首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Determination of regional distributions and seasonal variations of land surface heat fluxes from Landsat-7 Enhanced Thematic Mapper data over the central Tibetan Plateau area
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Determination of regional distributions and seasonal variations of land surface heat fluxes from Landsat-7 Enhanced Thematic Mapper data over the central Tibetan Plateau area

机译:利用青藏高原中部地区Landsat-7增强专题制图仪数据确定地表热通量的区域分布和季节变化

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In this study, a parameterization method based on Landsat-7 ETM data and field observations has been proposed and tested for deriving surface reflectance, surface temperature, NDVI, MSAVI, vegetation coverage, LAI, net radiation flux, soil heat flux, sensible heat flux and latent heat flux over heterogeneous landscape. As a case study, the methodology was applied to the experimental area of the CAMP/Tibet, which located at the central Tibetan Plateau. Two scenes of Landsat-7 ETM data were used in this study. The scene of 9 June 2002 was selected as a case of summer, and the scene of 2 December 2002 was selected as a case of winter. To validate the proposed methodology, the ground-measured surface reflectance, surface temperature, net radiation flux, soil heat flux, sensible heat flux and latent heat flux are compared to Landsat-7 ETM derived values. The results show that the derived surface variables and land surface heat fluxes in two different months over the study area are in good accordance with the land surface status. These parameters show a wide range due to the strong contrast of surface features. Also, the estimated land surface variables and land surface heat fluxes are in good agreement with ground measurements, and all their absolute percent difference is less than 9.9% in the validation sites. It is therefore concluded that the proposed methodology is successful for the retrieval of land surface variables and land surface heat fluxes using the Landsat-7 ETM data and filed observations over the study area.
机译:在这项研究中,提出了一种基于Landsat-7 ETM数据和现场观测的参数化方法,并进行了测试,以得出表面反射率,表面温度,NDVI,MSAVI,植被覆盖率,LAI,净辐射通量,土壤热通量,显热通量。和非均匀景观上的潜热通量。作为案例研究,该方法应用于位于青藏高原中部的CAMP /西藏实验区。在这项研究中使用了两个Landsat-7 ETM数据场景。选择2002年6月9日为夏季的场景,选择2002年12月2日为冬季的场景。为了验证所提出的方法,将地面测量的表面反射率,表面温度,净辐射通量,土壤热通量,显热通量和潜热通量与Landsat-7 ETM得出的值进行了比较。结果表明,研究区域内两个月内得出的地表变量和地表热通量与地表状况基本吻合。由于表面特征的强烈对比,这些参数显示范围很广。而且,估计的地表变量和地表热通量与地面测量值非常吻合,在验证地点,它们的绝对百分比差异均小于9.9%。因此,可以得出结论,使用Landsat-7 ETM数据并在研究区域进行了观测,所提出的方法成功地检索了地表变量和地表热通量。

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