Again this year – contrary to predictions – there has been no early breakup of the sea ice on Hudson Bay and even though it’s the height of summer, there is plenty of ice throughout the Arctic to act as a feeding platform for polar bears. This makes it unlikely there will be a longer-than-average summer fast for polar bears again this year.
Sea ice maps around the Arctic for June 21 (and June 24, for Hudson Bay) reviewed and discussed below in relation to polar bear habitat — have a look.
Posted in Conservation Status, Sea ice habitat
Tagged Chukchi Sea, critical feeding period, early summer ice coverage, Hudson Bay breakup, Jon Aars, polar bear, polar bear habitat, sea ice maps, spring sea ice, summer fast, Svalbard, Svalbard cubs, western hudson bay
Polar bears are all out on the sea ice at this time of year, feeding on new-born seal pups. Here’s a look at what the ice conditions are like at this critical time.
The ice extent is still well within two standard deviations from the 1981-2010 average, which indicates no deviation from natural variation, as the graph (below) for May 1, 2014 from the US National Snow and Ice Data Center (NSIDC) shows.
Between the official spring maximum (according to the NSIDC ) on March 21, with a total extent of 14.8 million km2, the ice slowly retreated in some regions and increased in others, while most regions remained pretty much the same. This is an important reminder that the Arctic as a whole is not a homogeneous region but one with marked regional variation.
As has been noted elsewhere (Sunshine Hours), ice in the Greenland Sea (habitat of ‘East Greenland’ bears) and the Barents Sea both increased in extent over this period. Bering Sea ice (habitat of southern ‘Chukchi Sea’ bears) declined markedly but Baffin Bay/Gulf of St. Lawrence ice (habitat of ‘Davis Strait’ bears) declined much less, as NOAA’s MASIE maps copied below show very well.
Posted in Life History, Sea ice habitat
Tagged arctic sea ice, baffin bay, Barents Sea, Bering Sea, critical feeding period, Davis Strait, Greenland Sea, polar bear, regional variation, sea ice extent, sea ice thickness, spring ice maximum
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