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More frequent summer anticyclonic circulation over the Canadian Arctic Archipelago ( CAA ) between 2007 and 2012 caused more intense and sustained melt of ice caps and glaciers and increased rates of mass loss. To determine the frequency of the occurrence of anticyclonic circulation over the CAA and western Greenland, a self‐organizing map ( SOM ) was used to classify daily 500 hPa geopotential height (GPH) anomalies calculate...
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