热惯性法反演黑河流域土壤水分

Chunfeng Ma, Xujun Han, Weizhen Wang
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引用次数: 2

摘要

利用MODIS数据和实测数据,分别建立了反演黑河流域土壤热惯性的真实热惯性模型和计算黑河流域土壤水分的土壤热惯性-土壤水分模型。同时,利用流域内两个观测站的数据对反演结果进行了验证。两站反演与观测的相关系数分别为0.853和0.917。结果表明,该方法满足土壤水分反演的要求。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soilmoisture retrieval using thermal inertia method in Heihe River Basin, China
MODIS data and in situ data were used to establish a real thermal inertia model to retrieve soil thermal inertia of Heihe River Basin (HRB) and a soil thermal inertia-soil moisture model to calculate the soil moisture of the basin. Meanwhile, the data of two observation stations in the basin was used to validate the result of retrieval. The correlation coefficients of those between retrieved and observed at two stations were 0.853 and 0.917, respectively. The result shows the method meet the requirement of soil moisture inversion.
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