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Influence of Canopy Seasonal Changes on Turbulence Parameterization within the Roughness Sublayer over an Orchard Canopy

机译:林冠季节变化对果园林冠粗糙度下湍流参数化的影响

摘要

In this observational study, the role of tree phenology on the atmospheric turbulence parameterization over 10-m-tall and relatively sparse deciduous vegetation is quantified. Observations from the Canopy Horizontal Array Turbulence Study (CHATS) field experiment are analyzed to establish the dependence of the turbulent exchange of momentum, heat, and moisture, as well as kinetic energy on canopy phenological evolution through widely used parameterization models based on 1) dimensionless gradients or 2) turbulent kinetic energy (TKE) in the roughness sublayer. Observed vertical turbulent fluxes and gradients of mean wind, temperature, and humidity, as well as velocity variances, are used in combination with empirical dimensionless functions to calculate the turbulent exchange coefficient. The analysis shows that changes in canopy phenology influence the turbulent exchange of all quantities analyzed in this study. The turbulent exchange coefficients of those quantities are twice as large near the canopy top for a leafless canopy than for a full-leaf canopy under unstable and near-neutral conditions. This turbulent exchange coefficient difference is related to the differing penetration depths of the turbulent eddies organized at the canopy top, which increase for a canopy without leaves. The TKE and dissipation analysis under near-neutral atmospheric conditions additionally shows that TKE exchange increases for a leafless canopy because of reduced TKE dissipation efficiency relative to that when the canopy is in full-leaf stage. The study closes with discussion surrounding the implications of these findings for parameterizations used in large-scale models.
机译:在这项观察性研究中,量化了树木物候学对10米高和相对稀疏的落叶植被的大气湍流参数化的作用。通过基于1)无量纲的广泛使用的参数化模型,对冠层水平阵列湍流研究(CHATS)现场实验的观察结果进行了分析,以建立动量,热量和水分以及动能的湍流交换对冠层物候演化的依赖性。梯度或2)粗糙度子层中的湍动能(TKE)。将观测到的垂直湍流和平均风,温度和湿度的梯度以及速度方差与经验的无量纲函数结合使用以计算湍流交换系数。分析表明,冠层物候的变化会影响本研究中分析的所有量的湍流交换。在不稳定和接近中性的条件下,无叶顶篷的顶篷顶部附近的湍流交换系数是全叶顶篷的两倍。该湍流交换系数差异与在冠层顶部组织的湍流涡流的不同渗透深度有关,对于没有叶子的冠层,渗透深度增加。在接近中性的大气条件下的TKE和耗散分析还表明,相对于全叶阶段的TKE耗散效率降低,无叶冠层的TKE交换增加。该研究结束时围绕有关这些发现对大规模模型中使用的参数化的含义的讨论。

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