期刊
GEOPHYSICAL RESEARCH LETTERS
卷 42, 期 1, 页码 113-120出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL061796
关键词
Nordic Seas; seasonal variability; sea surface height; sea ice edge
资金
- UK Natural Environment Research Council
- TEA-COSI project [NE/I028947/1]
- NERC [NE/I028947/1, cpom30001] Funding Source: UKRI
- Natural Environment Research Council [noc010012, cpom30001, NE/I028947/1] Funding Source: researchfish
Sea surface height measured by the Envisat radar altimeter over open ocean and from leads in sea ice are combined to generate a complete view of variability in the Nordic Seas, geographically and seasonally. The observed seasonal variability is decomposed using empirical orthogonal functions and is consistent with seasonal variations in steric and dynamic forcing. Wintertime increase in sea surface height on the east Greenland shelf is hypothesized to be caused by wind-forced downwelling, which provides direct evidence for the regional play of coastal dynamics. High levels of eddy kinetic energy around the sea ice edge in Fram Strait and off east Greenland and Svalbard are consistent with the interaction of the wind with the ice edge.
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