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:
Laptev sea ice area decline has been in high gear recently:
At the beginning of May AWI’s high resolution AMSR2 extent metric is at the top of the historical range:
After a period of melt in the East Greenland Sea, export of sea ice from the Central Arctic via the Fram Strait has increased recently:
Sea ice area in the Barents Sea peaked in the first week of April and has declined steadily since then:
SMOS data is flowing again, and the gaps have been filled. Here’s the final pre melt ponding map of the spring:
It reveals large areas of thin ice that have recently developed in the Kara Sea. Here’s a pseudo colour glimpse of the region through the clouds:
Continue reading Facts About the Arctic in May 2023After 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:
In a press release last week the Alfred Wegener Institute announced that:
From her home port in Bremerhaven, the Polarstern will set course for Fram Strait and the marginal ice zone north of Svalbard, where warm, nutrient-rich Atlantic Water flows into the Arctic Ocean.
Closely monitoring energy and material flows in the marginal ice zone from the ship and from on ice floes is the goal of the team led by Prof Torsten Kanzow, expedition leader and a physical oceanographer at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI). “We will make transects from the open water into the dense sea ice and back. Along the way, we will gather a variety of physical, chemical and biological measurements in the marginal ice zone, which is especially productive and therefore especially interesting,” explains Kanzow.
“The team will also venture onto the ice to take a closer look at the thickness and characteristics of the sea ice and measure ocean currents and eddies away from the ship. We’ll also deploy so-called gliders in the ocean, buoys on the ice and moorings on the seafloor, all of which will record valuable data for the next several years. Lastly, we’ll extend our research radius with helicopter flights, during which we’ll observe, for instance, the melt ponds on the ice.”
Following the work in the MIZ north of Svalbard Polarstern will be heading for Northeast Greenland:
The two glaciers there (79 N Glacier and Zachariae Isstrom) are both characterised by ocean-driven ice loss and accelerated ice flows, making them contributors to sea-level rise. “We plan to install moorings in order to gauge the sensitivity of ocean-driven glacier melting to changing environmental conditions,” says Kanzow, who’s been pursuing research in the region since 2016. Accompanying geodetic-glaciological studies will be conducted on Greenland. On the one hand, they will assess how the solid ground is rising on extremely small scales, because it is still rebounding from the past weight of ice masses that melted after the last glacial maximum. On the other, they will explore temporal variations in supraglacial lakes; their drainage out to sea can have considerable effects on glacier flow speeds and glacier melting.
The progress of Polarstern can be followed on the expedition web site, and via the University of Bremen’s Polarstern centric sea ice concentration maps:
The AWI team have installed three seasonal ice mass balance buoys in the MIZ, without the usual thermistor string but with a new conductivity, temperature, depth (CTD) sensor fitted to measure salinity instead. Less colourful than usual sea ice thickness graphs can be viewed on the 2022 ice mass balance buoy page. Here’s one example:
The image above updates on a daily basis, but today’s version is worth preserving for posterity:
There is currently a large area of low concentration sea ice around the North Pole, and Polarstern has left its station in the marginal ice zone and is currently heading north of Greenland rather than in the direction of the 79N/ZI glaciers.
[Edit – July 27th]Further investigation reveals that:
Polarstern has been heading even further north to the Aurora Vent field (about 130 nautical miles northwest). As part of an extensive lithospheric study, ocean bottom seismometers will be deployed at depths of more than 4000 meters to record seismological activity as well as the physical properties of the hydrothermal plume.
Polarstern is now heading south again, where a team from the Technical University of Dresden will be deploying a modified surfboard on supra-glacial lakes! Here’s a test run in a melt pond:
I discovered something rather interesting whilst browsing the Marine Traffic ship tracking web site this morning:
It appears as if the AWI have recently installed two buoys that support AIS position reporting, as indeed does Polarstern itself:
Polarstern is now approaching the 79 N and Zachariae Isstrom glaciers:
Watch this space!
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.
A detailed dissection of the 2021 minimum of various Arctic sea ice extent metrics can be found on a dedicated thread. All other Arctic news in September will be found below.
Let’s start with a map of sea ice age at the beginning of August:
Firstly notice the absence of 3+ year old ice off the coast of north east Greenland. Also visible is a band of 4+ year old ice across the Pacific side of the Arctic Basin, which has slowed melting in the region and explains the following regional sea ice area graphs:
Next here’s the current AMSR2 concentration map:
There is currently a large area of open water in the Wandel Sea to the north of Greenland. There is also an arm of old ice across the Beaufort and Chukchi Seas which is still clearly visible, but also visible is the recent reduction in sea ice concentration in the region. By way of explanation, here’s another look at the thickness of an ice floe currently situated to the north of the Chukchi at 74.84 N, 164.29 W, as measured by an ice mass balance buoy:
As the 2021 melting season draws towards its conclusion the floe is experiencing rapid bottom melt. How much longer will this floe and others like it last? Will it survive to become an “old ice” dot on next year’s ice age maps?
[Edit – September 6th]As Wipneus puts it on the Arctic Sea Ice Forum, “PIOMAS has updated the gridded thickness data up to the 31st of August”. Here’s the latest modelled thickness map, which shows the thickest remaining ice located north of the Canadian Arctic Archipelago rather than north of Greenland:
The accompanying volume graph shows 2021 in 7th lowest position, at 4.7 thousand km3:
Here too are the current PIOMAS volume trends for each month of the year:
The Swedish icebreaker Oden has recently been exploring the area between northern Greenland and the North Pole as part of the Synoptic Arctic Survey expedition:
Here are the measurements of water temperature it has recorded over the past few days:
Ranging between -0.4 °C and -1.0 °C it doesn’t look as though the 2021 refreeze will be starting in the Wandel Sea just yet.
[Edit – September 10th]A picture of the sea ice at the North Pole from Ponant’s Le Commandant Charcot on September 6th:
Here’s the latest NSIDC sea ice age map:
That shows plenty of old ice still left in the Beaufort Sea. However ice mass balance buoy 52460 now appears to floating free of its ice floe at 75.56 N, 165.99 W:
“New ice” has started to appear in previously open water on the Canadian Ice Service charts. See area E south east of Resolute:
In answer to Frozen Earth’s metaphorical prayer, Wipneus has just released the mid September PIOMAS gridded thickness numbers on the Arctic Sea Ice Forum. First of all the thickness map:
followed by the volume graph:
and the monthly volume trends:
Volume calculated from the thickness data currently show that 2021’s minimum was reached on September 7th at 4.64 thousand km3, which is the 8th lowest value in the Polar Science Center’s record.
[Edit – September 23rd]NASA have just announced a new paper about clouds in the Arctic. Highly relevant given their recent overview of the 2021 melting season!
Clouds are one of the biggest wildcards in predictions of how much and how fast the Arctic will continue to warm in the future. Depending on the time of the year and the changing environment in which they form and exist, clouds can both act to warm and cool the surface below them.
For decades, scientists have assumed that losses in Arctic sea ice cover allow for the formation of more clouds near the ocean’s surface. Now, new NASA research shows that by releasing heat and moisture through a large hole in sea ice known as a polynya, the exposed ocean fuels the formation of more clouds that trap heat in the atmosphere and hinder the refreezing of new sea ice.
The findings come from a study over a section of northern Baffin Bay between Greenland and Canada known as the North Water Polynya. The research is among the first to probe the interactions between the polynya and clouds with active sensors on satellites, which allowed scientists to analyze clouds vertically at lower and higher levels in the atmosphere.
The approach allowed scientists to more accurately spot how cloud formation changed near the ocean’s surface over the polynya and the surrounding sea ice.
Watch this space!
The new month starts with JAXA extent “lowest for the date in the satellite record” by a whisker:
The high resolution Arctic sea ice area and extent graphs based on the University of Hamburg’s AMSR2 concentration data are also in “statistical ties” for that honour, in records going back to 2013:
The 2020 melting season currently seems to be a game of two (geographical) halves. The sea ice on the Siberian side of the Arctic is currently at record lows:
Whereas the Beaufort Sea is near a record high:
Currently the tell tale signs of surface melt are visible across most of the central Arctic, as are the large number of wildfires across Arctic Siberia:
The June 30th PIOMAS gridded thickness numbers have been released, and here are the results of Wipneus’s number crunching:
This month including a visualisation of the increasing negative anomaly:
A break in the clouds over the North Pole reveals the onset of surface melt:
After a brief hiatus there are once again some ice mass balance buoys installed at assorted locations across the Arctic. Some have ceased to function, but one of the buoys installed as part of the MOSAiC expedition is still sending back data as it heads towards the Fram Strait. Buoy 387850 is currently located at 81.66 N, 4.19 E. Here’s its ice mass balance plot:
As you can see, both surface and bottom melt are well under way, with just over a meter of ice still remaining.
Now let’s take a look at buoy 386840, currently located at 74.30 N, 132.60 W in the Beaufort Sea:
It looks as though the ice thickness has increased, but surely that can’t be right at this time of year? To try and find out I downloaded the raw data and plotted the temperature readings from the buoy’s thermistor string:
It looks to me as though the ice floe carrying the buoy is currently floating on some warm fresh water from a recently drained melt pond, which is confusing the sensor designed to measure the position of the bottom of the ice. There certainly seems to be far less than the claimed “1.653 m snow and ice thickness” still remaining to be melted!
A very unusual image. Hardly a cloud in the sky over the North Pole yesterday:
The July 2020 extent “plummet” shows no signs of ending just yet. Here’s the JAXA/ViSHOP version:
JAXA AMSR2 extent is now below 7 million km², and the high resolution version is lower still:
As the “Laptev Bite” and the Atlantic periphery of open water extends further towards the North Pole, Central Arctic Basin extent is now also at record lows for the date in the AMSR2 record:
Wipneus has crunched the mid month PIOMAS gridded thickness numbers, and here are the results:
Extent is currently lowest in the satellite era by a long way, but modelled volume is only fourth lowest!
Watch this space!
At long last there’s a sub 1000 hPa MSLP low pressure area slowly wending its way across the central Arctic:
It seems to have bottomed out at 997 hPa. Perhaps this will inhibit the ongoing “plummet” in extent? JAXA extent fell by 114,342 km2 yesterday.
The Northern Sea Route has opened unusually early this year:
Based on the AMSR2 concentration maps from the University of Hamburg that happened on July 13th. The final choke point, as is so often the case, was the Vilkitsky Strait. According to the charts from the Russian Arctic and Antarctic Research Institute, by the 14th there was a narrow way through occupied by no more than 3/10 concentration ice:
A mere three days away, and the GFS and ECMWF forecasts are in agreement, so there is a decent chance this setup will materialise in the real world:
A 972(ish) hPa MSLP cyclone sitting over the ice Beaufort Sea by 12Z on Tuesday.
The Sea Ice Prediction Network July forecast for this year’s September minimum extent have been released. Here’s the graphical overview:
This year’s median projected value from the July forecasts of 4.3 million square kilometers is essentially identical to the median from the June forecasts. Quartiles are 4.1 and 4.6 million square kilometers. As was also the case for June, only two projections, both by dynamic models, are for a new record low, below the mark of 3.57 million square kilometers set in 2012. One dynamical model predicts the September sea-ice extent above 5.0 million square kilometers, compared to two in the June report.
Note that the numbers quoted are for the average NSIDC extent across the month of September, not the lowest daily JAXA extent, which I suggested earlier would be “below 4 million km²” this year.
Meanwhile over on Twitter this evening (UTC):
The MSLP of the (Great?) Arctic cyclone sank below 970 hPa overnight:
Here’s an early false colour snapshot of how (s)he looks from on high this afternoon (UTC), courtesy of the MODIS instrument on the Terra satellite:
First up today we have a more complete “true colour” image of the cyclone doing its worst yesterday, including a fairly clear view in the bottom left corner of the initial damage to the sea ice covering the eastern Beaufort Sea. This one is from the Aqua satellite:
Watch this space!
Whilst we await the PIOMAS volume numbers which generally arrive around the 5th of each month, and before we look at graphs of extent, with the refreeze well under way some “measured” thickness maps are coming back! Here’s the first SMOS map this autumn:
Then of course there’s our usual Arctic wide high resolution AMSR2 area and extent graphs:
They reveal both metrics currently still second lowest (in the brief AMSR2 record) after 2012. It looks as though that may well change soon, particularly area.
The MOSAiC Expedition has started in earnest, with Polarstern and Akademik Fedorov in amongst the sea ice at long last:
However:
The search for a suitable floe is still ongoing: Aboard Akademik #Fedorov survey flights take off whenever the often foggy #Arctic weather allows.#MOSAiCexpedition #Icedrift #Icefloe
Photo by: @AWI_de / Hans Honold pic.twitter.com/HmjaTsYNfP
— MOSAiC Expedition (@MOSAiCArctic) October 1, 2019
The near real time NSIDC monthly extent for September is 4.32 million km². Here’s the graph:
We’re eagerly awaiting the first ice mass balance buoy “near real time” data, but for now the 2019 PIOMAS minimum volume is expected to be revealed real soon now, so:
As previously perfectly predicted, the PIOMAS numbers have arrived over at the ASIF. Here’s the thickness map for the end of September:
and the volume graph:
Since I’m involved is a heated “debate” about Arctic sea ice trends over at ex Prof. Judy’s, here’s an added bonus this month. The September volume trend:
A marginally off topic excursion down under. The NSIDC 5 day average Antarctic sea extent looks to have peaked at 18.40 million km² on September 30th:
The first of the MOSAiC Expedition’s Ice Mass Balance buoys has been installed, presumably on the ice floe Polarstern is moored to. It reveals sea ice that is currently just over 1 meter thick with a sprinkling of snow on top:
P.S MOSAiC IMB buoy #3 has gone live today too:
There’s currently only 0.5 meters of ice under this one.
Here’s the latest annual PIOMAS “ice cube” animation from Andy Lee Robinson:
Here’s the latest DMI “high Arctic” temperature graph:
Needless to say that means the DMI Freezing Degrees Days graph is tracking the lowest readings in the DMI’s records:
MOSAiC IMB buoy #2 has now been installed and is beaming back data:
The sea ice at this location is decidedly on the thin side at present. A mere 20 cm or thereabouts!
The JAXA ViSHOP web site is down at the moment, so by way of a change here is the University of Bremen’s AMSR2 based extent graph instead:
2019 Arctic sea ice is extent is now once again “lowest for the date” (since AMSRx satellite records began).
The JAXA/ADS/ViSHOP web site is back online after being down over the weekend, presumably due to the effects of Typhoon Hagibis:
Sure enough the Japanese flavour of AMSR2 based extent is also now “lowest for the date”.
Plus a stunning image from Mike Horn and Borge Ousland as they attempt to “walk” to the North Pole then on towards Svalbard:
Mike and Borge’s current position was reported yesterday as: 89°35′51″N 140°30′32″E
The latest SMOS Arctic sea ice “thinness” map shows sea ice starting to form on the shores of the Laptev Sea:
The Centre for Polar Observation and Monitoring (CPOM) have just published the first CryoSat-2 Arctic sea ice thickness map of the 2019/20 freezing season:
Note in particular the dark blue area north of the Canadian Arctic Archipelago.
Wipneus has just crunched the October mid month PIOMAS numbers. Here are the results. Not only the modelled Arctic sea ice thickness map:
but also the Arctic sea ice volume graph:
Over on Twitter Judah Cohen suggests that:
Maybe I will discuss more in the next blog but the #Arctic sea ice growth season on the North Pacific side of the Arctic is just nuts, like it is drunk! Looks unprecedented to me. This needs to be watched through the #winter. Already had 2 unprecedented winters in the Bering sea pic.twitter.com/sAVoZXgNAX
— Judah Cohen (@judah47) October 20, 2019
Here’s the evidence:
I have been trying to bring the implications of this to the attention of the denizens of Judith Curry’s “Climate Etc.” blog, thus far with remarkably little success! This is the gist of my argument:
See:
“Warming of the interior Arctic Ocean linked to sea ice losses at the basin margins” Mary-Louise Timmermans, John Toole, Richard Krishfield (2018)
“Summer solar heat absorption by the surface waters has increased fivefold over the same time period, chiefly because of reduced sea ice coverage.”
“The effects of an efficient local ice-albedo feedback are thus not confined to the surface ocean/sea ice heat budget but, in addition, lead to increased heat accumulation in the ocean interior that has consequences far beyond the summer season.”
“In the coming years, however, excess Beaufort Gyre halocline heat will give rise to enhanced upward heat fluxes year-round, creating compound effects on the system by slowing winter sea ice growth.”
Watch this space!
