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Performance of various similarity functions for nondimensional wind and temperature profiles in the surface layer in stable conditions

机译:在稳定条件下对表层中的无量纲风和温度曲线执行各种相似功能

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摘要

The linear functions for non-dimensional wind and temperature profiles are commonly used to describe the surface layer fluxes in atmospheric models. However, their applicability is limited to smaller values of the stability parameter z/L (where z is the height above ground and L is the Obukhov length) i.e. z/L1.0 under strongly stable conditions, in view of this, the objective of the present study is to analyze the performance of these similarity functions to compute surface fluxes in stable conditions.rnThe meteorological observations from the Cooperative Atmosphere-Surface Exchange Study (CASES-99) experiment are utilized for computing the surface fluxes in stable conditions. The computed fluxes are found to be reasonably close to those observed. The ratio of observed to computed fluxes reveals that the computed fluxes are close to the observations for all the similarity functions for z/L< 1.0 whereas the computed values show relatively a large scatter from observations for z/L > 1.0. The computed values of u* and heat flux do not show significant differences from those observed at 99% confidence limit. The performance of all the similarity functions considered here is found to be comparable to each other in strongly stable conditions.
机译:无量纲风和温度剖面的线性函数通常用于描述大气模型中的表层通量。但是,它们的适用性仅限于稳定性参数z / L的较小值(其中z是地面上的高度,L是Obukhov长度),即z / L 1.0在强稳定条件下,鉴于此,本研究的目的是分析这些相似函数在稳定条件下计算表面通量的性能.rn来自合作的大气-地表交换研究的气象观测( CASES-99)实验用于计算稳定条件下的表面通量。发现计算出的通量与观察到的通量相当接近。观察到的通量与计算通量之比表明,对于z / L <1.0,所有相似函数的计算通量都接近于观测值,而对于z / L> 1.0,计算值显示出相对较大的分散。 u *和热通量的计算值与在99%置信极限下观察到的值没有显着差异。发现此处考虑的所有相似性函数的性能在非常稳定的条件下彼此可比。

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