Regehr, E. V., N. J. Lunn, S. C. Amstrup, and I. Stirling, 2007: Effects of earlier
sea ice breakup on survival and population size of polar bears in western Hudson Bay.
Rapid
sea ice breakup along the Ronne - Filchner Ice Shelf.
Relative to recent years and potential impacts on polar bear health and survival in Canada, there is nothing alarming in the pattern or speed of
sea ice breakup for 2017, either over Hudson Bay, the southern Beaufort, or the eastern high Arctic.
Unlike 2007, which had a strong unusual wind pattern during all the summer months that contributed to major sea ice loss, summer 2012 meteorology was generally unremarkable, except for a strong storm in early August that contributed to
sea ice breakup.
All of which indicates 2017 won't be an early
sea ice breakup year for WHB polar bears.
Not exact matches
Scientists still do not know what triggers the
breakup of an
ice shelf or when future ones will occur, so they struggle to estimate how quickly glaciers will dump their
ice into the ocean and therefore how much
sea level will rise.
The region is getting stormier, which threatens settlements, aids ocean mixing that funnels nutrients to deeper waters, and could speed the
breakup of
sea ice.
The
breakup and melting of floating
ice has no direct effect on global
sea levels.
«There are suggestions in the literature that accelerated
breakup of
ice shelves will lead to rise of
sea level by several meters by the end of the century,» Godin said.
The consequences of global
sea level rise could be even scarier than the worst - case scenarios predicted by the dominant climate models, which don't fully account for the fast
breakup of
ice sheets and glaciers, NASA scientists said today (Aug. 26) at a press briefing.
Sea ice extent has dropped precipitously as has the amount of old
ice, which is less prone to
breakup.
Since IPCC (2001) the cryosphere has undergone significant changes, such as the substantial retreat of arctic
sea ice, especially in summer; the continued shrinking of mountain glaciers; the decrease in the extent of snow cover and seasonally frozen ground, particularly in spring; the earlier breakup of river and lake ice; and widespread thinning of antarctic ice shelves along the Amundsen Sea coast, indicating increased basal melting due to increased ocean heat fluxes in the cavities below the ice shelv
sea ice, especially in summer; the continued shrinking of mountain glaciers; the decrease in the extent of snow cover and seasonally frozen ground, particularly in spring; the earlier
breakup of river and lake
ice; and widespread thinning of antarctic
ice shelves along the Amundsen
Sea coast, indicating increased basal melting due to increased ocean heat fluxes in the cavities below the ice shelv
Sea coast, indicating increased basal melting due to increased ocean heat fluxes in the cavities below the
ice shelves.
While the
breakup and slipping of
ice sheets is a small part of
sea rise now, he wrote last year, it could easily accelerate under the heating from a «business as usual» path for emissions.
I wonder once the front has retreated from salt water and
sea mist that ultracold deep
ice could refreeze fresh water and slow the
breakup.
«in Western Hudson Bay, the decline in population size, condition, and survival of young as a consequence of earlier
breakup of the
sea ice brought about by climate warming have all been well documented (Stirling et al., 1999; Gagnon and Gough, 2005; Regehr et al., 2005; I. Stirling and N.J. Lunn, unpub.»
I believe that what the phrase is trying to get at is either the acceleration relative to the pause in the 1950 - 1970 period, or the acceleration in accumulation of noticeable consequences — worldwide glacier melt,
sea ice retreat, earlier onset of springtime, (possibly) increasingly intense hurricanes, Larsen - B
breakup, melting of Greenland along the margins, etc..
# 146: my understanding is that
ice shelf
breakup does contribute to eustatic
sea - level rise, as you say, but only a little, and less so for larger
ice shelves (the anchoring is more distant).
Small changes in global
sea level or a rise in ocean temperatures could cause a
breakup of the two buttressing
ice shelves.
There has been discussion of the role of an August storm in 2012; the storm contributed to
breakup of the
sea ice and perhaps enhanced
sea ice decay.
The findings indicate that
ice shelf
breakup may rapidly lead to
sea level rise.
A run of bad news from the climate scientists might convince a government that the
breakup of the Greenland
ice sheet was accelerating, and that Earth's low - lying areas were facing an imminent rise of 3 feet or more in
sea level.
Tagged adaptation, declining
sea ice, early
breakup, evolution, historical
sea ice record, indivdual variation, late freeze - up, natural selection, NSIDC, polar bear, resilience,
sea ice minimum,
sea ice variability, Stirling, Stroeve, survival, western hudson bay
Tagged Arviat, BBC,
breakup, freeze - up, invasive research, Lunn, mark - recapture, Nunavut, polar bear,
sea ice, Tyrrell, western hudson bay
In 1992 when
breakup of
sea ice was delayed by 25 days, the body condition of all ringed seals declined.
While the iceberg isn't hugely concerning, it could herald the
breakup of the entire Larsen C
ice shelf, which could trigger more
sea - level rise.
Comments Off on
Breakup of
sea ice on track in Canada as critical feeding period for polar bears ends
The high temperatures also helped fuel wildfires and hastened the
breakup of
sea ice in the Chukchi Sea.&raq
sea ice in the Chukchi
Sea.&raq
Sea.»
«Satellite photos from mid-May depict an early
sea -
ice breakup with an ominous series of openings, known as leads, extending deep into the Arctic,» said a statement from NOAA.
Tagged
breakup, Churchill, climate change, East Greenland, global warming, grizzly, grizzly bears, habitat, Henrik Hansen, hybrids, Nunavut, polar bear, Polar Bears International, polarbearscience, population estimate, problem bears, radio,
sea ice,
sea ice declines, Wapusk National Park, western hudson bay, WWF
IMO, the strongest argument for
sea ice decline over the last decade for being unusual and at least in part attributable to global warming is this (from Polyakov et al.): The severity of present
ice loss can be highlighted by the
breakup of
ice shelves at the northern coast of Ellesmere Island, which have been stable until recently for at least several thousand years based on geological data.