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

Summer 2014 Melt Season to Ramp up in Early May Heat Wave: Fixed Jet Stream, Dual Ridges Form Sea Ice Achilles Heel

For many months the weather pattern has been essentially fixed. A ridge over China and Eastern Russia combined with warm air flows over Central Asia to amplify heat from Siberia and on into the Arctic Ocean. On the other side of the Pacific, a harmonic pattern involving warm southerly air flows over Alaska and Western Canada has also transported an inordinate amount of highly anomalous heat into the Arctic.

These warm ridges have been consistently reinforced by high amplitude Jet Stream waves. During the Winter of 2013-2014, these same atmospheric heat transport engines collapsed the polar vortex, causing melt, avalanches, and 60 degree F temperatures for Alaska in January all while pulling Arctic air down over the Eastern United States throughout the winter months.

For Alaska, Western Canada and the Eastern US, it is a general pattern that has now lasted nearly 14 months. A blocking pattern that weather historians everywhere should take note of as a general evidence of atmospheric changes resulting from human-caused warming and a validation in observation to the findings of Dr. Jennifer Francis.

Early Season Melt in the Bering Sea

This warm air flow also severely retarded sea ice formation in the Bering Sea between Alaska and far Eastern Russia throughout winter. Now, this poorly formed ice is rapidly melting out as a barrage of storms and continued warm, southerly air flows result in ongoing degradation. Recent observations show a rather extreme loss of sea ice in this region over the past 18 days:

Bering and Chukchi Seas April 10Bering and Chukchi Seas April 27

(LANCE-MODIS comparison of Bering and Chukchi Sea Ice on April 10 [left image] and April 27 [right image]. Image source: LANCE MODIS. Hat Tip to Arctic Sea Ice Forums Poster Frivolousz21.)

As we can clearly see in the two images above, both snow cover and sea ice have experienced severe losses in this region from April 10 to April 27. Warm southerly winds have continued to push ice northward enhancing melt as temperatures typically remained near or above -2 C (the temperature at which sea ice begins to melt) in most regions. Snow losses amplified warmer than freezing water flows into adjacent ocean basins, also enhancing sea ice losses as land masses continued to warm.

Heat Pulse for Bering, Chukchi, East Siberian and Beaufort Seas

Over the next six days, this general warming trend is expected to spike, bringing with it a front of much hotter than usual temperatures extending along a broad zone of the Arctic Ocean north of Canada, Alaska and East Siberia and nearly reaching the North Pole at maximum extent.

The pulse is expected to bring 18-32 F above average temperatures for this region, pushing daily highs into the mid 30s to mid 40s over the Arctic Ocean and to nearly 50 F over waters directly adjacent to the Alaskan coast. GFS model runs for May 2, 2014 show this powerful warm air invasion, indicated by the wave of green on the map below, extending well into the Arctic Ocean with extraordinarily warm temperatures in the mid-to-upper 60s over a broad swath of Central Alaska:

Arctic Heatwave Friday May 2

(GFS temperature model for May 2, 2014. Image source: University of Maine.)

Such an intense warm pulse will greatly involve the Bering, the Chukchi, the East Siberian and Beaufort Seas. It will likely most significantly impact sea ice in regions of the Bering Sea and near-shore zones of the Chukchi and Beaufort. The early season heat wave may also enhance the ice weakening process throughout the affected zone by softening the sea ice and by creating the potential for melt pond formation.

The Major Impact of Early Season Melt Pond Formation

During May and June, early melt pond formation can have a dramatic impact on sea ice melt much later in the season as the darker pools reduce ice sheet albedo serving as a kind of heat lens that bores down through the ice surface. Eventually, the melt ponds connect, forming larger and larger volumes over the ice face until the sea ice is almost completely overwhelmed. In the last phase, melt breaks down through the ice surface to contact the ocean. At this point, the sea ice is typically splintered into much smaller and disassociated fragments.

A recent paper in the journal Nature has found that a multiplication of such early season melt ponds may well be a predictive indicator of end season sea ice extent, area and volume values come September.

The paper notes:

Our simulations show that melt ponds start to form in May, a maximum extent of 18% is reached in the climatological mean at mid-July, and there are hardly any exposed ponds left by mid-August. The strong interannual variability and the positive trend are striking. Whereas in 1996, the year with the highest September ice extent since 1979, the maximum pond fraction reaches only 11%, in 2012, the year with the lowest September ice extent, up to 34% of the sea ice is covered by ponds.

Neven over at the Arctic Ice Blog recently provided an excellent assessment of the impact of melt ponds which is available here.

Massive interconnection of sea ice melt ponds

(Major expanse of dark sea ice melt ponds in the Chukchi Sea during June of 2010. Image source: The Polaris Project.)

Achilles Heel For the Arctic During the Summer of 2014

The most recent hot pulse for this region may just be the first of many as the spring and summer melt season progresses. Jet Stream patterns continue to remain fixed, delivering much hotter than normal temperatures throughout the Western Canadian, Alaskan, and East Siberian regions. Furthermore, snow cover losses for these regions are particularly well advanced further enhancing the likelihood of warm air invasions from these rapidly heating continental zones. Anomalously large and extreme early season fires may also result in a degree of albedo loss as smoke and soot is drawn northward to darken both remaining snow cover and sea ice.

As such, this zone represents a kind of sea ice Achilles heel as the 2014 melt season progresses. If we do see major losses and a progression toward record melt, it will likely come as a result of extreme weather patterns emerging from the continental zones spanning East Siberia, Alaska and Western Canada.



Arctic Sea Ice Forums

University of Maine

Global Forecast System Model

More on Melt Ponds

September Sea Ice Minimum Predicted By Sea Ice Melt Pond Fraction



Arctic Heat Wave Sets off Hottest Ever Winter-Time Temperatures, Major Melt, Disasters for Coastal and Interior Alaska

Major melt in the midst of winter. Doesn’t sound quite right, does it? We tend to think of winter as the time of freezing, as the time of ice accumulation. Not the time of melt and thaw.

Now try this — major melt in Alaska in the midst of winter. Average temperatures 40 degrees hotter than normal in the midst of winter. Rainfall over snow and ice causing avalanches, major road blockages and ice dams to rivers in the midst of winter.

In this instance we have been transported from the somewhat odd into a reality that is completely outside of our previously ‘normal’ context. In this instance we are transported to a time that may well seem like the beginning of the end of the age of ice on planet Earth.

And yet this is exactly what is happening: one of the coldest regions on the planet is experiencing melt and related record heat in January.

For the state of Alaska, the consequences are a strange and freakish winter heat wave, one that features the extreme temperatures mentioned above. For the city of Valdez, as we shall see below, the situation is far more stark.


(Massive Avalanche set off by rainfall, winter warmth, cutting off Richardson Highway to Valdez Alaska and forming a dangerous ice dam of the ironically named Keystone Canyon’s Lowe River. Image source: Alaska Department of Transportation and Public Facilities.)

Hottest ever Winter-time Temperatures for Alaska

On Sunday, a collapse event that flooded the Arctic with heat and ripped the polar vortex in half began. A freakish high amplitude ridge in the Jet Stream that had been pumping warmth over Alaska and into the Arctic for ten months running strengthened. The result was that many regions throughout the state experienced their hottest temperatures ever recorded for that day, month, or season.

Global Temperature Anomaly Reanalyzer

(Global Temperature Anomaly Data vs 1979-2000 mean with focus on Arctic for January 29. Note the extreme Arctic deviation of +5.58 degrees Celsius and the pool of 36+ F high temperature deviations still lingering over Alaska. Also note that global anomalies are +.32 C above the 1979-2000 mean which is, itself, about +.5 C above average temperatures during the 1880s, for a total of about +.82 globally. The above measure is an excellent illustration of both extreme polar amplification and very rapid warming coinciding with a strong negative Arctic Oscillation, related warm air influx, and polar vortex separation. Source: Climate Change Institute.)

According to reports from Weather Underground, Homer Alaska, for example, experienced an all time record high for the day of 55 degrees Fahrenheit, 4 degrees hotter than the previous all-time high set just a few years earlier. And Homer was just one of the many cities sitting in a broad region of extraordinary, 40 degree hotter than normal temperatures. A region extending from the interior to the southern and western coasts. Bolio Lake Range, about 100 miles south of Fairbanks in central Alaska, saw temperatures rocket to 60 degrees, just 2 degrees short of the all-time record high for any part of the state during January (the previous record high of 62 was set in Petersburg, nearly 700 miles to the south and east).

Typically colder high mountain regions also experienced record warmth for the day. A zone 10,600 feet above Fairbanks hit 32 degrees Fahrenheit on Sunday, the highest temperature ever measured for this region during any winter-time period from November through February.

Even before the most recent extreme Arctic temperature spike, January saw numerous powerful heat influxes for Alaska with Nome, Denali Park, Palmer, Homer, Alyseka, Seward, and Talkeetna each setting all-time record high temperatures during the month.

These records come on the back of a long period of rapidly increasing Alaskan heat stretching all the way back to the 1970s. In many cases, we are seeing all-time record highs broken with 5-10 year frequency. In the most extreme cases, these records fall again after only standing for 1-5 years.

Taken in this context, what we are seeing is the freakish continuation of an ongoing period of inexorable Arctic warming providing yet one more major insult to the Alaskan climate during the winter of 2013-2014.

Rain and Melt Sets off Major, Spring-like, Outflows From Streams and Rivers

The same anomalous Jet Stream pattern that has acted as a conveyer belt continuously transporting heat into the high north over Alaska has brought with it an almost endless series of rain events to coastal Alaska. Storm after storm, fueled by heat and high rates of evaporation over the northern Pacific, slammed into the Alaskan coastline, disgorging record levels of precipitation.

With temperatures freakishly high, mirroring conditions typically present during late spring or early summer, much of this precipitation fell in the form of rain. Valdez, Alaska, for example, has likely experienced its wettest January ever with rainfall measures just 1.35 inches short of the record on Sunday and a series of strong storms rushing into the city on Monday and Tuesday. Given the nearly endless train of storms lining up to sweep over Valdez, it is possible that its previous record of 15.18 inches for January could easily be surpassed by an inch or two at month-end.

The storms and cloudiness make it difficult to peer down and get a good view of what all this heat and rainfall is doing to the Alaskan snow and ice pack. But, for brief respite, on January 25th, just ahead of the most recent influx of rain and warmth, the clouds cleared, revealing the land and sea surface. And what we witness is extraordinary:

Alaska Melt Rain Sediment January 25

(Southern Coast of Alaska with major sediment outflow from snow and ice melt, record heat and rainfall in January 2014. Image source: Lance-Modis)

The entire southern coast of Alaska from Prince William Sound to Cook Inlet are visibly experiencing major snow and ice melt along with flooded streams and rivers flushing out a massive volume of sediment into the Gulf Alaska. Clearly visible in the satellite shot, the sediment now streaming into the ocean is more reminiscent of a major late spring flood event than anything that should be ongoing for Alaska in the midst of winter.

Yet here we are. A situation of continuous, never-before seen heat for Alaska during winter time bringing on a flooding thaw that is far, far too early.

Rainfall over Glaciers, Snow Pack Triggers Massive Avalanche that Cuts off Valdez

The constant assault of heat and record temperatures combined with an almost endless flow of moisture riding up from the Gulf of Alaska set off a devastating and freakish event near Valdez on Saturday. Severe and record rainfall over the mountain regions have continuously softened glacial ice and snow packs above this major Alaskan city. On Monday, the continuous insults of heat and water passed a critical threshold.

As the warm water filtered down through the colder snow and ice, the anchoring base was lubricated even as the capping snow grew heavily burdened with water. Eventually, the insults of heat and rainfall became too great and a major snow and ice slope system above the main road linking Valdez to mainland Alaska collapsed. The immense volume of snow and ice unleashed, spilling down to fill the base of Keystone Canyon, blocking both the Lowe River and the Richardson Highway running through it.

This snow and ice dam rose as high as 100 feet above the Canyon floor, causing the Lowe River to rapidly flood, inundating the already snow-and ice buried road under an expanding pool 20 to 25 feet deep and filled with ice-choked water.

You can see the massive avalanche-created ice dam and related road inundation in the video provided by akiwiguy below:

(video source: akiwiguy)

Warming-related rainfall events of the kind that has now cut Valdez off from the mainland are just one of the extraordinarily dangerous consequences of human-caused climate change. They are a phenomena linked to the massive glacial outburst flood that killed thousands in India this year together with other dangerous snow and ice melt events. Should such major heating and rainfall events impact Greenland and West Antarctica, the consequences could be even more extreme than what we are currently witnessing in Alaska.

Conditions in Context

In the context of our present extreme Jet Stream pattern that is setting off warmest-ever conditions for Alaska during January together with dangerous melt-outburst related events while at the same time periodically flushing Arctic air and extreme winter weather south into the United States, it is important to remember a few things. The first is that the Arctic is now experiencing never-before observed warmth with stunning frequency. Scientific papers now show that the Arctic is hotter than it has been for at least 44,000 years and possibly 120,000 years.

By comparison, the cold snaps, that could very well be seen as the death gasps of the Arctic we know, impacting the eastern US are relatively minor when put into this larger, more ominous context. Similar cold events were last seen about 20 years ago in the US. And so there is simply no comparison that can generate a rational equivalency between the, hottest in an age, Arctic temperatures and the, coldest in a few handfuls of years, temperatures in the Eastern US.

And if you’re one of those sensitive, perceptive souls who feels that the weather events you’re seeing, the extreme swings from very hot to somewhat cool temperatures, the extreme swings from drought to record rainfall, and the extreme events now accelerating the melting of the world’s ice and snow, are freakish, strange, and terrifyingly abnormal, then you are absolutely correct. Don’t let anyone, be they friends or family, or journalists in the media, tell you otherwise. There is reason for your discomfort and there is very serious cause for concern.


Colorado Bob’s Climate Feed

Weather Underground

NASA: Lance-Modis

Alaska Department of Transportation and Public Facilities

Climate Change Institute

Alaska All Time High For This Date, Warmer than Alabama

The Glacial Megaflood

Arctic Experiencing Hottest Temperatures in at Least 44,000 Years

Arctic Heat Wave to Rip Polar Vortex in Half


Massive Wildfires Follow Record-Shattering Heat-Wave in Alaska

Alaskan Wildfires

(Large fires in Alaska. Image source: Lance-Modis)

A week after a record heatwave set off highest ever temperatures in Alaska, massive forest fires are blanketing vast areas of wilderness.

More than 80 fires are now raging across the state. The largest include the Lime Hills Fire at 154,000 acres and the Moore Creek Fire at 126,00o acres. In total, nearly 400,000 acres have burned so far this summer. For reference, an average full fire season in the US results in around 3 million acres burned. So the 400,000 acres for Alaska alone represents an abnormally large area burned, especially so early in the fire season and for a region at or above the Arctic Circle.

Like Colorado, where blazes resulted in record damage during June, the largest of the Alaskan fires, Lime Hills, currently threatens a local community. As of Tuesday, the fire had moved to within a half mile of the town which is located on the upper Stoney River just west of Fairbanks. About 70 firefighters are working to ensure no structures are taken by the blaze.

Though not as hot as last week, temperatures still remain in the range of record heat for interior Alaska with some regions Tuesday showing temperatures near 80 degrees (Fahrenheit). Daily record highs for this area range in the high 70s for this time of year. So record-breaking temperatures have become a day-to-day event for this Arctic region.

Fires in Alaska are a direct result of the extreme record high temperatures there. And these temperatures are also linked to a long-period warming trend caused by human-spurred global warming. Increasing heat, dryness and wildfires in vulnerable regions are just one result of the climate change caused by an excessive and continuous burning of fossil fuels. May of 2013 was the 3rd hottest on record, according to NOAA’s National Climate Data Center. Overall, temperatures are about .8 degrees Celsius above temperatures when climate records started in the 1880s. This difference is equivalent to that caused by the Little Ice Age, but on the side of hot.

Also in May, global atmospheric CO2 levels hit a record 400 parts per million. This level of Greenhouse gas is enough to raise Earth’s temperatures another 2-3 degrees Celsius long-term or about half the difference between now and the last Ice Age, but also on the side of hot. Long term results of 400 ppm CO2 also include a 75 foot rise in sea level. Unfortunately, due to a failure by the world’s leaders to enact appropriate CO2 reduction policies, CO2 levels are set to rise to around 550 parts per million by mid-century, enough to bake in a total temperature increase of around 7 degrees Celsius long-term. A virtual fire age.

Between now and then, and without proper policy measures aimed at reducing the damage, we can expect gradual but continually increasing global temperatures with increasing instances of extreme weather events.

The current Arctic heatwave is just one example of the strange climate we are creating. Let us hope that policy makers have gotten the message. We need to get to work before we set off even more dangerous events.


Crews Battle Wildfires Across Alaska

US Wildfire Data

Heat Wave Sends Temperatures in Alaska to 94 Degrees

Unprecedented West Fork Fires Explode to 60,000 Acres

What Does a World at 400 PPM CO2 Look Like?

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