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Multi-Scale Sensible Heat Fluxes in the Suburban Environment from Large-Aperture Scintillometry and Eddy Covariance

机译:大口径闪烁法和涡动协方差在郊区环境中的多尺度感热通量

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摘要

Sensible heat fluxes (Q(H)) are determined using scintillometry and eddy covariance over a suburban area. Two large-aperture scintillometers provide spatially integrated fluxes across path lengths of 2.8 and 5.5 km over Swindon, UK. The shorter scintillometer path spans newly built residential areas and has an approximate source area of 2-4 km(2), whilst the long path extends from the rural outskirts to the town centre and has a source area of around 5-10 km(2). These large-scale heat fluxes are compared with local-scale eddy-covariance measurements. Clear seasonal trends are revealed by the long duration of this dataset and variability in monthly Q(H) is related to the meteorological conditions. At shorter time scales the response of Q(H) to solar radiation often gives rise to close agreement between the measurements, but during times of rapidly changing cloud cover spatial differences in the net radiation (Q*) coincide with greater differences between heat fluxes. For clear days Q(H) lags Q*, thus the ratio of Q(H) to Q* increases throughout the day. In summer the observed energy partitioning is related to the vegetation fraction through use of a footprint model. The results demonstrate the value of scintillometry for integrating surface heterogeneity and offer improved understanding of the influence of anthropogenic materials on surface-atmosphere interactions
机译:感热通量(Q(H))使用闪烁法和郊区的涡动协方差确定。在英国史云顿,两个大孔径闪烁仪提供了在2.8和5.5 km路径长度上的空间积分通量。较短的闪烁仪路径跨越新建的居民区,并且具有大约2-4 km(2)的源区域,而长路径从乡村郊区延伸到镇中心,并且具有大约5-10 km(2)的源区域。 )。将这些大规模的热通量与局部规模的涡旋协方差测量结果进行比较。该数据集的持续时间揭示了明显的季节性趋势,并且月度Q(H)的变化与气象条件有关。在更短的时间尺度上,Q(H)对太阳辐射的响应通常会导致测量之间的紧密一致性,但是在云层快速变化的时期,净辐射(Q *)中的空间差异与热通量之间的较大差异相吻合。对于晴天,Q(H)落后于Q *,因此Q(H)与Q *的比率在一天中增加。在夏季,通过使用足迹模型,观察到的能量分配与植被比例有关。结果证明了闪烁法对于整合表面异质性的价值,并提供了对人为物质对表面-大气相互作用影响的更好理解。

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