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A comparison of eddy-covariance and large aperture scintillometer measurements with respect to the energy balance closure problem

机译:涡动协方差和大口径闪烁仪测量关于能量平衡关闭问题的比较

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We analyzed the seasonal variations of energy balance components over threedifferent surfaces: irrigated cropland (Yingke, YK), alpine meadow (A'rou,AR), and spruce forest (Guantan, GT). The energy balance components weremeasured using eddy covariance (EC) systems and a large aperturescintillometer (LAS) in the Heihe River Basin, China, in 2008 and 2009. Wealso determined the source areas of the EC and LAS measurements with afootprint model for each site and discussed the differences between thesensible heat fluxes measured with EC and LAS at AR. The results show thatthe main EC source areas were within a radius of 250 m at all of the sites.The main source area for the LAS (with a path length of 2390 m) stretchedalong a path line approximately 2000 m long and 700 m wide. The surfacecharacteristics in the source areas changed with the season at each site,and there were characteristic seasonal variations in the energy balancecomponents at all of the sites. The sensible heat flux was the main term ofthe energy budget during the dormant season. During the growing season,however, the latent heat flux dominated the energy budget, and an obvious"oasis effect" was observed at YK. The sensible heat fluxes measured byLAS at AR were larger than those measured by EC at the same site. Thisdifference seems to be caused by the so-called energy imbalance phenomenon,the heterogeneity of the underlying surfaces, and the difference between thesource areas of the LAS and EC measurements.
机译:我们分析了三种不同表面上的能量平衡成分的季节性变化:灌溉农田(Yingke,YK),高山草甸(A'rou,AR)和云杉林(关丹,GT)。在2008年和2009年,使用涡协方差(EC)系统和大孔径闪烁闪烁仪(LAS)在中国黑河流域测量了能量平衡成分。我们还使用足迹模型确定了每个站点和区域的EC和LAS测量的源区域。讨论了用AR和EC和LAS测量的显热通量之间的差异。结果表明,所有站点的主要EC源区域均在250 m半径范围内.LAS的主要源区域(路径长度为2390 m)沿约2000 m长,700 m宽度的路径线伸展。每个地点的源区地表特征都随季节而变化,并且所有地点的能量平衡成分都存在典型的季节变化。显热通量是休眠季节能量预算的主要术语。然而,在生长季节,潜热通量支配了能量收支,并且在YK观察到明显的“绿洲效应”。在同一地点,LAS在AR处测得的显热通量大于EC所测得的显热通量。这种差异似乎是由所谓的能量失衡现象,下层表面的异质性以及LAS和EC测量的源区域之间的差异引起的。

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