Arctic Sea Ice

ASI 2016 update 2: closing the gap

During the melting season I'm writing (bi-)weekly updates on the current situation with regards to Arctic sea ice (ASI). Because of issues with data based on the SSMIS sensor aboard DMSP satellites, I mainly focus on higher-resolution AMSR2 data from the Japan Aerospace Exploration Agency (JAXA), as reported on the Arctic Data archive System website. I also look at other things like regional sea ice area, compactness, temperature and weather forecasts, anything of particular interest.

The animation on the right consists of NSIDC
sea ice concentration maps, one for each ASI update.

Check out the Arctic Sea Ice Graphs website (ASIG)
for daily updated graphs, maps, live webcam images, and
the Arctic Sea Ice Forum (ASIF) for detailed discussions.

June 11th 2016

This update could have easily borne the same title as update 1: Both sides. Two weeks ago the ice pack was shrinking on both sides of the Arctic, causing sea ice extent to drop to unprecedented daily lows. In the meantime, weather patterns have switched and the ice pack is now expanding on both sides!

Of course, a dispersing ice pack will cause extent loss to slow down, or even stall completely for a while. Especially if extent was extremely low to begin with. And so that enormous gap between this year and 2012 is getting smaller every day, fast. 2012 had perfect weather for melting during the first two weeks of June, and there was a large amount of thin ice that kept extent artificially high.

More importantly, these weather conditions set the tone for the rest of the 2012 melting season, as a large amount of melt ponds preconditioned the ice for big melts during July and August. This is where 2016 is falling behind now, even though it has been and still is lowest in many respects (extent, volume, snow cover).

2012 is punching hard in this round. Will it be enough to knock 2016 out?

Meanwhile, on the other side

Lately the focus has been on the Beaufort Sea where a high-pressure area has caused the ice pack to crack on a massive scale, even earlier than in previous years, with ice being transported away from the North American coast (see here). But such a large and persistent high-pressure system is bound to have an impact elsewhere in the Arctic as well, so here's an overview of what's been happening on the Atlantic side of the Arctic (and a bit of Siberia as well).

As we saw in the recent 2015/2016 Winter analysis blog post, the Arctic experienced an incredibly warm/non-cold winter:

On top of that, a string of cyclones crossed the Atlantic and veered off to the Arctic, causing increased ocean heat flux on the Atlantic side of the Arctic, which explains why the Barentsz Sea and Greenland Sea have been anomalously low in sea ice extent all winter. They're still extremely low:

In fact, Svalbard could almost be circumnavigated several times, with at one point very close to ice-free conditions from Svalbard all the way to Franz Josef Land.This graph from the PolarView website shows how anomalously low sea ice levels have been in the Svalbard region: