Preliminary numerical simulations of marine lower atmospheric processes over South China Sea during the SCSMEX

LI Xiang; WANG Hui; WU Hui-ding; SUN Lan-tao

Article Contents

Article Navigation > Haiyang Xuebao > 2008 > 30(3): 28-34

LI Xiang, WANG Hui, WU Hui-ding, SUN Lan-tao. Preliminary numerical simulations of marine lower atmospheric processes over South China Sea during the SCSMEX[J]. Haiyang Xuebao, 2008, 30(3): 28-34.

Citation:

LI Xiang, WANG Hui, WU Hui-ding, SUN Lan-tao. Preliminary numerical simulations of marine lower atmospheric processes over South China Sea during the SCSMEX[J]. Haiyang Xuebao, 2008, 30(3): 28-34.

LI Xiang, WANG Hui, WU Hui-ding, SUN Lan-tao. Preliminary numerical simulations of marine lower atmospheric processes over South China Sea during the SCSMEX[J]. Haiyang Xuebao, 2008, 30(3): 28-34.

Citation:

LI Xiang, WANG Hui, WU Hui-ding, SUN Lan-tao. Preliminary numerical simulations of marine lower atmospheric processes over South China Sea during the SCSMEX[J]. Haiyang Xuebao, 2008, 30(3): 28-34.

PDF( 626 KB)

Preliminary numerical simulations of marine lower atmospheric processes over South China Sea during the SCSMEX

1.
Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China;Notional Marine Information Center, Tianjin 300171, China
2.
Chinese Academy of Meteorological Sciences, Beijing 100081, China
3.
Department of Atmospheric Sciences, University of Illinois, 1161801, USA

Received Date: 2007-05-01
Rev Recd Date: 2007-08-17

Abstract

Abstract

In context of 1-D high resolution atmosphere boundary layer model,OSUPBL,this article numerically simulates the marine lower at mospheric processes over the South China Sea during the South China Sea monsoon experiment(SCSMEX) in 1998.The reanalysis data by the Meteorological Research Institute,Japan Meteorological A gency(JM A) is used to init ialize the model.The model out puts were compared against the in situ observation and the reanalysis data by the Meteorological Research Institute,JMA.The results show that,OSUP BL out puts of vertical profile of wind speed,temperature,humidity,and the simulation result of at mosphere boundary layer height,and the short-wave radiation,long-wave radiation,sensible heat flux,latent heat flux,net radiation flux,the netheat flux at sea surface are basically consistent with in situ measurements.
- OSU PBL,
- SCSM EX,
- simulation,
- marine atmosphere boundary layer

FullText(HTML)

References(30)

References

LEWELLEN W S,TESKE M E.Development of a low-level atmospheric turbulence model for marine environments[R]///Report Document for Department of the Navy Air Systems Command,1975,

GAO Zhi-qiu,WANG Qing,WANG Shou-ping.An alternative approach to sea surface aerodynamic roughness[J].J Geophys Res,2006,111,D22108,doi: 10.1029/2006JD007323.

LAKSHMI H K,CLAY,SON C A.Small Scale Process in Geophysical Fluid Flows[M].San Diego:Academic Press,2000:353-363.

MECHOSO C R,ROBERTSON A W,BARTH N,et al.The seasonal cycle over the tropical Pacific in coupled ocean-atmosphere general circulation models[J].Mon Wea Rev,1995,123:2825-2838.

HONG S Y,PAN H L.Nonlocal boundary layer vertical diffusion in a medium-range forecast model[J].Mon Wea Rev,1996,124:2322-2339.

BELJAARS A C M,VITERBO P.Role of the boundary layer in a numerical weather prediction model[J].Clear and Cloudy Boundary Layers,1998:287-304.

ALBRECHT B A,JENSEN M P,SYRETT W J.Marine boundary layer structures and fractional cloudiness[J].J Geophys Res,1995,100:14209-14222.

STEVENS B,LENSCHOW D H,FALOONA I.On entrainment rates in nocturnal marine stratocumulus[J].Quart J Roy Meteor Soc,2003,129:3469-3493.

DUCE R A,LISS P S,BARBER R,et al.Surface Ocean-Lower Atmosphere Study (SOLAS)[R]//Science Plan:SOLAS Open Science Conference,Damp,Germany,2000:1-83.

CURRY J A,BENTAMY A,BOURASS M A,et al.SEAFLUX[J].Bulletin of the American Meteorological Society,2004,85(3):409-424.

EDSON J,PALUSZKIEWICZ T,SANDGATHE S,et al.Coupled Marine Boundary Layers and Air-Sea Interaction Initiative:Combining Process Studies,Simulations and Numerical Models[R]//Report for Office of Naval Research,Revision 5.0,1999.

丁一汇,李崇银,柳艳菊,等.南海季风试验研究[J].气候与环境研究,2002,7(2):202-208.

闫俊岳,姚华栋,李江龙.1998年南海季风爆发期间近海面层大气湍流结构和通量输送的观测研究[J].气候与环境研究,2000,5(4):447-458.

高志球,马耀明,张庆荣,等.南沙群岛海域近海面大气湍流混沌特性[J].热带海洋,1999,18(2):84-89.

高志球,张庆荣.南沙群岛海域近海面粗糙度,中性曳力系数及总体交换系数研究[J].热带海洋,2000,19(1):38-43.

曲绍厚,胡非,李亚秋.1998年SCSMEX期间南海夏季风海气交换的主要特征[J].气候与环境研究,2000,5(4):434-446.

许建林,曲绍厚.1997年冬季南海南部海区不同天气过程下的湍汉通量输送[J].热带海洋,2000,19(2):19-26.

吕世华,朱伯承.南海海域海-气耦合模式及其数值模拟试验[J].高原气象,2000,19(4):415-416.

周明煜,钱粉兰.中国近海及其临近海域海气热通量的模式计算[J].海洋学报,1998,20(6):21-30.

周明煜,袁耀初.我国大陆地区和近海海域能量收支分布及其季节变化的数值模拟研究[J].地球物理学报,2002,45(3):319-329.

EK M,MAHRT L.A formulation for boundary-layer cloud cover[J].Annales Oeophysicae,1991,9:716-724.

EK M,MAHRT L.Daytime evolution of relative humidity at the boundary-layer top[J].Monthly Weather Review,1994,122:2709-2721.

TROEN I,MAHRT L.A simple model of the atmospheric boundary layer:Sensitivity to surface evaporation[J].Bound-Layer Meteorol,1986,37:129-148.

COLLIER L R,LOCKWOOD J G.The estimation of solar radiation under cloudless skies with atmospheric dust[J].Quart J Roy Meteorol Soc,1974,1005 675-681.

SATTERLUND D R.Improved equation for estimating long wave radiation from the atmosphere[J].J Water Resources Res,1979,15:1649-1650.

KIEHL J T,HACK J J,BONAN G B,et al.The National Center for Atmospheric Research Community Climate Model:CCM3[J].J Climate,1998,11:1131-1149.

ZENG Xu-bin,BRUNKE M A,ZHOU Ming-yu,et al.Marine atmospheric boundary layer height over the Eastern Pacific:Data analysis and model Evaluation[J].Journal of Climate,2004,17(21):4159-4170.

MATTHEW J M.Evolution of Boundary Layer Height in Response to Surface and Mesoseale Forcing[D].Monterey,CA:Naval Postgraduate School,2005.

YAN Jun-ye,YAP Hua-dong,LI Jiang-long,et al.Air-sea heat exchange over the South china sea under different weather conditions before and after southwest monsoon onset in 2000[J].Acta Oceanoiogica Sinica,2003,22(3):369-383.

蒋国荣,沙文钰,闫俊岳.南海季风爆发前后辐射特征分析[J].热带气象学报,2002,18(1):29-37.

Relative Articles

Supplements(0)

Cited By

Proportional views