Central West Antarctica among the most rapidly warming regions on Earth

David H. Bromwich,      Julien P. Nicolas,      Andrew J. Monaghan,     Matthew 
A. Lazzara,     Linda M. Keller,        George A. Weidner       & Aaron B. 
Wilson
AffiliationsContributionsCorresponding author
Nature Geoscience (2012) doi:10.1038/ngeo1671
Received 02 May 2012 Accepted 15 November 2012 Published online 23 December 2012
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Abstract
Abstract        Author information Supplementary information
There is clear evidence that the West Antarctic Ice Sheet is contributing to 
sea-level rise. In contrast, West Antarctic temperature changes in recent 
decades remain uncertain. West Antarctica has probably warmed since the 1950s, 
but there is disagreement regarding the magnitude, seasonality and spatial 
extent of this warming. This is primarily because long-term near-surface 
temperature observations are restricted to Byrd Station in central West 
Antarctica, a data set with substantial gaps. Here, we present a complete 
temperature record for Byrd Station, in which observations have been corrected, 
and gaps have been filled using global reanalysis data and spatial 
interpolation. The record reveals a linear increase in annual temperature 
between 1958 and 2010 by 2.4±1.2 °C, establishing central West Antarctica as 
one of the fastest-warming regions globally. We confirm previous reports of 
West Antarctic warming, in annual average and in austral spring and winter, but 
find substantially larger temperature increases. In contrast to previous 
studies, we report statistically significant warming during austral summer, 
particularly in December–January, the peak of the melting season. A continued 
rise in summer temperatures could lead to more frequent and extensive episodes 
of surface melting of the West Antarctic Ice Sheet. These results argue for a 
robust long-term meteorological observation network in the region.

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