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

机译:2003-13年东格陵兰海的海冰分布和变化

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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°N to 84°N and from 53°W to 15°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.
机译:这项研究提供了对东格陵兰海2003年1月至2013年12月期间海冰面积时间序列的分析。所用数据是从无源微波传感器的观测中得出的北极海冰浓度数据集的子集AMSR-E和AMSR-2,由环境研究所每天生产。不来梅大学物理学。感兴趣的区域大约从57°N到84°N,从53°W到15°E。在先前研究的基础上,引入参数“海冰面积”作为海冰浓度高于70%的所有像素的总和,以测量海冰范围。格陵兰海数据集的首次调查显示,2012年出现了异常现象。当使用重新采样的SSM / I数据时,该异常明显与从AMSR-E到AMSR-2的过渡期有关,已通过线性回归程序进行了部分纠正。进一步研究了月平均海冰面积与其他地球物理参数(如气温,地表风和云量)之间的相关性。确认了在气温,海平面和五个不同对流层之间的高反相关系数,并观察到了冰盖。我们的分析表明,在过去的10年中,格陵兰东部海域没有观察到北极海冰面积的急剧下降;这意味着加拿大和俄罗斯的北极地区出现了大幅减少。这一结果证实了一个最近被假设用来解释北极和南极地区海冰下降的假说。

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