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:
[Edit – March 22nd]
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.
[Edit – March 23rd]
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:
[Edit – March 24th]
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:
[Edit – March 25th]
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:
[Edit – March 27th]
Here’s another week’s merged CryoSat-2/SMOS thickness data from the Finnish Meteorological Institute:
[Edit – March 30th]
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?
[Edit – March 31th]
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:
March 2019 has arrived, which in recent years has proved to be by far the likeliest month to contain the maximum extent of Arctic sea ice for the year. To begin with, here’s our favourite high resolution extent graph calculated by “Wipneus” from University of Hamburg/JAXA AMSR2 data:
Hopefully you can plainly see the pronounced sharp peak towards the end of February 2019? The current maximum Arctic sea ice extent for 2019 is 13.83 million square kilometers on February 22nd. Here’s Arctic sea ice area for good measure:
The current maximum area for 2019 is 13.10 million square kilometers, also on February 22nd. Here too is the NSIDC’s 5 day averaged extent:
This reveals a current maximum extent for 2019 of 14.705 million square kilometers on February 24th.
At this juncture you may well be wondering what the cause of that sudden sharp peak might be? Here’s your starter for ten:
Whilst overall Arctic sea ice area is unremarkable for the current decade, sea ice area in the Bering Sea is remarkable low for the time of year! What’s more much like last year the Chukchi Sea is not currently full to overflowing with sea ice, and is also lowest for the date in the AMSR2 satellite records:
I’ve also been experimenting with the new gridded CryoSat-2/SMOS thickness data from the Finnish Meteorological Institute, which reveals this:
That’s a weekly overview dated February 24th, but it does perhaps explain how such a large area of sea ice could melt so swiftly?
As luck would have it the skies are reasonably clear over the Bering Strait this morning (UTC). Here’s Terra’s view from on high of the current situation:
In addition, here is the underlying sea ice concentration data from the OSI-SAF:
Since Michael is also asserting that there currently exists “the greatest February Arctic sea ice extent (according to DMI) in your blog’s history”, here’s Arctic sea ice area excluding the extremely peripheral Okhotsk and St. Lawrence regions:
P.S. Wipneus’ Pi has processed the AMSR2 data now, and area shows another, more modest, decline today:
Both area and extent are still moving inexorably upwards:
The late February maximum still holds, on the high resolution numbers at least. The JAXA/VISHOP web site is down at the moment, so we’ll have to wait for an update to that particular metric, as well as a post weekend update to the NSIDC’s Charctic chart.
P.S. Jaxa is still down this afternoon, but here’s the latest from the NSIDC:
[Edit – March 13th]
Arctic wide area and extent have blasted past their respective late February maxima:
However Arctic sea ice area excluding the Okhotsk and St. Lawrence peripheral regions has still not exceeded the maximum formed on January 25th:
[Edit – March 14th]
This morning’s data reveal the first decline in extent for several days:
The (extremely!) tentative new maximum Arctic sea ice extent for 2019 is 13.89 million square kilometers on March 12th.
[Edit – March 15th]
JAXA is back!
UH AMSR2 confirms that extent is still declining:
[Edit – March 16th]
Arctic sea ice extent continues to decline, whilst area is still flatlining:
Meanwhile a look at freezing degree days based on the DMI’s dubiously weighted data for north of 80 degrees reveals the story of the freezing season. A historically warm start, but now back in amongst the pack of the 2010s:
[Edit – March 17th]
It looks as though there’ll be no going back from this. Arctic sea ice area is finally following extent’s decline in no uncertain terms:
Barring exceedingly unforeseen circumstances after this year’s “double top” that leaves the 2019 Arctic sea ice maximum extent numbers as follows:
UH/Wipneus AMSR2 – 13.89 million square kilometers on March 12th
JAXA/VISHOP AMSR2 – 14.27 million square kilometers on March 12th
NSIDC 5 day SSMIS – 14.78 million square kilometers on March 13th
[Edit – March 19th]
Arctic sea ice area has fallen off the proverbial cliff over the last few days. There can now be no doubt that the 2019 maximum extent has been reached:
That being the case, all other Arctic sea ice discussion for the month of March can now take place over at:
On March 13, 2019, Arctic sea ice likely reached its maximum extent for the year, at 14.78 million square kilometers (5.71 million square miles), the seventh lowest in the 40-year satellite record, tying with 2007. This year’s maximum extent is 860,000 square kilometers (332,000 square miles) below the 1981 to 2010 average maximum of 15.64 million square kilometers (6.04 million square miles) and 370,000 square kilometers (143,000 square miles) above the lowest maximum of 14.41 million square kilometers (5.56 million square miles) set on March 7, 2017. Prior to 2019, the four lowest maximum extents occurred from 2015 to 2018.
The date of the maximum this year, March 13, was very close to the 1981 to 2010 median date of March 12.
Please note this is a preliminary announcement of the sea ice maximum. At the beginning of April, NSIDC scientists will release a full analysis of winter conditions in the Arctic, along with monthly data for March.
We generally write our periodic reports on the state of Arctic sea ice around the time the PIOMAS volume numbers are published. It seems as though we’ll have a long wait for that to happen at the moment though. According to The Economist today:
America’s government shutdown has become the longest in history. Hundreds of thousands of federal workers remain either stuck at home or forced to work without pay. To reopen the government President Donald Trump is demanding $5.7bn for his border wall. Nancy Pelosi, who presides over the most polarised House of Representatives in recent memory, does not want to give it to him.
Due to the US Government Shutdown, PIOMAS ice volume and thickness data which depend on federal government generated reanalysis products, are currently not updated.
Instead of PIOMAS, let’s start instead with the January 2019 edition of the National Snow and Ice Data Center’s Arctic Sea Ice News:
As 2018 came to a close, Arctic sea ice extent was tracking at its third lowest level in the satellite record, while sea ice in the Antarctic remained at historic lows. Slightly faster growth in the first few days of the new year, mostly in the Pacific sea ice areas, has the daily sea ice extent at fifth lowest as of this post.
Now let’s take a look at our favourite high resolution AMSR2 area and extent metrics:
You can see that towards the end of December Arctic sea ice extent was verging on lowest for the date, since when it has risen quickly to reach highest for the date in the brief AMSR2 records a few days ago.
The NSIDC also mention the US Government shutdown:
Unfortunately, as a result of the partial government shutdown, we are unable to access the National Oceanic and Atmospheric Administration (NOAA) pages to retrieve information on atmospheric air temperatures and sea level pressure patterns. Instead, we turn to daily (2 meters above the surface) mean air temperatures north of 80 degrees North from the European Centre for Medium-Range Weather Forecasts (ECMWF) operational model. This analysis shows that air temperatures remained above the 1958 to 2002 average for all of December.
That brings us on to our Arctic freezing degree days graph, based on DMI data:
After a very slow start to the freezing season the FDD numbers are now vying for second place with last year, behind the astonishingly warm winter of 2016/17. In the absence of the PIOMAS volume numbers we can at least take a look at sea ice thickness. Here’s CryoSat-2:
All those sources seem to be agreed that large areas of both the Barents and Kara Seas are currently covered by young thin ice. Finally, for the moment at least, let’s take a look at some extracts from the NSIDC’s review of 2018:
January 2018 began the year with record low sea ice extents for the Arctic as a whole.
The seasonal maximum, reached on March 17, 2018, was the second lowest in the satellite record. While low extent persisted through April and May, sea ice loss during early summer was unremarkable despite above average 925 hPa air temperatures over the Arctic Ocean and Eurasia.
Air temperatures over the Arctic Ocean in July were below average, followed by above average temperatures in August. In fact, on average, August temperatures were higher than July temperatures in 2018. This is highly unusual in the Arctic and something not seen in at least 40 years.
The September 2018 seasonal minimum extent ended up slightly above the long-term linear trend line, tying with 2008 for the sixth lowest in the satellite record. After the minimum, the ocean was slow to freeze up, and October sea ice extent ended up as the third lowest. However, ice growth was very rapid in November, such that November 2018 extent approached the interquartile range of the 1981 to 2010 median. Nevertheless, large amounts of open water remained in the Barents and Chukchi Seas. By the end of December, ice conditions in the Chukchi Sea were back to average, while extent remained unusually low in the Barents Sea.
Coverage of old ice (greater than 4 years old) over the Arctic continued to decline. Such old ice covers only 5 percent of the area it used to in 1980s.
[Edit – January 13th]
Arctic sea ice area and extent have both been falling over the last few days, possibly as a result of the recent cyclone which created strong northerly winds in the Fram Strait. This is from Earth at 09:00 UTC on January 10th, showing a MSLP of 946 hPa:
Here’s what used to be referred to as JAXA extent:
A somewhat belated start to our October 2018 coverage, but firstly please take a look at this graph:
Following a remarkably sluggish refreeze this year JAXA extent is currently the lowest for the date since their records began. Meanwhile Wipneus has just released his mid month PIOMAS volume update on the Arctic Sea Ice Forum:
That graph reveals that Arctic sea ice volume has been increasing much more slowly than usual during October. The fact that the DMI freezing degree days graph is currently below all previous years in their records no doubt has something to do with that:
Wipneus has also updated the mid month PIOMAS gridded thickness map:
For a handle on the areas of thinner ice where refreezing is taking place around the periphery of the pack, here’s the latest SMOS map:
Finally, for the moment at least, here’s our favourite high resolution AMSR2 area and extent metrics based on JAXA data processed by the University of Hamburg to produced gridded concentration which is then used to derive area and extent by the inimitable Wipneus once again:
[Edit – October 28th]
Here’s the latest thickness maps from SMOS:
and CryoSat-2:
There’s been a recent rapid refreeze, leaving large areas of thin ice around the edges of the central pack:
September is upon us once again, the month in which the assorted Arctic sea ice area and extent metrics (almost) always reach their respective annual minima. Now we are free to start speculating about what the assorted minima will be, and on what date.
To begin with let’s take a look at our much beloved high resolution AMSR2 metrics derived by “Wipneus” from the University of Hamburg’s AMSR2 concentration data:
There’s currently some divergence between the area and extent graphs. Area is declining rapidly for the time of year, whilst extent seems to almost have come to a standstill!
Before looking at some of the other metrics we’ll wait for the effect of the assorted storms currently circling the Arctic to play out. Here’s how the AMSR2 concentration map looks at the moment:
whilst here’s the University of Bremen’s summer SMOS sea ice “thinness” map:
[Edit – September 3rd]
UH AMSR2 area and extent both increased yesterday, so we have a (very!) provisional minimum extent of 4.35 million square kilometres on September 1st.
[Edit – September 4th]
Area and extent have both increased again:
Is the minimum already in, or will the storms still circulating around the Arctic Ocean reverse that trend over the next few days?
[Edit – September 6th]
High resolution area and extent both posted marginal new lows for the year yesterday:
On September 19 and 23, Arctic sea ice appeared to have reached its seasonal minimum extent for the year, at 4.59 million square kilometers (1.77 million square miles). This ties 2018 with 2008 and 2010 for the sixth lowest minimum extent in the nearly 40-year satellite record.
Please note that this is a preliminary announcement. Changing winds or late-season melt could still reduce the Arctic ice extent, as happened in 2005 and 2010. NSIDC scientists will release a full analysis of the Arctic melt season, and discuss the Antarctic winter sea ice growth, in early October.
The NSIDC numbers are based on a 5 day average, whereas the one day high resolution AMSR2 extent reached a minimum of 4.195 million square kilometers on September 17th:
The AMSR2 area minimum occurred significantly earlier. 3.737 million square kilometers on September 9th:
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?
[Edit – August 23rd]
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:
[Edit – August 26th]
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:
First of all Wipneus has been very quick off the mark this month with his PIOMAS gridded thickness map. Here is what it reveals for the last day of March:
Here too is the latest PIOMAS volume graph:
together with the associated anomaly graph:
They show 2018 still in second lowest position, albeit much closer to third place than last year’s line, which is currently leading the pack by a considerable margin.
By way of comparison here are the current Arctic sea ice thickness maps from SMOS:
and CryoSat-2:
All eyes are still on the Bering and Chukchi Seas, where significant extent declines look likely over the coming days.
Meanwhile “JAXA” extent has just edged above 2016!
[Edit – April 11th]
The focus has been on the Bering and Chukchi Seas until now. However there were clear skies over the Mackenzie Delta yesterday, revealing some open(ish) areas in the Beaufort Sea:
NASA Worldview “true-color” image of the Beaufort Sea on April 10th 2018, derived from the MODIS sensor on the Terra satellite
There’s only the merest hint of a blip on the area graph so far though:
It will be interesting to see if the decline in Beaufort Sea area continues from here, or whether this year’s “flatline” resumes and continues for a while longer.
[Edit – April 19th]
It’s not so apparent on the other extent metrics, but as the periphery melts the high resolution AMSR2 version looks to be heading into virgin territory on the downside:
According to the latest edition of the National Snow and Ice Data Center’s “Arctic Sea Ice News”
On March 17, 2018, Arctic sea ice likely reached its maximum extent for the year, at 14.48 million square kilometers (5.59 million square miles), the second lowest in the 39-year satellite record, falling just behind 2017. This year’s maximum extent is 1.16 million square kilometers (448,000 square miles) below the 1981 to 2010 average maximum of 15.64 million square kilometers (6.04 million square miles).
The four lowest seasonal maxima have all occurred during the last four years. The 2018 maximum is 60,000 square kilometers (23,200 square miles) above the record low maximum that occurred on March 7, 2017.
Here’s a close up view of recent maxima via the NSIDC’s Charctic interactive sea ice graph:
Next let’s take a look at extent data from the Japanese National Institute of Polar Research, colloquially referred to as “JAXA extent”
In this case the maximum was 13.89 million square kilometers, also on March 17th.
Here too are the extent and area graphs based on Wipneus’ processing of the University of Hamburg’s AMSR2 based concentration data:
They highlight the surge in Arctic sea ice area in the middle of March due to the sudden “cold snap”:
Looking at the third Arctic dimension, here’s the latest SMOS thickness map from the University of Bremen:
and here’s the latest CryoSat-2 thickness map:
They reveal large areas of relatively thin sea ice in the Okhotsk and Barents Seas where the ice can now be expected to melt as quickly as it formed. There is also remarkably little sea ice in the Bering Sea for the time of year:
Christmas is coming, and Santa’s secret summer swimming pool has frozen over once again. However the same can’t be said for the Chukchi Sea! More on that in due course, but first let’s take a look at the PIOMAS volume graph at the end of November, courtesy of the wondrous Wipneus on the Arctic Sea Ice Forum:
2017 is currently third lowest, behind 2012 and 2016. Next let’s take a look at Wipneus’ PIOMAS Arctic sea ice thickness map:
followed by the University of Bremen’s SMOS Arctic sea ice thickness map:
Note the large area of pale blue open ocean still visible in the Chukchi Sea towards the top left of both maps.
For another perspective on Arctic sea ice thickness here’s the latest Cryosat-2 map, which currently is based on the month up to November 24th:
Finally, for the moment at least, here’s our very own Arctic Freezing Degree Days graph based on the DMI’s >80N data:
2017 is currently occupying the wide open space between the astonishingly low numbers last year and all previous years in DMI’s record. Here’s their graph for 2017 so far:
[Edit – December 10th]
Current Arctic sea ice area and extent derived from the University of Hamburg’s high resolution AMSR2 data:
Plus the latest update on the Chukchi Sea situation:
Particularly in view of all the balderdash concerning “climate science” being spouted in Washington DC on Wednesday lets first of all run through some Arctic sea ice facts from April 1st 2017 or thereabouts:
Northern Hemisphere Snow Extent:
Arctic Sea Ice Area:
Arctic Sea Ice Extent:
Arctic Sea Ice Concentration:
Thin ice map from the University of Bremen SMOS:
Thick ice map from CPOM CryoSat-2
Beaufort Sea ice thickness growth graph:
DMI sea ice temperature map:
DMI atmospheric temperature graph:
DMI Arctic Freezing Degree Days:
PIOMAS volume for March will follow in a few days, but it’s extremely unlikely to be anything other than “lowest for the date”.
What preliminary conclusions can we draw from this plethora of pretty pictures? First of all the Arctic hasn’t suddenly gone into “deep freeze” mode. Temperatures above 80 degrees north are rising again and are well above the climatology. Freezing degree days are still the lowest on record by a wide margin. Northern hemisphere snow cover is falling fast and is currently just above last year.
In contrast to last year, and thanks to lots of cyclones and very little in the way of anticyclones, there’s plenty of sub half meter sea ice in the Laptev and East Siberian Seas and hardly any in the Beaufort Sea. There’s also plenty of thin ice to be seen on both the Atlantic and Pacific peripheries.
The usual southerly arch hasn’t formed in the Nares Strait between Greenland and Ellesmere Island, and as SMOS shows the sea ice in the strait is consequently very thin. That leads one to wonder when the northern arch in the Lincoln Sea might give way.
It’s not immediately apparent from the still images above, but there’s been relatively large amounts of “old ice” exported from the Central Arctic on the Atlantic side, hence the recent increase in overall extent which is now second lowest for the date (since satellite records began). Area has been creeping up as well over recent days, but is still lowest for the date, as it has been for most of the last year. Sea ice “compactness” has decreased somewhat and given all the thin ice around the edges extent will soon start dropping once again.
All in all, the Arctic sea ice prognosis is not good. Are you watching Lamar Smith? (Pun intended!)
[Edit – April 4th]
The March PIOMAS update is out! As suspected, Arctic sea ice volume is still by far the lowest on record:
Volume on March 31st 2017 was 20.398 thousand cubic kilometers. The previous lowest volume for the date was 22.129 thousand km³ in 2011.
Here too is the PIOMAS modelled Arctic sea ice thickness map:
PIOMAS daily gridded thickness for March 31st 2017
[Edit – April 12th]
The latest edition of the NSIDC’s Arctic Sea Ice News confirms that their monthly extent metric for March 2017 was the lowest in the satellite record for the month:
As well as highlighting the anomalously warm temperatures across much of the Arctic:
the NSIDC article includes this telling pressure anomaly map:
New work by an international team led by Igor Polyakov of the University of Alaska Fairbanks provides strong evidence that Atlantic layer heat is now playing a prominent role in reducing winter ice formation in the Eurasian Basin, which is manifested as more summer ice loss. According to their analysis, the ice loss due to the influence of Atlantic layer heat is comparable in magnitude to the top down forcing by the atmosphere.
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