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A site-level comparison of lysimeter and eddy covariance flux measurements of evapotranspiration

机译:蒸散发蒸渗仪和涡流协方差流量测量的站点水平比较

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Accurate measurements of evapotranspiration are required for many meteorological, climatological, ecological, and hydrological research applications and developments. Here we examine and compare two well-established methods to determine evapotranspiration at the site level: lysimeter-based measurements?(iE/isubL/sub) and eddy covariance?(EC) flux measurements?(iE/isubEC/sub). The analyses are based on parallel measurements carried out with these two methods at the research catchment Rietholzbach in northeastern Switzerland, and cover the time period of June?2009 to December?2015. The measurements are compared on various timescales, and with respect to a 40-year lysimeter-based evapotranspiration time series. Overall, the lysimeter and EC measurements agree well, especially on the annual timescale. On that timescale, the long-term lysimeter measurements also correspond well with catchment water-balance estimates of evapotranspiration. This highlights the representativeness of the site-level lysimeter and EC measurements for the entire catchment despite their comparatively small source areas and the heterogeneous land use and topography within the catchment. Furthermore, we identify that lack of reliable EC measurements using open-path gas analyzers during and following precipitation events (due to limitations of the measurement technique under these conditions) significantly contributes to an underestimation of iE/isubEC/sub and to the overall energy balance gap at the site.
机译:许多气象,气候,生态和水文研究应用和开发都需要准确测量蒸散量。在这里,我们检查并比较了两种确定站点蒸发蒸腾量的成熟方法:基于溶渗仪的测量值( E L )和涡流协方差值(EC)通量测量值?( E EC )。这些分析是基于在瑞士东北部研究流域Rietholzbach上用这两种方法进行的并行测量得出的,覆盖时间为2009年6月至2015年12月。在不同的时间尺度上对测量结果进行比较,并基于40年的基于蒸渗仪的蒸散时间序列进行比较。总体而言,溶渗仪和EC的测量结果非常吻合,尤其是在年度时间表上。在该时间尺度上,长期的测渗仪测量值也与蒸散量的流域水平衡估计值非常吻合。这突出显示了整个集水区的站点级溶度计和EC测量的代表性,尽管它们的源区相对较小,并且集水区内的土地利用和地形不均。此外,我们发现,在降水事件期间和之后(由于在这些条件下测量技术的局限性),使用开路气体分析仪缺乏可靠的EC测量值明显导致了 E 的低估。 EC 和该站点的整体能量平衡差距。

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