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Melt Detection in Antarctic Ice-Sheets Using Spaceborne Scatterometers and Radiometers

机译:使用星载散射仪和辐射计仪在南极冰片中熔化检测

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Backscatter measurements from the Sea Winds on QuikSCAT scatterometer are used to determine periods of surface freeze and melt on Antarctic ice-shelves. A maximum likelihood method is used to infer the daily ice-surface conditions for various study points located on the Ronne, Ross, Larsen, Fimbul, Amery, and Shackleton Ice-shelves. Criteria for determining the dates of melt-onset and freeze-up for each Austral summer are presented. Validation of the ice-state and melt-onset date estimates is performed by analyzing the corresponding brightness temperature (T{sub}b) measurements from Special Sensor Microwave/Imager (SSM/I) radiometers, QuikSCAT σ° measurements from 1999 through 2003 are analyzed and found to be very useful for determining periods of melt in Antarctic ice-sheets and provide high temporal and spatial resolution ice-state estimates.
机译:Quikscat散射仪上海风的反向散射测量用于确定南极冰架上的表面冻结和熔化。 最大的似然方法用于推断出位于Ronne,Ross,Larsen,Fimbul,Amery和Shackleton冰架上的各种研究点的日常冰地面条件。 提出了确定每个澳大利亚夏季融化和冻结冻结日期的标准。 通过分析来自特殊传感器微波/成像仪(SSM / I)辐射仪(SSM / I)辐射仪(SSM / I)辐射仪的相应亮度温度(T {Sub} B)测量来执行冰状态和熔融发作日期估计,从1999到2003年的Quikscatσ°测量 分析并发现对于确定南极冰盖中的熔体期间非常有用,并提供高时和空间分辨率的冰状态估计。

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