Tough call. There aren't a lot of tasty seals on dry land, for one thing. Could they pick up a new food source that is high enough in fat to sustain them?Anyone think small populations of polar bears could adapt and survive in northern greenland/canada if summer ice is scarce?
which also shows that the Antarctic ice is hovering around a bit of a maximum
This NOAA set of graphs suggests we have reached and are about to surpass the temperatures of the Medieval Warm Period in the northern hemisphere, at least as far back as 800 CE. However, there is enough ice cover left from the Little Ice Age so that we probably have more perennial ice right now than during the maximum of the Medieval Warm Period.This is hardly an unprecidented loss of sea ice. A thousand years ago the Vikings sailed the Artic pretty much unencumbered by ice. They gave Greenland its name because of its lush green pastor land. Then everything froze up and they abandoned that island. For the next 500 years everyone called it the little ice age, until recently when things began to warm up we started calling it global warming. Well, warming is what you expect when we come out of an ice age to re-establish what was normal several centuries ago.
Arctic Cyclone Breaks Up Sea Ice
A powerful storm wreaked havoc on the Arctic sea ice cover in August 2012. This visualization shows the strength and direction of the winds and their impact on the ice: ...cont'd.
Interesting. I don't recall this being mentioned in broadcast discussions of the loss of Arctic sea ice cover. However, there has been a steady decline in multi-year sea ice over the past decade. The older thicker ice is more resistant to storms. Right now, winter re-freezing will leave about 2/3 of the Arctic Ocean with single year ice when the sea ice area reaches its maximum.
Yes, NSIDC comments.....
It seems a reasonable comment that it is total ice volume rather than simply ice extent which is critical here. So ice may have continued thinning at a steady rate since the last record melt in 2007, which is what makes it more prone to mechanical break up and an apparent more abrupt lurch in one year.However, the effects of an individual strong storm, like that observed in early August, can be complex. While much of the region influenced by the August cyclone experienced a sudden drop in temperature, areas influenced by winds from the south experienced a rise in temperature. Coincident with the storm, a large area of low concentration ice in the East Siberian Sea (concentrations typically below 50%) rapidly melted out. On three consecutive days (August 7, 8, and 9), sea ice extent dropped by nearly 200,000 square kilometers (77,220 square miles). This could be due to mechanical break up of the ice and increased melting by strong winds and wave action during the storm. However, it may be simply a coincidence of timing, given that the low concentration ice in the region was already poised to rapidly melt out.