All of which indicates 2017 won't be an early sea
ice breakup year for WHB polar bears.
Not exact matches
«Within a few months» of a
breakup, explains glaciologist Ted Scambos of the National Snow and
Ice Data Center at the University of Colorado at Boulder, the glacier «accelerates significantly, and within a year or two, it can be moving [toward the ocean] up to four times as fast as it moved when the ice shelf was intact.&raq
Ice Data Center at the University of Colorado at Boulder, the glacier «accelerates significantly, and within a
year or two, it can be moving [toward the ocean] up to four times as fast as it moved when the
ice shelf was intact.&raq
ice shelf was intact.»
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.
With this unofficial time, this
year places 4th earliest for the
breakup of
ice in the Tanana river.
-- There is a discrepancy between the above map showing the retreat of the
ice breakup points and the NASA map over 150
years (7 MB.
Negative interactions between polar bears and humans, such as bears foraging in garbage dumps, have historically been more prevalent in
years when
ice - floe
breakup occurred early and polar bears were relatively thin.
Summer
ice breakup on western Hudson's Bay now occurs two weeks earlier than it did 20
years ago, and killer whales have moved their hunting into the bay.
The tipping point was 1998, after which the trend has been later
ice breakups, at a rate of about half of a day per
year.
Although they never knew exactly when it would happen, they had come to expect and prepare for
ice breakups, which have become more common in recent
years.
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.
Even watching the annual
ice breakup is a few weeks, but the problem on the West Antarctic
ice sheet is that it is building up less every
year.
Breakup for Western Hudson Bay (WHB) is looking to be later than usual this year, given that the average breakup date since 1991 has been July 1 (using a 30 % threshold)-- only a few days from now — and the ice in WHB is nowhere near 50 % coverage, let alon
Breakup for Western Hudson Bay (WHB) is looking to be later than usual this
year, given that the average
breakup date since 1991 has been July 1 (using a 30 % threshold)-- only a few days from now — and the ice in WHB is nowhere near 50 % coverage, let alon
breakup date since 1991 has been July 1 (using a 30 % threshold)-- only a few days from now — and the
ice in WHB is nowhere near 50 % coverage, let alone 30 %.
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.