However,
ice shelves play a very important role in «buttressing» their tributary glaciers.
Not exact matches
Suture zones are complex and more heterogeneous than the rest of the
ice shelf, containing
ice with different properties and mechanical strengths, and therefore
play an important role in controlling the rate at which rifts grow.
But the same process of sea
ice formation and brine production along coastal
shelves plays a critical role wherever it occurs.
Surface melting is thought to have
played a big part in the break - up of the nearby Larsen B
ice shelf in 2002.
For example, some exciting work being done by David Pollard and Rob DeConto suggests that processes such as
ice - cliff collapse and
ice -
shelf hydrofracturing may
play important roles in future
ice sheet behavior that have not been well incorporated into most
ice sheet models.
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 circulati
ice sheet's mass balance, and are important for ocean stratification and bottom water formation; this helps drive the world's thermohaline circulation.
Meanwhile, compressed recordings of an Antarctic
ice shelf are
played through speakers, like slow, foreboding sirens.
There is already strong evidence that anthropogenic forcing has
played a significant role in the collapse of
ice shelves on the Antarctic Peninsula, cause by significant melting at the surface during summer.
Larsen B glaciers are too small to significantly affect sea level, but the processes that acted on this area could
play out on other, bigger
ice shelves.
«We conclude that
ice -
shelf basal melting
plays a role in determining patterns of surface and basal crevassing.
That suggests that the 1940s tropical warming could have started the changes in the Amundsen Sea
ice shelves that are being observed now... He emphasized that natural variations in tropical sea - surface temperatures associated with the El Niño Southern Oscillation
play a significant role.»
Indeed, the long lifetime of fossil fuel carbon in the climate system and persistence of the ocean warming ensure that «slow» feedbacks, such as
ice sheet disintegration, changes of the global vegetation distribution, melting of permafrost, and possible release of methane from methane hydrates on continental
shelves, would also have time to come into
play.
Recent fieldwork at the Larsen C
ice shelf, a much bigger one, showed that the same process may soon
play out there.
They calculated that only 13 % of the total
ice shelf area of Antarctica could be called «passive»
ice − that is, it
plays no role in buttressing or slowing the land - borne
ice.
The
shelf ice plays an important role in slowing the progress of south polar glaciers: remove the
shelf ice and the glacier flow accelerates.