There's an article about this year's rapid loss of Arctic sea-ice in
today's New York Times.  Here's the link:

http://www.nytimes.com/2007/08/10/science/earth/10arctic.html

As the sea-ice extent declines, it's thickness also decreases.  I
think it's likely that the thickness will decline so much that there
will be the chance of a mechanical failure, even before the extent
could actually reaches zero.   The result could look much like the
breakup of the Larson B ice shelf along the Antarctic Peninsula, which
was sudden and spectacular .

Last summer, there was the formation of a large polynya which formed
just to the north of Alaska.  Hers's a discussion of last year's sea-
ice cycle:

http://nsidc.org/news/press/2006_seaiceminimum/20060816_arcticseaicenews.html

That polynya may have been the result of a large tropical cyclone,
which moved out of the tropics and then tracked over Alaska and the
Arctic.  As the sea-ice extent and thickness declines further, one
might reasonably expect that other such storms could trigger a
shattering of the remaining sea-ice, as the tropical cyclones tend to
occur at about the same time as the minimum extent of the Arctic sea-
ice.

As I understand it, there has never been a period in the history of
civilization in which there was no sea-ice over the Arctic.  I'll
leave it to the experts to tell us just what things will be like once
the sea-ice extent has declined to zero, after which there won't be
any multi-year ice in the following winter.   Given that there is a
positive feedback associated with the difference between the albedo of
sea-ice and that of open ocean, it's plausible that multi-year sea-ice
might not reappear in succeeding years.

E. S.


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