Sorry for the forum being offline some hours, guys! DM
could it be that the increased water vapour content of the atmosphere will result in more snow being deposited on high altitude glaciers?
subgeometerQuoteIs there a thread where image retrieval and animation are discussed?Yes, to the animation part, anyway.http://forum.arctic-sea-ice.net/index.php/topic,1259.msg89520.html#msg89520[/quoTigertown
Is there a thread where image retrieval and animation are discussed?
Granted this is valid for 5 days most, but I wonder if this is the recurrent configuration Ding was referring to: highs persistent over Greenland Canada and Arctic with lows pulling warmth from the continents (in summer). Just a comment, not sure it is even close :-)
Look for major drops in extent in the Bering over the next few days.
The temperature at Utqiagvik (Barrow), by contrast, might not reach the melting point until well into May. That's the difference between 64 and 71 degrees N.
And still at least 2 weeks before getting April PIOMAS update. Am I the only one in confusion ?
So much data saying Melt (DMI, Arctic anomaly, Fram export, destruction of sea ice sheets integrity from multiple observations etc. etc.). And yet jaxa sea ice decline remains at a glacial pace, and sea ice volume not declining yet. And still at least 2 weeks before getting April PIOMAS update. Am I the only one in confusion ?
Quote from: gerontocrat on April 20, 2017, 06:28:45 PMSo much data saying Melt (DMI, Arctic anomaly, Fram export, destruction of sea ice sheets integrity from multiple observations etc. etc.). And yet jaxa sea ice decline remains at a glacial pace, and sea ice volume not declining yet. And still at least 2 weeks before getting April PIOMAS update. Am I the only one in confusion ?I think the answer is dispersion, GC. Less ice, spread more thinly.
Great chart. One more idea... fwiw: If you went 3D and made the z axis the ytd measure. So the 3D chart grows in depth each day of the year.
The Bering and Chukchi from April 15-21 with april 19 2016 by way of comparison. Doesn't look good
.... The pattern by now seems to be a continuation of that movement away from the Russian side. That is now driving a bifurcation, with some of the compressed ice turning left and heading towards the Atlantic side kill zone and the rest turning right towards the Beaufort Sea. ....
Quote from: jdallen on April 20, 2017, 08:42:44 PMQuote from: gerontocrat on April 20, 2017, 06:28:45 PMSo much data saying Melt (DMI, Arctic anomaly, Fram export, destruction of sea ice sheets integrity from multiple observations etc. etc.). And yet jaxa sea ice decline remains at a glacial pace, and sea ice volume not declining yet. And still at least 2 weeks before getting April PIOMAS update. Am I the only one in confusion ?I think the answer is dispersion, GC. Less ice, spread more thinly.AKA -- Winter Storms.
On the left 21 April 2012, and on the right 20 April 2017.
This opening is very unusual up that high. I suspect warm SSTs and atlantification.
Quote from: meddoc on April 22, 2017, 08:16:54 AMThis opening is very unusual up that high. I suspect warm SSTs and atlantification.meddoc your suspicion is wrong, please read the "Nares Strait" thread in the Greenland section. There is an almost-constant surface flow from the Lincoln Sea southwest down the strait. When the thick ice gets stuck at the entrance it may form an "arch", as happened this year (more often an arch is created in Kane Basin at the other end of the strait). The surface flow then keeps clearing the area below the arch.Also search the web for the "North Water Polynya".
Quote from: Thomas Barlow on April 21, 2017, 09:33:26 PMOn the left 21 April 2012, and on the right 20 April 2017.2012 was not particularly thin ice (compared to other recent years) in mid-april. Yes, whatever weather condition cleared the ice out in 2012 re-occurs in 2017, the ice is going to have a big problem. 2011 and 2016 might be better comparisons for relatively thin ice in April and a low extent in September?
... Barents + Greenland Sea (victims of Fram export) and Baffin (southbound drift) are running high in extent - this is ice on its way to hell - while the Pacific side (Bering, Okhotsk, Chukchi) is running low. The ice is weak, thin and broken but is still covering the same extent....
Here is the comparison for 2016 .Are there any charts that try to gauge thickness or volume for just the main Arctic Basin?All the charts take into account all the channels and east Greenland, and may not say much about state of main Arctic Basin icepack.( I took out the thick ice that is pushed up against land masses, as I think some of that would be there anyway, even in a future meltdown, and doesn't tell us too much about the state of the overall icepack in the Arctic Basin. And I took out ice in channels and Fram export, as those are not really part of the main state of the Arctic basin icepack)I'd say 2017 looks in worse shape than 2016?
This compares thickness, for certain thickness ranges only.Between 2016 and 2017.(I'm guessing most sources out there are just approximate, with a wide margin of error?)
Interesting that this polynya that appeared about 1 week ago in ESS is about the only one within the Arctic proper not showing signs of refreeze. Why there?Being April 22 big chances it will stay open.
A close-up of the evolution of SST anomalies in Bering sea during past 30 days or so (from the DMI SST anomalies maps). Insolation and ocean currents make a difference there already.
Its quite stunning how fast the current is surging along there.
Lets try a homemade one rather than a NASA nasty.Its quite stunning how fast the current is surging along there. I know that often warmer salty water slides in on the bottom through the Bering straight, while it can even be flowing out on the surface. Certainly if its Pacific water making it all the way along there, the offshore wind would blow the fresher lens away and help it surface.Still not playing. is there a size limit?I guess yes.