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Estimating root zone soil moisture at distant sites using MODIS NDVI and EVI in a semi-arid region.

机译:在半干旱地区,使用MODIS NDVI和EVI估算远处的根区土壤水分。

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摘要

This study investigated the potential of Normalized Difference Vegetation Index (NDVI) and Enhanced Vegetation Index (EVI) to estimate root zone soil moisture at native in situ measured sites, and at increasingly distant sites within the same climatic setting. In situ data were obtained from Soil Climate Analysis Network (SCAN) sites near the Texas-New Mexico border area, and NDVI and EVI products from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensor on board the Terra satellite. Results show that soil moisture values at the same depth are highly correlated ( r = 0.53 to 0.85) at distant sites as far as 150 Km from the native site, and NDVI and EVI are highly correlated at each site (r = 0.95 to 0.98). Raw time series has higher mean correlations than deseasonalized time series at every depth. Deseasonalized time series using NDVI and EVI are significantly correlated with soil moisture at distant sites (NDVI r = 0.35 to 0.73). The correlation reaches maximum value when the Vegetation Index (VI) lags soil moisture by 5 to 10 days. NDVI has a slightly higher correlation with soil moisture than EVI. Values of r decrease with distance from the native site. Regression analysis was also conducted using deseasonalized NDVI and deseasonalized soil moisture time series with a 5 day time lag of NDVI. The model estimated soil moisture at all depths, with adjusted R2 ranging from 0.44 to 0.59. Overall, deseasonalized NDVI values produce consistent results, and show that NDVI can estimate root zone soil moisture at distant sites in the study area.
机译:这项研究调查了归一化植被指数(NDVI)和增强植被指数(EVI)的潜力,以估计本地就地测量地点以及同一气候环境中越来越远的地点的根区土壤水分。从得克萨斯州-新墨西哥州边界地区附近的土壤气候分析网络(SCAN)站点以及从Terra卫星上的中分辨率成像光谱仪(MODIS)传感器获得的NDVI和EVI产品获得了现场数据。结果表明,相同深度处的土壤水分值在距本地站点150 km的远处高度相关(r = 0.53至0.85),而在每个站点上NDVI和EVI高度相关(r = 0.95至0.98) 。在每个深度,原始时间序列的平均相关性都比反季节化的时间序列高。使用NDVI和EVI的淡季时间序列与远处土壤湿度显着相关(NDVI r = 0.35至0.73)。当植被指数(VI)落后土壤水分5至10天时,相关性达到最大值。 NDVI与土壤水分的相关性高于EVI。 r的值随与本机站点的距离而减小。还使用经过反季节化的NDVI和经过反季节化的土壤水分时间序列(具有NDVI的5天时滞)进行了回归分析。该模型估算了所有深度的土壤水分,R2的调整范围为0.44至0.59。总体而言,反季节的NDVI值产生一致的结果,并表明NDVI可以估算研究区域遥远地点的根区土壤水分。

著录项

  • 作者

    Schnur, Mark T.;

  • 作者单位

    The University of Texas at San Antonio.;

  • 授予单位 The University of Texas at San Antonio.;
  • 学科 Hydrology.;Remote Sensing.;Environmental Sciences.;Agriculture Soil Science.
  • 学位 M.S.
  • 年度 2008
  • 页码 111 p.
  • 总页数 111
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:39:25

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