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Spatial EvapoTranspiration Modelling Interface (SETMI)

机译:空间蒸发蒸腾建模接口(SETMI)

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摘要

In order to obtain improved estimates of spatial-temporal evapotranspiration (ET) and to study the related effects of land and near-surface atmosphere interactions, different soil vegetation atmosphere transfer models (SVAT) are coupled with a water balance model of vegetation root zone using data assimilation techniques to update soil moisture. Within this context we developed the Spatial EvpoTranspiration Modelling Interface (SETMI) in which three different thermal remote sensing-based models are included: the one layer model (OLEM), the two source model (TSM), and the Surface Energy Balance (SEBAL) to provide estimates of surface energy fluxes and daily ET. The water balance model of the root zone is the one proposed in the FAO Paper 56 which was included to provide daily and seasonal estimates of ET and was modified to use the reflectance-based basal crop coefficient (K_(cbrf)) obtained from remote sensing. SETMI can also be combined with simple soil water dynamics models to provide multilayer root zone soil moisture estimates.
机译:为了获得对时空蒸散量(ET)的改进估计并研究土地和近地表大气相互作用的相关影响,将不同的土壤植被大气转移模型(SVAT)与植被根区的水平衡模型结合使用,数据同化技术来更新土壤湿度。在此背景下,我们开发了空间蒸发蒸腾建模接口(SETMI),其中包括三个基于热遥感的不同模型:一层模型(OLEM),两个源模型(TSM)和表面能平衡(SEBAL)提供表面能通量和每日ET的估算值。根部区域的水平衡模型是粮农组织第56号文件中提出的模型,其中包括提供ET的每日和季节性估算,并进行了修改,以使用从遥感获得的基于反射率的基础作物系数(K_(cbrf)) 。 SETMI还可以与简单的土壤水分动力学模型结合使用,以提供多层根区土壤水分估算。

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