首页> 外文会议>International conference on intelligent earth observing and applications >Assessing potential of vertical average soil moisture (0-40cm) estimation for drought monitoring using MODIS data: A case study
【24h】

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

机译:利用MODIS数据评估垂直平均土壤湿度(0-40cm)估计潜力以进行干旱监测的案例研究

获取原文

摘要

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:土壤水分是水文学,农业和气象学研究的重要参数。本研究旨在评估使用MODIS数据估算垂直平均土壤湿度(0-40厘米)的潜力。已经发现归一化植被指数(NDVI)和土地表面温度(LST)与地表土壤水分有关,并且可以建立地面测量土壤水分与NDVI和LST之间的二阶多项式关系。因此,将2010年10月至2011年5月由山东省Terra中分辨率成像光谱仪(MODIS)计算的六天NDVI和LST数据与不同深度(10cm,20cm,40cm和垂直)的地面土壤含水量进行了组合。平均值(0-40cm))和不同的土壤类型来确定回归关系。结果表明,NDVI和LST与10cm和20cm深度的土壤水分之间存在显着的关系,垂直平均土壤水分(0-40cm)的相关系数较小,而40cm深度的土壤水分的相关系数最差。 。另外,那些回归关系是土壤类型的依赖。这意味着使用MODIS数据估算垂直平均土壤湿度(0-40cm)以进行干旱监测是可行的。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号