The study by Australian and British researchers indicates that even small increases in temperature could now lead to significant spike in summer ice melt on the peninsula.
The scientists drilled a 364m
(1,197ft) deep ice core on James Ross Island, near the northern tip of the
Antarctic Peninsula, to measure past temperatures and compare them with summer
ice melt levels.
Visible layers in the ice core
indicated periods when summer snow on the ice cap thawed and then refroze.
They found that, while the
temperatures have gradually increased by 1.6C (2.9F) over 600 years, the rate
of ice melting has been most intense over the past 50 years.
In fact, summer ice
melt has been 10 times more intense over the past 50 years compared with 600
years ago, the study shows.
"What it 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 ice melt," lead
researcher Nerilie Abram said.
"This has important
implications for ice instability and sea level rise in a warming climate."
Dr Abram said the findings are
"definitely evidence that the climate and the environment is changing in
this part of Antarctica".
Robert Mulvaney, from the British
Antarctic Survey, said the stronger ice melts are likely responsible for faster
glacier ice loss and some of the dramatic collapses from the Antarctic ice
shelf over the past 50 years.
The research from the Australian
National University and the British Antarctic Survey was published in the Nature Geoscience journal.
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