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Surface soil moisture status over the Mackenzie River Basin using a temperature/vegetation index

机译:利用温度/植被指数,丘陵河流域的表面土壤水分状况

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This paper presents an approach to assess soil moisture status in Northern Basins using MODIS land surface temperature (Ts) and the normalized difference vegetation index (NDVI). The methodology is based on the interpretation of the land surface temperature- vegetation (Ts-NDVI) space. For the study site over the Mackenzie River Basin, a positive correlation was noted between surface temperature and NDVI. The dry edge and the wet edge of the Ts-NDVI space are function of the NDVI values. A satisfactory agreement was obtained between the temperature-vegetation dryness index (TVDI) and the precipitation and elevation patterns. The TVDI index was therefore able to describe the spatiotemporal variation of the soil moisture in a cold climate and humid area.
机译:本文介绍了一种使用MODIS陆地表面温度(TS)和归一化差异植被指数(NDVI)评估北部盆地土壤水分状态的方法。该方法基于陆地温度 - 植被(TS-NDVI)空间的解释。对于麦肯齐河流域的研究现场,表面温度和NDVI之间的阳性相关性。 TS-NDVI空间的干边缘和湿边是NDVI值的功能。在温度 - 植被干燥指数(TVDI)和降水和升降模式之间获得了令人满意的协议。因此,TVDI指数能够描述冷气候和潮湿区域的土壤水分的时空变化。

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