欢迎访问《草业学报》官方网站,今天是 分享到:

草业学报 ›› 2017, Vol. 26 ›› Issue (6): 16-27.DOI: 10.11686/cyxb2016331

• 研究论文 • 上一篇    下一篇

基于MODIS数据的新疆地区土壤湿度反演

李海霞1,2, 杨井1,*, 陈亚宁1, 郝兴明1   

  1. 1.中国科学院新疆生态与地理研究所,荒漠与绿洲生态国家重点实验室,新疆 乌鲁木齐 830011;
    2.中国科学院大学资环学院,北京 100049
  • 收稿日期:2016-09-01 修回日期:2016-10-19 出版日期:2017-06-20 发布日期:2017-06-20
  • 通讯作者: E-mail:yangjing@ms.xjb.ac.cn
  • 作者简介:李海霞(1989-),女,山东滨州人,在读硕士。E-mail:sdrzlhx@163.com
  • 基金资助:
    中国科学院“率先行动”计划特色研究所主要服务项目(Y674123001)和青年千人计划(Y371051001)资助

Retrieval of soil moisture information in Xinjiang using MODIS

LI Hai-Xia1,2, YANG Jing1,*, CHEN Ya-Ning1, HAO Xing-Ming1   

  1. 1.State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
    2.University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2016-09-01 Revised:2016-10-19 Online:2017-06-20 Published:2017-06-20

摘要: 以新疆地区为研究对象,选取2016年5和6月的植被指数产品数据和地表温度产品数据,构建新疆地区NDVI-Ts和EVI-Ts特征空间,分析新疆地区土壤干湿状况的空间分布格局及土壤水分的影响因素。结合野外同步重复采样获得的土壤含水量对TVDI进行验证,并分析EVI和Ts所包含的旱情信息。结果表明:(1)构建NDVI-Ts和EVI-Ts特征空间,其散点图符合三角形的关系。(2)新疆地区5和6月土壤湿度总体以干旱(0.6<TVDI<0.8)为主。空间上,新疆北部的阿尔泰山、中部的天山、南部的昆仑山为极湿润和湿润,而新疆北部的准噶尔盆地、南部的塔里木盆地为干旱和极干旱。(3)5月份林地的TVDI值最低,6月份高度覆盖草地的TVDI值最低;随高程的增加土壤湿度变大。(4)和基于NDVI的TVDI相比,基于EVI的TVDI更适合于监测5月与6月的农业旱情状况。(5)相对于植被指数,陆地表面温度更能反映旱情。

Abstract: MOD13A2, MOD11A2 and field measurements were utilized to study soil moisture variation in Xinjiang during May and June. Relationships between NDVI (Normalized Difference Vegetation Index) and Ts (Land Surface Temperature), and EVI (Enhanced Vegetation Index) and Ts were investigated. The spatial pattern of the temperature vegetation dryness index (TVDI) and influencing factors were analyzed. Results: (1) NDVI-Ts and EVI-Ts follow the classic triangle relationship. (2) Soil moisture in Xinjiang was mainly dominated by drought conditions (0.6<TVDI<0.8); Spatially, Alta, the middle slope area of the Tianshan Mountains, and the south slopes of the Kunlun Mountains are characterized by extremely wet conditions, while the north Junggar basin and southern Tarim Basin are dry. (3) The TVDI of forested land was lowest in May while the TVDI of grassland was lowest in June; soil moisture generally increased with elevation. (4) For regions with high vegetation coverage, EVI based TVDI is more suitable than NDVI based TVDI for drought monitoring. (5) The land surface temperature was better able to reflect drought conditions compared to vegetation index.