The JAXA/ViSHOP web site is currently undergoing maintenance, but here is how their 2 day average extent graph looked for June 2nd:
Extent was 3rd lowest in the JAXA record, behind 2016 and 2019.
The Alfred Wegener Institute’s sea ice concentration data shows that the Bering Sea is now largely free of sea ice, and the areas of open water in the Beaufort, Chukchi, East Siberian and Laptev Seas continue to expand:
The sea ice concentration map also shows open water in much of Lancaster Sound. Also apparent is the widespread presence of melt ponds along the southern part of the Canadian Arctic Archipelago. Here’s a closer, albeit somewhat cloudy, look:
“False colour” image of the Canadian Arctic Archipelago on June 3rd from the MODIS instrument on the Aqua satellite
JAXA have updated their visualisations of Arctic sea ice extent data. The “traditional” 2 day average graph is now labelled “preliminary”, and currently shows 2026 in a tie with 2020 for third lowest for the date:
5 day averaged “confirmed” data is also available, including regional graphs. By way of example here’s JAXA’s latest extent graph for the Bering Sea, dated May 15th:
The Alfred Wegener Institute’s sea ice concentration data reveals open water in the Beaufort, Chukchi, East Siberian and Laptev Seas:
Hudson Bay has fully frozen over during January. However, there is still open water north of Svalbard and in the North Water Polynya. It’s even possible to go swimming in the Nares Strait according to the latest AMSR2 concentration map from the Alfred Wegener Institute:
JAXA extent is currently 3rd lowest for the date, in a “statistical tie” with 2017:
Looking at the third dimension next, PIOMAS volume was second lowest for the date by a whisker at the end of January:
At the beginning of August JAXA/ViSHOP extent is 3rd lowest for the date in the satellite era:
In 2012 extent had just started its unprecedented plunge towards the record September minimum, and 2024 seems certain to cross above the 2012 curve shortly. However, the latest AMSR2 sea ice concentration map from the Alfred Wegener Institute reveals areas of open water across the majority of the Central Arctic Basin:
In particular the sea ice between the North Pole and northern Greenland is remarkably fragmented:
“False colour” image of the North Pole on August 3rd from the MODIS instrument on the Terra satellite
The JAXA/ViSHOP web site is currently down, so here is the current OSI SAF extent graph for the end of May:
2012’s “June cliff” is almost upon us, and if 2024’s current trajectory continues extent will cross above 2012 for the first time since February in a week or so.
Whilst waiting for the all important thickness and volume data to arrive, we’ll start the new year in traditional fashion with a graph of JAXA extent:
The 2023 calendar year finished with this particular extent metric sitting at 15th lowest in the satellite era.
From Niall Dollard on the Arctic Sea Ice Forum comes evidence via the Sentinel 1A satellite that an arch formed in the Nares Strait between Greenland and Ellesmere Island in late December:
Please note the current record low NH snow extent. Matt predicts all that is about to change:
How sure? And in what way "totally different"?
Have you pointed out to Tony yet that the current daily snow cover data you cite utterly negates his recent assertion that "Autumn/Winter snow cover has been increasing for almost 60 years"?
Hot off the Scandinavian virtual printing presses, here is the official December Arctic sea ice extent trend graph from the OSI SAF:
That’s “Steve”/Tony’s current metric du jour. When do you suppose he will bring it to the attention of his horde of regular readers? It’s accompanied by this matching concentration map:
Here too is the CryoSat-2/SMOS thickness map for December 31st, in a different format to the one usually used here:
[Update – January 3rd]
The December PIOMAS modelled gridded thickness data has been released. The calculated volume is 6th lowest in the satellite era:
Here is the equivalent CS2/SMOS volume graph
Here too is the PIOMAS thickness map for December 31st:
This uses the same Greenland down orientation and 2.5 meter maximum scale value as the CS2/SMOS map above.
The end of 2023 had above average sea ice growth, bringing the daily extent within the interdecile range, the range spanning 90 percent of past sea ice extents for the date. Rapid expansion of ice in the Chukchi and Bering Seas and across Hudson Bay was responsible.
Average Arctic sea ice extent for December 2023 was 12.00 million square kilometers, ninth lowest in the 45-year satellite record . Sea ice extent increased by an average of 87,400 square kilometers per day, markedly faster than the 1981 to 2010 average of 64,100 square kilometers per day.
After a delayed start to the freeze-up in Hudson Bay, sea ice formed quickly from west to east across the bay, leaving only a small area of open ocean near the Belcher Islands at month’s end. In the northern Atlantic, sea ice extent remained below average extent, as has been typical for the past decade.
For December overall, 2023 had the third highest monthly gain in the 45-year record at 2.71 million square kilometers, behind 2006 at 2.85 million square kilometers and 2016 at 2.78 million square kilometers.
Moving on to the “Conditions in context” section:
Warm conditions prevailed over the central Arctic Ocean and Beaufort Sea regions, as well as over Hudson Bay and much of northern Canada, with air temperatures at the 925 millibar level (around 2,500 feet above sea level) 8 to 9 degrees Celsius above the 1991 to 2020 average. Elsewhere, relatively cool conditions prevailed, with air temperatures 2 to 4 degrees Celsius below average in southwestern Alaska, easternmost Russia, Scandinavia, and southeast Greenland. Cool conditions in the Bering and southern Chukchi Seas explain the rapid ice growth there. By contrast, the warm conditions over Hudson Bay, continuing since November, explain its delayed start of ice formation there.
The atmospheric circulation pattern for December was marked by low sea level pressure over the Gulf of Alaska and northern Europe and high sea level pressure over central Russia. This pattern led to cold Arctic air flowing across the Chukchi Sea and into the Bering Sea as well as advection of relatively warm air across Canada into the Beaufort Sea:
Here’s a taste, but there’s much more at the dedicated article linked to above:
[Update – January 12th]
A change is as good as a rest, so here’s the AWI “high resolution” AMSR2 Arctic wide sea ice extent graph
It’s currently highest for the date in the AMSR2 era by a significant margin.
Here too is the ice age map for the end of 2023:
[Update – January 19th]
Something seems to have gone wrong with the processing of the mid-month PIOMAS gridded thickness data. For the moment we’ll have to make do with just the CryoSat-2/SMOS thickness map:
and volume graph:
With the perennial caveat of a probable upward revision when the reanalysed data is released, Arctic sea ice volume is still close to the bottom of the range during the CryoSat-2 era.
In addition especially for Matt, “Steve”/Tony and numerous others of a “skeptical” persuasion, here are the latest Environment & Climate Change Canada snow extent and snow water equivalent graphs for the northern hemisphere:
Last but certainly not least is the Rutgers Global Snow Lab northern hemisphere snow cover anomaly chart for December:
[Update – January 29th]
A winter cyclone is stirring up the far North Atlantic. It’s currently forecast to bottom out later today with a minimum MSLP of 937 hPa:
The storm has been creating a long period swell directed at the ice edge in the Barents Sea. By midnight that swell will be battering the ice in the Fram Strait too:
[Update – January 30th]
According to Environment Canada the cyclone bottomed out with an MSLP of 939 hPa at 12 PM UTC yesterday:
Associated with the storm is a pulse of abnormally warm air reaching to the North Pole and beyond:
Here’s how JAXA extent looks as the big swell arrives:
And here’s the lead enhanced AWI AMSR2 concentration map of the Atlantic periphery:
Let’s see how things change over the next few days.
[Update – January 31st]
Here’s a preliminary look at the effect of the recent Arctic cyclone and other “weather” on the sea ice in the Fram Strait and Barents & Kara Seas:
There is also another cyclone heading for the Barents Sea. This one is forecast to bottom out at 936 hPa at around midnight tonight near the Norwegian coast:
P.S. The cyclone mentioned just above has been named Storm Ingunn by the Norwegian Meteorological Institute:
👀 This swirl of cloud is #StormIngunn – an intense area of low pressure that's still rapidly deepening
😮 Wind gusts of over 120 mph have been reported in the Faroe Islands with the storm now moving towards Norway pic.twitter.com/TNuo52L7MW
By 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:
“False colour” image of the Lena Delta on June 1st from the MODIS instrument on the Aqua satellite
At the beginning of the New Year all the central regions of the Arctic are now refrozen apart from a small area of the Kara Sea:
Most Arctic sea ice metrics are near the middle of their respective ranges over the last decade. By way of example, here is a graph of Arctic Freezing Degree Days based on the Danish Meteorological Institute’s temperature data for the area north of 80 degrees latitude:
Here too are the high resolution AWI AMSR2 area and extent graphs:
The latest AWI CryoSat-2/SMOS volume graph tells a similar story:
Although overall volume is in the middle of the pack, the associated thickness map:
and the thickness anomaly map from the Finnish Meteorological Institute reveal an unusual distribution of thicker ice:
A considerable volume of ice currently situated between Svalbard and North East Greenland seems destined to exit the Central Arctic Basin via the Fram Strait over the coming months.
[Edit – January 24th]
In a somewhat belated mid month update, here’s the PIOMAS daily Arctic sea ice volume graph:
together with the PIOMAS thickness map on January 15th:
For comparison purposes here’s the AWI CryoSat-2/SMOS thickness map using the same scale:
Note the change of scale from the beginning of the month CS2/SMOS map at the top.
Here too is Lars Kaleschke’s animation of recent Arctic sea ice concentration, with the width of leads exaggerated to reveal ice motion:
Click to animate (10 Mb!)
Evidently sea ice export from the so called “last ice area” is continuing via the Nares Strait and in particular via the Fram Strait between Greenland and Svalbard.
Although not on the same scale as the cyclone at around the same time last year, surface pressure of a storm near Svalbard bottomed out at 965 hPa yesterday:
It will be interesting to see what effect the storm has on the ice on the Atlantic periphery over the next few days.
Extremely belatedly I’ve just discovered that many weeks ago Sébastien Roubinet set out on another expedition to cross the Arctic Ocean in an ice skating catamaran, now christened Babouch-ty. Seb has already led several similar expeditions in the high Arctic, and on this occasion he is accompanied by Eric André and Jimmy Hery. They set sail from Sachs Harbour on Banks Island at the end of June, and have seen many sights since then! Here are a few of them:
Here too is a more recent image of Babouch-ty and Ellesmere Island:
The Nagalaqa tracking map shows that Babouch-ty looks set to round Cape Columbia, the northernmost point on Ellesmere Island, round about now:
The original aim of the expedition was to reach Svalbard via Cap Morris Jesup, but given the length of time it has taken the team to get this far they have sensibly decided to take an early exit from the Central Arctic via the Nares Strait:
[Edit – September 26th]
Seb has decided to terminate the Nagalaqa Expedition in the Nares Strait, north of the Kane Basin:
Winds of more than 30 knots are forecast. The weather window didn’t really open. Luckily we’re not on the water, with our wobbly little boat, it would have been catastrophic… Here and now, the winds, the cold, the snow, the darkness remind us that winter is back. The Arctic requires patience, perseverance, but also a large dose of humility. We are waiting for better weather conditions so that a helicopter can take off and pick us up. In a few days, we will leave Babouch-ty, dismasted, coiled in a fold of ground and moored to bags of stones… This expedition ends here for this year.
2021 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…
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.
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:
[Edit – January 25th]
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!
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