A group of scientists, led by a team from the University of Bristol,
has observed a sudden increase of ice loss in a previously stable region
of Antarctica. The research is published today in Science.
Using
measurements of the elevation of the Antarctic ice sheet made by a suite
of satellites, the researchers found that the Southern Antarctic
Peninsula showed no signs of change up to 2009. Around 2009, multiple
glaciers along a vast coastal expanse, measuring some 750km in length,
suddenly started to shed ice into the ocean at a nearly constant rate of
60 cubic km, or about 55 trillion litres of water, each year.
This makes the region the second largest contributor to sea level rise in Antarctica and the ice loss shows no sign of waning.
Dr Bert Wouters,
a Marie Curie Fellow at the University of Bristol, who lead the study
said: “To date, the glaciers added roughly 300 cubic km of water to the
ocean. That's the equivalent of the volume of nearly 350,000 Empire
State Buildings combined.”
The changes were observed using the
CryoSat-2
satellite, a mission of the European Space Agency dedicated to
remote-sensing of ice. From an altitude of about 700km, the satellite
sends a radar pulse to Earth, which is reflected by the ice and
subsequently received back at the satellite. From the time the pulse
takes to travel, the elevation of the ice surface can retrieved with
incredible accuracy. By analysing roughly 5 years of the data, the
researchers found that the ice surface of some of the glaciers is
currently going down by as much as 4m each year.
The ice loss in
the region is so large that it causes small changes in the gravity field
of the Earth, which can be detected by another satellite mission, the
Gravity Recovery and Climate Experiment (GRACE).
“The
fact that so many glaciers in such a large region suddenly started to
lose ice came as a surprise to us,” continued Dr Wouters. “It shows a
very fast response of the ice sheet: in just a few years the dynamic
regime completely shifted.”
Data from an Antarctic climate model
shows that the sudden change cannot be explained by changes in snowfall
or air temperature. Instead, the team attributes the rapid ice loss to
warming oceans.
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