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A Semi-Analytical Approach for Parametrization of the Obukhov Stability Parameter in the Unstable Atmospheric Surface Layer

机译:不稳定大气表层Obukhov稳定性参数参数化的半解析方法

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A semi-analytical scheme is proposed to parametrize the Obukhov stability parameter zeta (= z/L; z is the height above the ground and L is the Obukhov length) in terms of the bulk Richardson number (R-iB) in unstable conditions within the framework of Monin-Obukhov similarity (MOS) theory. The scheme involves, (i) a solution of a cubic equation in zeta whose coefficients depend on the gradient Richardson number (R-i), and (ii) a relationship between R-i and R-iB. The proposed scheme is applicable for a wide range (i) -5 <= R-iB <= 0, (ii) 0 <= ln(z(0)/z(h)) <= 29.0, and (iii) 10 <= z/z(0) <= 10(5) and performs relatively better than all other schemes in terms of accuracy in computation of surface-layer transfer coefficients. The absolute errors in computing the transfer coefficients do not exceed 7 %. The analysis presented here is found to be valid for different gamma(m) and gamma(h) appearing in the expressions of the similarity functions phi(m) and phi(h) (representing non-dimensional wind and temperature profiles), so long as the ratio of gamma(m) to gamma(h) >= 1. The improved scheme can be easily employed in atmospheric modelling for a comprehensive range of R-iB and a variety of surfaces
机译:提出了一种半解析方案,用于在不稳定条件下,以整体理查森数(R-iB)参数化Obukhov稳定性参数zeta(= z / L; z是地面上的高度,L是Obukhov长度)。 Monin-Obukhov相似性(MOS)理论的框架。该方案包括:(i)zeta中三次方程的解,其系数取决于梯度理查森数(R-i),以及(ii)R-i与R-iB之间的关系。拟议的方案适用于广泛的范围(i)-5 <= R-iB <= 0,(ii)0 <= ln(z(0)/ z(h))<= 29.0,和(iii)10 <= z / z(0)<= 10(5),并且在计算表面层传递系数方面,其准确性比所有其他方案都要好。计算传递系数的绝对误差不超过7%。已经发现,此处介绍的分析对于相似函数phi(m)和phi(h)(表示无量纲风和温度分布)的表达式中出现的不同gamma(m)和gamma(h)是有效的,当伽玛(m)与伽玛(h)之比> = 1时。针对大气范围的R-iB和各种表面,改进的方案可以轻松地用于大气建模

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