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Decadal Mass Balance of the Greenland and Antarctic Ice Sheets from High Resolution Elevation Change Analysis of ERS-2 and Envisat Radar Altimetry Measurements

机译:高分辨率高度改变分析的格陵兰岛和南极冰盖的额外平衡分析和Entisat雷达高度测量

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Here we measure fine-scale polar ice sheet elevation change and estimate decadal mass balance for the Greenland and Antarctic ice sheets from ERS-2 and ENVISat satellite radar altimeter data. The Greenland results show that moderate to slightly positive elevation change rates (ECRs) dominate the interior areas while large negative ECRs are observed for many coastal areas. In Antarctica, glaciers in the coastal areas of the West Antarctic Ice Sheet (WAIS) are experiencing rapid thinning. The strong thinning of some of these glaciers extends well into the interior of the continent. Over the East Antarctic Ice Sheet (EAIS), positive ECRs dominate the interior areas while some glaciers in coastal areas are experiencing thinning. The equivalent mass change for the GIS, EAIS, WAIS, and AIS over the period 1995-2006 is -20, 27, -53, and -26 Gt/yr, respectively.
机译:在这里,我们测量精细尺寸的极地冰盖升高变化,从EAS-2和Envisat卫星雷达高度计数据中估算格陵兰和南极冰盖的估计额外量平衡。格陵兰植物结果表明,中度至略微正高度变化率(ECRS)主导内部区域,同时观察到许多沿海地区的大负面ECR。在南极洲,西南极冰盖(WAIS)沿海地区的冰川正在经历快速变薄。其中一些冰川的强烈变薄良好地延伸到大陆的内部。在东南南极冰盖(EAIS)上,积极的ECRS主导内部区域,而沿海地区的一些冰川正在经历变薄。 GIS,EAI,WAIS和AIS在1995 - 2006期间的等效质量变化分别为-20,27,-53和-26 gt / Yr。

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