A new international study is the first to use a high-resolution,
large-scale computer model to estimate how much ice the West Antarctic
Ice Sheet could lose over the next couple of centuries, and how much
that could add to sea-level rise. The results paint a clearer picture of
West Antarctica’s future than was previously possible. The study has
been published in The Cryosphere, an open access journal of the European Geosciences Union (EGU).
“The
IPCC’s [Intergovernmental Panel on Climate Change] 4th and
5th Assessment Reports both note that the acceleration of West Antarctic
ice streams in response to ocean warming could result in a major
contribution to sea-level rise, but that models were unable to
satisfactorily quantify that response,” says Stephen Cornford, a
research assistant at the University of Bristol, UK and lead-author of
the study.
The work is a legacy of the ice2sea project, an EU
funded programme which developed techniques and data to reduce
uncertainty in the future contribution to sea level rise of melting ice
in the polar regions. Prof. David Vaughan, Director of Science at
British Antarctic Survey (BAS), was co-ordinator of the programme. He is
also a co-author on the paper:
“This is our best effort yet to
include all the key processes and all the main techniques developed
during ice2sea, in one state-of-the-art ice sheet model of the most
vulnerable part of Antarctica. Its results are within the range of the
last IPCC projections, but we have even greater confidence in these
projections of sea-level rise”.
West Antarctica is one of the
fastest warming regions on Earth and its ice sheet has been stage to
dramatic thinning in recent years. The West Antarctic Ice Sheet (WAIS)
is out of balance because it is losing significant amounts of ice to the
ocean, with the losses not being offset by snowfall. The lost ice,
drained by the ice sheet’s several ice streams, amounts to a significant
contribution to sea-level rise, which is expected to increase in the
future
0 comments:
Post a Comment