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Determination of Roughness Lengths for Heat and Momentum Over Boreal Forests

机译:北方森林热量和动量粗糙度的确定

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The roughness length for momentum (z0m), zero-plane displacementheight (d), and roughness length for heat (z0h) are importantparameters used to estimate land-atmosphere energy exchange. Although many different approaches have been developed to parameterizemomentum and heat transfer, existing parameterizations generally utilizehighly simplified representations of vegetation structure. Further, a mismatch exists between the treatments used for momentum and heat exchange and those used for radiative energy exchanges. In this paper, parameterizations are developed to estimate z0m, d, and z0h for forested regimes using information related to tree crown density and structure. The parameterizations provide realistic representationfor the vertical distribution of foliage within canopies, and include explicit treatment for the effects of the canopy roughness sublayer and leaf drag on momentum exchange. The proposed parameterizationsare able to realistically account for site-to-site differences in roughness lengths that arise from canopy structural properties.Comparisons between model predictions and field measurements show good agreement, suggesting that the proposed parameterizations capture the most important factors influencing turbulent exchange of momentumand heat over forests.
机译:动量的粗糙度长度(z0m ),零平面位移高度(d)和热的粗糙度长度(z0h )是用于估算陆地-大气能量交换的重要参数。尽管已经开发出许多不同的方法来对动量和热传递进行参数化,但是现有的参数化通常利用植被结构的高度简化表示。此外,在用于动量和热交换的处理与用于辐射能交换的处理之间存在不匹配。本文利用与树冠密度和结构有关的信息,开发了参数化方法来估计森林状态的z0m ,d和z0h 。参数化为冠层内的叶子的垂直分布提供了逼真的表示,并且包括对冠层粗糙度子层和叶阻力对动量交换的影响的显式处理。拟议的参数化能够真实地解释冠层结构特性引起的粗糙度长度之间的位置差异,模型预测与现场测量之间的比较显示出很好的一致性,这表明拟议的参数化捕获了影响动量和湍流交换的最重要因素。森林上热。

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