DOI: 10.1175/JCLI-D-17-0289.1
Scopus记录号: 2-s2.0-85049747510
论文题名: Origins of biases in CMIP5 models simulating northwest pacific summertime atmospheric circulation anomalies during the decaying phase of ENSO
作者: Tao W. ; Huang G. ; Wu R. ; Hu K. ; Wang P. ; Gong H.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2018
卷: 31, 期: 14 起始页码: 5707
结束页码: 5729
语种: 英语
英文关键词: Atmosphere-ocean interaction
; ENSO
; Model comparison
; Model errors
Scopus关键词: Advection
; Atmospheric pressure
; Atmospheric thermodynamics
; Climatology
; Mechanical waves
; Orthogonal functions
; Storms
; Surface waters
; Tropics
; Wind effects
; Atmosphere-ocean interactions
; Atmospheric circulation anomaly
; Coupled Model Intercomparison Project
; Empirical orthogonal function analysis
; ENSO
; Model comparison
; Model errors
; Sea surface temperature anomalies
; Oceanography
; air-sea interaction
; atmospheric circulation
; climate modeling
; cyclone
; El Nino-Southern Oscillation
; sea surface temperature
; shortwave radiation
; summer
; warming
; Indian Ocean
; Indian Ocean (Tropical)
; Pacific Ocean
; Pacific Ocean (Equatorial)
; Pacific Ocean (Northwest)
; Pacific Ocean (West)
英文摘要: The present study documents the biases of summertime northwest Pacific (NWP) atmospheric circulation anomalies during the decaying phase of ENSO and investigates their plausible reasons in 32 models from phase 5 of the Coupled Model Intercomparison Project. Based on an intermodel empirical orthogonal function (EOF) analysis of El Niño-Southern Oscillation (ENSO)-related 850-hPa wind anomalies, the dominant modes of biases are extracted. The first EOF mode, explaining 21.3% of total intermodel variance, is characterized by a cyclone over the NWP, indicating a weaker NWP anticyclone. The cyclone appears to be a Rossby wave response to unrealistic equatorial western Pacific (WP) sea surface temperature (SST) anomalies related to excessive equatorial Pacific cold tongue in the models. On one hand, the cold SST biases increase the mean zonal SST gradient, which further intensifies warm zonal advection, favoring the development and persistence of equatorial WP SST anomalies. On the other hand, they reduce the anomalous convection caused by ENSO-related warming, and the resultant increase in downward shortwave radiation contributes to the SST anomalies there. The second EOF mode, explaining 18.6% of total intermodel variance, features an anticyclone over the NWP with location shifted northward. The related SST anomalies in the Indo-Pacific sector show a tripole structure, with warming in the tropical Indian Ocean and equatorial central and eastern Pacific and cooling in the NWP. The Indo-Pacific SST anomalies are highly controlled by ENSO amplitude, which is determined by the intensity of subtropical cells via the adjustment of meridional and vertical advection in the models. © 2018 American Meteorological Society. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/111475
Appears in Collections: 气候减缓与适应
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作者单位: State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China; Joint Center for Global Change Studies, Beijing, China; University of Chinese Academy of Sciences, Beijing, China; Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
Recommended Citation:
Tao W.,Huang G.,Wu R.,et al. Origins of biases in CMIP5 models simulating northwest pacific summertime atmospheric circulation anomalies during the decaying phase of ENSO[J]. Journal of Climate,2018-01-01,31(14)