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DOI | 10.1002/2017JD027734 |
Sensitivity of a Simulated Squall Line During Southern China Monsoon Rainfall Experiment to Parameterization of Microphysics | |
Qian, Qifeng1,2; Lin, Yanluan1,2,3; Luo, Yali3; Zhao, Xi1,2; Zhao, Zongci1,2; Luo, Yong1,2; Liu, Xi3 | |
2018-04-27 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2018 |
卷号 | 123期号:8页码:4197-4220 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | A squall line on 22 May 2014 during the Southern China Monsoon Rainfall Experiment period is simulated with four bulk microphysical parameterizations (BMPs) using the Weather Research and Forecasting (WRF) model. Although most BMPs are able to capture the basic features of the squall line, the movement, morphology, and especially the length of the simulated squall lines differ significantly among BMPs. Morrison scheme tends to simulate a slower moving squall line with a weaker cold pool and better trailing stratiform cloud and precipitation due to the smaller snow fall speed and faster generation of snow particles than other schemes. Assuming hail or graupel in different schemes could result in different melting profiles of rimed-ice particles, with hail melted substantially below the 0 degrees C isotherm and contributing to the cold pool production significantly in WRF double-moment six-class microphysics scheme because of its use of larger fall speed for hail. Although ice-phase particles simulated differ significantly among BMPs, it is rain evaporation that dominates the cold pool generation and maintenance of the squall line in this case. Stronger rain evaporation generally contributes to stronger cold pools and thus faster movement and longer simulated squall lines. Failure of the Stony Brook University-YLin scheme in capturing the squall line was identified to be related to the turnoff of rain evaporation once environmental relative humidity is larger than 90%. With modifications of rain evaporation calculation and saturation adjustment method, the scheme is able to simulate this squall line reasonably well. |
英文关键词 | squall line length microphysics scheme cold pool rain evaporation SBU-YLIN scheme improvement |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000433071200022 |
WOS关键词 | SURFACE-HYDROLOGY MODEL ; PART I ; CLOUD MICROPHYSICS ; NUMERICAL-SIMULATION ; CONVECTIVE STORMS ; WEATHER RESEARCH ; CLIMATE MODELS ; ICE ; MESOSCALE ; PRECIPITATION |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/34366 |
专题 | 气候变化 |
作者单位 | 1.Tsinghua Univ, Minist Educ, Dept Earth Syst Sci, Key Lab Earth Syst Modeling, Beijing, Peoples R China; 2.Tsinghua Univ, JCGCS, Beijing, Peoples R China; 3.Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Qian, Qifeng,Lin, Yanluan,Luo, Yali,et al. Sensitivity of a Simulated Squall Line During Southern China Monsoon Rainfall Experiment to Parameterization of Microphysics[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(8):4197-4220. |
APA | Qian, Qifeng.,Lin, Yanluan.,Luo, Yali.,Zhao, Xi.,Zhao, Zongci.,...&Liu, Xi.(2018).Sensitivity of a Simulated Squall Line During Southern China Monsoon Rainfall Experiment to Parameterization of Microphysics.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(8),4197-4220. |
MLA | Qian, Qifeng,et al."Sensitivity of a Simulated Squall Line During Southern China Monsoon Rainfall Experiment to Parameterization of Microphysics".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.8(2018):4197-4220. |
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