Sea-ice distribution and variability in the East Greenland Sea, 2003-13

被引:0
|
作者
Boccolari, Mauro [1 ]
Guerrieri, Lorenzo [1 ]
Parmiggiani, Flavio [2 ]
机构
[1] Univ Modena & Reggio E, Dept Chem & Geol Sci, Modena, MO, Italy
[2] ISAC CNR, I-40129 Bologna, Italy
关键词
sea-ice; Greenland Sea; AMSR-E; SSM/I; AMSR-2; air temperature; surface wind; cloud cover;
D O I
10.1117/12.2066489
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
This study presents an analysis of the sea-ice area time series for the East Greenland Sea for the period January 2003 - December 2013. The data used are a subset of the Arctic Sea Ice Concentration data set derived from the observations of the passive microwave sensors AMSR-E and AMSR-2 and produced, on a daily basis, by the Inst. of Environ. Physics of the University of Bremen. The area of interest goes, approximately, from 57 degrees N to 84 degrees N and from 53 degrees W to 15 degrees E. On the basis of previous studies, the parameter Sea Ice Area as the sum of all pixels whose sea ice concentration is above 70%, was introduced for measuring sea-ice extent. A first survey of the Greenland Sea data set showed a large anomaly in year 2012; this anomaly, clearly linked with the transition period from AMSR-E to AMSR-2 when re-sampled SSM/I data were used, was partially corrected with a linear regression procedure. The correlation between monthly mean Sea Ice Area and other geophysical parameters, like air temperature, surface wind and cloud cover, was further investigated. High anti-correlation coefficients between air temperature, at sea level and in five different tropospheric layers, and observed ice cover is confirmed. Our analysis shows that the strong decline of Arctic sea-ice area in the last 10 years is not observed in the East Greenland Sea; this implies that large reductions have occurred in the Canadian and Russian Arctic. This result confirms a hypothesis recently postulated to explain the different sea-ice decline in the Arctic and Antarctic regions.
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页数:8
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