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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:大孔径闪烁仪和涡流协方差系统的应用,以监测海里河流域不同表面的能量和水蒸气势态

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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势态的季节变化,特别关注蒸散(ET)在各种表面上:灌溉农田(yingke,YK),高山草甸(A'rou,Ar)和云杉森林(瓜丹,GT )。使用Eddy协方差系统(EC)和Heihe River Basin,2008年和2009年,使用涡流协方差系统(EC)和大型光圈闪烁计(LAS)测量能量和水蒸气。我们还确定了每个站点的EC和LAS测量的源区。结果表明,主EC源区在所有网站的半径范围内。 LAS的主要源区(具有2390米的路径长度)沿着大约2000米长的路径线延伸,宽700米。源区的地表条件随季节和场地而变化,并且在所有地点都有特征季节性变化。明智的热量通量是休眠期间能量预算的主要术语。在生长季节期间,潜热通量主导了能源预算,在YK时观察到明显的“绿洲效应”。每月ET于2008年和2009年7月在yk和6月达到了峰值,而在2008年8月在2008年8月在2009年达到其高峰期。通过不同尺度(公里规模,LAS;百仪表规模,EC)具有类似的月度变化,呈现单一峰值模式(在2008年8月出现)。由于EC系统的能量不平衡,不同的源区和表面异质性,LAS和EC测量之间也存在一些差异。

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