黄土丘陵沟壑区蒸散的遥感反演——以静宁县水土保持世行贷款项目区为例

Remote-Sensing-Based Reproduction of Evapotranspiration in Loess Hilly-Gully Region:A Case Study of Jingning World Bank Project Area

  • 摘要: 蒸散量是热量平衡和水量平衡的重要分量。利用TM遥感影像和地表热量平衡模型估算静宁县水土保持世行贷款项目区的蒸散量,并结合地面实测资料进行检验,分析蒸散的分布规律,研究蒸散量与土地利用、地表参数、地形参数的关系。结果表明:研究区日蒸散量介于0.70~9.05mm之间,平均5.31mm,分布上呈现由西北向东南递增的趋势;不同下垫面的蒸散能力有一定差别,其中水域和林地的日蒸散量最大;日蒸散量与归一化植被指数(INDV)呈线性正相关,而与地表温度呈线性负相关。

     

    Abstract: Evapotranspiration(ET) is an important heft in heat balance and water balance,and its significance is obvious in estimating ET in large areas using remote sensing technology.TM images and a surface energy balance equation were used to estimate ET of the Jingning World Bank Project area on the Loess Plateau with results verified against available field data.Then relationships of ET with land use,surface parameters,terrain parameters were analyzed.Results show that daily ET value ranges from 0.70 to 9.05 mm,with an average of 5.31 mm on August 15,2003.Spatially,it displayed a rising trend from northwest to southeast,and varied with the underlying surface,being the highest with water and forest.A positive linear correlation was observed between ET and normalized difference vegetation index,but a negative one between ET and surface temperature.The findings demonstrate that the method is applicable to the estimation of ET in the study area.

     

/

返回文章
返回