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毛乌素沙地土壤水分的遥感监测

Remote sensing monitoring of soil moisture in the Mu Us sandland

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【作者】 周会珍刘绍民白洁毛德发

【Author】 Zhou Huizhen1,2,Liu Shaomin1,Bai Jie1,Mao Defa3(1.State Key Laboratory of Remote Sensing Science,Beijing Normal University,Beijing 100875,China;2.Beijing Landview Mapping Information Technology Co.,Ltd.,Beijing 100096,China;3.Beijing Water Technology Center,Beijing 100073,China)

【机构】 北京师范大学遥感科学国家重点实验室地理学与遥感科学学院北京宇视蓝图信息技术有限公司北京水利水电技术中心

【摘要】 利用毛乌素沙地腹地——乌审旗1982-1993年间的AVHRR遥感数据、常规气象数据和土壤水分观测资料,建立基于条件温度植被指数的0~50 cm土壤水分遥感估算模型,并计算出0~50 cm土体各层土壤水分。结果表明:乌审旗多年平均土壤水分的变化量约为-3.47mm,逐年土壤水分变化量Δw在-118~82 mm之间。乌审旗土壤水分的年际变化不大,基本在±50 mm之间变动。除1986、1987、1991以及1993年外,其余年份乌审旗土壤水分变化量Δw都为正。乌审旗土壤水分的年内波动也不大,基本在±10 mm之间。通过误差分析可知,遥感反演土壤水分的平均绝对百分比误差为14.77%,均方差为77.54 mm。基于条件温度植被指数的土壤水分遥感估算模型是可行的。

【Abstract】 Based on NOAA-AVHRR,meteorology and soil moisture data during 1982-1993 in Wushen County of the Mu Us sandland,the satellite-derived estimation model of soil moisture was established by using VTCI(vegetation temperature condition index),and the soil moisture of each layer between 0~50 cm were estimated.The results show that the multi-annual mean soil moisture variation Δw is –3.47 mm.The annual soil moisture variations(Δw) are between –118 mm and 82 mm from 1982 to 1993,and the inter-annual changes of soil moisture Δw are between ±50 mm,which was positive except for the year of 1986,1987,1991 and 1993.The inner-annual changes of soil moisture Δw are between ±10 mm.Compared with ground measurements,the RMSD and MAPD of soil moisture are 14.77% and 77.54 mm respectively.As a result,the satellite-derived estimation model of soil moisture is feasible.

【基金】 国家重点基础研究发展规划项(2007CB714401);国家高技术研究发展计划课题(2007AA12Z175);公益性行业(气象)科研专项(GYHY200706046);国家自然科学基金项目(40671128)
  • 【文献出处】 农业工程学报 ,Transactions of the Chinese Society of Agricultural Engineering , 编辑部邮箱 ,2008年10期
  • 【分类号】S152.7
  • 【被引频次】18
  • 【下载频次】489
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