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Improved elevation-change measurement of the southern Greenland ice sheet from satellite radar altimetry

机译:卫星雷达测高仪改进了格陵兰南部冰盖的海拔变化测量

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A new analysis of Seasat and Geosat satellite radar altimeter measurements over the Greenland ice sheet was performed to determine surface elevation change. The new analysis includes twice as many measurements and has 50% greater spatial coverage than the authors' previous study. In addition, a precise global ocean reference network created from four years of Topex/Poseidon altimeter data is used to obtain improved estimates of altimeter orbit errors and measurement system biases. The results show that the average elevation change of the southern Greenland ice sheet above 2000 m from 1978 to 1988 is not significantly different than zero. This contradicts earlier and even more recent studies that reported positive ice sheet growth rates and suggested increased precipitation due to a warmer polar climate.
机译:对格陵兰冰盖上的Seasat和Geosat卫星雷达高度计测量值进行了新的分析,以确定表面高度变化。新的分析包括两倍的测量值,并且空间覆盖率比作者以前的研究大50%。此外,根据四年的Topex / Poseidon高度计数据创建的精确的全球海洋参考网络可用于获取高度计轨道误差和测量系统偏差的改进估算。结果表明,1978年至1988年格陵兰南部冰盖2000 m以上的平均海拔变化没有明显的零变化。这与早些时候甚至更近期的研究相矛盾,后者报道了冰盖的正增长率,并建议由于极地气候变暖而增加降水。

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