The
evidence comes from a 364-metre ice core containing a record of freezing and
melting over the previous millennium
Press
Assocition
Summer ice is melting
at a faster rate in the Antarctic peninsula than at any time in the last 1,000
years, a new study has shown. Photograph: Nasa/AFP/Getty Images
Summer ice is melting
at a faster rate in the Antarctic peninsula than at any time in the last 1,000
years, new research has
shown.
The
evidence comes from a 364-metre ice core containing a record of freezing and
melting over the previous millennium.
Layers
of ice in the core, drilled from James Ross Island near the northern tip of the
peninsula, indicate periods when summer snow on the ice cap thawed and then
refroze.
By
measuring the thickness of these layers, scientists were able to match the
history of melting with changes in temperature.
Lead
researcher Dr Nerilie Abram, from the Australian National University and
British Antarctic Survey (BAS), said: "We found that the coolest
conditions on the Antarctic peninsula and the lowest amount of summer melt occurred
around 600 years ago.
"At
that time temperatures were around 1.6C lower than those recorded in the late
20th century and the amount of annual snowfall that melted and refroze was
about 0.5%.
"Today,
we see almost 10 times as much (5%) of the annual snowfall melting each year.
"Summer
melting at the ice core site today is now at a level that is higher than at any
other time over the last 1,000 years. And while temperatures at this site
increased gradually in phases over many hundreds of years, most of the
intensification of melting has happened since the mid-20th century."
Levels
of ice melt on the Antarctic peninsula were especially sensitive to rising
temperature during the last century, he said.
"What
that means is that the Antarctic peninsula has warmed to a level where even
small increases in temperature can now lead to a big increase in summer
melt," Abram added.
Dr Robert Mulvaney,
from the British Antarctic Survey, who led the ice core drilling expedition in
2008 and co-authored a paper on the findings published on Sunday in the journal Nature Geoscience.
He
said: "Having a record of previous melt intensity for the Peninsula is
particularly important because of the glacier retreat and ice shelf loss we are
now seeing in the area.
"Summer
ice melt is a key process that is thought to have weakened ice shelves along
the Antarctic peninsula leading to a succession of dramatic collapses, as well
as speeding up glacier ice loss across the region over the last 50 years."
The ice core record
suggested a link between accelerated melting and man-made global warming. But a
different and more complex picture has emerged from another region of Antarctica.
A
separate US study, published in the same journal, shows that thinning ice from
the West Antarctic Ice Sheet Divide cannot confidently be blamed on greenhouse
gas emissions.
An
ice core record from this site indicates a strong influence from unusual
conditions in the tropical Pacific during the 1990s.
In
that decade, an El Niño event – a cyclical system of winds and ocean currents
that can affect the world's weather – caused rapid thinning of glaciers in the
west Antarctic.
The
spike in temperature was little different from others that occurred in the
1830s and 1940s, which also saw prominent El Niño events.
"If
we could look back at this region of Antarctica in the 1940s and 1830s we would
find that the regional climate would look a lot like it does today, and I think
we also would find the glaciers retreating much as they are today," said
lead author Prof Eric Steig, from the University of Washington.
He
said the same was not true for the Antarctic peninsula, the part of the
continent closer to South America. Here, more dramatic changes were
"almost certainly" a result of human-induced global warming.
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