Researchers hope to incorporate all of these factors into computer models of ice sheets, which still struggle to mimic how real ice
sheets respond to climate change.
It's the fast - moving ice that determines how the ice
sheet responds to climate change on a short timescale,» said Robert Bindschadler, a NASA scientist at the Goddard Space Flight Centre in Maryland, one of the study's co-authors.
Not exact matches
Their field - based data also suggest that during major
climate cool - downs in the past several million years, the ice
sheet expanded into previously ice - free areas, «showing that the ice
sheet in East Greenland
responds to and tracks global
climate change,» Bierman says.
A report in the last issue of Nature finds that between April 2002 and April 2006, the rate at which southern Greenland's ice liquefied jumped by 250 percent — supporting the idea that the Greenland ice
sheet responds quickly
to slight
changes in
climate.
A new study suggests some of Antarctica's ice
sheet grows from the bottom up, adding a new wrinkle
to efforts
to predict how the continent's glaciers will
respond to climate change.
«Simply put, the shape of the ice
sheet and the contact with the ocean makes it likely that these areas
respond more pronouncedly
to changes in
climate boundary conditions — be they atmospheric, oceanic or glaciological.»
However, effec - tive communication with the public of the urgency
to stem human - caused
climate change is hampered by the inertia of the
climate system, especially the ocean and the ice
sheets, which
respond rather slowly
to climate forcings, thus allow - ing future consequences
to build up before broad public con - cern awakens.
Implications include (i) the expectation of additional global warming of about 0.6 °C without further
change of atmospheric composition; (ii) the confirmation of the
climate system's lag in
responding to forcings, implying the need for anticipatory actions
to avoid any specified level of
climate change; and (iii) the likelihood of acceleration of ice
sheet disintegration and sea level rise.
The time needed for ice
sheets to respond to climate change is uncertain, and there are proponents for time scales covering a huge range.
IceBridge is a six - year campaign
to survey and monitor areas of Earth's polar ice
sheets, glaciers and sea ice and how they are
responding to climate change.
A significant uncertainty in future projections of sea level is associated with dynamical
changes in the Antarctic and Greenland ice
sheets and a key aspect of this uncertainty is the role of ice shelves, how they might
respond to climate change, and the effect this could have on the ice
sheets.
His research focuses on understanding the interactions of ice, ocean and
climate, in particular using imaging radar observations from satellites and airplanes
to determine how the ice
sheets in Antarctica, Greenland and Patagonia will
respond to climate change and affect global sea level.