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Estimating surface fluxes over middle and upper streams of the Heihe River Basin with ASTER imagery

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Ma WQ, Ma YM, Hu ZY, Su B, Wang JM, Ishikawa H. Estimating surface fluxes over middle and upper streams of the Heihe River Basin with ASTER imagery. Hydrology and Earth System Sciences, 2011, 15(5): 1403-1413. doi:10.5194/hess-15-1403-2011.
Literature information
Type Of Reference JOUR
Title Estimating surface fluxes over middle and upper streams of the Heihe River Basin with ASTER imagery
Authors Ma, W.| Ma, Y.| Hu, Z.| Su, Z.| Wang, J.| Ishikawa, H.|
Secondary Title Hydrology and Earth System Sciences
Abstract Land surface heat fluxes are essential measures of the strengths of land-atmosphere interactions involving energy, heat and water. Correct parameterization of these fluxes in climate models is critical. Despite their importance, state-of-the-art observation techniques cannot provide representative areal averages of these fluxes comparable to the model grid. Alternative methods of estimation are thus required. These alternative approaches use (satellite) observables of the land surface conditions. In this study, the Surface Energy Balance System (SEBS) algorithm was evaluated in a cold and arid environment, using land surface parameters derived from Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data. Field observations and estimates from SEBS were compared in terms of net radiation flux (Rn), soil heat flux (G0), sensible heat flux (H) and latent heat flux (λE) over a heterogeneous land surface. As a case study, this methodology was applied to the experimental area of the Watershed Allied Telemetry Experimental Research (WATER) project, located on the mid-to-upstream sections of the Heihe River in northwest China. ASTER data acquired between 3 May and 4 June 2008, under clear-sky conditions were used to determine the surface fluxes. Ground-based measurements of land surface heat fluxes were compared with values derived from the ASTER data. The results show that the derived surface variables and the land surface heat fluxes furnished by SEBS in different months over the study area are in good agreement with the observed land surface status under the limited cases (some cases looks poor results). So SEBS can be used to estimate turbulent heat fluxes with acceptable accuracy in areas where there is partial vegetation cover in exceptive conditions. It is very important to perform calculations using ground-based observational data for parameterization in SEBS in the future. Nevertheless, the remote-sensing results can provide improved explanations of land surface fluxes over varying land coverage at greater spatial scales.
Date 2011//06/
Year 2011
DOI 10.5194/hess-15-1403-2011
Database Provider Copernicus Online Journals
volume 15
Issue Number 5
Start Page 1403
Alternate Title1 Hydrol. Earth Syst. Sci.
Issn 1607-7938
Url http://www.hydrol-earth-syst-sci.net/15/1403/2011/
Access Date 2013/11/02/10:19:16
file_attachments2 http://www.hydrol-earth-syst-sci.net/15/1403/2011/
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