长江流域资源与环境 >> 2018, Vol. 27 >> Issue (05): 1124-.doi: 10.11870/cjlyzyyhj201805019

• 生态环境 • 上一篇    下一篇

基于高分一号影像的江汉平原表层土壤湿度指数反演研究

聂艳,贾付生1,朱亚星1,于雷1,于婧2   

  1. (1.华中师范大学地理过程分析与模拟湖北省重点实验室,湖北 武汉 430079;
    2. 湖北大学资源环境学院,湖北 武汉 430062)
  • 出版日期:2018-05-20

Research on Surface Soil Moisture Index Inversion in #br# Jianghan Plain Based on GF1 WFV Image#br#

#br# NIE Yan1, JIA Fusheng1, ZHU Yaxin1, YU Lei1, YU Jing2   

  1.  
    (1. Hubei Provincial Key Laboratory for Geographical Process Analysis and Simulation, Central China Normal University,
     Wuhan 430062,  China;2. College of Resources and Environment, Hubei University, Wuhan 430062,  China)
  • Online:2018-05-20

摘要:

土壤湿度指数遥感监测在农业生产中具有重要的作用。为探讨国产高分一号(GF1)遥感数据在江汉平原农情参数快速获取中的适用性,以潜江市2017年3月8日的GF1 WFV影像和106个采样点的土壤湿度实测数据为数据源,选择垂直干旱指数(PDI)、改进型垂直干旱指数(MPDI)和植被调整垂直干旱指数(VAPDI),对土壤湿度指数反演的效果进行比较和验证。研究结果表明:PDI、MPDI、VAPDI与土壤湿度实测含水量的决定系数分别达到0.649、0.802和0.821,实测土壤含水量验证精度评价也表明各模型均能满足反演的精度要求,说明基于GF1 WFV影像开展江汉平原的大尺度土壤湿度反演是可行的;在植被覆盖中等区域,MPDI和VAPDI能够在一定程度上克服混合像元对土壤湿度光谱信息的影响,反演的精度要比PDI高,但在高植被覆盖度区,采用垂直植被指数(PVI)修正的VAPDI不易出现植被覆盖饱和现象,具有更高的反演精度;基于3种指数模型反演的土壤湿度指数空间异质性基本一致,但MPDI、VAPDI对土壤湿度变化更为敏感,能反映出不同植被覆盖类型下土壤湿度的实际水平。研究结果可为江汉平原大范围和动态监测表层土壤湿度指数提供理论基础和实践参考。
关键词: 高分一号;土壤湿度指数;PDI;MPDI;VAPDI;江汉平原

Abstract:

Monitoring soil moisture by remote sensing plays a significant role in the dynamic characterization and management of surface heat balance, water evapotranspiration and soil moisture in agricultural production. In order to verify the applicability of GF1 data in the rapid acquisition of agricultural parameters in Jianghan Plain, this study simulated, compared and validated the effectiveness of soil moisture inversion. All of the data were Sampled in the vegetation area of Qianjiang City on March 8, 2017, GF1 WFV image and measured soil moisture data were used to retrieve the Perpendicular Drought Index(PDI), the Modified Perpendicular Drought Index(MPDI) and the Vegetation Adjusted Perpendicular Drought Index(VAPDI). The results showed as follows: firstly, determinate coefficients of correlation analysis on PDI, MPDI, VAPDI and measured soil moisture were 0.649, 0.802 and 0.821 respectively. All of the models met the accuracy requirements of inversion in the accuracy evaluation of soil moisture. Both of them indicated that using GF1 WFV image is feasible for soil moisture inversion in large scale in Jianghan Plain. Secondly, in the area of moderate vegetation coverage, MPDI and VAPDI had higher inversion accuracy than PDI. To a certain extent, they overcome the influence of mixed pixels on soil moisture spectral information. While in the area of high vegetation coverage, VAPDI modified by Perpendicular Vegetation Index(PVI) were not susceptible to vegetation saturation and thus had higher inversion accuracy. Thirdly, spatial heterogeneity of soil moisture retrieved by three models were similar. However, MPDI and VAPDI were more sensitive to the change of soil moisture, which reflected the actual soil moisture level that covered by different vegetation. The results can provide practical reference for dynamic monitoring of surface soil moisture in large scale in Jianghan Plain.
Key words:GF1; soil moisture; PDI; MPDI; VAPDI; Jianghan Plain

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