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Assimilating multi-source data into land surface model to simultaneously improve estimations of soil moisture, soil temperature, and surface turbulent fluxes in irrigated fields

机译:将多源数据同化为地表模型,以同时改善对灌溉田地土壤湿度,土壤温度和地表湍流通量的估计

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摘要

The optimal estimation of soil moisture, soil temperature, and surface turbulent fluxes in irrigation fields is restricted by a lack of accurate irrigation information. To resolve the input uncertainty from imprecise irrigation quantity, an improved data assimilation scheme that is EnKS (Ensemble Kalman Smoother) implemented with inflation and localization (referred to as ESIL) is proposed to estimate soil moisture, soil temperature, and surface turbulent fluxes for irrigated fields by assimilating multi-source observations. The Daman station, which is located at an irrigated maize farmland in the middle reaches of the Heihe River Basin (HRB), is selected in this study to investigate the performance of the proposed assimilation scheme. The measured land surface temperature (LST) and surface soil moisture (SSM) in the first soil layer are taken as observations to conduct a series of data assimilation experiments to analyze the influence of a lack of irrigation information and combinations of multi-source observations on estimations of soil moisture, soil temperature, and surface turbulent fluxes. This study demonstrates the feasibility of ESIL in improving the estimation of hydrothermal conditions under unknown irrigation. The coefficient correlation (R) with the ESIL method increases from 0.342 and 0.703 to 0.877 and 0.830 for the soil moisture and soil temperature in the first layer, respectively. Meanwhile, the surface turbulent fluxes are significantly improved and the RMSE decreases from 173 W/m(2) and 186 W/m(2) to 97 W/m(2) and 111 W/m(2) for the sensible and latent heat fluxes, respectively. (C) 2016 Elsevier B.V. All rights reserved.
机译:缺乏准确的灌溉信息限制了灌溉田中土壤湿度,土壤温度和地表湍流通量的最佳估算。为了解决灌溉量不精确造成的输入不确定性,提出了一种改进的数据同化方案,即EnKS(Ensemble Kalman平滑器),该方法采用充气和局部化(称为ESIL)来估算灌溉的土壤水分,土壤温度和表面湍流通量吸收多源观测资料。本研究选择位于黑河流域(HRB)中部灌溉玉米农田的Daman站,以研究拟议的同化方案的性能。以第一土壤层中测得的地表温度(LST)和地表土壤水分(SSM)为观测值,进行一系列数据同化实验,以分析缺乏灌溉信息和多源观测值组合对土壤的影响。估算土壤湿度,土壤温度和地表湍流。这项研究证明了ESIL在改善未知灌溉条件下热液条件估计方面的可行性。对于第一层中的土壤水分和土壤温度,ESIL方法的系数相关性(R)从0.342和0.703分别增加到0.877和0.830。同时,显着和潜在的表面湍流通量得到显着改善,RMSE从173 W / m(2)和186 W / m(2)降至97 W / m(2)和111 W / m(2)热通量分别。 (C)2016 Elsevier B.V.保留所有权利。

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