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论文:基于混合双源模式和梯形状态空间的遥感蒸散发模型HTEM

已有 6066 次阅读 2013-3-6 19:44 |个人分类:论著|系统分类:论文交流| 蒸散发, 混合双源模式, 梯形状态空间, 遥感模型

 
A Hybrid Dual Source Scheme and Trapezoid Framework Based Evapotranspiration Model (HTEM) Using Satellite Images: Algorithm and Model Test
  1. Yuting Yang,
  2. Songhao Shang*

DOI: 10.1002/jgrd.50259

Author InformationPublication History

Author Information
  1. State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing, China

*Corresponding Author: Songhao Shang, Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China Email: shangsh@tsinghua.edu.cn Telephone: 86-10-62796674 Fax: 86-10-62796971

  • This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process, which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1002/jgrd.50259

Publication History
  1. Accepted manuscript online: 4 MAR 2013 09:43AM EST
  2. Manuscript Accepted: 7 FEB 2013
  3. Manuscript Revised: 30 JAN 2013
  4. Manuscript Received: 19 JUL 2012
Keywords:
  • Satellite remote sensing;
  • Evaporation;
  • Hybrid dual source scheme;
  • Trapezoid framework;
  • Transpiration
Abstract

[1] Satellite remote sensing techniques are widely considered as the most promising way to estimate evapotranspiration (ET) over large geographic extents. In this study, a hybrid dual source scheme and trapezoid framework based evapotranspiration model (HTEM) is developed to map evapotranspiration from satellite imagery. It adopts a theoretically-determined vegetation index/Land surface temperature trapezoidal space to decompose bulk radiative surface temperature into component temperatures (soil & canopy), and uses a hybrid dual source scheme of the layer approach and patch approach to partition net radiation and estimate sensible and latent fluxes separately from the soil and canopy. The proposed model was tested at the Soil Moisture-Atmosphere Coupling Experiment (SMACEX) site in central Iowa, U.S., on three days during the campaign in 2002 using Landsat TM/ETM + data, and at the Weishan flux site on North China Plain during the main growing season of 2007 with MODIS Terra images. Results indicate that HTEM is capable in estimating latent heat flux (LE) with the mean absolute percentage error of 6.4% and 11.2% for the SMACEX and the Weishan sites, respectively. Besides, the model was found to be able to give reasonable evaporation and transpiration partitioning at both sites. Compared with other models, the HTEM generally produced better sensible and latent flux estimates at the two sites and had comparable ability to estimate net radiation and ground heat flux. Sensitivity analysis suggests that HTEM is most sensitive to temperature variables and less sensitive to other meteorological observations and parameters.



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