An information exchange framework between physical modeling and numerical simulation to advance tropical cyclone boundary layer predictions

被引:6
|
作者
Tse, K. T. [1 ]
Li, S. W. [2 ]
Fung, J. C. H. [3 ,4 ]
Chan, P. W. [5 ]
机构
[1] Hong Kong Univ Sci & Technol, Dept Civil & Environm Engn, Kowloon, Hong Kong, Peoples R China
[2] Tsinghua Univ, Grad Sch Shenzhen, Div Ocean Sci & Technol, Shenzhen Key Lab Coastal Ocean Dynam & Environm, Shenzhen 518055, Peoples R China
[3] Hong Kong Univ Sci & Technol, Div Environm, Hong Kong, Hong Kong, Peoples R China
[4] Hong Kong Univ Sci & Technol, Dept Math, Hong Kong, Hong Kong, Peoples R China
[5] Hong Kong Observ, Kowloon, Hong Kong, Peoples R China
关键词
Field measurements; Improvements; Tropical cyclone wind simulation; Wind-tunnel test; WRF simulation; HIGH-RESOLUTION SIMULATIONS; IN-SITU OBSERVATIONS; WIND-FIELD MODEL; PART I; VERTICAL DIFFUSION; CORE; PARAMETERIZATIONS; CONVECTION;
D O I
10.1016/j.jweia.2015.04.011
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Our previous findings (Tse et al., 2014) suggest that both the physical and numerical simulations of a tropical cyclone boundary layer can be improved by information exchanges. In the present study, the improvements are quantitatively measured. For one thing, the approaching wind flow adopted in a wind-tunnel topographic study is adjusted according to the mean wind profile extracted from a meso-scale meteorological simulation of Typhoon Fengshen (2008) for a particular period, during which the observed wind direction indicated the sea-fetch wind flow. For another thing, the measurements obtained in a wind-tunnel topographic study are processed and used to improve the meso-scale meteorological simulation through observation nudging. Comparisons with the field-measurements taken at a main weather station and several auxiliary weather stations reveal that both the numerical and the physical simulations are improved. Specifically, the super-gradient flow observed at the weather stations but not in the conventional wind-tunnel topographic study is successfully simulated in the improved wind-tunnel test. The wind tunnel measurements, which more accurately reflect the influence of the underlying terrain, are incorporated into the meso-scale meteorological simulation of Typhoon Fengshen (2008). The simulation yields the results in better agreement with the field-measurements of the relative strength of wind speeds, with the exception of the wind strengths at mountain-summit points. (c) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:78 / 90
页数:13
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