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Antarctic snow accumulation mapped using polarization of 4.3-cm wavelength microwave emission

机译:南极积雪映射使用4.3厘米波长微波极化发射

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Different parts of Antarctica receive different amounts of snowfall each year. In this paper we map the variations of the mean annual snow accumulation across the ice sheet. We also quantify the uncertainty in our estimates more objectively than has been possible for earlier maps. The new map is produced using observations from satellites and ground-based measurements. After a logarithmic transformation, these are combined using the geostatistical method of continuous-part universal kriging to give an estimate of the snow accumulation within each cell of a rectangular grid covering Antarctica. We also derive spatial averages over the major drainage systems of the ice sheet, along with their confidence intervals. We obtain a value of 143 ± 4 kg m?2 a?1 for the average rate of snow accumulation upon the grounded ice sheet of Antarctica.
机译:南极洲接收不同的不同部分每年大量的降雪。地图的变化意味着每年的雪积累在冰原。在我们估计更量化的不确定性比有可能客观地图。从卫星和地面测量。对数变换后,这些都是利用地质统计学相结合的方法连续部分给出一个通用克里格在每个估计的积雪细胞的一个矩形网格覆盖南极洲。我们也得出空间主要的平均值冰盖的排水系统,以及他们的置信区间。143±4公斤?积累的冰盖接地南极洲。

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