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Ice mass change in Greenland and Antarctica between 1993 and 2013 from satellite gravity measurements

机译:根据卫星重力测量,1993年至2013年格陵兰和南极洲的冰块变化

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摘要

We construct long-term time series of Greenland and Antarctic ice\udsheet mass change from satellite gravity measurements. A statistical reconstruction\udapproach is developed based on a Principal Component Analysis to combine\udhigh-resolution spatial modes from the Gravity Recovery and Climate Experiment\ud(GRACE) mission with the gravity information from conventional satellite track-ing data. Uncertainties of this reconstruction are rigorously assessed; they include\udtemporal limitations for short GRACE measurements, spatial limitations for the\udlow-resolution conventional tracking data measurements, and limitations of the estimated\udstatistical relationships between low and high degree potential coe�cients\udre\udected in the PCA modes. Trends of mass variations in Greenland and Antarctica\udare assessed against a number of previous studies. The resulting time series\udfor Greenland show a higher rate of mass loss than other methods before 2000,\udwhile the Antarctic ice sheet appears heavily in\uduenced by interannual variations.
机译:通过卫星重力测量,我们构建了格陵兰岛和南极冰/冰盖质量变化的长期时间序列。基于主成分分析的统计重建方法是将重力恢复和气候实验任务中的高分辨率空间模式与常规卫星跟踪数据中的重力信息相结合。严格评估此重建的不确定性;它们包括短GRACE测量的时间限制,常规分辨率的低分辨率跟踪数据测量的空间限制以及PCA模式中低和潜在势能系数之间估计/统计关系的限制。格陵兰岛和南极洲的质量变化趋势已根据许多先前的研究进行了评估。格陵兰岛的时间序列ud显示出比2000年之前其他方法更高的质量损失率,而南极冰盖受到年际变化的影响很大。

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