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The research of soil moisture difference using the delaying effect of the precipitation on the vegetation

机译:利用降雨对植被的延迟效应研究土壤水分差异

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A new method to analyze the differences of soil moisture in an area is advanced. Soil moisture is related closely to vegetation growth. An experiment was conducted in the Yellow River Basin in China. The change of vegetation cover is the result of many factors. We postulate that soil moisture in the Yellow River Basin is mainly determined by the precipitation. The delaying effect of the precipitation on the vegetation cover was analyzed in the Yellow River Basin using the cross partial correlation index between precipitation and NDVI. The cross partial correlation index has already excluded the impact of temperature on vegetation cover. Different delaying effects represent different soil moisture. The delaying interval can be adapted to measure soil moisture difference at different levels. On the basis of the above result, the difference of soil moisture in the Yellow River Basin was analyzed, and the difference map of soil moisture in the Yellow River Basin was made.
机译:一种新方法,分析了地区土壤水分差异的新方法。土壤水分与植被生长密切相关。在中国黄河流域进行了一个实验。植被覆盖的变化是许多因素的结果。我们假设黄河盆地的土壤水分主要由沉淀决定。在黄河盆地中,在黄河盆地中使用沉淀和NDVI之间的横偏相关指数分析了沉淀对植被覆盖的延迟效果。横局部相关指数已经排除了温度对植被覆盖的影响。不同的延迟效应代表不同的土壤水分。延迟间隔可以适于测量不同水平的土壤湿度差异。在上述结果的基础上,分析了黄河流域土壤水分的差异,制作了黄河流域土壤水分的差异图。

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