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Assessing potential of vertical average soil moisture (0-40cm) estimation for drought monitoring using MODIS data: A case study

机译:使用MODIS数据评估垂直平均土壤湿度(0-40cm)估计的潜在估计案例研究

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Soil moisture is an important parameter in the research of hydrology, agriculture, and meteorology. The present study is designed to evaluate the potential of estimating vertical average soil moisture (0-40cm) using MODIS data. It has been found that the Normalized Difference Vegetation Index (NDVI) and Land Surface Temperature (LST) are related to surface soil moisture, and a second order polynomial relationship between ground measurement soil moisture and NDVI and LST can be developed. Therefore, six days' NDVI and LST data calculated from Terra Moderate Resolution Imaging Spectroradiometer (MODIS) of Shandong province during October in 2010 to May in 2011 were combined with ground measured volumetric soil moisture in different depth (10cm, 20cm, 40cm, and vertical average (0-40cm)) and different soil type to determine regression relationships. The result shows that significantly relationship exists between the NDVI and LST and soil moisture at 10cm and 20cm depth, slighter lower correlation coefficients are obtained for vertical average soil moisture (0-40cm), and worst correlationships are found for soil moisture at 40 cm depth. In addition, those regression relationships are soil type dependent. This means that it is feasible to estimate vertical average soil moisture (0-40cm) for drought monitoring using MODIS data.
机译:土壤水分是水文,农业和气象研究的重要参数。本研究旨在使用MODIS数据评估估算垂直平均土壤水分(0-40cm)的潜力。已经发现,归一化差异植被指数(NDVI)和陆地温度(LST)与表面土壤水分有关,并且可以开发地面测量土壤水分和NDVI和LST之间的二阶多项式关系。因此,2010年10月的山东省Terra中等分辨率成像光谱仪(MODIS)计算的六天NDVI和LST数据与2011年5月的不同深度(10cm,20cm,40cm和垂直)相结合了地面测量的体积土壤水分。平均(0-40cm))和不同的土壤类型来确定回归关系。结果表明,在10cm和20cm深度的NDVI和LST和土壤水分之间存在显着关系,获得垂直平均土壤水分(0-40cm)的较小相关系数,并且发现40厘米深度的土壤水分最差的相关性。此外,这些回归关系是依赖的土壤类型。这意味着使用MODIS数据来估计垂直平均土壤水分(0-40cm)的垂直平均土壤水分(0-40cm)是可行的。

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