宝瓶号海冰厚度检索:初步结果

P. de Matthaeis, C. Utku, D. L. Le Vine, A. Moyer
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引用次数: 3

摘要

宝瓶号的亮温数据被用来计算北极地区的海冰厚度。该方法基于海冰辐射传输模型的反演。使用这种技术,从Aquarius数据中获取的初始海冰厚度值与SMOSIce数据以及美国宇航局冰桥行动的估算值进行比较。结果表明,由SMOS和水瓶座估算的海冰厚度有相似的变化趋势,但水瓶座估算的海冰厚度往往比相应的SMOS值更高,噪声更大。反演的Aquarius冰厚精度可能受到辅助输入参数的不确定性和Aquarius的粗分辨率的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Aquarius retrieval of sea ice thickness: Initial results
Aquarius brightness temperature data are used to calculate sea ice thickness in the Arctic region. The method is based on the inversion of a radiative transfer model for ice-covered sea. Using this technique, the initial sea ice thickness values retrieved from Aquarius data are compared to the SMOSIce Data as well as to estimates from NASA's Operation IceBridge. The results show similar trends between the SMOS- and Aquarius-derived sea ice thickness, however the Aquarius estimates tend to be higher and noisier than the corresponding SMOS values. The accuracy of retrieved Aquarius ice thickness is possibly influenced by uncertainties in the ancillary input parameters and by the coarser resolutions of Aquarius.
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