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Remotely sensed land surface temperature, lakes area and water level and ground discharge for hydrological model calibration in the Yangtze river basin

机译:遥感流域地表温度,湖泊面积,水位和地表流量对长江流域水文模型的标定

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Distributed hydrological models of energy and mass balance usually need in input many soil and vegetation parameters, which are usually difficult to define. This paper will try to approach this problem performing a parameters calibration based on remote sensing land surface temperature data (LST) as a complementary method to the traditional calibration with ground data. A pixel to pixel calibration procedure of soil hydraulic and vegetation parameters for each pixel of the domain is proposed according to the comparison between observed and simulated land surface temperature. A distributed hydrological model, FEST-EWB, that solves the system of energy and mass balance equations as a function of the representative equilibrium temperature (RET) will be used. RET is comparable to the land surface temperature as retrieved from operational remote sensing data. This equilibrium surface temperature, which is a critical model state variable, is compared to land surface temperature from MODIS. A similar calibration procedure will also be applied performing the traditional calibration using only discharge measurements at different available control cross sections. The effects on river discharge of the Three Gorges dam will be evaluated. The dynamic of the three large lakes (Poyang, Dongting and Taihu), which change considerably their area during the seasons, will also be anlyazed using MERIS data to infer surface area changes and LEGOS altimetry data (Topex/Poseidon, Jason, ENVISAT) for water level. Good correlation has been found between area and water level changes. The FEST-EWB hydrological model is then calibrated and validated against water level data, while lake area changes are used as input data. FEST-EWB is run in for the whole Yangtze River basin at spatial resolution of 0.05° and temporal resolution of 3 hours. Results are provided in terms of hourly evapotranspiration, soil moisture and land surface temperature maps for the period between 2003 to 2006.
机译:能量和质量平衡的分布式水文模型通常需要输入许多土壤和植被参数,而这些参数通常很难定义。本文将尝试解决此问题,并基于遥感地表温度数据(LST)进行参数校准,作为对传统的地面数据校准的补充方法。根据观测到的和模拟的地表温度之间的比较,提出了该域每个像素的土壤水力和植被参数的像素到像素的标定程序。将使用分布式水文模型FEST-EWB,该模型根据代表平衡温度(RET)求解能量和质量平衡方程组。 RET可与从操作遥感数据中检索到的地表温度相媲美。将此平衡表面温度(这是一个关键的模型状态变量)与MODIS的陆地表面温度进行比较。在仅使用不同可用控制横截面处的放电测量值的情况下,也将采用类似的校准程序执行传统的校准。将评估三峡大坝对河流流量的影响。三个大型湖泊(Po阳湖,洞庭湖和太湖湖)的动态在季节会发生很大变化,还将利用MERIS数据推断出表面积变化和LEGOS测高数据(Topex / Poseidon,Jason,ENVISAT)进行分析。水位。已发现面积与水位变化之间具有良好的相关性。然后针对水位数据对FEST-EWB水文模型进行校准和验证,而将湖泊面积变化用作输入数据。 FEST-EWB在整个长江流域以0.05°的空间分辨率和3小时的时间分辨率运行。根据2003年至2006年期间的每小时蒸散量,土壤湿度和地表温度图提供了结果。

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