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

机译:卫星雷达测高仪改进的格陵兰冰盖高程变化测量

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Elevation change measurements from satellite altimetry for the southern Greenland ice sheet (south of 72/spl deg/N) are re-examined after incorporating technical advancements that significantly improve measurement accuracy. A spatial average of 33,610 crossover points between the Seasat and Geosat altimeters yields a 5.4/spl plusmn/0.4 cm/yr growth rate from 1978 to 1988. This is over four times smaller than previously reported results. Large spatial variations in elevation change from -7 to +20 cm/yr are observed over the ice sheet for the first time. Interannual variations in elevation change of 5-10 cm/yr are also observed. Given the large spatial and interannual variations in elevation change, the 5.4/spl plusmn/0.4 cm/yr growth rate is too small to determine whether or not the Greenland ice sheet is undergoing a long-term change due to a warmer polar climate.
机译:在结合了可以显着提高测量精度的技术进步之后,重新检查了来自南极格陵兰冰原的卫星测高仪的仰角变化测量值(南极72 / spl deg / N)。从1978年到1988年,Seasat和Geosat高度表之间的33,610个交叉点的空间平均值产生了5.4 / spl plusmn / 0.4 cm / yr的增长率。这是以前报告的结果的四倍多。首次在冰盖上观测到海拔高度从-7到+20 cm / yr的大的空间变化。还观察到海拔变化为5-10 cm / yr的年际变化。考虑到海拔变化的空间和年际变化较大,因此5.4 / spl plusmn / 0.4 cm / yr的增长速度太小,无法确定格陵兰冰盖是否由于极地气候变暖而正在经历长期变化。

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