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Generation of spatially complete and daily continuous surface soil moisture of high spatial resolution

机译:高空间分辨率的空间完整和每日连续表面土壤水分的产生

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Surface soil moisture (SSM), as a vital variable for water and heat exchanges between the land surface and the atmosphere, is essential for agricultural production and drought monitoring, and serves as an important boundary condition for atmospheric models. The spatial resolution of soil moisture products from microwave remote sensing is relatively coarse (e.g., similar to 40 km x 40 km), whereas SSM of higher spatiotemporal resolutions (e.g., 1 km x 1 km and daily continuous) is more useful in water resources management. In this study, first, to improve the spatiotemporal completeness of SSM estimates, we downscaled land surface temperature (LST) output from the China Meteorological Administration Land Data Assimilation System (CLDAS, 0.0625 degrees x 0.0625 degrees) using a data fusion approach and MODIS LST acquired on clear-sky days to generate spatially complete and temporally continuous LST maps across the North China Plain. Second, spatially complete and daily continuous 1 km x 1 km SSM was generated based on random forest models combined with quality LST maps, normalized difference vegetation index (NDVI), surface albedo, precipitation, soil texture, SSM background fields from the European Space Agency Soil Moisture Climate Change Initiative (CCI, 0.25 degrees x 0.25 degrees) and CLDAS land surface model (LSM) SSM output (0.0625 degrees x 0.0625 degrees) to be downscaled, and in situ SSM measurements. Third, the importance of different input variables to the downscaled SSM was quantified. Compared with the original CCI and CLDAS SSM, both the accuracy and spatial resolution of the downscaled SSM were largely improved, in terms of a bias (root mean square error) of -0.001 cm(3)/cm(3) (0.041 cm(3)/cm(3)) and a correlation coefficient of 0.72. These results are generally comparable and even better than those in published studies, with our SSM maps featuring spatiotemporal completeness and relatively high spatial resolution. The downscaled SSM maps are valuable for monitoring agricultural drought and optimizing irrigation scheduling, bridging the gaps between microwave-based and LSM-based SSM estimates of coarse spatial resolution and thermal infrared-based LST at a 1 km x 1 km resolution.
机译:表面土壤水分(SSM),作为土地表面和大气之间的水和热交换器的重要变量,对于农业生产和干旱监测至关重要,并用作大气模型的重要边界条件。微波遥感的土壤水分产品的空间分辨率相对粗糙(例如,类似于40 km x 40km),而较高的时空分辨率的SSM(例如,1 km x 1公里和每日连续)在水资源方面更有用管理。在这项研究中,首先,提高SSM估计的时空完整性,我们缩小了陆地表面温度(LST)从中国气象管理土地数据同化系统(CLDA,0.0625度×0.0625度)使用数据融合方法和MODIS LST在明确的天天获得,在华北平原上生成空间完整和时间连续的LST地图。其次,空间完整和每日连续1 km x 1 km ssm是基于随机森林模型,与质量LST地图相结合,归一化差异植被指数(NDVI),Surface Albedo,降水,土壤纹理,SSM背景领域来自欧洲空间机构土壤湿气气候变化措施(CCI,0.25度x 0.25度)和CLDAS陆地面模型(LSM)SSM输出(0.0625度×0.0625度)尺寸,原位SSM测量。第三,量化了不同输入变量对缩小SSM的重要性。与原始CCI和CLDAS SSM相比,就-0.001厘米(3)/ cm(3)(0.041厘米( 3)/ cm(3))和相关系数为0.72。这些结果通常比公布研究中的那些甚至更好,我们的SSM地图具有时尚完整性和相对高的空间分辨率。较低的SSM地图对于监测农业干旱和优化灌溉调度,拓展灌溉调度是有价值的,促进基于微波和基于LSM的基于LSM的SSM估计的间隙,粗糙的空间分辨率和基于热红外的LST的估计,1公里分辨率。

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