However, the ice shelves around Antarctica are extremely important
for ice sheet stability, because they hold back the land ice.
Not exact matches
These findings suggest that Greenland's glaciers have been experiencing increasing
ice loss
for at least three decades — a result that may reinforce scientists» concerns over the
stability of the melting
ice sheet.
Working together we can make seismic and GPS measurements that are needed
for understanding key issues about Antarctic and Greenland
ice sheet stability.
Ice shelves are important, because they play a role in the stability of the Antarctic Ice Sheet and the ice sheet's mass balance, and are important for ocean stratification and bottom water formation; this helps drive the world's thermohaline circulati
Ice shelves are important, because they play a role in the
stability of the Antarctic
Ice Sheet and the ice sheet's mass balance, and are important for ocean stratification and bottom water formation; this helps drive the world's thermohaline circulati
Ice Sheet and the ice sheet's mass balance, and are important for ocean stratification and bottom water formation; this helps drive the world's thermohaline circula
Sheet and the
ice sheet's mass balance, and are important for ocean stratification and bottom water formation; this helps drive the world's thermohaline circulati
ice sheet's mass balance, and are important for ocean stratification and bottom water formation; this helps drive the world's thermohaline circula
sheet's mass balance, and are important
for ocean stratification and bottom water formation; this helps drive the world's thermohaline circulation.
Currently, the major focus of this thread is on reconstructing past sea - level changes and understanding the implications of these changes
for ice -
sheet stability and
for ocean dynamics.
Thus the entire 3 — 4 meters of global sea level contained in that
ice sheet may be vulnerable to rapid disintegration, although arguments
for stability of even this marine
ice sheet have been made [94].
The potential
for unstable
ice sheet disintegration is controversial, with opinion varying from likely
stability of even the (marine) West Antarctic
ice sheet [94] to likely rapid non-linear response extending up to multi-meter sea level rise [97]--[98].
The «details» are important and interesting, and may in fact be of key importance to society (rather than just of academic interest...
for example the
stability of the Greenland
ice sheet), but they are called details
for a reason.
states, in part, «Thus, in the foreseeable future, sea - level rise should not threaten the
ice sheet's stability [for Whillans Ice Stream out to the Ross ice shelf].&raq
ice sheet's
stability [
for Whillans
Ice Stream out to the Ross ice shelf].&raq
Ice Stream out to the Ross
ice shelf].&raq
ice shelf].»
Burning all fossil fuels, if the CO2 is released into the air, would destroy creation, the planet with its animal and plant life as it has existed
for the past several thousand years, the time of civilization, the Holocene, the period of relative climate
stability, warm enough to keep
ice sheets off North America and Eurasia, but cool enough to maintain Antarctic and Greenland
ice, and thus a stable sea level.
The potential
for unstable
ice sheet disintegration is controversial, with opinion varying from likely
stability of even the (marine) West Antarctic
ice sheet [94] to likely rapid non-linear response extending up to multi-meter sea level rise [97]--[98].
Ice shelves are perhaps the most important part of the Antarctic ice sheet for its overall stabili
Ice shelves are perhaps the most important part of the Antarctic
ice sheet for its overall stabili
ice sheet for its overall
stability.