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Evaluation of modeled high resolution virtual brightness temperatures compared to space-borne observations for the neckar catchment

机译:评估高分辨率虚拟亮度温度与内部集水区空间观测相比

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Synthetic space-borne brightness temperatures have been generated by exploiting CMEM radiative transfer simulations at L-band and land-surface-atmosphere coupled models. The community land model CLM coupled with the atmospheric model COSMO have been used in order to create a full representation of subsurface, soil and vegetation of a catchment located in the south-west Germany, as a virtual reality framework (VR). These VR simulations are used as forcing for CMEM to simulate high resolution 1.4GHz brightness temperature (TB) at H&V polarization. Satellite-like synthetic observations are then generated including foot-print, orbital path and incidence angle. The satellite synthetic TBs are compared with real observations to show the degree of agreement on magnitude and dynamic. It has been found that the synthetic TBs have values of 20 to 60 K less compared to the mean distribution of the real satellite observations within the catchment. This biases vary according to the season with summer exhibiting the maximum and winter the minimum discrepancy. The general bias is largely explained by the fact that the catchment's soil moisture is overestimated by 45% when compared with satellite retrievals. A reduction applied to SM of 55% yields a partial reduction on TB bias, yet not enough to match the real satellite data. The remaining discrepancy is attributed to radiative effects introduced by inappropriate vegetation parametrization and inadequate orography assumptions.
机译:通过在L波段和陆地 - 大气耦合模型中利用CMEM辐射转移模拟来产生合成空间亮度温度。已经使用了与大气模型COSMO耦合的社区土地模型CLM,以便为位于德国西南部的地下,土壤和植被的全面代表,作为虚拟现实框架(VR)。这些VR仿真用作CMEM的强调,以模拟H&V极化的高分辨率1.4GHz亮度温度(TB)。然后产生卫星状合成观察,包括脚印,轨道路径和入射角。将卫星合成TBS与真正的观察结果进行比较,以显示对数量和动态的一致性程度。已经发现,与集水区内的真实卫星观测的平均分布相比,合成TB的值少于20至60k。这种偏见根据夏季的季节而变化,展示最大和冬季的最小差异。与卫星检索相比,集水区的土壤水分在很大程度上解释了一般偏见。应用于55%的SM的减少产生TB偏差的部分减少,但不足以匹配真实卫星数据。剩余的差异归因于不适当的植被参数化和不足的地区假设引入的辐射效应。

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