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Turbulence Spectra and Cospectra Under the Influence of Large Eddies in the Energy Balance EXperiment (EBEX)

机译:能量平衡实验(EBEX)中大涡度影响下的湍流谱和共谱

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During the Energy Balance EXperiment, the patch-by-patch, flood irrigation in a flat cotton field created an underlying surface with heterogeneous soil moisture, leading to a dry (warm)-to-wet (cool) transition within the cotton field under northerly winds. Moreover, the existence of an extremely dry, large bare soil area upstream beyond the cotton field created an even larger step transition from the bare soil region to the cotton field. We investigated the turbulence spectra and cospectra in the atmospheric surface layer (ASL) that was disturbed by large eddies generated over regions upstream and also influenced by horizontal advection. In the morning, the ASL was unstable while in the afternoon a stable internal boundary layer was observed at the site. Therefore, the turbulence data at 2.7 and 8.7m are interpreted and compared in terms of interactions between large eddies and locally generated turbulence under two atmospheric conditions: the unstable ASL beneath the convective boundary layer (CBL) (hereafter the unstable condition) and the stable ASL beneath the CBL (hereafter the stable condition). We identified the influences of multiple sizes of large eddies on ASL turbulence under both stratifications; these large eddies with multiple sizes were produced over the dry patches and dry, large bare soil areas upstream. As a consequence of the disturbance of large eddies, the broadening, erratic variability, and deviation of spectra and cospectra, relative to those described by Monin-Obukhov similarity theory, are evident in the low- to mid-frequencies. Transfer of momentum, heat, and water vapour by large eddies is distinctly observed from the turbulence cospectra and leads to significant run-to-run variations of residuals of the surface energy balance closure. Our results indicate that these large eddies have greater influences on turbulence at higher levels compared to lower levels, and in the unstable ASL compared to the stable ASL.
机译:在能源平衡试验期间,在平坦的棉田中逐块进行洪水灌溉,形成了下层土壤水分不均的底层表面,导致北下的棉田内发生了从干(暖)到湿(凉)的转变风。而且,棉田上游上游极度干燥的大裸土面积的存在,导致了从裸土区到棉田的更大的阶跃过渡。我们研究了大气表层(ASL)的湍流光谱和共谱,该湍流光谱和共谱受到上游区域上方产生的大涡流的干扰,并且还受到水平对流的影响。早晨,ASL不稳定,而下午则在现场观察到稳定的内部边界层。因此,在两种大气条件下,即对流边界层(CBL)下的不稳定ASL(以下称不稳定条件)和稳定条件下的大涡与局部湍流之间的相互作用来解释和比较2.7和8.7m处的湍流数据。 CBL下方的ASL(此后为稳定状态)。我们确定了两种分层下大涡的多种尺寸对ASL湍流的影响。这些具有多种尺寸的大涡流产生于干燥的斑块和上游干燥的大裸露土壤区域。由于大涡流的扰动,相对于Monin-Obukhov相似性理论描述的那些,光谱和共谱的扩宽,不稳定的可变性以及谱和共谱的偏差在中低频率中很明显。从湍流共谱中可以清楚地看到动量,热量和水蒸气通过大涡流的传递,并导致表面能平衡封闭的残差之间存在显着的差异。我们的结果表明,与较低的水平相比,这些较大的涡流在较高水平时对湍流的影响更大,在稳定ASL中则对不稳定的ASL有更大的影响。

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