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From:The Cryosphere (Vol. 16, Issue 1) Peer-ReviewedThe future rates of ice sheet melt in Greenland and Antarctica are an important factor when making estimates of the likely rate of sea level rise. Global climate models that took part in the fifth Coupled Model...
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From:Earth System Science Data (Vol. 13, Issue 10) Peer-ReviewedThe mass of the Greenland ice sheet is declining as mass gain from snow accumulation is exceeded by mass loss from surface meltwater runoff, marine-terminating glacier calving and submarine melting, and basal melting....
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From:The Cryosphere (Vol. 15, Issue 9) Peer-ReviewedAntarctic surface mass balance (SMB) is largely determined by precipitation over the continent and subject to regional climate variability related to the Southern Annular Mode (SAM) and other climatic drivers at the...
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From:Climate of the Past (Vol. 12, Issue 9) Peer-ReviewedInsolation changes during the Eemian (the last interglacial period, 129â¯000--116â¯000 years before present) resulted in warmer than present conditions in the Arctic region....
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From:The Cryosphere (Vol. 14, Issue 11) Peer-ReviewedObservations and models agree that the Greenland Ice Sheet (GrIS) surface mass balance (SMB) has decreased since the end of the 1990s due to an increase in meltwater runoff and that this trend will accelerate in the...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 13) Peer-ReviewedThe Arctic is warming 2 to 3 times faster than the global average, partly due to changes in short-lived climate forcers (SLCFs) including aerosols. In order to study the effects of atmospheric aerosols in this warming,...
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From:The Cryosphere (Vol. 14, Issue 11) Peer-ReviewedPerennial snow, or firn, covers 80 % of the Greenland ice sheet and has the capacity to retain surface meltwater, influencing the ice sheet mass balance and contribution to sea-level rise. Multilayer firn models are...
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From:Proceedings of the National Academy of Sciences of the United States (Vol. 114, Issue 50) Peer-ReviewedAbstract Only