer than normal 1980 to 2000 period. Image source: CIRES.)

Temperatures for the Arctic are expected to range between 2.5 and 3.5 C above average over the next seven days. Very warm conditions that will continue to hammer freezing degree day totals that have now exceeded an unprecedented -1000 since the start of the year in the High Arctic region above the 80 degree North Latitude Line. In layman’s terms, the less freezing degree days the Arctic experiences, the closer it is to melting. And losing 1000 freezing degree days is like removing the coldest month of Winter entirely from the heat balance equation in this highest Latitude region of the Northern Hemisphere.

From just about every indicator, we find that the Arctic sea ice is being hit by heat like never before. And the disturbing precipitous early season losses we now see in combination with the excessive, extreme warmth and melt accelerating weather patterns are likely to continue to reinforce a trend of record losses. Such low sea ice measures will also tend to wrench weather patterns around the globe — providing zones for extreme heatwaves and droughts along the ridge lines and related warm wind invasions of the Arctic that will tend to develop all while generating risk of record precipitation events in the trough zones. To this point, the North American West is again setting up for just such a zonal heatwave pattern. Extreme heat building up in India and Southeast Asia also appears to be following a similar northward advance.






Climate Reanalyzer

Earth Nullschool

Arctic Sea Ice Graphs

Hat tip to DT Lange

Sarc. Hat tip to Exxon Mobile (For its failure to report scientific findings on the impacts of climate change, and for its never-ending political and media campaign aimed at preventing effective climate change mitigation policy over the past 40+ years)

Conditions Promoting Arctic Sea Ice Collapse Are Exceptionally Strong This Spring

It didn’t take long for Arctic sea ice to start to respond to a fossil-fuel based accumulation of hothouse gasses in the Earth’s atmosphere. For since the 1920s, that region of ocean ice along the northern polar zone has been in a steady, and increasingly rapid, retreat. Rachel Carson wrote about the start of the Northern Hemisphere ocean ice decline in her ground-breaking 1955 book — The Edge of the Sea.

But it wasn’t until the late 1970s that consistent satellite observations began to provide an unbroken record telling the tale of Arctic sea ice decline. The National Snow and Ice Data Center, The Polar Science Center (PIOMAS), Japan’s JAXA, The Danish Meteorological Institute, and others have since that time provided a loyal recording of the stark impact human-forced warming has had on this sensitive and critical region.

(Severe sea ice volume losses since 1979 illustrated in the above video by Andy Lee Robinson.)

Perhaps the most poignant and direct telling of this tale has been provided in the form of Andy Lee Robinson’s tragic and resonant re-rendering of sea ice volume declines as measured by PIOMAS. Others, like Neven over at the Arctic Sea Ice Blog, have heroically and often thanklessly provided the essential week-to-week analysis of this tragic decline. Rising to the task of a necessary telling of a key chapter in the human tale that our mainstream media sources have all-too-often neglected. Before we go on to today’s update on an Arctic Ocean ice cap that is now in a critically weak condition, I want to add one last mention — these scientists, analysts, experts, and creative and artistically inclined laymen have done the right thing. They were the modern-day prophets providing the critical warning that has been oft-ignored.

A Tale of Devastating Losses

It’s a warning that has been written in the record of the ice itself. A decline that since 1979 has followed a steepening descent curve. An overall downward trend punctuated by the abrupt and severe loss years of 2007 and 2012. A trend that has, nonetheless, featured a few weak challenges in the form of pseudo-recovery years like 2008, 2013, and 2014. A precipitous loss that, all too soon, will likely terminate with abrupt finality in temporally-expanding blue ocean events. Periods when little or no sea ice is observed on the surface of oceans and seas within the Arctic.

JAXA sea ice

(After the warmest Winter and early Spring period on record, Arctic sea ice extent, area and volume are now at or near new record lows. With abnormal heat persisting and with the ice showing an extraordinary lack of resiliency, there appears to be a heightened risk that Arctic sea ice will hit new record all-time lows by September and October of 2016. Image source: JAXA.)

Why should we talk about blue ocean events now? Well, we have only to look at the sea ice record to find that substantial losses have occurred during single years. Years when Arctic heat hit new peaks — lining up with severe adverse weather conditions to take a terrible toll on the ice. Years like 2007 when nearly 2 million square kilometers of ice was lost over the previous year and 2012 which featured about 800,000 square kilometers of extent lost below the 2007 low mark. And if a blue ocean event does happen, it will be during one of these severe loss years.

Extremely Frail Sea Ice During the Spring of 2016

2016 and 2017 could be years when such precipitous declines occur. Heat from an extraordinarily powerful El Nino already skipped over the weakening atmospheric wall of the Jet Stream to invade the High Arctic during Winter of this year. As a result, Winter and Springtime Arctic temperatures are currently at their warmest levels ever recorded.

All this extra heat is doing a number on the ice. Sea ice extent, volume and area, which had experienced a false recovery during the years of 2013 and 2014, have again retreated to seasonally record low levels. In particular, the new near record low seasonal volume measure is disturbing. For while area and extent measure the expanse of surface ice as visible from above, volume measures the ice in three dimensions — giving a better idea of overall resiliency or lack thereof. It’s worth noting that the PIOMAS volume measure is based on a model of assimilated observational data. And, as with any model, there are a few assumptions built in. But overall, PIOMAS has tended to provide data that has matched with other observational findings.

Broken Beaufort

(Extreme fracturing of Beaufort sea ice over recent days has come after a record warm Arctic Spring and Winter and during a period when a powerful high pressure system has been breaking and compacting the ice. Image source: LANCE-MODIS.)

Sea ice frailty seen in the measures is also verified by current satellite observations of the ice surface. This frailty is particularly visible in the region of the Beaufort Sea north of Alaska and Canada. There, extensive fracturing of the ice is clearly visible in yesterday’s MODIS satellite shot. Here we find huge regions of thin ice and open water as the torquing influence of a powerful high pressure system has turned the greatly weakened Beaufort ice into a sea of ice cubes.

During recent years in the post 2012 timeframe, Beaufort ice has shown a considerable lack of resiliency to fracturing. This is particularly disturbing as, historically, the Beaufort Sea has tended to house the thickest, toughest ice in the Arctic. If such a great former bastion for the ice can now be torn to ribbons by the slightest fluxes of wind and weather, then the sea ice is, indeed, in a rather wretched state. And last year, just this kind of early fracturing and warm up in the Beaufort greatly contributed to an overall return to the trend of an Arctic sea ice death spiral in 2015.

Neven notes in a recent blog at his Arctic sea ice portal:

Last year’s April cracking event caused a lot of fragmented multi-year ice to be transported all the way up to the Chukchi Sea (see here), leaving a vulnerable looking barrier on the Pacific side of the Arctic. When this was followed by an early heat wave in May (see here), the ice in the Beaufort and Chukchi Seas received a beating it never really recovered from during the rest of the melting season. This was also because continental snow had melted out really quickly, making it possible for warm winds to blow in from the land.

Heating From Both Water and Land

Compared to last year, this year looks quite a bit worse. A wide-ranging Beaufort break-up is happening on the back of last year’s losses and is concurrent with new record and near record low sea ice extent, area and volume values and is happening during a period in which Arctic heat has hit new all-time highs. The result is a risk of compounding melt factors hitting the greatly weakened ice all at the same time.

Locally, the kind of widespread fracturing we now observe can result in a loss of protective reflectivity for the sea ice. As the Springtime sun rises and more of its direct rays fall upon the ice, darker thin ice patches and areas of open water will absorb more of the solar heat. That extra heat will then go to melting the islands of thicker ice that remain.

This situation can generate a compounding effect of ice losses if weather conditions and atmospheric temperatures line up. In addition, loss of the thicker sea ice cap during break-up can result in the ventilating of heat from the warmer waters beneath the ice. In fact, it is the heating of waters beneath the sea ice by means of current transport of warming ocean waters from around the world and into the Arctic that is one of the chief drivers of Arctic Ocean ice losses as the globe has been forced to warm by human fossil fuel emissions. So not only does an ice crack up in the Beaufort reduce the ice’s resiliency to the sun, it also tears the lid off the deeper ocean warming rising up from below.

Warmer Arctic Ocean Cooler Land

(Lower albedo due to ice fracturing results in more of the sun’s rays being absorbed into the ocean surface. A warmer Arctic Ocean surface then radiates more heat into the surrounding environment. Such conditions can result in periods when temperatures over the, previously colder and solidly frozen, Arctic Ocean are far warmer than even over land masses on the verge of tipping into a springtime thaw. Image source: Earth Nullschool.)

During Arctic Spring, when land surfaces are now retaining snow cover even as the sea ice breaks up, the effect of lower albedo and ocean heat ventilation can be found in the form of warmer temperatures over thin ice, broken ice, and in open water regions when compared to nearby land masses. Such a condition of newly added heat over ocean zones can have substantial impacts come Summer if melt-favorable weather patterns continue to hold sway. The result is a kind of melt synergy developing between the land, the waters, and the sun. Early on, during Spring, the warmer ocean zone weakens ice and provides warm air pools that aid in the initiation of snow melt over adjacent land. Then, as land warming ramps up, the warm winds coming from regions of early snow withdrawal provide further pressure to the already greatly weakened ice.

A Big Burly High as the Final Ingredient

Weather patterns that favor melt during Spring and Summer include powerful high pressure systems dominating large regions of the Arctic. And for much of the past week, an extremely intense high in the range of 1040 to 1045 mb has stooped over the Beaufort, torqued the ice, and developed the kind of strong clockwise wind flow that has tended to result in fracturing, ice compaction, and the opening of darker ice and open water areas (please read Neven’s fantastic recent blog on this observation here).

This kind of weather system is the last ingredient necessary to trigger an early, rapid melt for the side of the Arctic where the last of the thick, old ice now remains. And it appears that, for at least two weeks, such conditions will hold strong sway over the Beaufort.

So overall, more and more conditions are lining up to deliver a ramping up of melt pressure on the Arctic sea ice. Record atmospheric heat, early break-up, record low or near record low area, extent, and volume, and a powerful high pressure system over the Beaufort do not at all bode well. In fact, this looks like a near perfect early season set-up for a record melt in 2016 should this clearly ominous trend continue.


Beaufort Under Early Pressure

The National Snow and Ice Data Center

The Polar Science Center (PIOMAS)

The Danish Meteorological Institute


Andy Lee Robinson

The Edge of the Sea



Earth Nullschool

Northern Polar Melt Re-Asserts With A Vengeance — Arctic Sea Ice Volume Closed on New Record Lows During February

Arctic sea ice volume hit near new record lows during February. That’s kinda a big deal. What it means is that whatever sea ice resiliency was recovered during 2013 and 2014 are now mostly gone. That record all-time lows for sea ice set in September of 2012 are likely to see a serious new challenge during 2016 and 2017.


A flood of severe Arctic heat — flowing up through the Barents and Greenland seas in the East and over Alaska and the Bering Sea in the West — has been hammering the Arctic Sea Ice all Winter long. During February of 2016, new record lows in sea ice extent and area were breached. Meanwhile, sea ice volume — as measured by PIOMAS — also greatly declined to hover just above previous record lows for this time of year set in 2011.

PIOMAS Daily Volume

(Arctic sea ice volume, as measured by the Polar Science Center, plunged back to near record low territory during February. Many consider sea ice volume to be the key measure determining sea ice health. So these new drops in the volume measure are a bit spine-tingling. Image source: Wipneus.)

Looking at the above graph, provided by Wipneus, and based on model and observation data collected by the Polar Science Center, it appears that for some days during February, volume measurements even briefly descended into record low territory. As of early March, volume totals were in the range of just above 20,000 cubic kilometers — beating out 2012 as second lowest volume on measure and hovering just above 2011.

Winter Warming Grand Finale

Over the past ten days, abnormal warmth in the Arctic has faded somewhat. The lower Latitudes have heated up with the onset of spring and this has tended to strengthen the circumpolar winds. Perhaps the last bit of seasonal change that can have this effect given the alterations to atmospheric circulation produced by a human-forced warming of the globe and a particular high concentration of this added heat centering on the Arctic.

Ironically, the time-frame of late February to mid-March is when the higher Latitudes in the Northern Hemisphere tend to experience their coldest temperatures. During 2016, we did see some of this atmospheric effect take hold. As a result, temperatures in the High Arctic above the 80 degree North Latitude line have fallen from record warm readings in late February to far above average warm temperatures over recent days.

Temperature above 80 north

(Ever since Early January, Arctic temperatures have been in near record or record warm ranges. This consistent heat has resulted in the warmest Winter temperatures ever experienced for the region above the 80 North Latitude Line. Image source: CIRES/NOAA.)

Today, another very strong pulse of warmth is building up through the region of the Barents and Greenland seas. This heat pulse representing yet another warm wind event for 2016. Another very strong south to north atmospheric draw flooding in front of yet another chain of strong low pressure systems in the North Atlantic. A flow of heat drawn up from the tropics and delivered to the Arctic that will briefly drive regions near the North Pole above the -2 C melting point of sea ice even as a wide wedge of 20 degree Celsius above average temperatures invades a region stretching from Northeast Greenland to the North Pole and back to the isle of Novaya Zemlya in Russia.

Overall, the sea ice in this region is much weaker than normal. Volume is greatly thinned as both the relentless heat influxes and strong sea ice export through the Fram Strait this Winter has leeched the area of thick ice. Most sea ice measures show a loss in concentration and volume for this area. But we’ll know more as the Earth tilts back toward the sun and visible satellite coverage again takes in the entire Arctic.

Given atmospheric changes taking place with Spring — where Continental and lower Latitude warming hold greater sway over atmospheric circulation — this may be the last burst of heat we see through this zone that produces such high temperature anomalies. A grand finale for the record warm Arctic Winter of 2016.

Warm North Atlantic Winds

(Warm North Atlantic Winds are predicted to blow into the Arctic yet again on Saturday, March 12. These winds will push temperatures over a broad region of sea ice to near freezing, driving such anomalously warm temperatures all the way to the North Pole. Image source: Earth Nullschool.)

To be clear, long range model forecasts do identify far above average sea surface temperatures and above average 2 meter air temperatures for this region through Spring and on into Summer. However, the Arctic overall is not as capable of producing such high temperature anomalies during Summer as it is during Winter when the human supplied greenhouse gas overburden and the related warming of the oceans holds a much stronger sway — re-radiating an insane amount of heat throughout the long polar night.

High Arctic Temperature Anomalies Predicted to Fall-off For a Short While, Melt Potential Through Summer Looks Rather Bad

To this point, it appears the Arctic may be in for a brief respite on the 3-7 day horizon. GFS model runs indicate overall cooling for the region above the 66 North Latitude line and temperatures above 80 North may see their first period of near average temperatures since late December of 2015. This respite for the High Arctic, though, comes as temperatures in the Sea of Okhotsk, the Bering, and along Hudson Bay are expected to warm.

Arctic Sea Ice Area lowest on record

(Arctic sea ice area remains at record low levels during March of 2016. Image source: Cryosphere Today.)

It’s a mixed signal that may continue some of the very slight Arctic sea ice rejuvenation we’ve seen during March — with sea ice area still in record low territory, but with sea ice extent edging back to second lowest on record and just slightly above 2015.

To be clear, we’re at a very low launching pad for the start of melt season in 2016. Record low or near record low sea ice volumes in February and continuing record low area show that sea ice resiliency is pretty terrible at this time. Furthermore, Northern Hemisphere snow cover totals also at or near new record lows hint that warming of the land masses surrounding the Arctic may be very rapid come mid to late March and throughout April. To this point, 10 day Euro model runs show a tendency for rapid warming over the Northwest Territories, Alaska, the Bering Sea, the Sea of Okhotsk, the East Siberian Sea, and far Eastern Siberia during this period even as the thaw line pretty much everywhere jumps swiftly northward.

A fading record El Nino in the Eastern Pacific will also tend to result in ample excess Equatorial heat heading northward. As a result, the overall risk of strong sea ice melt through the Summer of 2016 remains very high.


The Polar Science Center


The Arctic Sea Ice Blog

Arctic Sea Ice Graphs


Climate Reanalyzer

Arctic Explorer

Earth Nullschool

Cryosphere Today

Euro Model Runs


Sea Ice Death Spiral Continues — Start of 2016 Sees Arctic Ocean Ice Hitting New Record Lows

In January, Arctic sea ice extent hit a new record average low for the month. Meanwhile, during the first days of February, both Arctic sea ice extent and area hit new daily record lows even as global sea ice area also entered the second lowest range ever recorded. And so it seems that the sea ice death spiral of a record warm world continues.

January lowest sea ice on record

(According to the National Snow and Ice Data Center, Arctic sea ice extent averages were the lowest on record for the month of January since at least 1979. The new low beats out 2011, continuing an ongoing decadal January decline of about 420,000 square kilometers every ten years. Image souce: NSIDC.)

But before we go more into the new spate of record low Arctic and global sea ice measures, it’s important to consider the context — our world has not seen the current level of heat forcing from greenhouse gasses (CO2 + methane + NOx + other greenhouse gasses) in the atmosphere since about 15 million years ago. It’s an unprecedented amount of hothouse potential that is having equally unprecedented results.

Unprecedented Volume of Heat Trapping Gasses Drives Raging Atmospheric and Ocean Warming

About 50 billion tons of CO2 equivalent from all those greenhouse gasses hit the Earth’s atmosphere each year these days. In vast part driven by industrial fossil fuel burning and extraction, this unconscionable, monstrous, and difficult-to-imagine accumulation of heat-trapping vapors is pushing the world to warm up at an unprecedented rate. A pace that is now at least 20 times faster than the widespread warming that occurred at the end of the last ice age.

Temperatures above 80 North

(It’s likely been a record warm start of the year for the Arctic above the 80 degree North Latitude Line. Temperatures in that high Arctic region have tended well outside the 2 standard deviation range and have hit above the record line on numerous occasions. Image source: NSIDC.)

Back then, it took about 2,500 years for the Earth’s atmosphere to heat by 1 degree Celsius for a total of a 4 C temperature increase over 10,000 years. By just this past year, in 2015, fossil fuel burning had managed to do more in 135 years than what an Earth System rising up out of an ice age did in all of two and one half millenia. For 2015 hit a new record high of about 1.1 C above 1880s averages in all the major global temperature monitors (NASA, NOAA, JMA, UK MET Office). It’s amazing, crazy, terrifying to think about. The end of the last glacial period was a great upheaval that violently re-shaped our world. And fossil fuel industry is running a similar, if much more dangerous, geological process in fast forward by pumping out heat trapping gasses at a rate at least six times faster than anything seen in all of Earth’s history.

Yet as amazing as the current rate of atmospheric warming is, it’s just the thin lens through which a vast amount of heat is transferring into the world’s ocean systems. In fact, according to Peter Gleckler, an oceanographer at the Lawrence Livermore National Laboratory “Ninety, perhaps 95 percent of the accumulated heat is in the oceans.”

Arctic Sea Ice Concentration January

(What was possibly the warmest January on record for the Arctic contributed to major sea ice losses in almost all of the major ice formation basins. Image source: NSIDC.)

And all that extra heat doesn’t just sit there. It goes to work transforming water to water vapor — shoving atmospheric moisture content 7 percent higher for each degree Celsius of warming even as it amps up the rate at which water evaporates from the Earth’s surface or falls down in the form of precipitation. Perhaps still more ominously, this heat goes to work melting the great white ice coverings it comes into contact with at the shoreline and upon the ocean surface.

Arctic Sea Ice Hits New Record Lows For January Through Early February

For 2016, that heat has led to new record lows in Arctic sea ice extent and area even as it has pushed global sea ice coverage within striking distance of a scant range never before seen in the whole of the modern era. New record daily lows for sea ice extent — now an almost annual occurrence for at least some time during the calendar year — are now also being breached.

Arctic Sea ice area new record lows

(Arctic sea ice area explores new record low territory on January 29 through 31 of 2016. Image source: Cryosphere Today.)

In the major monitors, Arctic sea ice extent hit a new record low average for the month of January, 2016. This average included a number of record daily lows early in the month even as the entire monitor held within 1st to 3rd lowest on record for each day throughout January. Record daily lows were again breached in the NSIDC measure on January 29th. A streak that continued on through February 1st with totals hitting 13.911 million square kilometers for the day. That’s 119,000 square kilometers below the previous record daily low for February 1 set in 2011 at 14.030 million square kilometers or a region of ice lost below the previous minimum extent slightly larger than the State of Virginia.

Arctic sea ice area as recorded by Cryosphere Today (see graphic above) followed a similar record low range through the end of January. By January 31st, the most recent date in the measure, Arctic sea ice area had hit 12.27 million square kilometers or about 61,000 square kilometers below the previous record daily low for sea ice area set during 2006.


(A very warm Arctic during January of 2016 likely contributed to shoving the global sea ice area measure into striking distance of new record lows by early February. Image source: Pogoda i Klimat. Data Source: Cryosphere Today.)

Also disturbing is the fact that global sea ice area — which has shown consistent losses over time — has also now come within striking distance of new record lows. The Cryosphere Today monitor now shows global sea ice area in the range of 14.5 million square kilometers or just above previous record lows set during 2006 for this time of year.

Conditions In Context — Amazing Sea Surface Temperature Anomalies, Major Winter Warm-ups Hit Sea Ice Hard

Arctic sea ice area negative anomaly is now in the range of -1.23 million square kilometers. With Antarctic sea ice at around 200,000 square kilometers below average, it’s pretty clear that the bulk of current global sea ice losses are now ongoing in the Arctic.

Warm ocean waters, especially in the Barents Sea and the Greenland Strait are likely major contributors to record low sea ice extents during recent weeks. These sea surface temperatures now show between 1 and an amazing 8 C above average reading in the NOAA sea surface temperature anomaly map below.

NOAA Sea surface temperature anomalies

(Sea surface temperatures are in the range of 4-8 degrees Celsius or 7-14 degrees Fahrenheit above average near sections of sea ice in the Northern Barents Sea. These very warm sea surfaces continue to suppress refreeze and provide melt pressure on into early February. Image source: NOAA.)

Such amazingly warm waters likely helped contribute to major atmospheric warming events in the high north over the past two months including one above freezing event at the North Pole during late December and another near freezing event for the same region during late January, likely added to the overall melt pressure. The very warm water in the Barents likely helped to enable the observed warm air slots that formed north of Svalbard and on toward the North Pole on numerous occasions.

Over the next seven days, Arctic air temperatures are expected to range about 1 C above average — as opposed to the 2-3 C above average range seen during the past month. This slight cooling may allow for a more rapid freezing of some regions including the Sea of Okhotsk. But overall warm waters and airs along the sea ice edge in the Bering and Barents should continue to suppress major ice formation there. By the second week of February, risk increases that high amplitude Jet Stream waves will deliver another burst of warm air to the far Northern Latitudes, potentially continuing the trend of extreme above average atmospheric temperatures in the region of the Arctic Ocean during 2016.






Arctic Sea Ice Graphs

The Arctic Sea Ice Blog

This is Where 90 Percent of Global Warming is Going

CO2 Rising Ten Times Faster Than PETM


Cryosphere Today

Pogoda i Klimat

Fossil Fuel Ecocide Forces Starving Polar Bear to Hold Breath For Three Minutes in Seal Hunt

(A starving polar bear is forced to hold breath for a record three minutes in a failed hunt for seals.)

Like so many other innocent creatures on this planet, polar bears are facing ever-worsening life-threatening conditions due to the fossil fuel industry’s insistence to keep burning, and to keep us dependent on their horrific energy sources. The bears’ Arctic home has been transformed in ways that are profound and terrible. The sea ice they used for hunting grounds is greatly depleted. The seals they hunted for prey have ever-more-numerous avenues of escape into dark and warming waters.

It’s a merciless and terrible burning. One that encompasses many genocides together. Ecocide, ecological shock, growth shock, the sixth great extinction. All words to describe what we now watch. What fossil fuel industry influence is preventing us from stopping. But to the bears themselves, it’s a wrenching torture. A forced orphaning and starvation combined as the bears grow increasingly emaciated, weak, and desperate. Transformed into walking skeletal beings, they’re ghosting off toward the obliteration fossil fuel interests are sentencing them to.

(Plunging Arctic sea ice driven by Northern Hemisphere polar amplification is the chief agent of habitat loss and extinction pressure for polar bears. As you can see in the superbly rendered video above by Andy Robinson, the fall has been merciless and precipitous.)

To a climate change denier, the plight of these poor creatures is a subject of ridicule and derision. ‘Who cares about stupid bears’ is the rallying cry of heartless ignoramuses everywhere. They’d rather us be worried about our own petty day-to-day existences. The back and forth, stuck in traffic, want more money, pay less taxes, fear of far off ISIS daily grind of the right wing soundtrack. Or when the tinny siren song of that ever-more-stuffed-with-straw appeal fails it’s back to the old — pretend it’s not happening — trick. Starving polar bears so desperate that they’re now forced to hibernate in summer to conserve energy must be photo-shopped by some imaginary government agency after all, right?

Deny as deniers do, for the bears it’s all too real. For one bear in particular, recently filmed in the above video, it was a life and death struggle. Not some narcissist’s thrill like the needless poaching of innocent wild lions for blood-sport in Africa. No, for this bear, success in the hunt meant a continuation of blessed life. A second chance to keep going, to keep living in the great world. Failure meant weakness, fading, pain and death.

The bear, in dire need of food, was forced to hunt in a way it was not adapted to — by stalking in the water. It was forced, in desperation to swim toward near-water seals. And it was forced to hold its breath underwater. Hold it for longer than any polar bear ever witnessed. Hold it for a full 3 minutes where a mere 72 seconds was the previous record. It was as if the starved bear had been forced to perform impossible feats — or die. That’s the situation the callous greed and disregard of some have put them in. Do the impossible, or just die.

Gaunt and Emaciated Polar Bear that Broke Diving Record

(The gaunt, emaciated and obviously starving polar bear that broke the recent diving record in a photo by Rinie van Meurs. Image source: Meurs Study and The Weather Network.)

This bear’s struggle is not one occurring in isolation. It’s not just the struggle of a single individual. But the struggle of an entire race that is now being torn from the fabric of existence.

The cliche phrase to say at this time is that we are all responsible. That we all share the guilt. But it’s not true. In fact to say such a thing is a terrible lie providing an out for the real perpetrators of this egregious harm. There are some of us who want to change the bear’s situation. Some of us who want to improve its chances. Some of us who want to cut the destructive fossil fuel threads that bind the bear and us all to a terrible and ever worsening ecocide. The ones who want to help are not the problem. The ones attempting again and again to stop the ongoing damage are not the guilty party.

But the deniers and the fossil fuel industry the deniers wittingly or unwittingly serve are entirely different. They don’t care one whit about bears suffering an all-too-real existential crisis. And it seems they don’t care about their own children’s rising existential crisis either. They are the ones who deserve blame. For they are the authors of this great harm.


This one’s for Colorado Bob

Polar Bear Forced to Hold Breath for a Record Three Minutes

Record Breaking Polar Bear Spurs Climate Concerns

Food Situation so Bad, Polar Bears now Hibernate During Summer

Sea Ice Volume Decline By Andy Robinson

Arctic Sea Ice Bounce Wiped Out as 2015 Summer Tracks Third Lowest on Record

It’s been a rough summer for the Arctic sea ice. Extent values started off at record low levels during late spring, melt ponding and warming ramped up during early June, and July saw the ice pounded by intense high pressure cells located on the Greenland side.

Sea surface temperature anomalies

(Abnormally hot water surrounds the Arctic sea ice on all sides. High sea surface temperature anomalies in this range tend to aid in the maintenance of late season melt momentum. Image source: DMI.)

Warm Waters and Airs

Anomalously warm water invaded from almost every side. The Kara saw extreme sea surface temperature warming after an early ice recession, a flood of warm water from rivers, and a powerful albedo flip to dark ocean from white ice. The Chukchi, Beaufort, and East Siberian seas saw a continued influx of anomalously warm waters from the Pacific side — this flow was fed by the powerful and persistent blobs of warm water in the Northeast Pacific. A heat invasion that has been ongoing for that region since at least Winter. And in North Baffin Bay a pool of anomalously hot water has combined with an extended period of warmer than usual air temperatures to deliver heat to the remaining thick ice along the Northern Greenland and Canadian Archipelago boundary.

Warm Storms Smashing the Old Ice

By August, a series of storms had invaded the Beaufort, Chukchi and East Siberian Seas. Kicking up 20-35 mile per hour winds, they pushed 2-7 foot swells out through an expanding shattered ice zone. Though the storms cooled the air, they tapped heat from the ocean itself through the process of surface churning and the larger dynamic of cyclonic Ekman pumping. All this motion and heat energy created a very unfavorable environment for sea ice — essentially melting the ice rafts out from the water line on up.

Beaufort July 22

Beaufort August 4

(Top [July 22] and bottom [August 4] comparison of the same Beaufort grid showing large rafts of multi-year ice gradually being smashed to finer and finer pieces. Image source: LANCE – MODIS.)

Large pieces of multi-year ice were smashed together like rocks in the late 20th Century video game — asteroids. The ice, ground into ever-finer bits by these storms, then felt the heat of the moving waters and suffered an ongoing dissipation.

The result is that the Beaufort ice is being steadily hollowed out. A bank of thicker ice floes is expanding into the warmer waters of the Chukchi and near-shore Beaufort as it melts. This leading ice edge, though frail, is denser than the interior ice for scores of miles where three large polynyas are in the process of joining into one. If this keeps up for too much longer, the next ten-to-twenty days will see the Beaufort ice and the Chukchi boundary ice practically wiped out.

Melt Invading Past 80 North

Meanwhile, thinned ice and open water is gradually invading the Central Arctic past the 80 North Latitude line.

Arctic sea ice early Augustarctic_AMSR2_visual_small

(Arctic sea ice appears to be in a terrible state  in the AMSR2 visible measure. Beaufort and Chukchi ice continues dramatic thinning. Central Basin ice is retreating in numerous places behind the 80 North line. And the fabled Northeast Passage is open to shipping. Image source: Uni Bremen.)

Heat from the Atlantic side is eating away at the ice edge there. Laptev melt is biting in beyond the 80 North line. And the Beaufort storms are basally melting and dispersing the Central Arctic boundary ice. As a result, the monitors are showing sea ice that looks to be in a very unhealthy state overall. The Northeast Passage is open and the Northwest Passage appears to be just a week or two behind.

The Rebound is Wiped out in all Major Monitors

As a result of all this punishment, the sea ice monitors are looking increasingly bleak. Japan’s JAXA extent monitor is showing sea ice boundary measures in the same range as third lowest year on record — 2011. The National Snow and Ice Data Center measure is not too far behind at just a hair above 2011 and 2010 — now tracking at 5th lowest extent on record (a loss of two places since last week). These extent measures are swiftly catching up to the Cryosphere Today area totals that are now also just a hair above 2011 at 4th lowest on record. The area measure is also interesting in that overall area is at 4.13 million square kilometers — which is now starting to dip below the 2005 line.

But perhaps most concerning of all is the fact that sea ice volume, which showed a brief bounce back from 2012 record lows during 2013 and 2014, is now re-entering decline. For According to PIOMAS, the ongoing punishment we have visibly seen in the form of high atmospheric temperatures north of the Canadian Archipelago and in remaining thick ice being swept into the billiards pool that is the Beaufort has pushed that volume measure well below the 2014 line and back toward recent record low years.

Sea ice Volume Losses PIOMAS

(PIOMAS volume measure takes a nose-dive in July. Continued losses at this rate would put sea ice volume in the range of lowest years recently observed. Image source: PIOMAS.)

It’s a steep nose dive. One that will start to challenge the upper boundary of record low years without a slowing in the rate of losses soon.

Storms, Ocean Surface Warmth, El Nino Heat Transport, and Beyond 80 North Melt Drive Late Season Loss Risk

With a month and a half of melt still to go, we could see a softening in this high rate of loss and an adjustment that brings use closer to 2014 for end season. Or we could see the steep rate of loss continue to challenge the 2011 boundary in some measures and possibly even break lower to challenge 2007. But given the melt momentum coming out of July, it is very unlikely that measures return to 2014 levels. As a result, it looks like the summer of 2015 is wiping out the post-2012 sea ice bounce which, given the massive pace of human-forced warming and failing to see large enough melt from Greenland to counter that trend in the Arctic, appears to have been inevitable.

Looking forward there appears to be four factors that will play out their final hands for 2015 melt. The first are those very warm sea surface temperatures we mentioned earlier. The second is the fact that this is an El Nino year featuring a very warm Northern Pacific and a strong northward heat transport through the Canadian Archipelago and Alaska. The third involves the weak sea ice and persistent storms in the Beaufort, Chukchi, and ESS. And the final major factor involves the strong advancement of melt into the Central Arctic and the higher likelihood that the below 80 North boundary ice will be wiped out in the coming weeks.


(The northward propagation of anomalously warm ocean surface waters is bad news for late season sea ice. Extremely warm Northeastern Pacific surface waters and an associated El Nino warming of the Eastern Pacific equatorial waters creates a pathway for warm air transport into the Arctic over Alaska and Canada during late summer. Such a situation may result in an extension of late season melt beyond the September 15 date. Image source: NOAA ESRL.)

Abnormally warm sea surface temperatures plus the atmospheric feedback of El Nino hint that more energy to melt ice may remain in the Arctic for longer than during a typical year. Current transport of that abnormally warm water into the Chukchi, East Siberian Sea, and the Beaufort will continue. And the El Nino tendency to push warm air up over Alaska and the Bering will be reinforced by the strong warming in the lower Chukchi. These factors will tend to extend late season melt. Over on the Atlantic side, a similar dynamic is starting to come into play. Warm waters in the Laptev and Barents are increasingly being driven against the edge ice past the 80 North boundary line by warm southerly winds and through the action of storm systems invading the upper North Atlantic. Over the past few days a pattern has emerged in the models indicating an influx of these storms past Iceland and into the Barents near Svalbard. Swell propagation and warm water driven north will have a deleterious effect on the ice there.

As storms rise up from the North Atlantic, storms are predicted to continue to plague the ice in the Beaufort, Chukchi and East Siberian seas. According to GFS model runs, this tendency continues through at least the next five days. And with warm air firmly in place over Alaska and the Chukchi, while cooler air sits over the Beaufort, the gradient necessary to fuel these storms will remain in play. Ocean state forecasts pick up seven foot swells in the East Siberian Sea tomorrow, nine foot swells in the Chukchi on Friday, and 3-4 foot swells ranging the thick ice billiard room in the Beaufort on Sunday. Swells in the Laptev open water are also predicted to hit 6-7 feet over the coming days.

Stepping back and looking at the overall distribution of the sea ice, we find that much of the beyond 80 North region is invaded by melt. A substantial amount of weak boundary ice remains in the Beaufort, the Chukchi, the East Siberian Sea, near the land regions of the Laptev, and within the waterways of the Canadian Archipelago. Ice in these outlier regions is traditionally more vulnerable to rapid melt and it is doubtful that much of it will remain by end season.

Wipneus amsr2 graph

(Arctic Ocean sea ice extent measures are tracking in the range of 2012 according to the above graph by Wipneus. Low values that, entering final stage melt for August and September, may swing the overall measures lower come end season. Image source: Wipneus.)

Meanwhile, the beyond 80 North melt invasion is substantial to the point that we are now very close to the 2012 melt trend line in that key region. In fact, pretty much all the interior Arctic Ocean seas show extent values tracking near the 2012 record low line.

These low Arctic Ocean values imply a deeper vulnerability to hitting lower end season totals. A vulnerability the overall measures, so far have missed.




Uni Bremen

Arctic Sea Ice Graphs

Neven Sea Ice



Cryosphere Today




Earth Nullschool

“Massive” Arctic Heat Dome Sets Up to Bake Sea Ice

There’s a massive heat dome building over an Arctic sea ice pack that is looking increasingly fragile in both model forecasts and observations. In short, very bad weather for sea ice is rapidly settling in even as the ice pack, despite recent place gains in some measures, is looking increasingly weak.

*   *   *   *   *   *

First the somewhat good news… Arctic sea ice extent has backed off to about 8th lowest on record. Arctic sea ice area is at about 4th lowest on record. And Arctic sea ice volume, according to DMI, is in the range of 3rd lowest on record (PIOMAS looks even better). This report may sound rather bad, but when compared with  late May and early June when sea ice extent measures were at or near new record lows the data could arguably be characterized as an improvement. Yeah, there’s been some big area drops recently, but all in all, not too terrible, right?

Probably wrong… Because the Arctic is gearing up for a very powerful heat wave over the coming week. One that is likely to spike maximum summer temperatures in the High Arctic, a region that seldom shows much variance on the side of hot or cold at this time of year, by 0.5 to 1.5 C above average. A heatwave my somewhat more reserved fellow ice observer, Neven, has called ‘HUGE’ (note that Neven seldom uses caps lock) and is characterizing as something he’s not seen in all of his five years of sea ice observation. From The Arctic Sea Ice Blog Today:

However, there is one big difference compared to last year and that’s heat. Despite a very cold start, there have been several outbreaks of warm air over the ice, slowly but radically shifting the balance between extent and area data. The impact is felt on the surface of the ice pack, but doesn’t translate directly into a decrease. Not yet. In theory, it should percolate through after a while, especially if the heat persists. And right now the Arctic sea ice pack is undergoing a massive heat wave which shows no signs of letting up.

I find myself in agreement with Neven. The massive heat build in the Arctic predicted for this week is likely to be a significant event with potentially wide-ranging impact. But to understand why, it helps to get an overall picture of the broader context in which this particular heatwave is occurring. And that context includes two other stories as well — the story of human-forced climate change and the story of a still developing and potentially monstrous El Nino.

Ocean Warming Injects Heat into the Arctic

To get an idea how warming in the Equatorial Pacific and over-all greenhouse gas based warming can have such a far-flung impact, particularly on the currently building Arctic heatwave, it always helps to take a look at the behavior of the circumpolar Jet Stream. Large areas of persistently warmed water, like the one we have seen now for two years over the Eastern Pacific, have a tendency to generate high amplitude ridges in the Jet. Ridges that serve as open avenues for heat transport into the Arctic. Specifically yesterday a huge pulse of heat was traveling north along just such a high amplitude and ocean-warmed ridge:

Jet Stream July 6 2015

(Amazing high amplitude Jet Stream wave punching all the way through to the High Arctic on the back of the Eastern Pacific’s Ridiculously Resilient Ridge. Image source: Climate Reanalyzer.)

Our particular heat transporter should by now be very familiar — a ridiculously resilient ridge (RRR) — extending northward and buttressed by multiple high pressure cells stubbornly entrenched over abnormally hot water in the Eastern Pacific. Yesterday (Monday, July 6) the ridge elongated. South to north winds over-riding northward flowing warm, salty ocean water. Running up through Alaska, the heat pulse set off all-time daily highs in places like Anchorage (81 degrees and breaking the record set in 1972). The heat then spilled into the Bering, Chukchi and Beaufort Seas where it met with adjoining, though lesser heat pulses over-riding Greenland and the Laptev. A gathering pocket of hot, thick air that is now pooling in the so-called sea ice ‘safe zone’ just north of Greenland.’ A precursor to the very intense high pressure cell we see developing now.

But before we go on to tell the tale of our gathering Arctic heatwave we should first take a closer look at ocean surface temperatures. As these give us a rather clear picture of the Arctic’s current vulnerability — providing for us a hint as to why heat will intensify most strongly to the north of the Canadian Archipelago and Greenland. For it is ocean surface heat that built the road that warm air followed:

Warm water plume invades Arctic

(Heat plume running all the way from Equator to Pole clearly reflected in this July 6 NOAA/ESRL SSTA anomaly map.)

Taking a look at NOAA’s July 6 Sea Surface Temperature Anomaly (SSTA) map, we find a massive plume of much warmer than normal (1971-2000) waters extending up from a plainly visible El Nino pattern, all throughout a large sweep of the Eastern Tropical Pacific. Moving northward, these steamy waters spill into two hot blobs off the Mexican, US, and Canadian coasts — a heat pool that again punches up through the Chukchi and Beaufort Seas. An Equator to Pole expanse of ominously hot water that is enabling both sea ice melt in the regions directly impacted as well as a broader invasion of warmth into even the sea ice’s most secure haunts.

Heat Directly North of Greenland, Canadian Archipelago

Warmth that today aided in the formation of an Arctic high pressure ridge hitting significant heights of 1030 to 1035 mb directly between the Pole and Greenland. At 1245 Eastern Standard Time, the ridge had already intensified to 1032 mb. And for at least the next seven days both the GFS and the Euro model shows a 1025 to 1035 mb high pressure cell dominating the same region.


(Left frame shows strong, 1032 mb high pressure system settling in to the region just north of Greenland on July 7. By July 10 [right frame], this ridge is predicted to have greatly warmed the Central Arctic zone between Greenland and the Pole. Image source: Earth Nullschool.)

This persistent ridge will remove cloud cover in a large area between North America and the Pole. Sunlight, at its seasonally most intense, will multiply already widespread melt ponds on the sea ice surface. The combined solar forcing and loss of albedo will push surface temperatures higher as the ridge remains in place. And by Friday a broad band of 2-4 C temperatures is predicted to form in a bulge over the Arctic Ocean north of Greenland and the Pole. Abnormally warm temperatures and direct sunlight that will, over the next week, increase melt pressure over the last remnant of thick sea ice left to the Arctic.

In addition to reducing cloud formation and enhancing the melt-forcing impact of sunlight on the sea ice, high pressure cells in this region will have a couple of further influences. First, they will tend to compact the sea ice overall — drawing in the fringe ice while generating warm water upwelling at the ice edge. And second, the clockwise motion of air circulating around a strong high pressure cell will nudge sea ice out of the Central Arctic toward the gateway of the Fram Strait. Add in the significant impact due to reduced cloud formation allowing sunlight to contact sea ice during a period of peak solar radiative forcing and we end up with a substantial overall blow to the sea ice.

Arctic temperature anomaly

(Extraordinary high temperature anomalies are predicted for the Arctic from July 7-17. A departure more typical for winter when human greenhouse gasses have the greatest heat-amplifying impact. Image Source: meteomodel.)

Taking a look at the meteomodel anomaly map above, we find a very extreme warming of the Central Arctic predicted over the next ten days. A heat pulse to rival 2012 for this period. A melt multiplying heatwave that is predicted to push anomalies for the entire Arctic above +1.5 C beyond the early July average. A polar amplification similar to what is typically a winter manifestation of human emissions-driven anomalous warmth — this time anomalously occurring during a period when heat for the region is approaching peak intensity.

Impacts to Sea Ice Could Be Substantial

In the face of this oncoming weather, ice pack strength would be a deciding factor lending resiliency during melt-promoting conditions or a shift to a much more rapid rate of decline. Though some indicators, including a seemingly slower rate of decline during late June, may point toward more ice resiliency, a growing number of satellite reports and model analysis hint at a general and overall weakness throughout the ice pack.

This weakness can best be described as model indication of thin or low concentration ice, already widespread melt ponding, and visual indication of ice weakness in the satellite shot.

GLBb Holy Shit Model

(The US Navy’s GLBb model has always been unfriendly to sea ice. But other models are now starting to agree. Image source: US Navy.)

For low concentration ice, no model is more stark than the US Navy’s experimental GLBb sea ice thickness ensemble. I colloquially think of this as the ‘holy crap’ sea ice model. This label due to the fact that if sea ice state is really as bad as the model indicates, then the ice is basically toast. Starting in June, this model displayed a great overall weakness in the sea ice and, according to its analysis, the situation has progressed from bad to worse with most of the remaining Arctic Ice possessing a thickness of 1.2 meters or less. Easily thin enough for any nudge by weather to really start rapidly bringing the ice down and opening up very large expanses of open ocean.

If the GLBb ‘holy crap’ model were the only sea ice model making us want to say ‘holy crap!’ then we could probably breathe a bit easier. Unfortunately, another US Navy model is now also tending to elicit this response in reaction to its predictions for the next 7 days and more specifically for the next 3 days:

Arctic Sea Ice Concentration TodayArctic sea ice concentration forecast

(The US Navy’s ARCc sea ice concentration model predicts a very rapid rate of sea ice decline over the next few days. Image source US Navy.)

The top image in this up and down comparison shows the US Navy’s ARCc model’s interpretation of sea ice concentration for July 6 of 2015. Note the extensive green regions showing a 40-50 percent sea ice concentration. It’s a huge swath of ice including large sections of the Chukchi, the Beaufort the ESS, the Laptev, as well as remaining ice in the Kara Sea, and Baffin and Hudson Bay. Now watch what happens to those large sections of lower concentration ice from July 7 to July 10 in the ARCc model 30 day history and forecast summary. Almost all that green is wiped off the map. It’s like losing about 1 million square kilometers of extent and 600,000 kilometers of area in just 72 hours. Or about 10,000 square kilometers of ice per hour. A precipitous fall that would mark an extraordinary and likely unprecedented rate of loss should it emerge as the Navy model predicts.

But you know what they say about models — no model is perfect and every model ends up wrong in some manner or another. So the question here is — how likely is it that the Navy models could be correct or incorrect this time?

To try and tease this answer out we could also look at other sea ice concentration maps. Notably all the major ones including Cryosphere Today, Uni Bremen, and NSIDC currently show sea ice looking either thin or very thin. Specifically, Uni Bremen has shown some amazing contrast over the past 48 hours:

Uni Bremen July 5Uni Bremen July 6

(AMSR2 model analysis of sea ice surface state shows very rapid thinning in the Beaufort and Chukchi Seas during the past 24 hours. Image source: Uni Bremen)

The left image in the above comparison is from the AMSR2 model analysis for Arctic sea ice concentration on July 5. The right image is the same analysis but for July 6. Note the substantial change in the sea ice concentration for the Beaufort and Chukchi seas over just one day. A change that is consistent with the pulse of warm air and water riding up through the Eastern Pacific and through Alaska, the Bering and the Chukchi. Another holy crap moment, and not at all of the good variety. To say the least, a similar response north of Greenland and the CAA would be devastating.

Moving away from models and back to observations we find that from the satellite vantage the entire Arctic Ocean displays an ice pack in various shades of azure. By color analysis alone we can readily see that the 2015 ice (July 6 MODIS image) is far more melt pond embedded than 2014 or 2013. 2012 is a tough comparison due to NASA-MODIS’s format change from that year. But the widespread melt ponding alone hints at a reduced resiliency for the ice when compared with recent years.

Arctic Ice Pack July 6

(Arctic sea ice turns blue color characteristic of widespread proliferation of melt ponds on July 6. Also note very thin and diffuse sea ice in the Beaufort and Chukchi. Image source: LANCE-MODIS.)

Turning to the Chukchi and Beaufort, we see a visible confirmation of the weakness indicated in the US Navy and Uni Bremen models. Beneath the smoldering outflow of the Alaskan fires we can plainly see the decayed state of ice. The floes greatly disassociated with widening gaps appearing between diminishing ice clusters.

As satellite gives us an overall view of the Arctic from above, local observations can help provide a sense of the sea ice state at the surface. During recent years, cameras mounted on buoys throughout the Arctic have provided us with a first-hand account of the story of Northern Hemisphere sea ice decline. And during recent days almost every camera-based buoy has shown an extensive expansion of melt ponds and open water. (Extensive melt ponding extends as far north as the Pole).

In the swiftly thinning ice pack of the Beaufort even the contrast of a single day can be quite stark.

Beaufort Open WaterBeaufort Open Water Waves

(Warm storm kicks up under the gradient imposed by a building heat dome of the Arctic. Top and bottom frame provides a stark tale of impacts in just one 24-hour period. Image source: USIABP.)

In the above top-bottom comparison of RACS#2 ice buoy photos we find that wide but placid areas of sunlit open water in the Beaufort Sea on July 6th (top frame) have rapidly transformed to wind-driven 1-2 foot waves whipped up by 15-25 mile per hour winds on July 7th (bottom frame) in association with a tightening gradient around the strengthening high pressure in the Central Arctic. Waves of this kind can deliver a significant amount of melt forcing to the ice — mixing cooler surface waters with warmer waters below as well as rocking through the ice floes with a rain of incessant, ice-breaking blows.

Conditions in Context: Rapid Melt Likely On the Way

Increasing model agreement indicating rapid sea ice melt, observations of sea ice weakness via satellite and buoy based systems throughout the Arctic, and predictions of a substantial Arctic heatwave all point toward a high and rising risk of rapid sea ice melt. Larger global trends, particularly heat transport from the Equatorial Pacific all the way to the northern Polar zone through the mechanisms of El Nino, human based greenhouse gas heat forcing, and the associated Ridiculously Resilient Ridge, heighten this risk even further. Finally, a wide array of observations indicate that such rapid melt is already starting to set in. Given this increasing agreement and confluence, it appears that the late June ice dispersal is likely over and that serious trouble for Arctic sea ice has now set in and will remain in play for at least the next seven days.


The Arctic Sea Ice Blog

Cryosphere Today

Uni Bremen


The Polar Science Center


Earth Nullschool

US Navy


Hat Tip to Neven

Hat Tip to Frivolous

Hat Tip to Jim Hunt

Hat Tip to Climate Hawk



Hot Blob #2 Takes Aim at Sea Ice — Abnormally Warm Waters Invading the Arctic Through Bering and Chukchi

A lot of attention has been paid to a ‘Blob’ of unusual warmth at the ocean surface in the Northeastern Pacific. And for good reason, for that Blob of human-warmed water has had wide-ranging negative impacts on both weather and sea life. Now there’s a second hot Blob forming in the Bering and Chukchi seas. One that may also have some rather significant effects as the summer of 2015 continues.

Abnormally Warm Waters Running Toward the Sea Ice

Hot Blob #2 is a vast stretch of warm water covering the Bering and Chukchi seas between Alaska and Kamchatka (Neven, in his most recent sea ice summary, touched on this building warm water zone here). It encompasses surface waters in an usually frigid region that now feature temperatures ranging from 3 to 5.5 degrees Celsius above normal. Covering an area roughly 800 miles in diameter, this pool of outlandishly warm ocean waters is being fed by currents running up from the south and by heat bleeding off Alaskan and Siberian land masses. In this case, land masses that are also experiencing record heat.


(Hot Blob #2 forms in the Bering as its warm waters are swept north toward the Arctic sea ice pack. The above sea surface temperature anomaly map shows a broad stretch of much hotter than typical surface waters being pulled poleward by prevailing ocean currents. Image source: Earth Nullschool.)

Though the abnormal warmth is also likely fed by a powerful albedo switch from white, reflective sea ice, to dark, sunlight absorbing ocean, other factors associated with El Nino and related to the hot blob off the North American West Coast are also likely in play. And of particular interest in this present extreme hot water situation are currents flowing northward out of these warm pools and directly into the Arctic. Currents that have been eating away at the ice since winter.

One warm water bearing current — the Alaskan Coastal Current — runs directly out of the abnormally hot surface zone in the Northeastern Pacific (Blob #1). This current flows along the North American Continental Shelf, out past the Aleutian Island Chain and finally up into the Bering Sea. A second current — the Siberian Coastal Current — feeds into the Bering from the Asian Continental Shelf. These currents then combine and push Bering Sea waters on through the Bering Strait and up into the Chukchi Sea.

Algae bloom hot pool

(Algae blooms, like this one in the Chukchi Sea just south of the ice pack, have been a common feature of the Pacific Ocean hot pools. The warmer waters are a preferred environment for microbes which can see some amazingly rapid population explosions. If the blooms become too numerous they can rob the ocean surface waters of nutrients and die off en masse. The decay of dead masses of algae can then leech away the oceans’ life-giving oxygen, setting off and contributing to a chain of harmful ocean anoxia. In a warming world, this process, combined with disruption of ocean currents and the basic fact that warmer waters bear less oxygen in solution, is a major contributor to mass extinction events. Image source: LANCE MODIS.)

Northward propagation of these currents during spring and summer plays a critical role in the rate of sea ice recession in the Bering, Chukchi, Beaufort and East Siberian Seas. Waters warmed by the summer sun and by the more rapidly heating continents amplify in the Bering Strait before making contact with the sea ice and pushing it to melt and recede.

Impacts Already Visible Up the Coast

This year, waters in the Strait are extraordinarily warm — measuring 5.4 degrees above normal surface water temperatures. A plug of 5 C + above average water entering the Chukchi, Bering, Beaufort and East Siberian seas at a time when solar insolation is hitting peak intensity and during a period when nearby Arctic regions like Alaska are experiencing some of their hottest temperatures ever recorded. These waters, at temperatures in the range of 7-8 degrees Celsius, are warm enough to rapidly melt any ice they contact. And they’re flooding directly toward the ice pack.

Barrow Alaska

(Ice rapidly melting off of Barrow, Alaska on June 23, 2015. Ice is seen receding from the near shore zone even as the ice pack further out breaks into dark blue patches of open ocean. Image source: Barrow Ice Cam.)

Unusually warm surface water and air temperature impacts can already be seen further down the coast in places like Barrow, Alaska. Today, near shore sea ice dramatically melted and off-shore sea ice has retreated poleward — revealing the tell-tale blue of open ocean in the distance. An extreme one day change for Barrow sea ice, which only featured melt ponds and some near-shore melt 24 hours before.

Conditions, Model Runs Point Toward Substantial Thinning

Looking northward, we find ice pack conditions showing substantial thinning, significant melt pond formation over the surface ice and increasingly disassociated ice flows in the Beaufort, Chukchi, and East Siberian Seas. Near shore ice in the East Siberian Sea (ESS) has taken on a vivid blue or glassy appearance indicative of melt pond formation. Melt and compaction wedges have formed in the ESS along an axis pointing toward the pole. In the Chukchi, sea ice recession and thinning appear to be proceeding quite rapidly, while dispersing ice in the Beaufort is hitting warmer surface waters, fed by Mackenzie River outflow, and melting.

Navy ARCc Model Run

(The ARCc model run shows rapid thinning in the Beaufort, Chukchi and ESS through June 30. Image source: US Navy.)

The Navy’s ARCc historic and forecast model run for May 30 through June 30 shows rapid thinning of sea ice in the affected regions. The forecast run for the next seven days shows extreme thinning continuing through the ESS and Chukchi, with thicker ice in the Beaufort also experiencing substantial reductions (Note that the Navy’s GLBb model runs look even worse).

Overall, given the fact that storms are now ranging through substantial sections of the Arctic, pushing for more sea ice dispersal, losses will tend to show up more in the sea ice area and volume measures first. Dispersal will also tend to mute extent losses for a time. Given the delay in area and volume tracking, it’s likely that overall impacts to sea ice will tend to be muted in the measures over coming days with a clearer signal showing up by late June and early July. But despite these underlying and complicating weather conditions, the fact remains that a lot of unusually warm water is heading northward toward the ice, with likely greater impacts to follow.


Earth Nullschool

US Navy

Barrow Ice Cam

The Arctic Ice Blog

A Deadly Climb From Glaciation to Hothouse

Awakening the Horrors of the Ancient Hothouse — Hydrogen Sulfide in the World’s Warming Oceans

Hat Tip to Colorado Bob

Hat Tip to Ouse MD

Arctic Sea Ice Area Drops 340,000 Square Kilometers in Just One Day

Sea ice researchers like to talk a lot about what they call ‘Century Drops.’ Days when Arctic sea ice area or extent values fall more than 100,000 square kilometers. In the past, daily Century Drops were relatively rare — with steepest rates of loss occurring during late June through early August and featuring, perhaps, a handful of days in which 24 hour losses exceeded 100,000 square kilometers. But the record melt years of 2007 and 2012 showed a proliferation of daily drops that exceeded the 100,000 square kilometers daily threshold.

Well, a couple of days ago a three Century Drop showed up in the Cyrosphere Today measure. And it may just be something we’ve never seen before (UPDATE: actually the last time was 2008, see Neven’s comment below). At the least, it’s an event that’s pretty amazingly rare — or it should be, without the heat added to the Arctic by human fossil fuel emissions.

On Tuesday evening, the Cryosphere Today site showed Arctic sea ice at about 8,986,000 square kilometers. The next day the measure stood at about 8,646,000 square kilometers. That’s an extraordinary loss of 340,000 square kilometers in just one day.


(Cryosphere Today sea ice graph shows that losses basically went vertical on Tuesday, June 16. Image source: Cryosphere Today.)

340,000 square kilometers gone in a single 24 hour period. That’s an area of sea ice the size of the state of New Mexico gone in a single day. In the above graph, you can see the drop as the vertical turn in the yellow line denoting 2015.

The massive single day drop temporarily brought sea ice area in the Cryosphere Today sea ice area chart into the range of second lowest on record for the date. Area losses of around 70,000 square kilometers for Wednesday resulted in a retreat to around 4th lowest on record. But any period in which drops of this size become frequent would easily transport the measure into new record low territory.

Arctic Melt Ponds

(LANCE MODIS showing the tell-tale blue of melt ponds all over the Arctic Ocean and most concentrated in edge zone regions. Proliferation of melt ponds during early season, especially when combined with the impact of human caused global warming, can increase risk for new record lows by end season.)

The cause of such a large single day drop is likely due to a combination of factors. Lately, storms have been more prevalent in the Arctic Ocean proper and such storms have a tendency to spread the ice out more, opening gaps in the ice called polynyas which tends to push the sea ice area measure lower. In addition, there is melt pressure now in Baffin Bay, Hudson Bay, the Kara Sea, the Laptev Sea, the Beaufort Sea, the Chukchi Sea, The East Siberian Sea, the Canadian Archipelago waters, and in the Barents border region. This basically composes the entire border zone of the Arctic sea ice.

Finally, the NASA MODIS satellite composite for recent days has shown a marked shift toward a light blue coloration for the entire Arctic Ocean zone and especially for the border zones. Such a shift is indicative of a proliferation of melt ponds. Major snow cover losses over sea ice during the past two weeks have removed insulation to the sea ice pack and probably aided in the formation of these melt ponds. Melt ponds are a strong indicator for sea ice health throughout the melt season — so a proliferation of melt ponds at this time may be a sign of sea ice melt vulnerability (see more over at Neven’s Arctic Sea Ice blog where they do a bang-up job tracking seasonal melt ponds and their potential impacts).

Though a three Century drop occurred, melt overall still has some catching up to do to make 2012 levels. So though this massive daily drop occurred, we are not yet in the red zone for sea ice area. Sea ice extent measures, on the other hand, remain in the range of second to third lowest on record and are still very close to all time record low levels. So this particular melt season is certainly one to still keep watching.


Cryosphere Today


The Arctic Sea Ice Blog

Hat Tip to Neven

Big Warm-up Predicted for Northwest Territory as Pacific Side of Arctic Melts Out Early

The long-term trend for Arctic sea ice is inexorably down. Year-after-year, decade-after-decade, the human-driven accumulation of heat in the Arctic has taken a terrible toll. Recently, mid March through mid April showed record low sea ice extents for any period since record keeping began in 1979.

Over the past two weeks, extent levels bounced back to around 4th to 6th lowest on record as winds shifted to north-to-south through the broad region between Greenland and the Kara Sea. For this region, melt pressure had been quite strong throughout Winter as a powerful warm flow of air flooded up from the North Atlantic.

Sea ice concentration

(Ice in the Bering and the Sea of Okhotsk is rapidly melting. Warming and sea ice melt ramp-up may also be on tap for both the Hudson Bay and the Beaufort as south-to-north air flows associated with the Ridiculously Resilient Ridge intensify. Image source: NSIDC.)

The shift, which has occurred coincident with upper-level winds running up from the Ridiculously Resilient Ridge in the Eastern Pacific, over Alaska and the Northwest Territories of Canada, into the Beaufort and on past the pole, has been pushing sea ice southward toward the Barents and into the Fram Strait. The result has been minor sea ice expansion in the near Greenland region at the cost of much more rapid melt in the Bering Sea, the Sea of Okhotsk and a very earl season break up of ice in the Beaufort.

Pacific Side Warming and Beaufort Break-up

Overall, this Pacific-side warming of the Arctic has driven extent levels back down into the range of 3rd to 4th lowest on record for this time of year. And rapid melt in the Bering, the Sea of Okhost, together with warming in the Beaufort and Hudson Bay may result in new challenges to record lows over the coming days.

By late April, break-up of Beaufort Sea ice is particularly dramatic with very large polynyas forming in a broad region into and north of the Canadian Archipelago and extending on into the off-shore region of the Mackenzie Delta:

Beaufort Sea Ice April 26 2015

(The Beaufort Sea shows extensive break-up and lackadaisical re-freeze on April 26th 2015. Note the extensive dark cracks and polynyas [holes] in the MODIS satellite image above. Such late-spring proliferation of polynyas and cracks can critically reduce albedo as melt season progresses. The Beaufort’s location also makes it vulnerable to continued warm air influx over a very warm Northeastern Pacific Ocean. Image source: LANCE MODIS.)

Temperatures within the Beaufort Sea and near the Canadian Archipelago are still cold enough to support some re-freeze in the Polynya regions. However, closer to the Mackenzie Delta, temps have trended more and more toward near freezing or above freezing levels (sea water freezes at around 28 degrees Fahrenheit). The result is a rather large region with no new ice formation.

More Warm air on the Way

As of 5 PM Eastern Standard time, temperatures in the Mackenzie Delta on the shores of the Beaufort Sea were pushing 32 degrees Fahrenheit. Meanwhile, 50 degree temperatures dominated the region of Great Slave Lake further upstream and southward. These readings are in the range of 8-15 degrees above normal for this time of year, resulting in an early melt pressure for the Mackenzie River and for coastal regions near the post-thaw river outflow zones.


(Big warm-up near the Mackenzie River and through the Northwest Territory in April  28th’s GFS model prediction. Temperatures in the low 70s gather around Great Slave Lake as above freezing temperatures drift down the Mackenzie River reaching all the way to Arctic Ocean Shores. Note near and above sea water freezing temperatures [28 F] throughout the Bering, Beaufort, northwest sections of the Canadian Archipelago and Hudson Bay in the above image. Image source: Earth Nullschool.)

This warm pool is predicted to intensify through tomorrow with temperatures reaching the low 70s Fahrenheit (22 C) near Great Slave Lake and temperatures along Mackenzie Delta shores continuing to edge up over freezing. The warm pool will then linger for another few days before shifting east over Hudson Bay through early next week, pushing temperatures between 10 to 25 degrees Fahrenheit above normal there.

By late next week, long range forecasts show another warm ridge extension through the Mackenzie Delta and melt pressure on the near-shore Beaufort re-intensifying.

Overall, with Arctic Oscillation predicted to remain neutral, melt pressure in the Arctic would tend to reduce somewhat. However, with both Bering and Okhotsk rapidly melting out and with warmth predicted to persist and intensify for those seas as well as for the Beaufort and for Hudson Bay, it appears there’s an even shot that early melt season will proceed at a more brisk than typical pace — again challenging new record lows into early May.


National Snow and Ice Data Center


Earth Nullschool

The Euro Model

The Arctic Sea Ice Blog



Warm Storms Rage Through Barents as Arctic Sea Ice Enters 13th Day of Record Low Extent

On March 4, amidst a building polar heat amplification and a strong, thousands mile long, south to north wind and storm flow across the North Atlantic and into the Arctic, sea ice extent coverage for the northern polar region plunged to new record lows.


(26 foot wave heights [left frame] and 50-60 mph sustained southerly winds [right frame] in conjunction with warm storm near the ice edge at Svalbard on March 15, 2015. Storms of this kind have been raging up through the Barents delivering powerful, warm southerly winds and immense swells to the ice edge region for at least the past half month. This strong melt pressure and warm air delivery has contributed to record low sea ice extent totals continuing for the past 13 days running. Image source: Earth Nullschool. Data source: GFS.)

Human-forced heat continued to build throughout the Arctic as warm and intensely windy storms churned northward through the Barents, bringing with them powerful swells ranging from 15 to, at times, 40 feet in height. As these great swells ground away at the ice edge, temperatures hit daily anomalies greater than 4 C above the 1979-2000 average on Sunday, March 8 for the entire Arctic region. The next day, sea ice extent, according to NSIDC, plummeted to 14,273,000 square kilometers. A value 303,000 square kilometers, or an area about the size of Arizona, smaller than the previous record low value for the date set in 2006.

Ever since March 4, the Arctic has remained in new record low territory — a period that has now lasted 13 days. Though anomalous warmth has faded somewhat — dropping today to a range of 2.65 degrees Celsius above the 1979-2000 average — sea ice has only bounced back slightly. On March 15, the NSIDC extent measure had inched up to 14,333,000 square kilometers, still about 235,000 square kilometers below the previous record low for the date.


(Arctic sea ice extent as measured by NSIDC drops below previous record low values on March 4 of 2015 [bottom dark blue line] and has remained at record low levels ever since. For reference, previous record low years for March dates include 2006 [pink line], 2007 [light blue line], and 2011 [orange line]. The top dark blue line [1979] indicates how much sea ice extent has been lost during March over the past 36 years. Image source: NSIDC.)

Over the next week, however, these new record lows are more likely to continue to fade as warm Arctic surface temperature anomalies drop to around 1-2 C above average, the Arctic Oscillation shifts toward neutral or slightly negative, and the warm storm track through the Barents is interrupted by cold winds pushing south toward Scandinavia from the pole. Although mid-week warming forecast for Alaska and Baffin Bay may retard any potential rebound somewhat.

For the past two years, Arctic sea ice has experienced a bit of a rebound during the March through early April time-frame. This has appeared to coincide with a restrengthening of the polar Jet Stream as mid latitudes have warmed which, in turn, has weakened meridional patterns transporting heat into the Arctic during winter time. Low angle sunlight entering the Arctic at this time of year has also not yet gained enough momentum to significantly push the ice to melt. So we still have about a 2-3 week window for potential bounce-back before sunlight builds and begins to apply its steady heat forcing to the greatly diminished ice.

AO index forecast

(Arctic Oscillation [AO] index forecast shows dip toward slightly negative or neutral AO status by end week after a rather extreme high in early March, with a return to mildly positive AO values by end month. Positive AO enhances edge melt of sea ice by encouraging storm formation at the ice edge and warm air invasions over the central ice. Image source: NOAA/CPC.)

That said, the ice is quite frail now, even with potential volume rebounds to mid 2000s levels. So even the slight addition of solar insolation may be enough to keep ice coverage values depressed in the neutral or moderately positive Arctic Oscillation regime that is predicted through the end of March. Extent measures maintaining near record lows along the 2006, 2007 and 2011 tracks, or just below, would establish a very low launching pad for a melt season that, lately, has tended to include precipitous declines in ice during the summer months.

The ongoing record low extent status, despite a return to weather patterns that are more favorable for rebound or maintenance, therefore, should be closely monitored.




Earth Nullschool


Climate Reanalyzer

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