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An Error Analysis Method for Snow Depth Inversion Using Snow Emission Model

机译:利用雪发射模型进行雪深度反演的误差分析方法

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The snow depth and the amount of regional snow playan important role in the climate change and also affect themanagement of water resources, and the estimate of the runoffand flood forecasting. At present, snow depth is generallythought to be linearly dependent on the difference of thebrightness temperature (i.e. NASA algorithm) in passivemicrowave remote sensing. But some authors argued accordingto results of snow emission model simulation that it is not simplylinear relationship between them due to the influence of manyfactors (snow grains radius, land use/cover type). If snow depth isretrieved using the linearly dependent relationship, the error willeasily come out. In this paper the graphical representation ofprobability error is constructed based on the simulated multi-solution curve by snow emission model, which revealsquantitatively and visually the snow depth inversion error due tomulti-solution inversion. It will make a significant contribution toreduce the influence of uncertainty and increase the accuracy ofsnow depth inversion.
机译:雪深度和区域雪场的数量在气候变化中的重要作用,也影响水资源的审计,以及洪水预测的估计。目前,雪深度通常是线性地取决于PassivemroveaVeave遥感中的智能温度(即NASA算法)的差异。但是,一些作者认为这是由于雪排放模型模拟的结果,因为由于多种因素的影响(雪谷半径,土地使用/覆盖类型),它们之间不是它们之间的简单关系。如果使用线性依赖关系的雪深度识别,则错误会出现。本文基于雪发射模型基于模拟的多解决方案曲线构建了可支持误差的图形表示,其揭示了自由溶液反转的散发性和视觉上的雪深度反演误差。它将提出重大贡献使得不确定性的影响力并提高深度反转的准确性。

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