Extreme weather phenomena called atmospheric rivers were behind intense snowstorms recorded in 2009 and 2011 in East Antarctica. The resulting snow accumulation partly offset recent ice loss from the Antarctic ice sheet, report researchers from KU Leuven.
Atmospheric rivers are long, narrow water vapour plumes stretching thousands of kilometres across the sky over vast ocean areas. They are capable of rapidly transporting large amounts of moisture around the globe and can cause devastating precipitation when they hit coastal areas.
Although atmospheric rivers are notorious for their flood-inducing impact in Europe and the Americas, their importance for Earth's polar climate - and for global sea levels - is only now coming to light.
In this study, an international team of researchers led by Irina Gorodetskaya of KU Leuven's Regional Climate Studies research group used a combination of advanced modelling techniques and data collected at Belgium's Princess Elisabeth polar research station in East Antarctica's Dronning Maud Land to produce the first ever in-depth look at how atmospheric rivers affect precipitation in Antarctica.
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