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:
Whilst the official PIOMAS volume figures for January have yet to be released Wipneus has worked his usual magic on the gridded thickness numbers to reveal:
not to mention the calculated volume:
and the volume anomaly:
As Wipneus puts it:
Estimated from the thickness data, the latest value is from 31st of January: 17.57 [1000 km3], which is the second lowest value for that day, 2017 is lowest by a rather large margin at 16.16 [1000 km3].
Here are the “measured” thickness maps from SMOS:
and CryoSat-2:
Here are the end of January Arctic wide high resolution AMSR2 graphs based on University of Hamburg data:
In addition, since it’s that time of year, here too is Wipneus’ NSIDC global sea ice extent:
The minimum thus far is very slightly above last year’s value, but perhaps like last year there will be a “double dip”?
Getting back to the Arctic, here is the DMI >80N temperature plot for January:
together with the associated freezing degree days graph:
Here’s a video showing the effect of the mid January cyclones on the sea ice in the Fram Strait and north of Svalbard:
Finally, for the moment at least, here is the current Fram Strait surf forecast for 12:00 UTC on February 5th:
The latest edition of Arctic Sea Ice News has been published. As the NSIDC put it:
January of 2018 began and ended with satellite-era record lows in Arctic sea ice extent, resulting in a new record low for the month. Combined with low ice extent in the Antarctic, global sea ice extent is also at a record low.
Air temperatures at the 925 hPa level (about 2,500 feet above sea level) remained unusually high over the Arctic Ocean. Nearly all of the region was at least 3 degrees Celsius (5 degrees Fahrenheit) or more above average. The largest departures from average of more than 9 degrees Celsius (16 degrees Fahrenheit) were over the Kara and Barents Seas, centered near Svalbard. On the Pacific side, air temperatures were about 5 degrees Celsius (9 degrees Fahrenheit) above average. By contrast, 925 hPa temperatures over Siberia were up to 4 degrees Celsius (7 degrees Fahrenheit) below average. The warmth over the Arctic Ocean appears to result partly from a pattern of atmospheric circulation bringing in southerly air, and partly from the release of heat into the atmosphere from open water areas.
[Edit – February 10th]
The University of Hamburg’s high resolution AMSR2 derived area is bouncing back after the recent cyclone, but extent is currently still declining:
The recent drop in Arctic sea ice extent has pushed the NSIDC global extent to a new all time (satellite era!) low:
September has arrived once again, the month in which the assorted Arctic area and extent metrics (almost) always reach their respective annual minima. Now we can start to speculate about what the assorted minima will be, and on what date.
First of all let’s take a look at “Snow White’s” favourite high resolution AMSR2 metrics derived by “Wipneus” from University of Hamburg AMSR2 concentration data:
As you can see, today’s values are both higher than yesterday’s. Hence we already have potential minima to consider! In this case:
UH AMSR2 Area – 3.65 million km² on September 1st
UH AMSR2 Extent – 4.30 million km² on September 1st
Personally I don’t think those numbers will last long, and here’s one reason why. The “surf forecast” for the far North Atlantic for midday on September 6th:
Some significant swells are currently forecast to batter the ice edge on the Atlantic side of the Arctic over the next few days.
[Edit – September 3rd PM]
Shock news! Tony Heller has made a prediction about this year’s minimum!! Unlike last year, this year the NSIDC 5 day average extent seems to be his Arctic metric of choice:
Tony tells his faithful flock:
The Arctic sea ice minimum this year is very likely going to be be larger than 2016, 2015, 2012, 2011 and 2007.
It is also likely that the minimum extent will be higher than 2010 and 2008.
Instead of reporting the huge gain in ice and massive failure of their forecasts, climate alarmists will report that extent was “8th lowest on record.”
All those years are on the graph above. We shall see.
[Edit – September 15th]
Our normal Arctic sea ice extent 2017 minimum service will be restored as soon as possible. Meanwhile here is the test card:
On the way the cruise’s resident naturalist and Smithsonian lecturer, Michael Scott, risked the wrath of Trump supporters by pointing to some of the changes Greenland is undergoing.
A Nasa map based on data between 2004 and 2014 revealed that the ice is melting across most of Greenland – an area nine times the size of the UK.
Pulling together several papers, Michael said Greenland’s summer melt season now lasts 70 days longer than in the early 1970s.
This melting is unfreezing the fringes of the permafrost, which may explain why Nasa satellites are picking up fires raging where the ice has retreated.
[Edit – September 16th]
It is of course still to early to be 100% certain about this. However:
It certainly looks as though the bottom is in for the University of Hamburg AMSR2 extent: 4.25 million km² on September 11th.
It’s much the same story for JAXA extent:
4.47 million km² on September 9th and 10th.
[Edit – September 19th]
The NSIDC have followed in Snow White’s glass slippered footsteps and tentatively called the minimum:
On September 13, Arctic sea ice appears to have reached its seasonal minimum extent of 4.64 million square kilometers (1.79 million square miles), the eighth lowest in the 38-year satellite record. The overall rate of ice loss this summer was slowed by a persistent pattern of low sea level pressure focused over the central Arctic Ocean.
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.
Minimum volume was reached at 11th September: 4.542 103km3, which is fourth lowest after 2012, 2011 and 2016 (resp 3.673, 4.302, 4.402) and just below 2010 (4.582).
[Edit – September 23rd]
Here’s the 2017 edition of our annual NSIDC daily max/min extent graph:
The maximum extent was the lowest in the satellite record, and the minimum was just fractionally above the trend line. For those that concern themselves with “statistical significance”, the PIOMAS minimum volume was a “statistical tie” for second place:
What seems likely to be the most interesting period of the 2017 Arctic sea ice melting season is upon us! The PIOMAS gridded data hasn’t been released yet, but the overall volume numbers reveal that 2017 has now relinquished its “lowest ever” position to 2012. Here’s Wipneus’ graph of the volume data:
plus his anomaly plot:
Our favourite high resolution AMSR2 area and extent graphs now also allow comparison with 2012. Here’s how they look at the moment:
As you can see, round about now is when 2012 Arctic sea ice extent started to noticeably race ahead of the rest of the pack. Will 2017 follow suit? Are there any Arctic cyclones on the horizon for example? Well, the one forecast for August 4th hasn’t materialised. Here’s this morning’s Environment Canada synopsis:
However both ECMWF and GFS agree that a sub 985 hPa storm should have arrived by Sunday morning. Here’s the ECMWF version from MeteoCiel:
There’s stronger storms in the forecast further out, but once again we’ll believe them if and when we see them!
We’re keeping a close eye on the Northwest Passage once again this year. Most of the southern route is open already, but as we predicted the old ice in Larsen Sound has a lot of melting still to do. Here’s how it looked from the icebreaker Nordica a few days ago:
On top of that the old ice around O-Buoy 14 is currently rushing south down the McClintock Channel to replenish it. Here’s how that looks at the moment:
Meanwhile the melt along the Northern Sea Route is well ahead of last year. Here’s the University of Hamburg AMSR2 concentration map of the area:
There’s also now a lot of open water on the Pacific side of the Arctic, and Sunday’s cyclone is forecast to create a large area of 2 meter plus waves heading in the direction of the ice edge:
I expect that to have a noticeable effect on the already fragile sea ice by early next week, assuming the storm arrives as forecast! There is an ice mass balance buoy handily placed out on the ice in the path of the storm. Buoy 2017A is currently located near 77 N, 147 W, and its assorted sensors suggest the ice underneath it is now less than 20 cm thick:
Here’s how the area around the buoy looked a couple of weeks ago:
Image of 2017A from WARM 6 on July 18th 2017. NSF project: NSF OPP #1603548
The $64,000 question now is will the 2017 Arctic sea ice metrics stay in amongst the recent pack, or race after 2012 instead?
[Edit – August 6th]
This morning’s synopsis from Environment Canada suggests the cyclone has bottomed out at a MSLP of 982 hPa:
Here’s how the cyclone looked from space yesterday:
NASA Worldview “true-color” image of the sea ice north of the Beaufort Sea on August 5th 2017, derived from the VIIRS sensor on the Suomi satellite
I think that I can convince myself that the salinity profile from ice tethered profiler 97, currently located at 73° N, 134° W, reveals mixing from depth in the wake of the storm:
The synthetic aperture radar on the Sentinel 1B satellite can certainly see through the clouds, and reveals open water in the Central Arctic north of the Beaufort Sea yesterday evening (UTC):
Sentinel 1B image of Arctic sea ice at 79° N, 160° W on August 5th 2017
The effects of this weekend’s storm are readily apparent! Just in case you’re wondering Wipneus reports:
Area: -172.0 (+324k vs 2016, +138k vs 2015, -669k vs 2014, -523k vs 2013, +493k vs 2012)
[Edit – August 8th]
The next pulse of swell is currently forecast to be somewhat higher and longer period than the last one. This one is also taking aim at the Beaufort Sea MIZ:
[Edit – August 9th]
According to Environment Canada the latest cyclone is already down to 980 hPa MSLP:
[Edit – August 9th PM]
The MSLP of the current cyclone is now down to 976 hPA:
The latest WaveWatch III forecast has increased the predicted peak height and period of the resulting waves once again:
[Edit – August 10th]
Large holes are appearing in the sea ice on the other side of the Arctic too. Take a look north of the Laptev Sea for example:
NASA Worldview “true-color” image of the “Laptev Bite” polynya on August 10th 2017
Meanwhile the current cyclone on the Pacific side of the North Pole appears to have bottomed out at 974 hPa:
[Edit – August 11th]
Here’s the latest sea ice concentration one day delta map from Wipneus:
Despite the expected divergence caused by a low pressure area crossing the ice, both are and extent of sea ice on the Pacific side of the Arctic are still falling.
[Edit – August 12th]
The waves are considerably smaller in the Beaufort Sea today, but not in the Bering Strait!
Here’s the latest one day delta map:
and here’s video showing the motion of sea ice in the Beaufort & Chukchi Seas so far this summer:
[Edit – August 13th]
Here’s an animation from Wipneus revealing the effect of the two recent cyclones on the Pacific side, plus everything else that’s been going on in the Arctic:
Click the image to see a much larger (3.3 Mb) version.
[Edit – August 16th]
AMSR2 Arctic sea ice extent has taken another tumble, and has dropped below 2016:
Only 2012 left to beat!
[Edit – August 18th]
A PIOMAS mid month update has been released, including gridded thickness data. 2017 modelled volume has failed to follow 2012’s trajectory towards the September minimum, and is now on a par with 2011:
[Edit – August 21st]
After a “brief hiatus” in the wake of the recent cyclones Arctic sea ice area has posted a new low for the year:
Extent has yet to follow suit:
The main loss of area has been in the “Beaufort Bite” once again:
After a comparatively cool May, surface air temperatures in the high Arctic are back up to “normal”:
The condition of the sea ice north of 80 degrees is far from normal however. Here’s what’s been happening to the (normally) land fast ice north west of Greenland:
NASA Worldview “true-color” image of the sea ice north west of Greenland breaking up on June 2nd 2017
Further south surface melt has set in across the southern route through the Northwest Passage:
NASA Worldview “false-color” image of the Coronation Gulf on June 1st 2017, derived from the MODIS sensor on the Terra satellite
Whilst the gap with previous years has narrowed during May, PIOMAS Arctic sea ice volume is still well below all previous years in their records:
The PIOMAS gridded thickness graph suggests that a large area of thick ice is currently sailing through the Fram Strait to ultimate oblivion:
and just in case melt ponds are now affecting those numbers here is extent as well:
The rate of decrease is inexorably increasing! 2012 extent is currently still well above that of 2017, but those positions may well be reversed by the end of June? Here’s NSIDC’s view on the matter:
[Edit – June 8th]
As requested by Tommy, here’s the current Arctic Basin sea ice area:
This includes the Beaufort, Chukchi, East Siberian and Laptev Seas along with the Central Arctic. It excludes the Atlantic periphery, which currently looks like this:
[Edit – June 10th]
At long last a clear(ish) image of water from the Lena Delta spreading out across the fast ice in the Laptev Sea:
NASA Worldview “true-color” image of the Lena Delta on June 10th 2017, derived from the MODIS sensor on the Terra satellite
NASA Worldview “true-color” image of the Lena Delta on June 10th 2012, derived from the MODIS sensor on the Terra satellite
[Edit – June 11th]
DMI’s daily mean temperature for the Arctic area north of the 80th northern parallel has reached zero degrees Celsius almost exactly on the climatological schedule:
We calculate our freezing degree days on the basis of the freezing point of Arctic sea water at -1.8 degrees Celsius. On that basis this winter’s grand total of 3740 was reached on June 1st:
Despite the “coolish” recent weather total FDDs are way below the climatology and other recent years. Consequently there’s a lot less sea ice in the Arctic left to melt at the start of this Central Arctic melting season than in any previous year in the satellite record. However whilst there are some melt ponds visible in the Arctic Basin on MODIS, in that respect 2017 is lagging behind both last year and 2012.
A sub 970 hPa cyclone is starting to enter the realms of realistic possibility, and also forecast are some significant waves in the Chukchi Sea and the expanding 2017 “Laptev Bite”:
[Edit – June 27th]
The forecast cyclone was nowhere near as deep as predicted. According to the analysis by Environment Canada it bottomed out at 980 hPa yesterday:
[Edit – June 29th]
O-Buoy 14 is currently firmly embedded in the fast ice of Viscount Melville Sound, deep in the heart of the Northwest Passage. Here’s the view from the buoy’s camera:
The February 2017 PIOMAS Arctic sea ice volume numbers are out. It’s no longer surprising to report that they are the lowest ever for the month of February in records going back to 1979:
Here’s the PIOMAS gridded thickness map for February 28th:
There does seem to be a small patch of slightly thicker ice in the East Siberian Sea off Chaunskaya Bay, but there’s still a much larger area of sub 0.5 meter thick ice in the Laptev and Kara Seas.
The Danish Meteorological Institute’s temperatures for the “Arctic area north of the 80th northern parallel” graph shows somewhat more “normal” readings in February 2017, but still without falling below the ERA40 climatology this year or in 2016:
The graph of cumulative Freezing Degree Days (FDD for short) is still far below all previous years in DMI’s records going back to 1958:
Finally, for the moment at least, here’s the high resolution AMSR2 Arctic sea ice area and extent:
I’m going to have to eat some humble pie, or crow pie as I gather it’s usually referred to across the Atlantic, following my tentative “2017 maximum prediction” a couple of weeks ago. Both area and extent posted new highs for the year yesterday, with area creeping above 13 million square kilometers for the first time this year.
[Edit – March 7th]
Commenter Michael Olsen suggests that “thicker ice being pushed into the Alaskan and Russian parts of the Arctic Ocean”. Here’s some evidence:
The United States’ National Weather Service current sea ice stage of development map for Alaskan waters:
This week’s Canadian Ice Service sea ice stage of development map is expected later today, so for now here’s last week’s:
Especially for Michael, a visual image of all the “thicker ice [that’s been] pushed into the Russian parts of the Arctic Ocean” courtesy of the nice folks at NASA:
NASA Worldview “true-color” image of the Chukchi Sea on March 10th 2017, derived from the MODIS sensor on the Aqua satellite
[Edit – March 12th]
Yet another strong Arctic cyclone has been battering the sea ice in the Arctic Basin. According to Environment Canada this one bottomed out at 971 hPa at 06:00 UTC today.
It’s far too early to be sure about this yet, but it’s not beyond the bounds of possibility that the 2017 maximum is already in place. Here’s our favourite high resolution extent graph calculated by “Wipneus” from University of Hamburg/JAXA AMSR2 data:
The current maximum Arctic sea ice extent for 2017 is 13.49 million square kilometers on February 19th. Here’s Arctic sea ice area for good measure:
The current maximum area for 2017 is 12.88 million square kilometers on February 20th. Here also is the NSIDC’s 5 day averaged extent:
This reveals a current maximum extent for 2017 of 14.302 million square kilometers on February 20th.
[Edit – March 1st]
Here are the high resolution AMSR2 area and extent graphs for the end of February:
With each day that passes the highs of February 19th/20th look more likely to have been this years maximum. Nonetheless past experience suggests it’s still far to soon to be sure about that.
[Edit – March 10th]
Arctic sea ice area and extent are declining again, having reached new heights for the year on March 3rd:
However the 2013/14 winter showed a late surge is still possible.
[Edit – March 18th]
A “late surge” is looking increasingly unlikely. That being the case, here is our provisional long term graph of NSIDC daily Arctic sea ice extent:
Subject to an unanticipated “surge” the 2017 maximum of 14.447 million square kilometers occurred on March 5th.
JAXA extent has dropped steeply over the last couple of days, and it is now once again “lowest for the date since records began”:
The 2017 JAXA maximum of 13.878 million square kilometers occurred on March 6th.
In the continuing absence of updates to Cryosphere Today area, here’s the high resolution Arctic sea ice area graph calculated by “Wipneus” from University of Hamburg/JAXA AMSR2 data:
The maximum for that particular metric was 13.03 million square kilometers on March 3rd.
The story got some legs. Zack got pushback from some “skeptics” and then the AGU blogged about the story.:
My attention was called to this issue last week thanks to the Twitter feed of Zack Labe, a PhD student in Earth Systems Science at the University of California – Irvine. He makes great graphics showing the latest data on polar climate.
It’s now December 18th, and as far as I’m aware that remains the case in the mainstream media (MSM for short). The Arctic Sea Ice Forum grew out the earlier Arctic Sea Ice Blog (ASIB for short). The proprietor of both the ASIB and ASIF has been revealed by CBC to be one Neven Curlin. They recently interviewed Neven, and even gave him top billing above Sir David Attenborough in the resulting podcast:
However the title of the CBC article is inaccurate, as CBC would surely have noticed if they’d read Neven’s article on the ASIB on the topic of his “sabbatical”.
Now comes news that the “astonishingly low level” of global sea ice area that we brought to the waiting world’s attention on November 7th has today been chosen by The Guardian as one of their:
The story outlined above and the associated graphic graphic are conspicuous only by their absence, but the Grauniad have thoughtfully provided this pretty stock photo of some sea ice:
Scroll down the Guardian’s article to number 11, pausing to read Tamsin Edwards’ section on atmospheric carbon dioxide levels at number 9 on the way down (unlike CO₂ concentrations). There you will discover Professor Andrea Sella’s opinion that:
In October, unprecedented weather patterns drove icy winds across Siberia, pushing Arctic temperatures up to 20C above normal and parts of the Arctic Ocean failed to refreeze; in the Antarctic, sea ice thawed faster than usual. For me the bombshell came from a Dutch blogger in late November: a plot of the Arctic plus Antarctic showed sea ice this autumn to be tracking 4m km2 (the size of western Europe) below the normal average. This is a 7-sigma event – with a chance of about one in a hundred billion of being random. The ice doesn’t lie. If we don’t take this seriously now, our children will ask us why.
The “plot of the Arctic plus Antarctic” Andrea refers to was created by “Wipneus”, who I suppose could reasonably be described as a “Dutch programmer”. Neven could reasonably be described as a blogger, although he is much more than that. Although he was born in The Netherlands he no longer lives there.
This is the Great White Con version as opposed to the NOAA version published during the Fall AGU conference earlier this week, although there is some overlap.
Hot off the presses, here’s how Arctic sea ice age has progressed over the last year and a bit:
The 4 and 5 year old ice looks to be edging away from the area north of the Canadian Arctic Archipelago towards the Fram Strait. Here’s the current CryoSat-2 Arctic sea ice thickness map:
Almost no ice over 2 meters thick to be found in the Beaufort sector or anywhere on the Siberian side of the Arctic. Here’s the current AMSR2 Arctic sea ice area graph:
Lowest for the date in the satellite record. Here’s the NSIDC’s long term trend in November sea ice extent:
Act 1 of a 3 act play according to Don Perovich at AGU. Here’s the current PIOMAS Arctic sea ice volume anomaly graph:
Lowest for the date in the satellite record. Here’s NOAA’s Arctic and global surface temperature graph:
Warmest in a record going back to 1900. Here’s the current DMI >80N surface temperature graph:
and here’s the current Arctic surface temperature anomaly map:
Finally, for the moment at least, here’s global sea ice area just for good measure:
Need I say more? How about this:
Ice has no agenda. It just melts.
Out of the labs and into the streets?
This website uses cookies to improve your experience. We'll assume you're ok with this, but you can opt-out if you wish. Cookie settingsACCEPT
Privacy & Cookies Policy
Privacy Overview
This website uses cookies to improve your experience while you navigate through the website. Out of these, the cookies that are categorized as necessary are stored on your browser as they are essential for the working of basic functionalities of the website. We also use third-party cookies that help us analyze and understand how you use this website. These cookies will be stored in your browser only with your consent. You also have the option to opt-out of these cookies. But opting out of some of these cookies may affect your browsing experience.
Necessary cookies are absolutely essential for the website to function properly. This category only includes cookies that ensures basic functionalities and security features of the website. These cookies do not store any personal information.
Any cookies that may not be particularly necessary for the website to function and is used specifically to collect user personal data via analytics, ads, other embedded contents are termed as non-necessary cookies. It is mandatory to procure user consent prior to running these cookies on your website.
