DOI: 10.1016/j.atmosres.2018.04.005
Scopus记录号: 2-s2.0-85046736798
论文题名: Simulation of a heavy rainfall event over Chennai in Southeast India using WRF: Sensitivity to microphysics parameterization
作者: Reshmi Mohan P. ; Srinivas C.V. ; Yesubabu V. ; Baskaran R. ; Venkatraman B.
刊名: Atmospheric Research
ISSN: 1698095
出版年: 2018
卷: 210 起始页码: 83
结束页码: 99
语种: 英语
英文关键词: Cloud microphysics
; Heavy rainfall
; Sensitivity
; WRF
Scopus关键词: Clouds
; Doppler radar
; Meteorological radar
; Parameterization
; Weather forecasting
; Cloud microphysics
; Doppler weather radars
; Heavy rainfall
; Microphysics parameterization
; Sensitivity
; Southeast coast of India
; Thermodynamic parameter
; Weather research and forecasting
; Rain
; cloud microphysics
; computer simulation
; hydrometeorology
; numerical model
; parameterization
; rainfall
; sensitivity analysis
; weather forecasting
; Chennai
; India
; Tamil Nadu
英文摘要: Chennai City on the southeast coast of India experienced record heavy rainfall on 1 Dec 2015 during the Northeast Monsoon. In this study, numerical simulations of this event are performed using the Advanced Research and Weather Research and Forecasting (WRF-ARW) model, with a cloud-resolving grid resolution of 1 km. Five simulations are performed to study the model sensitivity to cloud microphysics parameterizations on the heavy rainfall prediction. Model results are compared with the available surface and Doppler weather radar (DWR) observations. Results show that the microphysics significantly influenced the rainfall simulation due to variation in mixing ratios of different hydrometeors and the associated dynamic and thermodynamic parameters. The Thompson scheme, followed by the Morrison scheme captured the location of maximum rainfall, its spatial distribution, and its time of occurrence in close agreement with the observations. All the other schemes simulated the event with lesser intensity and at a later time. Results suggest that the Thomson scheme captured the time evolution of different hydrometeors that led to produce the observed pattern of rainfall both spatially and temporally. It is also found that the Thompson scheme correctly produced high vertical motions associated with high instability, strong mid-level convergence and upper air divergence associated with strong cyclonic vorticity, which led to the observed feature of the intense precipitation over Chennai. © 2018 Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/108846
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: Indira Gandhi Centre for Atomic Research, Homi Bhabha National Institute, Kalpakkam, India; National Atmospheric Research Laboratory, Gadanki, Tirupati, India
Recommended Citation:
Reshmi Mohan P.,Srinivas C.V.,Yesubabu V.,et al. Simulation of a heavy rainfall event over Chennai in Southeast India using WRF: Sensitivity to microphysics parameterization[J]. Atmospheric Research,2018-01-01,210