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The use of large aperture scintillometer and eddy covariance system for monitoring energy and water vapour fluxes over different surfaces in the Heihe River Basin, China

机译:利用大口径闪烁仪和涡动协方差监测黑河流域不同表面的能量和水蒸气通量

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We analysed the seasonal variations of energy and water vapour fluxes, with a special focus on evapotranspiration (ET) over various surfaces: irrigated cropland (Yingke, YK), alpine meadow (A'rou, AR), and spruce forest (Guantan, GT). Energy and water vapour fluxes were measured using eddy covariance systems (EC) and a large aperture scintillometer (LAS) in the Heihe River Basin, China, in 2008 and 2009. We also determined the source areas of EC and LAS measurements for each site. The results show that the main EC source area was within a radius of 200 m at all sites. The main source area for the LAS (with a path length of 2390 m) stretched along a path line about 2000 m long and 700 m wide. The ground surface conditions in the source areas changed with season and site, and there were characteristic seasonal variations in energy and water vapour fluxes at all sites. The sensible heat flux was the main term of the energy budget during the dormant season. During the growing season, the latent heat flux dominated the energy budget, and an obvious "oasis effect" was observed at YK. The monthly ET reached its peak in July at YK and June at GT in both 2008 and 2009, while at AR it reached its peak in August in 2008 and June in 2009. ET at AR measured by different scales (kilometres scale, LAS; hundred metre scale, EC) had the similar monthly variations, presenting single peak patterns (appearing in August in 2008). There are also some differences between LAS and EC measurements because of the energy imbalance of EC system, the different source areas and surface heterogeneity.
机译:我们分析了能量和水蒸气通量的季节性变化,特别关注了各种表面的蒸散量(ET):灌溉农田(Yingke,YK),高山草甸(A'rou,AR)和云杉林(关丹,GT) )。使用涡协方差系统(EC)和大孔径闪烁仪(LAS)在中国黑河流域分别于2008年和2009年测量了能量和水蒸气通量。我们还确定了每个站点的EC和LAS测量值的源区域。结果表明,所有地点的主要EC源区域均在200 m半径内。 LAS的主要来源区域(路径长度为2390 m)沿着约2000 m长和700 m宽的路径线延伸。源区的地表条件随季节和地点而变化,并且所有地点的能量和水汽通量都有典型的季节变化。显热通量是休眠季节能源预算的主要术语。在生长季节,潜热通量支配了能源预算,在YK观察到了明显的“绿洲效应”。月度ET分别在2008年和2009年的YK和6月的GT达到了峰值,而在AR,则分别在2008年8月和2009年6月达到了峰值。AR的ET用不同的尺度(千分尺,LAS;百电表规模,EC)具有类似的每月变化,呈现出单峰模式(2008年8月出现)。由于EC系统的能量不平衡,不同的源区域和表面异质性,LAS和EC测量之间也存在一些差异。

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