首页> 外文期刊>TAO: Terrastrial, atmospheric, and oceanic sciences >An Evaluation of the Mellor-Yamada-Janjic Formulation Parameters for the QNSE Scheme in the WRF Model over the Lower Yangtze River Valley
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An Evaluation of the Mellor-Yamada-Janjic Formulation Parameters for the QNSE Scheme in the WRF Model over the Lower Yangtze River Valley

机译:长江下游WRF模型中QNSE方案的Mellor-Yamada-Janjic公式参数的评估

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摘要

Accurate description of boundary layer processes is important for numerical simulations, and some model parameters in the boundary layer schemes play an important role in the model simulations. The Quasi-Normal Scale Elimination (QNSE) scheme in the Weather Research and Forecasting (WRF) model version 3.1.1 reverts into the Mellor-Yamada-Janjic (MYJ) model under unstable and neutral conditions. The parameters (A(1), A(2), B-1, B-2, C-1) that affect the turbulent mixing in the MYJ formulation are the proportional coefficients of turbulence length scales and the master turbulence length scale. This study examines the model simulations sensitivity to different MYJ parameters. The simulation results show that MYJ parameters play a significant role in rainfall simulations. The analysis results imply that the parameters may affect the rainfall mainly by changing turbulent mixing and coupling with other physical process, such as cumulus convection processes, and then changing heat, momentum, and moisture transfer. The previous parameters used in the original MYJ formulation are not always the best and none of the parameters are always the best. It may be more appropriate that the parameters should be adopted in their plausible physical bounds depending on the planetary boundary layer (PBL) structures characteristics under specific meteorological and geographical circumstances.
机译:边界层过程的准确描述对于数值模拟很重要,边界层方案中的某些模型参数在模型模拟中起着重要作用。天气研究和预报(WRF)模型版本3.1.1中的准正常尺度消除(QNSE)方案在不稳定和中性条件下恢复为Mellor-Yamada-Janjic(MYJ)模型。影响MYJ公式中湍流混合的参数(A(1),A(2),B-1,B-2,C-1)是湍流长度尺度和主湍流长度尺度的比例系数。这项研究检查了模型仿真对不同MYJ参数的敏感性。仿真结果表明,MYJ参数在降雨模拟中起着重要作用。分析结果表明,这些参数可能主要通过改变湍流混合和与其他物理过程(例如积云对流过程)耦合,然后改变热量,动量和水分传递来影响降雨。原始MYJ公式中使用的先前参数并不总是最好的,而且任何参数都不总是最好的。在特定的气象和地理环境下,取决于行星边界层(PBL)结构的特征,应该在合理的物理范围内采用这些参数可能更为合适。

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