The
Melting Antarctic Ice Sheet Is Heading Towards Irreversible Collapse
2
August, 2016
Computer
models suggest that the melting West Antarctic Ice Sheet (WAIS) is
melting at a rapidly accelerating rate. A new computer simulation
shows that at current melting rates, the ice sheet will hit a
critical point in about 60 years, and could result in a sea level
rise of as much as 10 feet over the next several centuries.
The
results of this latest simulation, run by a pair of scientists from
the Potsdam Institute for Climate Impact Research, just
appeared in
the latest edition of the Proceedings
of the National Academy of Science.
The
West Antarctic Ice Sheet (Credit: NASA)
Over
the past decade, scientists have carefully watched the Amundsen Sea
sector. This region of West Antarctica is
currently suffering tremendous losses in ice volume,
and its ongoing collapse is triggering downstream effects elsewhere
on the continent. A recent
NASA study suggests
that the Antarctic ice sheet is adding more ice than it’s losing,
but this won’t likely be the case for much longer.
To
get a sense of where this region is headed in the long-term, Johannes
Feldmann and Anders
Levermann ran
their simulation to project the topographical conditions hundreds,
and even thousands, of years from now —further in the future than
any previous study.
The
ultimate purpose was to determine whether or not the current Amundsen
instability could lead to the entire ice sheet collapsing into the
sea. The simulations suggest that this is in fact the case.
The
models show that 60 more years of meltage at the current rate—a
very reasonable estimate—will push the WAIS past a critical
point-of-no-return.
Beyond this threshold, a complete, long-term
disintegration is predicted to occur.
Feldmann and Levermann worry
that the WAIS has already become critically unstable, and that this
region has already passed the threshold point.
The
study also predicts that, over the course of the next several
centuries or millennia, the oceans will rise by as much as 10 feet (3
meters).
“Our
results show that if the Amundsen Sea sector is destabilized, then
the entire marine ice sheet will discharge into the ocean, causing a
global sea-level rise of about 3 m,” conclude the authors in the
study. “We thus might be witnessing the beginning of a period of
self-sustained ice discharge from West Antarctica that requires
long-term global adaptation of coastal protection.”
To
get a sense of what some major city centers around the world would
look like after a 10-foot rise in sea levels, go here and here.
Read
the entire study at Proceedings
of the National Academy of Sciences:
“Collapse
of the West Antarctic Ice Sheet after local destabilization of the
Amundsen Basin”.
No comments:
Post a Comment
Note: only a member of this blog may post a comment.