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The retrieval of snow-depth using SSM/I remotely sensed data and its results assessment in Qinghai-Xizang (Tibet) plateau

机译:青藏高原高原地区利用SSM / I遥感数据反演雪深及其结果评估

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Using Chang's revised algorithm and SSM/I 37 GHz and 19 GHz horizontally polarized brightness temperature, the authors retrieved the snow depth distribution in Qinghai-Xizang (Tibet) plateau. They also assessed the results' accuracy and analyzed its error sources. It showed that Chang's algorithm could describe the general trend of snow depth distribution in this area, in spite of overestimation in parts of the area. The errors are mainly from the effect of the existence of permafrost, depth-hoar and vegetation cover. The coarse spatial resolution of SSM/I remotely sensed data make the retrieved snow depth hard to compare with the ones from ground observation, make it difficult to evaluate the accuracy.
机译:利用Chang的修正算法以及SSM / I 37 GHz和19 GHz水平极化亮度温度,作者获得了青藏高原的雪深分布。他们还评估了结果的准确性,并分析了其错误来源。结果表明,尽管对该地区的部分地区进行了高估,Chang的算法仍可以描述该地区积雪深度分布的总体趋势。误差主要来自多年冻土,深层灰和植被覆盖的影响。 SSM / I遥感数据的粗略空间分辨率使得检索到的积雪深度难以与地面观测的积雪深度进行比较,从而难以评估准确性。

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