Top panels: 50 % annual sea ice concentration (dashed blue line) and buoyancy fluxes, where negative values (blue shading) are associated
with sea ice formation; note that these areas expand equatorward in the LGM simulation.
Not exact matches
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.
When combined
with increased ocean stratification due to this enhanced run off [11],
sea - surface temperatures are depressed, encouraging
sea -
ice formation.
As
sea levels rose during the last
Ice Age, the cave flooded and its roof collapsed into this sinkhole resulting in a marine wonder known for its sparkling blue waters, wealth of coral
formations, sharks and fish, and deep caves filled
with stalactites.
These models consist of connected sub-modules that deal
with radiative transfer, the circulation of the atmosphere and oceans, the physics of moist convection and cloud
formation,
sea ice, soil moisture and the like.
When the
sea -
ice coverage further decreases they become associated
with (irregular) deepwater
formation.
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.
The paper, combining evidence of driftwood accumulation and beach
formation in northern Greenland
with evidence of past
sea -
ice extent in parts of Canada, concludes that Arctic
sea ice appears to have retreated far more in some spans since the end of the last
ice age than it has in recent years.
Boundary layers came
with the
formation of
sea ice.
Experts
with the National Snow and
Ice Data Center say formation of sea ice around the Arctic Ocean probably petered out about two weeks a
Ice Data Center say
formation of
sea ice around the Arctic Ocean probably petered out about two weeks a
ice around the Arctic Ocean probably petered out about two weeks ago.
Negative delta C - 13 (as) values in glacial AABW were likely caused by poor ventilation during
formation, probably associated
with extensive
sea ice coverage.
The researchers show that models simulating strong LGM
sea ice formation also exhibit enhanced stratification and a shallower Atlantic Meridional Overturning Circulation (AMOC), largely consistent
with the geological evidence.
Thus, two - thirds of the 180 m
sea - level change between the
ice - free planet and the LGM occurred
with formation of Northern Hemisphere
ice (and probably some increased volume of Antarctic
ice).
With the use of a climate model of intermediate complexity, we demonstrate that with mwp - 1A originating from the Antarctic Ice Sheet, consistent with recent sea - level fingerprinting inferences, the strength of North Atlantic Deep Water (NADW) formation increases, thereby warming the North Atlantic region and providing an explanation for the onset of the Bølling - Allerød warm inter
With the use of a climate model of intermediate complexity, we demonstrate that
with mwp - 1A originating from the Antarctic Ice Sheet, consistent with recent sea - level fingerprinting inferences, the strength of North Atlantic Deep Water (NADW) formation increases, thereby warming the North Atlantic region and providing an explanation for the onset of the Bølling - Allerød warm inter
with mwp - 1A originating from the Antarctic
Ice Sheet, consistent
with recent sea - level fingerprinting inferences, the strength of North Atlantic Deep Water (NADW) formation increases, thereby warming the North Atlantic region and providing an explanation for the onset of the Bølling - Allerød warm inter
with recent
sea - level fingerprinting inferences, the strength of North Atlantic Deep Water (NADW)
formation increases, thereby warming the North Atlantic region and providing an explanation for the onset of the Bølling - Allerød warm interval.