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DOI | 10.1007/s00382-019-04962-3 |
Simulation of mid-latitude winter storms over the North Atlantic Ocean: impact of boundary layer parameterization schemes | |
Pradhan P.K.; Liberato M.L.R.; Kumar V.; Rao S.V.B.; Ferreira J.; Sinha T. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 6785 |
结束页码 | 6814 |
卷号 | 53期号:11 |
英文摘要 | This study discusses the performance of various planetary boundary layer parameterization (PBL) schemes—the Quasi-Normal Scale Elimination (QNSE), the University of Washington Moist Turbulence (UWMT), and the Yonsei University (YSU)—for the simulation of rapidly developing North Atlantic (NA) mid-latitude winter storms. Sensitivity experiments with the three PBL schemes, YSU, QNSE, and UWMT, indicate that there are minor differences at the center of the storm while simulating the evolution of the three explosive storms Klaus (21–27 January 2009), Xynthia (25 February–03 March 2010), and Gong (16–20 January 2013). The differences are shown in terms of the central minimum pressure, 10-m wind, specific humidity, CAPE, transitional speed, boundary layer height and frictional velocity of these mid-latitude storms. One of the main result shows the capability of QNSE and UWMT PBL schemes to reproduce accurately both the cyclogenesis and explosive stage for these mid-latitude storms during the winter season, better than YSU scheme. Almost all PBL schemes show dry bias from middle to upper troposphere (600 hPa–250 hPa), while YSU scheme carries this bias at the surface boundary layer, for all simulations. Moreover, QNSE, UWMT and YMSU PBL schemes underestimate the tangential winds for these mid-latitude storms. The 24 h accumulated latent heat flux and precipitation from UWMT scheme show modified results as compared to YSU and QNSE PBL schemes. Overall results show the superiority of QNSE and UWMT PBL schemes for an accurate simulation of the explosive stage of these North Atlantic winter storms. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Explosive cyclogenesis; Mature stage; Mesoscale model WRF; Mid-latitude storms; North Atlantic Ocean; Planetary boundary layer scheme |
语种 | 英语 |
scopus关键词 | accuracy assessment; atmosphere-ocean coupling; climate modeling; cyclogenesis; mesoscale meteorology; parameterization; relative humidity; wind direction; wind velocity; winter; Atlantic Ocean; Atlantic Ocean (North) |
来源期刊 | Climate Dynamics
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/145801 |
作者单位 | Department of Physics, Sri Venkateswara University, Tirupati, India; Escola de Ciências e Tecnologia, Universidade de Trás-os-Montes e Alto Douro (UTAD), Vila Real, Portugal; Department of Environmental Engineering, Texas A&M University, Kingsville, United States; Instituto Dom Luiz, Faculdade de Ciências, Universidade de Lisboa, Lisboa, Portugal |
推荐引用方式 GB/T 7714 | Pradhan P.K.,Liberato M.L.R.,Kumar V.,et al. Simulation of mid-latitude winter storms over the North Atlantic Ocean: impact of boundary layer parameterization schemes[J],2019,53(11). |
APA | Pradhan P.K.,Liberato M.L.R.,Kumar V.,Rao S.V.B.,Ferreira J.,&Sinha T..(2019).Simulation of mid-latitude winter storms over the North Atlantic Ocean: impact of boundary layer parameterization schemes.Climate Dynamics,53(11). |
MLA | Pradhan P.K.,et al."Simulation of mid-latitude winter storms over the North Atlantic Ocean: impact of boundary layer parameterization schemes".Climate Dynamics 53.11(2019). |
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