catchment of the southwestern Greenland ice sheet. We find that an abrupt 80% increase in runoff occurring between the 1976-2002 and 2003-2014 periods is due to a shift in atmospheric circulation, with meridional exchange events occurring more frequently over Greenland, establishing the first observation-based connection between ice sheet runoff and climate change.
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Ahlstrøm et al. (2017) studied this question.
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