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Momentum transfer by a mountain meadow canopy: a simulation analysis based on Massman's (1997) model

机译:山地草甸冠层的动量传递:基于Massman(1997)模型的模拟分析

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摘要

Using a mountain meadow as a case study it is the objective of the present paper to develop a simple parameterisation for the within-canopy variation of the phytoelement drag (C_d) and sheltering (P_m) coefficients required for Massman's model of momentum transfer by vegetation. A constant ratio between C_d and P_m is found to overestimate wind speed in the upper canopy and underestimate it in the lower canopy. Two simple parameterisations of C_d/P_m as a function of the plant area density and thecumulative plant area index are developed, using values optimised by least-squares regression between measured and predicted within-canopy wind speeds. A validation with independently measured data indicates that both parameterisations work reliably forsimulating wind speed in the investigated meadow. Model predictions of the normalised zero-plane displacement height and the momentum roughness length fall only partly within the range of values given in literature, which may be explained by the accumulation of plant matter close to the soil surface specific for the investigated canopies. The seasonal course of the normalised zero-plane displacement height and the momentum roughness length are discussed in terms of the seasonal variation of the amount and density of plant matter.
机译:本文以高山草甸为例,目的是为马斯曼植被动量传递模型所需的植物元素阻力(C_d)和遮蔽系数(P_m)的树冠内变化开发简单的参数化方法。发现C_d与P_m之间的比率恒定会高估上部冠层的风速,而低估下部冠层的风速。利用通过测量和预测冠层内风速之间的最小二乘回归优化的值,开发了两个简单的参数化C_d / P_m,它们是植物面积密度和累积植物面积指数的函数。对独立测量的数据进行的验证表明,这两个参数设置都可以可靠地模拟被调查草甸的风速。归一化零平面位移高度和动量粗糙度长度的模型预测仅部分落在文献中给出的值范围内,这可以通过靠近被调查树冠特定土壤表面的植物堆积来解释。归一化零平面位移高度和动量粗糙度长度的季节性过程根据植物数量和密度的季节性变化进行了讨论。

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