Not exact matches
Climate change models predict that the Arctic
sea ice will continue to shrink in a warming world (as much as 40 % of the
ice is expected to be gone
by midcentury), and the resulting changes — including later
formation of
ice in the autumn, rain falling on the snow, and decreasing snow depths — will make it increasingly difficult for the seals to construct their snow caves, NOAA says.
They are called polynyas,
formations that derive their name from the Russian word for «hole in the
ice,» and are typically an expanse of open seawater along the coast that is enclosed
by floating
sea ice and the continental shelf.
The upper part of the modern Arctic Ocean is flushed
by North Atlantic currents while the Arctic's deep basins are flushed
by salty currents formed during
sea ice formation at the surface.
Quick recovery is consistent with the Southern Ocean - centric picture of the global overturning circulation (Fig. 4; Talley, 2013), as the Southern Ocean meridional overturning circulation (SMOC), driven
by AABW
formation, responds to change in the vertical stability of the ocean column near Antarctica (Sect. 3.7) and the ocean mixed layer and
sea ice have limited thermal inertia.
Arctic winter
formation has been largely hit
by advection from cyclones easily punching through what was once a mighty fortress of cold air living in a physical symbiosis with much thicker
sea ice.
Sea ice formation in the Amundsen and Bellingshausen
seas has decreased
by 10 % per decade and has also shortened in seasonal length [40].
Negative delta C - 13 (as) values in glacial AABW were likely caused
by poor ventilation during
formation, probably associated with extensive
sea ice coverage.
That leads to stratification, which leads to an increased
formation of
sea ice, because it's effectively shielded [
by snow],» he said.
These results also increase our overall understanding of glacial − interglacial cycles
by putting further constraints on the timing and strength of other processes involved in these cycles, like changes in
sea ice and
ice sheet extents or changes in ocean circulation and deep water
formation.
The observed effects of cryosphere reduction include modification of river regimes due to enhanced glacial melt, snowmelt advance and enhanced winter base flow;
formation of thermokarst terrain and disappearance of surface lakes in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven
by ice and permafrost melting; regional ocean freshening;
sea - level rise due to glacier and
ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine ecosystems affected
by lake -
ice and
sea -
ice reduction; changes in livelihoods; reduced tourism activities related to skiing,
ice climbing and scenic activities in cryospheric areas affected
by degradation; and increased ease of ship transportation in the Arctic.