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[1]YU Hong-bo,BAO Yu-hai,LI He-ping,et al.Remote Sensing Retrieval of Evapotranspiration in Xilin River Watershed[J].Research of Soil and Water Conservation,2014,21(01):224-228.

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Remote Sensing Retrieval of Evapotranspiration in Xilin River Watershed

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 21 Number of periods: 2014 01 Page number: 224-228 Column: Public date: 2014-02-28

Title:: Remote Sensing Retrieval of Evapotranspiration in Xilin River Watershed

Author(s):: YU Hong-bo^1,2, BAO Yu-hai¹, LI He-ping³, WANG Jun³; 1. Inner Mongolian Key Laboratory of Remote Sensing and Geography Information System, Inner Mongolia Normal University, Hohhot 010022, China;
2. College of Geography Science, Inner Mongolia Normal University, Hohhot 010022, China;
3. Institute of Water Resources for Pastoral Area, IWHR, Hohhot 010020, China

Keywords:: Xilin River watershed; evapotranspiration; remote sensing

CLC:: P334.92

DOI:: -

Abstract:: The study area is the Xilin River watershed. Remote sensing approach was used to retrieve instantaneous evapotranspiration based on the estimation of land surface fluxes from MODIS image in 2012, and the auxiliary environmental data from the same time periods. Daily evapotranspiration was estimated by scaling. The result of evapotranspiration distribution was consistent with land surface conditions. The daily evapotranspiration in the upper reaches was higher than in the middle and lower reaches. The daily evapotranspiration of wetland vegetation and meadow grassland was higher. The daily evapotranspiration of dense vegetation such as farmland was higher than the sparse one. The distribution curve of daily evapotranspiration was characterized as Gaussian distribution. The main value was between 2 and 7 mm/d and the average value was 4.51 m/d. Results were verified by using the FAO method. This level of uncertainty was acceptable; therefore, the method that we developed was applicable.

References:: [1] 刘惊涛,刘世荣.植被蒸散研究方法的进展与展望[J].林业科学,2006,42(6):108-114.
[2] 刘佳慧,刘芳,王炜,等."3S"技术在生态用水量研究中的应用:以锡林河流域为例[J].干旱区资源与环境,2005,19(4):92-97.
[3] 宋炳煜,杨劼.关于生态用水研究的讨论[J].自然资源学报,2003,18(5):617-625.
[4] 肖向明,王义凤,陈佐忠.内蒙古锡林河流域典型草原初级生产力和土壤有机质的动态及其对气候变化的反应[J].植物学报,1996,38(1):45-52.
[5] 彭皓,李镇清.锡林河流域天然草地生态系统服务价值评价[J].草业学报,2007,16(4):107-115.
[6] 仝川,杨景荣,雍伟义,等.锡林河流域草原植被退化空间格局分析[J].自然资源学报,2002,17(5):571-578.
[7] 白永飞,张丽霞,张焱,等.内蒙古锡林河流域草原群落植物功能群组成沿水热梯度变化的样带研究[J].植物生态学报,2002,26(3):308-316.
[8] 顾晓鹤,何春阳,潘耀忠,等.基于生态风险评估的锡林河流域退化草地优化管理[J].应用生态学报,2007,18(5):968-976.
[9] 徐玉貌,刘红年,徐桂玉.大气科学概论[M].南京:南京大学出版社,2000.
[10] 马耀明,王介民.卫星遥感结合地面观测估算非均匀地表区域能量通量[J].气象学报,1999,57(2):180-189.
[11] 于红博,杨劼,宋炳煜.皇甫川流域蒸散量遥感估算及动态变化研究[J].水土保持研究,2013,20(1):107-111.
[12] 王介民,高峰.关于地表反照率遥感反演的几个问题[J].遥感技术与应用,2004,19(5):295-300.
[13] 赵军,刘春雨,潘竟虎,等.基于MODIS数据的甘南草原区域蒸散发量时空格局分析[J].资源科学,2011,33(2):341-346.
[14] 王军.基于TM数据的草地蒸散发研究[D].北京:中国水利水电科学研究院,2012.
[15] 潘志强,刘高焕.黄河三角洲蒸散的遥感研究[J].地球信息科学,2003(3):91-96.
[16] 谢贤群.遥感瞬时作物表面温度估算农田全日蒸散总量[J].环境遥感,1991,6(4):253-260.

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