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Modeling the spatial snow water equivalent using NOAA-AVHRR data for mesoscale catchments

机译:使用NOAA-AVHRR数据对Mesoscale Camperment的数据建模等同的空间雪水

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The spatially distributed, physically based snowsubmodel ESCIMO (Energy Balance Snow Cover GIS Integrated Model) is presented which is integrated in the multiscale modeling shell PROMET. ESCIMO calculates the spatial snow cover distribution and snowmelt runoff by an energy and mass balance assertion. The meteorological input parameter fields are derived from generally available measurements of the German Weather Service (DWD) climatic station network ensuring the transferability of the model. Thesemeasurements of precipitation, temperature, wind speed and cloudiness are temporally and spatially interpolated. To take the influences of different vegetation into account spatial landuse information is derived by a multitemporal spectral unmixing procedure of NOAA-AVHRR satellite data from the vegetation period 1995. Necessary model parameters are taken from literature and no calibration is conducted. The temporal distribution of the snow cover and snow water equivalent was modeled for the winter season of 1993/94 in the Weser catchment. The modeled snow water equivalent is verified with measurements. The resulting coefficient of determination between model and measurement is 0.62. The spatial performance of ESCIMO in the Weser catchment is validated by a comparison of the modeled with the snow cover derived from a NOAA-AVHRR image. The correspondence between the two images is 86.3 percent.
机译:介绍了空间分布式的物理基础的SnowsubModel ESCIMO(能量平衡雪覆盖GIS集成模型),该模型集成在MultiScale Modeling Shell Promet中。 ESCIMO通过能量和质量平衡断言来计算空间雪覆盖分布和雪花径流。气象输入参数字段来自德国天气服务(DWD)气候站网络的一般可用测量,确保模型的可转换性。沉淀,温度,风速和浑浊的测量,在时间上和空间内插。要考虑到不同植被的影响,所以通过来自1995年植被期间的NOAA-AVHRR卫星数据的多型光谱解密程序来源的。从文献中取出必要的模型参数,没有进行校准。雪覆盖和雪水等同物的时间分布是在Weser集水区的冬季为1993/94的冬季为模型。使用测量验证建模的雪水等效物。模型和测量之间的产生系数为0.62。通过与来自NOAA-AVHRR图像的雪盖建模的模型进行验证,验证了WESER集水器中ESCIMO的空间性能。两张图像之间的对应关系为86.3%。

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