W. Broecker, interview by Weart, Nov. 1997, AIP; data: e.g., a biologist reported pollen evidence that there was
no open polar sea in the Wisconsin glacial period.
Not exact matches
Discussions about the consequences of the vanishing ice usually focus either on the
opening up of new frontiers for shipping and mineral exploitation, or on the plight of
polar bears, which rely on
sea ice for...
As a result of atmospheric patterns that both warmed the air and reduced cloud cover as well as increased residual heat in newly exposed ocean waters, such melting helped
open the fabled Northwest Passage for the first time [see photo] this summer and presaged tough times for
polar bears and other Arctic animals that rely on
sea ice to survive, according to the U.S. Geological Survey.
With an overall length of 66 m, this versatile and stable vessel is suited for research on both coastal
seas and
open oceans (except for the
polar regions).
a) Satellite image showing fast disintegration of
sea ice over a
polar continental shelf; b) Zoobenthos on an Antarctic continental shelf; c) Examples of
sea mosses (specimens on the left are from an
open - water location and hence have had more plankton to feed on); and d) Dead bryozoan and other benthic skeletons covering the seabed, most likely to be buried, sequestering their blue carbon in the seabed.
Collapsing ice shelves and melting
sea ice leaves more
open water in the Earth's
polar regions (photo a in earlier figure).
The paper, «Long - distance swimming by
polar bears (Ursus maritimus) of the southern Beaufort
Sea during years of extensive
open water,» is published in the Canadian Journal of Zoology.
Historically, there had not been enough
open water for
polar bears in this region to swim the long distances we observed in these recent summers of extreme
sea ice retreat.»
A
polar sea without ice
opens a new stage in the glacial cycle.
It is not that the
polar regions are amplifying the warming «going on» at lower latitudes, it is that any warming going on AT THE POLES is amplified through inherent positive feedback processes AT THE POLES, and specifically this is primarily the ice - albedo positive feedback process whereby more
open water leads to more warming leads to more
open water, etc. *** «Climate model simulations have shown that ice albedo feedbacks associated with variations in snow and
sea - ice coverage are a key factor in positive feedback mechanisms which amplify climate change at high northern latitudes...»
These studies covered the entire spectrum of waterworld habitats — the
polar and temperate
seas, the
open oceans, the tropics, the coral reefs, the kelp forests, the marine estuaries, and the fishing grounds.
The intercontinental highway through the
polar sea has been
open since July and will begin closing again in late October.
... observations suggested the bears drowned in rough
seas and high winds and «suggest that drowning - related deaths of
polar bears may increase in the future if the observed trend of regression of pack ice and / or longer
open water periods continues.»
However, the fact that
polar bears in the Chukchi
Sea and Southern Davis Strait are thriving despite dramatic declines in summer sea ice (aka an extended open - water season), proves my point and disproves their premi
Sea and Southern Davis Strait are thriving despite dramatic declines in summer
sea ice (aka an extended open - water season), proves my point and disproves their premi
sea ice (aka an extended
open - water season), proves my point and disproves their premise.
«During aerial surveys in September 1987 — 2003, a total of 315 live
polar bears were observed with 12 (3.8 %) animals in
open water, defined for purposes of this analysis as marine waters > 2 km north of the Alaska Beaufort
Sea coastline or associated barrier islands.
Schliebe, S., K. D. Rode, J. S. Gleason, J. Wilder, K. Proffitt, T. J. Evans, and S. Miller, 2008: Effects of
sea ice extent and food availability on spatial and temporal distribution of polar bears during the fall open - water period in the Southern Beaufort S
sea ice extent and food availability on spatial and temporal distribution of
polar bears during the fall
open - water period in the Southern Beaufort
SeaSea.
For example, reductions in seasonal
sea ice cover and higher surface temperatures may open up new habitat in polar regions for some important fish species, such as cod, herring, and pollock.128 However, continued presence of cold bottom - water temperatures on the Alaskan continental shelf could limit northward migration into the northern Bering Sea and Chukchi Sea off northwestern Alaska.129, 130 In addition, warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.
sea ice cover and higher surface temperatures may
open up new habitat in
polar regions for some important fish species, such as cod, herring, and pollock.128 However, continued presence of cold bottom - water temperatures on the Alaskan continental shelf could limit northward migration into the northern Bering
Sea and Chukchi Sea off northwestern Alaska.129, 130 In addition, warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.
Sea and Chukchi
Sea off northwestern Alaska.129, 130 In addition, warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.
Sea off northwestern Alaska.129, 130 In addition, warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering
Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.
Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If ocean warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.134
They found that
open oceans are much less efficient than
sea ice when it comes to emitting in the far - infrared region of the spectrum, a previously unknown phenomenon that is likely contributing to the warming of the
polar climate.
Tagged Beaufort, Chukchi
Sea, Hudson Bay, ice cover, melt, open water, polar bear, polynya, sea ice, seals, shore leads, wi
Sea, Hudson Bay, ice cover, melt,
open water,
polar bear, polynya,
sea ice, seals, shore leads, wi
sea ice, seals, shore leads, winds
Sorry, but cute
polar bears swimming in the
open sea just isn't equivalent.