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首页> 外文期刊>Arctic, antarctic, and alpine research >Feasibility of retrieving land surface heat fluxes from ASTER data using SEBS: A case study from the NamCo area of the Tibetan Plateau
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Feasibility of retrieving land surface heat fluxes from ASTER data using SEBS: A case study from the NamCo area of the Tibetan Plateau

机译:利用SEBS反演ASTER数据反演地表热通量的可行性-以青藏高原纳木错地区为例。

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摘要

Surface fluxes are important boundary conditions for climatological modeling and the Asian monsoon system. The recent availability of high-resolution, multi-band imagery from the ASTER (Advanced Space-borne Thermal Emission and Reflection radiometer) sensor has enabled us to estimate surface fluxes to bridge the gap between local-scale flux measurements using micrometeorological instruments and regional scale land-atmosphere exchanges of water and heat fluxes that are fundamental for the understanding of the water cycle in the Asian monsoon system. A Surface Energy Balance System (SEBS) method based on ASTER data and field observations has been proposed and tested in this paper for deriving 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, the methodology was applied to an experimental area at NamCo, located at the central Tibetan Plateau, China. The ASTER data of 11 June 2006, 29 October 2007, and 25 February 2008 was used in this paper for the NamCo area case. To validate the proposed methodology, the ground-measured land surface heat fluxes (net radiation flux (Rn), soil heat flux (G0), sensible heat flux (H), and latent heat flux (λE)) were compared to the ASTER derived values. The results show that the derived land surface heat fluxes in different months over the study area are in good accordance with the land surface status. The tendency is basically to maintain consistency. It is therefore concluded that the proposed methodology is successful for the retrieval of land surface heat fluxes using the ASTER data and filed observations over the study area.
机译:地表通量是气候模拟和亚洲季风系统的重要边界条件。 ASTER(先进的星载热发射和反射辐射计)传感器最近提供了高分辨率,多波段图像,这使我们能够估算表面通量,以弥合使用微气象仪器和区域尺度进行的局部通量测量之间的差距陆地与大气之间的水和热通量交换,这对于理解亚洲季风系统的水循环至关重要。提出了一种基于ASTER数据和现场观测的表面能平衡系统(SEBS)方法,并进行了测试,以推导净辐射通量(Rn),土壤热通量(G0),显热通量(H)和潜热异质陆面上的通量(λE)。作为案例研究,该方法被应用于位于中国青藏高原中部的南科实验区。本文针对NamCo地区案例使用了2006年6月11日,2007年10月29日和2008年2月25日的ASTER数据。为了验证所提出的方法,将地面测量的地面热通量(净辐射通量(Rn),土壤热通量(G0),显热通量(H)和潜热通量(λE))与ASTER推导进行了比较。价值观。结果表明,研究区域内不同月份得到的地表热通量与地表状况基本吻合。趋势基本上是保持一致性。因此,可以得出结论,所提出的方法成功地利用了ASTER数据并在研究区域内进行了观测,从而成功地检索了地面热通量。

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