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Soil Moisture Estimation in Southeast Gansu with Ordinary Kriging

机译:普通克里格法估算甘肃东南部土壤水分

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Soil moisture is one of the most crucial information for drought monitoring, but its field observations encounters many embarrassments in practical application, one for the data inadequate caused by the sparse and uneven distribution of observation stations, the other for the poor regional effectiveness of this point-based observation data. It's worthwhile to do research in making credible extrapolation of soil moisture from single points to region in large scale. In this paper, Ordinary Kriging in Geostatistics is introduced to solve this problem. The spatial variability of soil moisture is analyzed firstly, then taking Southeast Gansu as the study area and basing on the field observation of 2008, experiment is carried out and the result for the regional estimation of soil moisture seems good.
机译:土壤水分是干旱监测的最关键信息之一,但其实地观测在实际应用中会遇到许多尴尬,其一是由于观测站稀疏分布不均引起的数据不足,其二是该地区的有效性较差。基于的观察数据。有必要进行研究以可靠地将土壤水分从单点大规模推算到区域。本文介绍了地统计学中的普通克里格法来解决这个问题。首先分析了土壤水分的空间变异性,然后以甘肃东南部为研究区域,并以2008年的实地观测为基础,进行了试验,得出土壤水分区域估计的结果似乎是好的。

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