At the beginning of July JAXA/ViSHOP Arctic sea ice extent is still “lowest for the date” in their record going back to 1979:
The PIOMAS sea ice thickness map for June 30th reveals that the previously thick ice in the Chukchi Sea has been noticeably thinning:
The associated volume graph shows that the 2025 curve has entered the pack of other recent years. and is now 4th lowest for the date:
Continue reading Facts About the Arctic in July 2025By way of a change, which is allegedly as good as a rest, let’s start the new month with a very pretty and almost cloud free “pseudo-colour” image of the Lena Delta and adjacent areas of the Laptev Sea:
Laptev sea ice area decline has been in high gear recently:
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 20222021 has been and gone, so first of all may I wish all our readers a very Happy New Year.
Sadly it’s not been a happy start to 2022 for the inhabitants of Boulder, Colorado, home of the National Snow and Ice Data Center. According to the Denver Post:
The Marshall fire destroyed an estimated 991 homes in Boulder County, damaged 127 more and may have killed three people, Sheriff Joe Pelle said Saturday afternoon.
Pelle added that the cause of the fire — the most damaging in Colorado history — remains under investigation, and confirmed that sheriff’s officials have served a search warrant on at least one property based on a tip.
Currently, two people are missing in Superior and another is missing in the Marshall area, Pelle said. All three are feared dead as each of their homes was lost to the fire, the sheriff said…
So far, officials say Thursday’s wildfire — exacerbated by 100-mph winds — burned more than 6,000 acres across Boulder County.
The fire destroyed 553 homes in Louisville, damaging 45, Pelle said Saturday. It also destroyed 332 homes in Superior, damaging 60 in that town, and destroyed 106 homes in unincorporated Boulder County, damaging 22…
Officials first thought downed power lines sparked the fire, but have been unable to confirm its origin. The abnormally dry conditions led to what is now the most destructive wildfire in Colorado history.
Moving north to examine snow and ice data from the Arctic, let’s start 2022 in traditional fashion with a look at high resolution AMSR2 area and extent:
Both metrics are now near the upper boundary of the last 10 years’ range. The AMSR2 instrument wasn’t launched into orbit until summer 2012, but according to both JAXA and NSIDC data extent on January 1st 2022 is almost identical to the same date in 2012. Regular readers will recall that year went on to produce the lowest annual minimum extent in the satellite era despite recording the highest annual maximum in the decade of the 2010s:
Note that sea ice volume tells a rather different story. Here’s the latest AWI CryoSat-2/SMOS volume graph:
The current near real time data is likely to be revised upwards slightly when the final reanalysis is complete, but even so volume seems likely to remain in the lower half of the recent range at the end of 2021.
Here too is the AWI Arctic sea ice thickness map:
together with the thickness anomaly map from the Finnish Meteorological Institute:
Once again the ice in the so called “last ice area” north of Greenland and Ellesmere Island is thinner than usual, as is the ice in the Fram Strait and East Greenland Sea.
[Edit – January 11th]As has been pointed out below, the Polar Science Center has now released the PIOMAS volume data for December 2021:
Average Arctic sea ice volume in December 2021 was 13,300 km3. This value is the 9th lowest on record for December, about 2100 km3 above the record set in 2016. Monthly ice volume was 51% below the maximum in 1979 and 37% below the mean value for 1979-2020. Average December 2021 ice volume was 1.2 standard deviations above the 1979-2020 trend line.
November and December of 2021 saw relative rapid ice growth for recent years, bringing the mean ice thickness (above 15 cm thickness) towards the thicker end of the recent values.
The ice thickness anomaly map for December 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 and stretching from the Beaufort, over the pole and into the Barents. Negative anomalies stretching from Fram Strait, North of Greenland and along the Canadian Archipelago. Areas North of Greenland again feature low ice thickness as in prior years.
Note that as revealed by this animation from NASA Worldview the sea ice in the Lincoln Sea is currently still breaking up and being exported from the Central Arctic via the Nares Strait:
The Atlantic side of the Arctic Ocean has been taking a bit of a battering from what I shall henceforth refer to as the Great Arctic Winter Cyclone of 2022, or GAWC 2022 for short. Unless there’s an even deeper one later in the year of course!
According to the Canadian Meteorological Centre the storm achieved a minimum Mean Sea Level Pressure of 937 hPa at 12 noon UTC yesterday:
Here are the visible effects of the storm on the sea ice in the area so far, now updated to January 25th:
Watch this space!
In my humble opinion summer in the Arctic summer starts on June 1st, so let’s check the current sea ice situation in the once frozen North. For details of the preconditioning of the ice during the Arctic spring see “Melt Pond May“, where I concluded that:
Compared with 2016 at the same time of year I am compelled to say that with June 1st just around the corner the 2019 summer melting season is primed to progress more quickly.
Currently extent is significantly below 2012, albeit somewhat above 2016 at the same time of year. And what of melt ponds? In 2012 there was evidence of less snow cover over land and more surface water on the ice on the Siberian side of the Arctic. Other than that Arctic sea ice in 2019 looks to be in worse shape than in 2012.
And how have things progressed over the last few days? Take a look at this:
Our “Arctic Basin” metric encompasses the Central Arctic plus the Beaufort, Chukchi, East Siberian and Laptev Seas. It is currently headed into uncharted waters. The effect on overall Arctic sea ice extent is also readily visible:
This year both the CPOM version of CryoSat-2 thickness and the University of Bremen’s SMOS thickness maps are continuing to be published during the melting season:
Take them with a large pinch of salt at this time of year!
Finally, for the moment at least, liquid water is starting to seep out of the Lena Delta:
For comparison purposes please also take a look at the same date in 2016:
and the previous date in 2012:
A significant area of the Laptev Sea ice is now turning a much darker shade of blue using the band 7-2-1 false colour combination:
In addition the DMI >80N temperature metric has reached the zero Celsius line well ahead of schedule:
The May PIOMAS numbers have been released! Here is the Wipneus generated state of play on May 31st:
and here is the all too familar multi-year graph:
As reported in this year’s Northwest Passage article:
Any early bird traversing the Northwest Passage from west to east could now sail through open water around Point Barrow, along the Alaskan and Canadian coast and into the Amundsen Gulf:
Arctic Basin sea ice extent is still descending through uncharted territory:
and Basin area currently looks poised to follow suit:
There’s a beautifully clear view of the Siberian coast today, with vast areas of melt ponds visible on VIIRS false colour:
The Arctic Basin area has indeed taken a nosedive into uncharted territory:
By way of comparison sea ice area on the Atlantic periphery is in amongst the recent pack, thanks to the almost continual drift in that direction over last winter:
High resolution AMSR2 extent has been in a “statistical tie” with 2016 for a few days:
However the NSIDC’s 5 day average extent has reached a clear new low for the date, in the satellite record at least:
Especially for AJBT, here’s the Slater Probabilistic Ice Extent prediction for August 3rd:
and here’s the current DMI >80N temperature graph:
Finally, for the moment at least, there is not very much fast ice left at Utqiaġvik:
The sea ice in the Laptev Sea is starting to break up:
As is the fast ice in the Beaufort Sea:
Meanwhile the MSLP of the cyclone currently spinning over Severnaya Zemlya was down to 976 hPa at 06:00 UTC this morning:
An early morning image from the Utqiaġvik webcam:
Especially for Mateo (see below) here’s the current high resolution Arctic Basin sea ice area:
and extent:
Note that the recent cyclones have caused a temporary jump in sea ice extent, but not in area.
The Lincoln Sea has turned noticeably bluer on MODIS bands 7-2-1 false colour:
The sea ice off the Lena Delta has started to collapse:
Meanwhile the clear water off Point Barrow is opening up further:
Finally, for the moment at least, here is the current view from the Utqiaġvik (Barrow as was) sea ice webcam:
P.S. The mid month PIOMAS numbers have been released, and Wipneus has worked his usual magic:
2019 sea ice volume is currently in a “statistical tie” with 2012, in 2nd place behind 2017:
The fast ice in the Vilkitsky Strait has started to break up:
Sea Ice area along the Northern Sea Route is currently the lowest for the date in the AMSR2 ere:
In addition the June 2019 Sea Ice Prediction Network report has been released. Here’s the summary:
Again, as in previous years, the spread in the dynamical models are larger compared with statistical models. Overall, the heuristic method has the lowest projected September sea-ice extent value with a median at 4.09 million square kilometers, and the dynamical models have the highest number with the median at 4.56 million square kilometers.
Arctic wide sea ice area is now lowest for the date in the high resolution AMSR2 record, although extent has yet to follow suit:
If you exclude the peripheral seas, which are all largely ice free by mid September in this day and age, the picture is extremely stark:
A brief glimpse through the clouds reveals that the North Pole is now starting to feel the recent heat:
Arctic wide sea ice extent is now lowest for the date in the high resolution AMSR2 record:
Here’s Arctic wide sea ice area, which is still well below the rest of the pack:
As the end of the month draws near let’s take a look at sea ice area along a couple of the famous sea routes above the Arctic Circle. First of all here’s the Northern Sea Route, comprising the Kara, Laptev, East Siberian and Chukchi Seas:
Next here’s the Northwest Passage, comprising the Chukchi and Beaufort Seas plus the channels of the Canadian Arctic Archipelago and Baffin Bay:
For completeness here too are the current Arctic wide area and extent numbers:
Watch this space!
Wipneus has recently updated the mid month PIOMAS gridded thickness map, which looks like this:
The accompanying PIOMAS volume graph currently shows 2019 in seventh place:
We now have a new thickness metric to peruse each month. Here’s the gridded merged CryoSat-2/SMOS thickness data from the Finnish Meteorological Institute:
Since the FMI make the gridded data available as well as that visualisation, here’s a closer look at the Bering/Chukchi area:
There’s an awful lot of thin ice in the region ripe for rapid melting now that the sun is shining down for a rapidly increasing number of hours per day. Over on the other side of the North Pole there’s also some significant swell forecast to hit the Atlantic edge of the Arctic ice pack. Here’s the current WaveWatch III forecast for 09:00 UTC tomorrow morning:
Finally, for the moment at least, here are the current Arctic wide high resolution AMSR2 sea ice area and extent graphs:
This Sentinel 1 SAR image of the Lincoln Sea from PolarView suggests that the northern arch of the Nares Strait is breaking up once again:
It is therefore conceivable that sea ice in the Lincoln Sea will continue to break up and flow south through the Nares Strait for the entire 2018/2019 winter.
Bering Sea ice area has “rebounded” over the last few days:
and taken the Arctic wide metrics with it:
Here’s the latest Sentinel 1 SAR image of the Lincoln Sea and northern Nares Strait:
The “rebound” has reversed:
With temperatures above freezing point across the Bering and Chukchi Sea forecast for tomorrow morning expect the decline in Arctic sea ice extent to accelerate:
There was a 162k decline in high resolution extent yesterday:
Here also is the current state of the thick sea ice exiting the Lincoln Sea via the Nares Strait:
Here’s another week’s merged CryoSat-2/SMOS thickness data from the Finnish Meteorological Institute:
We’re still waiting for Wipneus’ Raspberry Pi to crunch the high resolution AMSR2 numbers, but here’s the latest from JAXA:
2019 currently in 3rd place by a whisker.
P.S. The high resolution AMSR2 numbers are out:
Area is certainly lowest for the date in the AMSR2 era. Extent will almost certainly achieve that status tomorrow. Excluding the two most peripheral seas reveals perhaps an even more worrying picture?
Arctic sea ice coverage is now firmly in the “lowest extent for the date in the satellite record” category, whichever metric you care to choose:
The NSIDC 5 day average is in a “statistical tie” for first place with 2017:
Our regular reader(s) may recall our extended coverage on the plucky little yacht Northabout‘s ultimately successful attempt to circumnavigate the Arctic Ocean in the summer of 2016?
Many were the skeptics who said she stood no chance of finding a way through some “thick sea ice” apparently blocking her path across the Laptev Sea, but they were proved wrong:
As a thought experiment in the summer of 2018 we’re now thinking the unthinkable. If she put her mind to it could Northabout circumnavigate Greenland in 2018? Let’s take a look at the evidence shall we? The allegedly “oldest, thickest Arctic sea ice” north of Greenland isn’t there any more this summer:
The research icebreaker Polarstern has already inspected the open waters off Kap Morris Jesup, the most northerly tip of Greenland:
What’s more the waters of the Lincoln Sea currently look no more tricky to traverse than the Laptev Sea in August 2016:
In conclusion, for the moment at least, what’s the theoretical solution to our 2018 thought experiment?
Here’s another thought to ponder as well. I don’t suppose it’s in the Alfred Wegener Institute’s PS115 mission plan, but do you suppose Polarstern could circumnavigate Greenland at the moment?
The University of Bremen used not to publish their Arctic sea ice “thinness” maps in summer. However now they do, so here’s a close up of Northern Greenland for August 22nd:
First of all here’s one of our occasional sea ice motion videos:
This one reveals the open water north of Greenland in February as well as the much longer event in August. Next here’s a Sentinel 1B synthetic aperture radar image of the Kap Morris Jesup area from yesterday:
Meanwhile thanks to a heads up from Treform2 on the Arctic Sea Ice Forum comes evidence that on the other side of the Lincoln Sea the last remnants of the Ward Hunt Ice Shelf are “disintegrating”:
Before we got on to the more usual Arctic metrics let’s bear in mind that the beginning of May is the time when the ice on the mighty Mackenzie River begins to break up, ultimately sending a surge of (comparatively!) warm water rushing into the Beaufort Sea. The patches of open water visible in the Beaufort Sea off the Mackenzie Delta in early April refroze, but have recently opened up once again:
Meanwhile Northern Hemisphere snow cover is falling fast, albeit still above last year’s levels:
Here’s the current view of the Liard River in northern Canada, with the Mackenzie River running bottom to top on the right hand side:
The break-up of the Liard leads the Mackenzie, and taking a look at last year’s view of the same area it’s apparent that this year there’s somewhat more snow on the ground, and that this years Mackenzie break-up will therefore be a few days later than last year:
Whilst early melt in the Beaufort Sea is currently behind last year, the reverse is most certainly the case next door in the Chukchi Sea. The skies are rather cloudy there at the moment, but using the Suomi NPP day/night band to peer through the gloom reveals this:
Whilst sea coverage on the Pacific periphery has continued to fall, extent on the Atlantic side has not been following suit. Hence overall Arctic sea ice area is no longer lowest in the satellite record:
Finally, until the new PIOMAS numbers are released at least, here’s how DMI freezing degree days look at the moment:
The April PIOMAS numbers have been published: Arctic sea ice volume is yet again by far the lowest on record:
Greenland ice sheet surface melt has started early this year:
The ice break-up of the Mackenzie River is now visible as increased flow at the junction with Arctic Red River just south of the delta:
Meanwhile the sea ice in the Lincoln Sea north the Nares Strait is coming apart at the seams:
May seems to be shaping up as month of two halves, both spatially and temporally. Here’s an overview of the current state of play:
On the Pacific side of the Arctic sea ice area has been declining rapidly courtesy of the expanding areas of open water visible in the Beaufort, Chukchi and East Siberian Seas. It’s currently tracking below other recent years:
However over on the Atlantic side area has been flatlining, and is currently above other recent years:
Ice mass balance buoy 2017A is now located near the boundary between the Beaufort and Chukchi Seas and as the melting season in that vicinity rapidly approaches it reveals that thermodynamic thickening has thus far achieved a mere 119 cm:
Arctic wide sea ice area has recently started to decline at an increasing rate:
During the second half of the month it will be interesting to see whether the forecast high temperatures produce significant melt ponding. If so it’s conceivable that 2017 area could drop below 2016 again by the beginning of June. There already signs of surface melt at places as far apart as Franklin Bay, Chaunskaya Bay and even the Great Bear Lake!
Watch this space!
References
Muhammad, P., Duguay, C., and Kang, K.-K.: Monitoring ice break-up on the Mackenzie River using MODIS data, The Cryosphere, 10, 569-584, doi:10.5194/tc-10-569-2016, 2016.
Rood S. B., Kaluthota S., Philipsen L. J., Rood N. J., and Zanewich K. P. (2017) Increasing discharge from the Mackenzie River system to the Arctic Ocean, Hydrol. Process., 31, 150–160. doi: 10.1002/hyp.10986.
Kwok, R., L. Toudal Pedersen, P. Gudmandsen, and S. S. Pang (2010), Large sea ice outflow into the Nares Strait in 2007, Geophys. Res. Lett., 37, L03502, doi:10.1029/2009GL041872.