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Influence of the Arctic Circumpolar Vortex on the Mass Balance of Canadian High Arctic Glaciers
Journal of Climate
Variability in July mean surface air temperatures from 1963 to 2003 accounted for 62% of the variance in the regional annual glacier mass balance signal for the Canadian High Arctic. A regime shift to more negative regional glacier mass balance occurred between 1986 and 1987, and is linked to a coincident shift from lower to higher mean July air temperatures. Both the interannual changes and the regime shifts in regional glacier mass balance and July air temperatures are related to variationsdoi:10.1175/jcli4268.1 fatcat:freh5socirfpxhz33llgqmcjb4