作者: Sebastian H. Mernild , Glen E. Liston
DOI: 10.1175/JCLI-D-11-00592.1
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摘要: AbstractRunoff magnitudes, the spatial patterns from individual Greenland catchments, and their changes through time (1960–2010) were simulated in an effort to understand runoff variations adjacent seas illustrate capability of SnowModel (a snow ice evolution model) HydroFlow routing link terrestrial with ocean processes other components Earth’s climate system. Significant increases air temperature, net precipitation, local surface lead enhanced statistically significant sheet (GrIS) mass balance (SMB) loss. Total surrounding oceans increased 30%, averaging 481 ± 85 km3 yr−1. Averaged over period, 69% originated GrIS 31% came outside rain melting glaciers caps. The increase was due 87% melt extent, 18% duration, a 5% decr...