光纤分布式温度传感用于揭示森林-空气界面混合过程和高阶矩的适用性

O. Peltola, K. Lapo, I. Martinkauppi, E. O'connor, Christoph K. Thomas, T. Vesala
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引用次数: 15

摘要

摘要对光纤分布式温度传感(DTS)技术观测森林内外大气混合剖面的适用性进行了量化分析。在北方松林125 m高的桅杆上进行空间连续观测。由于粗糙度元素(即树木)对气流的影响,森林冠层附近的气流与典型的边界层气流存在差异。理想情况下,这些复杂的气流应该用空间连续测量来研究,但这种测量方法不能用传统的微气象测量方法来实现,比如声波风速计。从而量化了DTS测量对冠层流量研究的适用性。DTS测量能够识别湍流波动的连续剖面和沿桅杆的空气温度平均值,提供有关混合过程的信息(例如冠层涡流,夜间逆温层的演变)以及森林-大气界面的三阶湍流统计数据。在现场使用三维声速仪和多普勒激光雷达进行的湍流测量也被用于分析。紊流统计的连续剖面与前人在风洞和冠层流动大涡模拟中所做的研究一致。DTS测量包含一个显著的噪声成分,然而,量化和它对湍流统计的影响是考虑的。对高频率下气温波动的低估导致了…在典型流动条件下,温度变化低估30%。尽管有这些限制,DTS测量在其他集中在粗糙元素和/或非平稳时期附近流动的研究中也应该证明是有用的,因为测量揭示了流动的时空模式,这是不可能从固定在空间中的单点测量中辨别出来的。
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Suitability of fibre-optic distributed temperature sensing for revealing mixing processes and higher-order moments at the forest–air interface
Abstract. Suitability of fibre-optic distributed temperature sensing (DTS) technique to observe atmospheric mixing profiles within and above forest was quantified and these profiles were analysed. The spatially continuous observations were made at a 125 m tall mast in a boreal pine forest. Air flows near forest canopies diverge from typical boundary layer flows due to the influence of roughness elements (i.e. trees) on the flow. Ideally these complex flows should be studied with spatially continuous measurements, yet such measurements are not feasible with conventional micrometeorological measurements with e.g. sonic anemometers. Hence the suitability of DTS measurements for studying canopy flows was quantified. The DTS measurements were able to discern continuous profiles of turbulent fluctuations and mean values of air temperature along the mast providing information about mixing processes (e.g. canopy eddies, evolution of inversion layers at night) and up to third order turbulence statistics across the forest-atmosphere interface. Turbulence measurements with 3D sonic anemometers and Doppler lidar at the site were also utilised in this analysis. The continuous profiles for turbulence statistics were in line with prior studies made at wind tunnels and large eddy simulations for canopy flows. The DTS measurements contained a significant noise component which was however quantified and its effect on turbulence statistics was accounted for. Underestimation of air temperature fluctuations at high frequencies caused 20...30 % underestimation of temperature variance at typical flow conditions. Despite these limitations, the DTS measurements should prove useful also in other studies concentrating on flows near roughness elements and/or non-stationary periods, since the measurements revealed spatio-temporal patterns of the flow which were not possible to discern from single point measurements fixed in space.
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