As part of his March PIOMAS gridded sea ice thickness update Wipneus also produced this graph of sea ice export from the central Arctic via the Fram Strait:
So far this winter export has been remarkably subdued, but that has now changed. A persistent dipole with high pressure over Greenland and low pressure over the Barents Sea is generating strong northerly winds in the Fram Strait, and even bringing some April snow showers to South West England:
Wondering why it's so #cold? We're still sat in Arctic air across the UK today
A change to milder #weather arrives tonight for Thursday and Friday, bringing temperatures much closer to average
Precisely how high the pressure has been over Greenland is the subject of much debate. See for example this discussion on the Arctic Sea Ice Forum about whether a new world high pressure record has just been set. Different weather forecasting models have come to very different conclusions about the mean sea level pressure of a high pressure area situated over the Greenland ice sheet, which reaches an altitude of over 3,000 metres. Here’s GFS for example, showing 1097 hPa at 06Z on April 4th:
whereas the Canadian Meteorological Centre synopsis for the same time shows a mere 1070 hPa:
At least all the assorted models agree that the isobars are closely packed over the Fram Strait, and hence some of the thickest sea ice remaining in the Arctic is currently heading towards oblivion in the far north Atlantic Ocean:
Maximum volume is still several weeks away, but let’s first of all take a look at the PIOMAS modelled volume numbers for February. They are not yet available via the University of Washington’s Polar Science Center web site, but Wipneus has once again crunched the gridded thickness numbers which are already available. Here is what they reveal:
As you can see, it will be a big surprise if the 2021 volume maximum occurs in March rather than April, and 2021 is currently 3rd lowest for the date, behind 2017 and 2018. For completeness here too is the PIOMAS thickness map for the end of February:
This does contain some surprises, such as an area of thick ice along the shore of the East Siberian Sea, but no such thing along the north coast of Greenland, the traditional bastion of “the thickest ice in the Arctic Ocean”.
The “measured” Arctic sea ice volume calculated from CryoSat-2 and SMOS thickness data has also updated to February 28th:
Note that the “near real time” figures graphed in blue will almost certainly be revised upwards when the “reanalysed” data is released in a couple of weeks. Equally certainly they will be “lowest for the date” in the 11 year record.
Here also is the CS2/SMOS thickness map for February 28th for comparison purposes:
Here’s the latest graph of Arctic sea ice extent from JAXA/ViSHOP, with 2021 and 2015 highlighted:
Extent fell by over 100,000 square kilometres between February 16th and 17th! Can that steep fall continue, as it did for one more day in 2015?
Here too is Zack Labe’s 2021 overview of JAXA maximum extent over the previous couple of decades:
2015’s maximum was very early, on February 15th. Hence the current extremely tentative 2021 maximum is already both higher and later than that. The decadal average extent graphs show the date of the maximum getting later and later, and the 2010’s peaks in the middle of March.
It therefore seems likely that there is more freezing still to come this year. However lets take a look at the high resolution AMSR2 sea ice area graph for the Sea Of Okhotsk:
The recent fall in Arctic wide extent has evidently been driven by the recent rapid decline in this peripheral sea, where SMOS reveals more thin ice ripe for further melting:
In conclusion, the high res AMSR2 extent metric shows the tentative 2021 peak below that of 2015!
Arctic sea ice volume is of course far more important in the grand scheme of things. However sea extent is easier to measure, and the JAXA AMSR2 flavour thereof has now nudged into second place for the date above 2016:
[Edit – November 4th]
The PIOMAS gridded thickness numbers have been released, to reveal this end of October thickness map:
and these calculated volume graphs:
These show Arctic sea ice volume to be lowest for the date, even if extent has slipped into 2nd place.
For comparison purposes here too is the latest AWI CryoSat-2/SMOS merged thickness map:
Let’s start this somewhat belated article by looking at Arctic sea ice volume. The mid month PIOMAS gridded thickness numbers have been released to reveal these volume graphs:
Minimum volume for 2021 was 4.03 thousand km3 on September 17th, 2nd lowest in the PSC record.
Modelled volume is now in a “statistical tie” with 2012 for lowest on record for mid October. Here too is the PIOMAS thickness map:
Meanwhile for comparison purposes here is the first merged Cryosat-2/SMOS thickness map of the 2020/21 freezing season, hot off the presses at the Alfred Wegener Institute:
A detailed dissection of the 2020 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. As is usually the case, let’s set the ball rolling by taking a look at Wipneus’s visualisations of the August PIOMAS gridded thickness data:
together with the computed volume:
and anomaly graphs:
PIOMAS volume at the end of August was still firmly in 3rd place behind 2012 and 2019.
I’ve been waiting for the results of the ARCUS SIPN August call, but despite the timetable specifying “26 August 2020 (Wednesday)” they’ve still not been published and I can wait no longer!
Hopefully the August “predictions” will be available soon, but for the moment let’s take a look at the July 2020 Sea Ice Outlook instead:
For the Arctic, the median July Outlook for September 2020 average sea-ice extent is 4.36 million square kilometers, essentially identical to the median prediction in the June report, with quartiles of 4.1 and 4.6 million square kilometers. For comparison, the historical record September low over the period of satellite observations was set in 2012 at 3.57 million square kilometers, and the second lowest record was 4.27 million square kilometers set in 2007. This year’s projection is close to the 2019 observed September sea-ice extent of 4.32 million square kilometers. As was also the case for the June report, only two of the outlooks project September sea-ice extent below the 2012 record. The consensus judgement against a new record low September sea-ice extent hence remains unchanged. Interestingly, as of this report, observed extent stands at a record low for this time of year.
Note that those numbers represent “September 2020 average sea-ice extent” and not the daily minimum. Let’s now take a look at the assorted different flavours of “Arctic sea ice extent” metric. Firstly here’s the NSIDC’s “Charctic” 5 day average extent:
Next here’s JAXA/ViSHOP extent, generally assumed to be a “2 day average”:
Next here’s the DMI version, which neglects to include 2012:
Our title today is shamelessly plagiarised from the “Watts Up With That” blog of our old friend Anthony Watts. However daring to be different we have redacted the initial word “Claim -“.
The Last Interglacial (LIG), a warmer period 130,000–116,000 years before present, is a potential analogue for future climate change. Stronger LIG summertime insolation at high northern latitudes drove Arctic land summer temperatures 4–5 °C higher than in the pre-industrial era. Climate model simulations have previously failed to capture these elevated temperatures, possibly because they were unable to correctly capture LIG sea-ice changes. Here, we show that the latest version of the fully coupled UK Hadley Center climate model (HadGEM3) simulates a more accurate Arctic LIG climate, including elevated temperatures. Improved model physics, including a sophisticated sea-ice melt-pond scheme, result in a complete simulated loss of Arctic sea ice in summer during the LIG, which has yet to be simulated in past generations of models. This ice-free Arctic yields a compelling solution to the long-standing puzzle of what drove LIG Arctic warmth and supports a fast retreat of future Arctic summer sea ice.
There’s no mention of “2035” in there, so let’s look instead at yesterday’s press release from the British Antarctic Survey:
A new month begins today, and at the moment it looks as though it’s going to be the most interesting one since August 2012. Here once again is the satellite image of the enormous cyclone that was spinning over the Beaufort/Chukchi Seas just a few days ago:
Here too is the effect of the cyclone on the trajectory of the JAXA Arctic sea ice extent graph:
Here too is the current prognosis of the late Andrew Slater’s “Slater Probabilistic Ice Extent” 50 day forecast:
The cyclone has obviously resulted in a reduction in the rate of extent decline, but take a look at the high resolution AMSR2 “compaction” graph:
The gaps between the remaining sea ice floes have evidently increased, and hence the ice area is declining more rapidly than its extent.
[Edit – August 2nd]
Here’s an animation, based on the University of Hamburg’s AMSR2 concentration maps, which reveals the motion of the sea ice across the Beaufort and Chukchi Seas for the last two months:
Note in particular the side effects of the recent cyclone, visible at the end of the video.
Here too is a close up of the current state of the remaining ice in the Chukchi Sea, snapped by the Suomi NPP satellite through a gap in the clouds:
Plus the current open water north of Greenland. Perhaps once Polarstern has been flushed out into the open water of the Fram Strait at the end of the MOSAiC expedition she could take another look at this almost completely unexplored area of the Arctic Ocean?
[Edit – August 6th]
The latest gridded thickness data has been released by the PIOMAS team, and here are Wipneus’s visualisations:
Average Arctic sea ice volume in July 2020 was 9,300 km3. This value is only 400 km3 above the record minimum value of 8,900 km3 set in 2019. This makes 2020 the fourth lowest on record for July with 2012, 2017,2019 falling just below 2020.
JAXA extent is still lowest for the date, but following the recent cyclone it looks as though it will not maintain that position for much longer:
Now we’re in the month of August it’s possible to do a direct comparison with AMSR2 data for 2012. Here’s sea ice area for the Central Arctic Basin:
[Edit – August 8th]
All of a sudden JAXA extent is in 3rd place in the race to the minimum:
However let’s also take a close look at the state of the sea ice in the Beaufort and Wandel Seas shall we?
At this juncture I reckon that come mid September second place is now more likely than first. However as always, it still all depends on the weather.
[Edit – August 9th]
Surprising as it may seem, high resolution AMSR2 Central Arctic Basin sea ice area has so far managed to keep up with the precipitous drop in 2012:
North of Greenland the clouds have cleared closer to the North Pole, to reveal this:
Fresh this morning from Terra, a rather cloudy view of the devastation near 80N, 150W:
[Edit – August 10th]
In a not entirely unexpected development one of ex Prof. Judy’s denizens is quibbling about the current condition of sea ice in the Arctic. Hence here is a close up of some “gaping holes in the sea ice cover” at 88N between Greenland and the North Pole:
[Edit – August 13th]
A nice clear view this morning of the marginal ice zone of the “Laptev Bite” and thereabouts from the Suomi satellite :
[Edit – August 16th]
JAXA AMSR2 extent has fallen below 5 million km²:
Having been flushed out of the Central Arctic through the Fram Strait the polar research vessel Polarstern is back, seemingly intent on taking a close look at the North Pole:
[Edit – August 19th]
The mid month PIOMAS gridded thickness numbers have been published:
According to the Polar Science Center model Arctic sea ice volume is currently third lowest after 2012 and 2019.
[Edit – August 24th]
Arctic sea ice area based on NSIDC concentration data is now in a “statistical tie” with 2012 for the honour of “lowest for the date” in the satellite record:
High resolution AMSR2 area isn’t far behind:
[Edit – August 24th]
A nice clear view of the disintegrating sea ice north of the East Siberian and Chukchi Seas yesterday:
Watch this space very closely for the next few weeks!
Whilst the Northern Sea Route has opened up early this year, it will be be quite some time before the Northwest Passage follows suit. Nevertheless our old friend Northabout is currently sailing in the direction of Baffin Bay, so now seems as good a time as any to start speculating about the prospects for the Summer of 2020. The passage through Lancaster Sound is already navigable:
However as the Canadian Ice Service chart also shows, there are still some areas of 7-8/10 concentration along the Beaufort Sea coast en route to the Bering Strait. The central Canadian Arctic Archipelago is solid 9-10/10 at present, but what’s the prognosis? Here’s the final CryoSat-2/SMOS merged thickness map of the winter, from April 15th:
This suggests that the thickest ice on the usual route through the Northwest Passage for small vessels was around 1.2 meters in Larsen Sound. This seemed suspiciously thin to me, so next I tried the underlying Cryosat-2 data from AWI, which revealed this:
Suspicions confirmed. It looks like AWI are ignoring CS2 data in the CAA for 2020! Here’s how the CPOM Cryosat-2 numbers look for a similar date, which is hopefully nearer the reality:
The CAA was fairly cloud free on June 23rd, and this satellite image shows that surface melt had started across the entire central section of the Northwest Passage:
NASA Worldview “false-color”image of the Canadian Arctic Archipelago on June 23rd 2020, derived from the MODIS sensor on the Terra satellite
All in all it looks to me as though “small vessels” will be able to successfully make it through the Northwest Passage later in the summer of 2020, with thicker ice drifting south into Larsen Sound from the McClintock Channel being a potential bottleneck.
[Edit – August 1st]
Whilst there are certainly some cruise ships planning on voyaging through the Northwest Passage this summer it looks as though there will be very few yachts or other small vessels. According to Transport Canada:
To better protect Arctic communities, pleasure craft are prohibited from operating in Canada’s Arctic coastal waters north of the 60th parallel until October 31, 2020, at the earliest:
to limit any potential interaction with remote and vulnerable coastal communities in consideration of minimal health care infrastructure in these waterways that notably comprise the Northwest Passage as well as the territorial sea of Canada surrounding Nunatsiavut, Nunavik and the Labrador Coast).
to allow the Canadian Coast Guard to focus efforts on essential operations including community resupply ice-breaking, environmental response, and search and rescue.
With this proviso:
In the Canadian Arctic coastal waters, the following measures will not apply to:
Foreign pleasure craft exercising their right of innocent passage within the territorial sea. However, any such transits will be subject to receipt of a 60-day written notice in advance of arrival in Canadian Arctic coastal waters to Transport Canada, and be subject to any conditions the Minister determines necessary to ensure the protection of marine personnel and of local communities (for example, additional insurance, rescue strategy).
[Edit – August 6th]
The skies were clear over the Northwest Passage yesterday, and this is what could be seen from the Aqua satellite:
I don’t know about you, but based on that image I reckon a plucky little yacht like Northabout could just about squeeze past the remaining sea ice along the coast of the Boothia Peninsula?
However let’s also take a look at the charts of the Canadian Ice Service shall we? The daily regional maps don’t cover the “squeeze point” yet, but the weekly map dated August 3rd reveals this:
We’re forced to conclude that officially the Northwest Passage isn’t quite “open” yet!
[Edit – August 7th]
The Canadian Ice Service have extended their daily coverage to the “choke point” we looked at above:
The Northwest Passage is still not “officially” open!
[Edit – August 8th]
The southern “choke point” is still blocking the way, and winds are currently pushing ice into the north of Peel Sound:
This Sentinel 2 image from August 6th shows the Bellot Strait to be completely clear of ice, so despite that route 6 through the Northwest Passage may well be very open soon.
[Edit – August 11th]
Snow White is pleased to announce that she cut the ribbon at the 2020 Northwest Passage route 6 opening ceremony earlier today:
[Edit – August 14th]
Whilst this is no doubt only temporary, the route along the coast of the Boothia Peninsula is now blocked by an area of 7-8/10 concentration ice:
[Edit – August 16th]
Route 6 is open once again, and it is also now possible to take a circuitous route around the north of both Somerset and King William Islands without encountering anything worse than 6/10 concentration ice:
[Edit – August 25th]
As one door opens, another one closes?
[Edit – August 27th]
Making one of my periodic visits to MarineTraffic I couldn’t help but notice a “pleasure craft” approaching Bellot Strait!
According to the Canadian government, he has no business being there. But 72-year-old Peter Smith is sailing the Northwest Passage anyway, in violation of COVID-19-related orders prohibiting most foreign yachts from entering Canadian waters.
But according to a Facebook post on Aug. 20, Bobby Klengenberg, a local observer with the Inuit Marine Monitoring Program, spotted Smith’s custom yacht, the Kiwi Roa, off the coast of Cambridge Bay, Nunavut.
Transport Canada confirmed the sighting in an email to CBC News, and said the vessel was told “to depart Canadian waters and not make landfall.”
A spokesperson said the Canadian Coast Guard will “monitor the vessel’s transit out of the region.” If Smith is indeed found to have broken the law, they wrote, the agency “will not hesitate to take appropriate enforcement action,” including penalties of up to $5,000.
Watch this space!
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