A new month is upon us and Christmas is coming! Here’s another look at Lars Kaleschke’s high resolution AMSR2 area and extent graphs for the Arctic as a whole:
Extent increase stalled for the last few days of November, and as a result extent is now in a “statistical tie” with 2017 for 4th lowest extent for the date in the AMSR2 record.
Continue reading Facts About the Arctic in December 2022A change is allegedly as good as a rest, so here’s an alternative view of high resolution AMSR2 area and extent created using the experimental tools provided by the AWI’s Lars Kaleschke at: https://sites.google.com/view/sea-ice/
After a brief pause mid-month the refreeze has accelerated again. Both metrics are in the upper half of the decadal range, with extent this year just above 2021 and area just below last year.
Next let’s take a look at sea ice concentration at the end of October:
The 2022/23 freezing season has begun, so to begin with here are Arctic sea ice area and extent during its early stages:
Both metrics are currently tracking 2021 quite closely.
Here too is an AMSR2 animation of the transition from melting to freezing in the Central Arctic. Click to animate, and be warned that the file size is almost 10 Mb:
Another big storm is heading for the Chukchi Sea. The GFS forecast currently shows a sub 960 hPa low developing on Thursday:
Continue reading Facts About the Arctic in October 2022As in previous years there is already a thread devoted to this year’s minimum extent. By way of a summary here are the end of August numbers for our favourite “high resolution” AMSR2 area and extent metrics:
Extent is currently near the top of the range of the last 10 years.
We have now reached the stage of the “melting season” when “refreezing” has started in the Central Arctic but melting at the periphery is outpacing it. However the Canadian Ice Service stage of development charts now show the arrival of new ice in the high latitudes of the Canadian Arctic Archipelago:
After a long hiatus courtesy of the demise of the annual Barneo ice camp and the Covid-19 pandemic we are pleased to be able to report that an ice mass balance buoy has once again been installed on a floe in the vicinity of the North Pole. Here’s the evidence:
The ship in the background is not a traditional research icebreaker. It is Ponant Cruises’ Le Commandant Charcot, one of a number of new ice hardened cruise ships voyaging across the Arctic Ocean and adjacent seas. Le Commandant Charcot reached 90N on July 13th:
After a relatively rapid decline at the beginning of June Arctic sea extent is now very close to the 2010s average:
Both 2020 and 2021 began relatively rapid declines of their own at the beginning of July, so it will be interesting to see if 2022 follows suit.
Most of the fast ice off Utqiaġvik has recently disappeared:
Meanwhile further out into the Chukchi Sea the sea ice looks to be in poor shape at the moment, with surface melting apparent across the entire region:
Continue reading Facts About the Arctic in July 2022By way of a change we’ll start the month of May with a closer look at one of the ice mass balance buoys deployed in the Beaufort Sea last Autumn. IMB buoy 569620 was deployed at 78.5 N, 147.0 W on September 3rd 2021, and since then it has drifted to 81.0 N, 147.7 W. Here is the buoy’s record of atmospheric conditions above the ice floe it’s embedded in since then:
Here too is the buoy’s record of the temperature of the ice floe itself, as well as the thickness of the ice and the snow layer covering it:
There’s a few things to note at first glance. The ice floe continued to decrease in thickness into November. It’s thickness then started to increase, but is currently still less than 2 meters. Also the snow depth has gradually been increasing, and (apart from some data glitches!) is now ~38 cm. Finally, for the moment at least, the ice surface temperature has been slowly warming since mid February and is now ~-11 °C.
Returning to more familiar territory, high resolution AMSR2 Arctic sea ice area has taken a bit of a tumble recently:
followed less steeply by extent:
Not unexpectedly, the Pacific periphery is currently leading the decline:
The Rutgers Snow Lab has updated its northern hemisphere snow cover bar chart for April 2022:
The May edition of the NSIDC’s Arctic Sea Ice News has also just been published. It summarises April 2022 as follows:
Average Arctic sea ice extent for April 2022 was 14.06 million square kilometers (5.43 million square miles). This was 630,000 square kilometers (243,000 square miles) below the 1981 to 2010 average and ranked eleventh lowest in the 44-year satellite record.
Extent declined slowly through the beginning of the month, with only 87,000 square kilometers (33,600 square miles) of ice loss between April 1 and April 10. The decline then proceeded at an average pace for this time of year through the reminder of the month.
During April, temperatures at the 925 mb level (about 2,500 feet above the surface) over the Arctic Ocean were above average. Most areas were 2 to 3 degrees Celsius (4 to 5 degrees Fahrenheit) above average, but in the Beaufort Sea, April temperatures were up to 5 to 6 degrees Celsius (9 to 11 degrees Fahrenheit) above average:
This was accompanied by a strong Beaufort High pressure cell through the month:
The NSIDC’s update also refers to the Chukchi Sea polynya we’ve been keeping an eye on here:
Strong offshore winds over the northwest coast of Alaska led to openings in the ice cover, called polynyas. The first pulse of winds began on March 21. At that time, surface air temperatures were still well below freezing, and the water in the coastal polynya quickly refroze. By April 9, the offshore push of the ice ceased and the polynya iced over completely.
However, starting on April 12, a second round of offshore wind pushed the ice away from the coast, initiating another polynya. Refreezing began anew in the open water areas, but the ice growth was noticeably slower, reflecting the higher surface air temperatures by the end of the month
The NSIDC also updated their graph of sea ice age, on this occasion for the week of March 12th to 18th over the years:
Arctic sea ice news concludes with brief news of the recent death of Canadian Arctic scientist David Barber. CBC News’s obituary for David provides more details:
Family and friends are mourning the loss of the visionary Arctic researcher and University of Manitoba professor David Barber.
Barber, who was a distinguished professor, the founding director of the Centre for Earth Observation Science and associate dean of research in the faculty of environment, earth and resource, passed away on Friday after suffering complications from cardiac arrest.
Barber, 61, is survived by his wife Lucette, three children and two grandchildren.
The waters of the Mackenzie River are starting to spread over the fast ice off the delta:
The Polar Science Center at the University of Washington has released the PIOMAS volume data for April 2022:
Average Arctic sea ice volume in April 2022 was 23,000 km3. This value is the 9th lowest on record for April, about 2,300 km3 above the record set in 2017. Monthly ice volume was 30% below the maximum in 1979 and 15% below the mean value for 1979-2021. Average April 2022 ice volume was 1.45 standard deviations above the 1979-2021 trend line.
The daily volume numbers reveal the PIOMAS maximum volume for 2022 to be 23,225 km3 on April 26th.
The PSC report continues:
Ice growth anomalies for April 2022 continued to be at the upper end of the most recent decade with a mean ice thickness (above 15 cm thickness) at the middle of recent values.
The ice thickness anomaly map for April 2022 relative to 2011-2020 divides the Arctic in two halves with positive anomalies in the “Western Arctic” but negative anomalies in “Eastern Arctic”. A narrow band of negative anomalies remains along the coast of North Greenland but a positive anomaly exists north of Baffin Island.
Note that the “positive anomaly north of Baffin Island” referred to is not apparent in the CryoSat 2 ice thickness anomaly map, although there is agreement about the thicker ice in the eastern Beaufort Sea:
CryoSat-2 thickness maps stopped for the Summer in mid April. I’ve been hoping for mid May data from the PIOMAS team, but in vain so far. In its continuing absence here is a “work in progress” PIOMAS thickness map for the end of April:
The sea ice in Chaunskaya Bay and along the adjacent coast of the East Siberian Sea is starting to look distinctly damp:
That’s not too surprising when you also look at recent temperatures in Pevek, which have been approaching all time highs for the date:
P.S. The Mackenzie River has reappeared from under the clouds and is now largely liquid:
Some surface melt is now visible on the fast ice at Utqiaġvik:
No doubt the recent above zero temperatures are responsible, but the forecast is for colder conditions to return:
Discussion continues on the new open thread for June 2022.
The April edition of the NSIDC’s Arctic Sea Ice News summarises March 2022 as follows:
Average Arctic sea ice extent for March 2022 was 14.59 million square kilometers (5.63 million square miles), ranking ninth lowest in the satellite record…
The total decline, after a series of small ups and downs, was only 250,000 square kilometers (96,500 square miles):
Counter to what might be expected given the very slow rate of sea ice loss over the month as a whole, air temperatures at the 925 millibar level (about 2,500 feet above the surface) were above average over all of the Arctic Ocean:
March temperatures were up to 9 degrees Celsius (16 degrees Fahrenheit) higher than average north of the Canadian Arctic Archipelago, up to 6 degrees Celsius (11 degrees Fahrenheit) above average in the East Siberian Sea, but up to 5 degrees Celsius (9 degrees Fahrenheit) above average over a wide area.
The key features of the sea level pressure pattern were high pressure (an anticyclone) over the central Arctic Ocean, a trough of low pressure extending into the Barents Sea, and an unusually high pressure over Northern Europe:
While having an anticyclone over the central Arctic Ocean is quite typical for this time of year, the combination of the high pressure over northern Europe and the pressure trough to the west led to a strong pressure gradient, leading to strong winds from south through the Norwegian and Barents Seas…
This can be tied to the extreme warm event over the Arctic Ocean seen in the middle of the month, associated with strong water vapor transport and the passage of several strong cyclones.
The Polar Science Center at the University of Washington has also released the PIOMAS volume data for March 2022:
Average Arctic sea ice volume in March 2022 was 21,700 km3. This value is the 6th lowest on record for March, about 2,200 km3 above the record set in 2017. Monthly ice volume was 38% below the maximum in 1979 and 25% below the mean value for 1979-2021:
Ice growth anomalies for March 2022 continued to be at the upper end of the most recent decade with a mean ice thickness (above 15 cm thickness) at the middle of recent values:
The ice thickness anomaly map for March 2022 relative to 2011-2020 divides the Arctic in two halves with positive anomalies in the “Western Arctic” but negative anomalies in “Eastern Arctic”. A narrow band of negative anomalies remains along the coast of North of Greenland but positive anomaly exists north of Baffin Island.
CryoSat 2 ice thickness shows an similar pattern of sea ice thickness anomalies though the areas North of Greenland and Baffin Bay show substantial differences:
Here are the latest graphs of our favourite “high resolution” AMSR2 metrics, which combine recent data from the Alfred Wegener Institute with historical data from the University of Hamburg:
As you can see, there have indeed been a few ups and downs! Click the image below to see a 10 Mb animation of ice motion over the last few weeks:
The obvious point to note at the moment is that there are currently long flaw leads on both the Siberian and Canadian sides of the Arctic Ocean. The animation also reveals episodes of open water in the Beaufort and Chukchi Seas, as well as north of Franz Josef Land and Svalbard.
The ice in those areas is still very thin on the latest AWI CryoSat-2/SMOS sea ice thickness map:
Here too is the latest AWI CryoSat-2/SMOS volume graph:
The reanalysed data is now showing something of a surge towards the end of February.
[Edit – April 23rd]Here’s the last “near real time” AWI CryoSat-2/SMOS Arctic sea ice thickness map for Spring 2022:
The significantly thinner areas in the Beaufort and Chukchi Seas are even more pronounced than previously. Here also is the associated CS2/SMOS volume graph:
The 2022 maximum volume based on NRT data is 19719 km³ on April 5th. Expect that to be revised upwards when the reanalysed data is ultimately published.
Going back to 2 dimensions, the assorted “ups and downs” now seem to have resolved into the melting season proper:
The peripheral sea have been responsible for most of the recent decline:
However as mentioned above, the Chukchi Sea has been experiencing some ups and downs of its own. Perhaps the sun is now high enough in the sky for the most recent “down” to stick around for the summer?
Over the last couple of days some open water has appeared in the Beaufort Sea off the Mackenzie Delta:
Especially for Taylor, here’s the GFS Arctic snow depth forecast for 10 days into the future:
See in particular the Beaufort and Chukchi areas.
Please also see the new open thread for May 2022
For detailed analysis of Arctic sea ice extent over the next few weeks please see the 2022 maximum extent thread. However to get the new open thread going here is the current JAXA/ViSHOP extent graph:
It’s looking more and more as though the real maximum for 2022 occurred close the false peak on February 23rd.
Arctic sea ice volume will keep increasing for a while longer. Here is the current AWI CryoSat-2/SMOS volume graph:
The recent “flat line” in extent is in part due to recent events on the Pacific periphery of the Arctic. Take a look at this animation of AMSR2 sea ice concentration:
The gap varies depending on how the wind blows, but there is still evidence of open water (or very thin ice) along the shore of the Beaufort and Chukchi Seas. Here’s the Mackenzie Delta and the adjacent Beaufort Sea on March 5th:
Continue reading Facts About the Arctic in March 2022Christmas is coming. Santa’s secret summer swimming pool has frozen over. The time has come for a new monthly Arctic update.
The JAXA/ADS/ViSHOP web site is undergoing maintenance for a week, so let’s start the festive season with a look at high resolution AMSR2 area and extent:
After a brief hiatus in early November both metrics are once again tracking within, but near the upper bound of the last 10 years.
Next let’s take a look at the latest AWI CryoSat-2/SMOS thickness map:
together with the anomaly map from the Finnish Meteorological Institute:
Still thinner than usual in the so called “last ice area” north of Greenland and Ellesmere Island, and thicker than usual on the Siberian side of the Arctic, particularly in the Chukchi Sea.
Finally, for the moment at least, here’s the latest CryoSat-2/SMOS volume graph:
Unlike the previous metrics, this particular one is close to the middle of the pack.
[Edit – December 5th]The National Snow and Ice Data Center issued their latest monthly Arctic Sea Ice News update earlier than usual this month:
Sea ice extent increased at a faster than average pace through November and by the end of the month, extent was just within the interdecile range. Extent was above average in the Bering Sea, but Hudson Bay remained unusually ice free through the month.
The November 2021 monthly average extent was 9.77 million square kilometers (3.77 million square miles), which ranked tenth lowest in the satellite record. The 2021 extent was 930,000 million square kilometers (359,000 million square miles) below the 1981 to 2010 long-term average. Extent was higher than average in the Bering Sea, but is extremely low in Hudson Bay.
Air temperatures at the 925 millibar level (about 2,500 feet above the surface) were well above average north of the Canadian Archipelago, by as much as 6 degrees Celsius. Conversely, temperatures over southwest Alaska and the eastern sector of the Bering Sea were as much as 6 degrees Celsius below average:
The sea level pressure pattern for November featured widespread low pressure over the Atlantic side of the Arctic and extending into the Barents and Kara Seas, paired with a moderately strong Beaufort Sea High. Strong low pressure over the Gulf of Alaska resulted in a circulation pattern in the eastern Bering Sea that brought cold air from the north. This pattern was favorable for sea ice growth, and can explain the above average ice extent in the region:
Since the start of December high resolution AMSR2 extent has been flatlining:
Sea ice area has even declined slightly over the past few days:
Here too is an animation created by Uniquorn on the Arctic Sea Ice Forum using AWI ASMR2 data to reveal ice movement through the Nares Strait during December:
The JAXA/ADS/ViSHOP web site is down again, so let’s take another look at high resolution AMSR2 area and extent:
It seems that the “brief hiatus” is over, and extent is now in a “statistical tie” with 2018/19 at 4th lowest for the date amongst recent year.
[Edit – December 13th]The PIOMAS Arctic sea ice volume data for November 2021 has been released:
Average Arctic sea ice volume in November 2021 was 7,830 km3. This value is the 7th lowest on record for November, about 1600 km3 above the record set in 2016. Monthly ice volume was 61% below the maximum in 1979 and 45% below the mean value for 1979-2020. Average November 2021 ice volume was about one sigma above the 1979-2020 trend line. October saw relative rapid ice growth for recent years bringing the mean ice thickness (above 15 cm thickness) above the recent low values:
The ice thickness anomaly map for November 2021 relative to 2011-2020 continues to show anomalies divided into positive and a negative halves with areas of positive anomalies increasing since the two prior months. Negative anomalies stretching from North of Greenland and along the Canadian Archipelago across the Eastern Arctic into the Barents Sea. Areas North of Greenland again feature very low ice thickness as in prior years (see our recent paper). Positive anomalies are notable in the Beaufort and Chukchi seas due to advection of thicker older ice into the areas during the previous winter (See recent paper on this). The Alaskan summer has also been relatively cold contributing to unusually thick ice in this area:
CryoSat-2 ice thickness shows a similar picture sea ice thickness anomalies but with the maxima slightly displaced which maybe due to temporal sampling of the composite:
The JAXA web site is still down, so here’s another set of high resolution AMSR2 graphs:
NOAA have just released their 2021 Arctic Report Card. Here’s the introductory video:
and here is the report itself:
Ice hardened LNG tanker Vladimir Vize is about to enter the Vilkitsky Strait on the Northern Sea Route:
Meanwhile Science.org reports that “The Arctic is warming four times faster than the rest of the world“:
[Edit – December 23rd]“Everybody knows [the Arctic] is a canary when it comes to climate change,” says Peter Jacobs, a climate scientist at NASA’s Goddard Space Flight Center, who presented the work on 13 December at a meeting of the American Geophysical Union. “Yet we’re misreporting it by a factor of two. Which is just bananas.”
Jacob’s co-authors include researchers who oversee several influential global temperature records, and they noted the faster Arctic warming as they prepared to release the global temperature average for 2020. NASA’s internal peer reviewer challenged the higher figure, suggesting the scientific literature didn’t support it. But the researchers have found the four times ratio holds in record sets from both NASA (3.9) and the United Kingdom’s Met Office (4.1), and they hope to soon include the Berkeley Earth record. (Their work also has company: In July, a team at the Finnish Meteorological Institute posted a preprint also arguing for the four times figure.)
The researchers found Arctic warming has been underestimated for a couple of reasons. One is climate scientists’ tendency to chop each hemisphere into thirds and label the area above 60°N as the “Arctic”—an area that would include, for example, most of Scandinavia. But the true definition of the Arctic is defined by Earth’s tilt. And, as has been known for centuries, the Arctic Circle is a line starting at 66.6°N. When researchers lump in the lower latitudes, “you’re diluting the amount of Arctic warming you’re getting,” Jacobs says. “That is not a trivial thing.”
The other difference is the choice of time periods over which the warming rate is calculated. Jacobs and his colleagues focused on the past 30 years, when a linear warming trend emerged for the Arctic. Analyses that look at longer term trends see less divergence between the Arctic and the world.
Here is the latest CryoSat-2/SMOS volume graph, now including some reanalysed data which seems to have come in slightly higher than the earlier “near real time” numbers:
Plus the AWI thickness map:
Further discussion of the divergence between volume and extent continues in the new New Year 2022 thread: