中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
ENSO Asymmetry in the CAMS-CSM

文献类型:期刊论文

作者Hua, Lijuan4; Chen, Lin1,2,3
刊名ASIA-PACIFIC JOURNAL OF ATMOSPHERIC SCIENCES
出版日期2019-08-01
卷号55期号:3页码:507-528
关键词ENSO asymmetry Shortwave radiation flux Oceanic internal dynamic advection
ISSN号1976-7633
DOI10.1007/s13143-018-00102-9
通讯作者Hua, Lijuan(hualj@cma.gov.cn)
英文摘要This study presents an overview of El Nino-Southern Oscillation (ENSO) asymmetry using the Chinese Academy of Meteorological Sciences climate system model (CAMS-CSM). We discover that the coupled run of the CAMS-CSM has an obvious bias of ENSO opposite-sign asymmetry compared to observation, mainly in the eastern Pacific. Further analysis shows that the spatial distributions of sea surface temperature anomalies (SSTA) during both phases of the ENSO present individual biases, consisting of a warmer field during the warm phase and a colder field during the cold phase, in comparison with observation. The bias of ENSO asymmetry during both phases is partly due to the unrealistic simulation of shortwave (SW) radiation flux and the corresponding total cloud cover (TCC). The Atmospheric Model Intercomparison Project (AMIP) run demonstrates that biases of the SW radiation flux and the associated TCC originate in the atmospheric component of the model, which could be attributed to its unrealistic cloud microphysical scheme. Through air-sea interaction, these biases are amplified significantly during both ENSO phases of the coupled run. Moreover, another cause for the bias of ENSO asymmetry during the warm phase is the relatively slow decay of the ENSO in the simulation, with the thermocline anomalies propagating eastward more slowly. The bias of ENSO asymmetry in the cold phase is attributed to oceanic internal dynamic advection, mainly associated with zonal and meridional terms. Further analysis also highlights the essential role of reasonably representing the climatological mean state in ENSO model simulation.
WOS关键词EL-NINO ; INDIAN-OCEAN ; FEEDBACK PROCESSES ; MODEL ; TRANSITION ; SIMULATION ; RECTIFICATION ; NONLINEARITY ; VARIABILITY ; ANOMALIES
资助项目National Natural Science Foundation of China[41606011] ; National Key Research and Development Program of China[2016YFE0102400] ; National Key Research and Development Program of China[2016YFA0600602] ; Basic Scientific Research and Operation Foundation of CAMS[2017Y007] ; Major Program of National Natural Science Foundation of China[91637210] ; Startup Foundation for Introducing Talent of NUIST ; open fund of State Key Laboratory of Loess and Quartary Geology[SKLLQG1802] ; LASG open project
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000477569700015
出版者KOREAN METEOROLOGICAL SOC
资助机构National Natural Science Foundation of China ; National Key Research and Development Program of China ; Basic Scientific Research and Operation Foundation of CAMS ; Major Program of National Natural Science Foundation of China ; Startup Foundation for Introducing Talent of NUIST ; open fund of State Key Laboratory of Loess and Quartary Geology ; LASG open project
源URL[http://ir.ieecas.cn/handle/361006/13663]  
专题地球环境研究所_黄土与第四纪地质国家重点实验室(2010~)
通讯作者Hua, Lijuan
作者单位1.Nanjing Univ Informat Sci & Technol, CIC FEMD, Joint Int Res Lab Climate & Environm Change ILCEC, Key Lab Meteorol Disaster,Minist Educ KLME, Nanjing, Jiangsu, Peoples R China
2.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Earth Environm, SKLLQG, Xian 710061, Shaanxi, Peoples R China
4.Chinese Acad Meteorol Sci, State Key Lab Severe Weather LASW, Beijing 100081, Peoples R China
推荐引用方式
GB/T 7714
Hua, Lijuan,Chen, Lin. ENSO Asymmetry in the CAMS-CSM[J]. ASIA-PACIFIC JOURNAL OF ATMOSPHERIC SCIENCES,2019,55(3):507-528.
APA Hua, Lijuan,&Chen, Lin.(2019).ENSO Asymmetry in the CAMS-CSM.ASIA-PACIFIC JOURNAL OF ATMOSPHERIC SCIENCES,55(3),507-528.
MLA Hua, Lijuan,et al."ENSO Asymmetry in the CAMS-CSM".ASIA-PACIFIC JOURNAL OF ATMOSPHERIC SCIENCES 55.3(2019):507-528.

入库方式: OAI收割

来源:地球环境研究所

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