A new month is upon us and Christmas is coming! Here’s another look at Lars Kaleschke’s high resolution AMSR2 area and extent graphs for the Arctic as a whole:
Extent increase stalled for the last few days of November, and as a result extent is now in a “statistical tie” with 2017 for 4th lowest extent for the date in the AMSR2 record.
Continue reading Facts About the Arctic in December 2022The 2022/23 freezing season has begun, so to begin with here are Arctic sea ice area and extent during its early stages:
Both metrics are currently tracking 2021 quite closely.
Here too is an AMSR2 animation of the transition from melting to freezing in the Central Arctic. Click to animate, and be warned that the file size is almost 10 Mb:
Another big storm is heading for the Chukchi Sea. The GFS forecast currently shows a sub 960 hPa low developing on Thursday:
Continue reading Facts About the Arctic in October 2022We’ll start the new month in traditional fashion. Here’s the high resolution AMSR2 sea ice extent and area:
Extent decline in July proved to be somewhat sluggish by recent standards. A week ago I posed the question:
Is 2022 more likely to follow the path of 2012, 2013 or 2016 to this year’s minimum?
At the moment the answer seems to be “2013 Jim!”. However what about the condition of all that ice? Here’s the latest AMSR2 concentration map:
Continue reading Facts About the Arctic in August 2022After 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:
For detailed analysis of Arctic sea ice extent over the next few weeks please see the 2022 maximum extent thread. However to get the new open thread going here is the current JAXA/ViSHOP extent graph:
It’s looking more and more as though the real maximum for 2022 occurred close the false peak on February 23rd.
Arctic sea ice volume will keep increasing for a while longer. Here is the current AWI CryoSat-2/SMOS volume graph:
The recent “flat line” in extent is in part due to recent events on the Pacific periphery of the Arctic. Take a look at this animation of AMSR2 sea ice concentration:
The gap varies depending on how the wind blows, but there is still evidence of open water (or very thin ice) along the shore of the Beaufort and Chukchi Seas. Here’s the Mackenzie Delta and the adjacent Beaufort Sea on March 5th:
Continue reading Facts About the Arctic in March 2022A 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!
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!
Next here’s the prediction of the late, great Andrew Slater’s Probabilistic Ice Extent algorithm:
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:
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.
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?
High resolution area and extent both posted marginal new lows for the year yesterday:
According to the latest edition of the NSIDC’s Arctic Sea Ice News:
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:
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?
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:
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):
Here is Wipneus’ latest AMSR2 concentration delta map:
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)
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:
According to Environment Canada the latest cyclone is already down to 980 hPa MSLP:
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:
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:
Meanwhile the current cyclone on the Pacific side of the North Pole appears to have bottomed out at 974 hPa:
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.
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:
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.
AMSR2 Arctic sea ice extent has taken another tumble, and has dropped below 2016:
Only 2012 left to beat!
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:
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:
The SIPN August sea ice outlook has been released. Here are the predictions:
Watch this space!
In 2017 Antarctic sea ice extent is beating all the records. All flavours of the metric are already below the minimum of all previous years in the satellite record, and it looks like there’s still some more melting left to go. Here’s the NSIDC’s 5 day averaged extent:
and here’s JAXA’s 2 day averaged version:
Finally, for the moment at least, here’s the current map of Antarctic sea ice concentration from the University of Bremen:
It seems highly likely that the 2017 Antarctic sea ice minimum extent has now been reached. Here’s the NSIDC 5 day averaged extent graph:
The minimum extent of 2.106 million square kilometers was reached on March 3rd. Here’s the University of Bremen’s Antarctic sea ice concentration map for March 3rd:
We asked this question last year, albeit a couple of weeks later. It looks like it is if you only peruse passive microwave visualisations such as this one:
However if you were the captain of a yacht attempting to sail through the Northwest Passage this year you might well have some reservations. For example, the Barrow webcam (currently stuck on July 31st) reveals this:
Here’s the associated National Weather Service ice chart:
Meanwhile further east the approach to the often troublesome “choke point” of Bellot Strait looks like this from the Suomi satellite:
whilst the associated Canadian Ice Service ice chart looks like this:
Discretion being the better part of valour, in all the circumstances waiting a day or two longer before casting off might prove prudent:
Clearer skies over the Northwest Passage yesterday reveal the remaining ice:
Here’s the CIS chart of the area from yesterday evening:
Here’s the August 7th CIS chart for the Queen Maud Gulf and points north:
Today there looks to be a route past Gjoa Havn and through Bellot Strait that doesn’t involve negotiating more than 3/10 concentration sea ice. The ice has been pushed back from Point Barrow too, so by my reckoning we can now declare one route through the Northwest Passage “open”, for the moment at least.
A nice clear MODIS image of the Northwest Passage yesterday:
backed up by the CIS ice charts:
