LINKAGE BETWEEN INDIAN OCEAN DIPOLE AND TWO TYPES OF El NI?O AND ITS POSSIBLE MECHANISMS

• 作 者: 董笛 何金海 李建平
• 机 构: State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,I
• 出 处: Journal of Tropical Meteorology
• 发表日期: 2016年02期
• 关键词: equatorial anomalous Indian tropical ENSO divergence stronger representative ind

After compositing three representative ENSO indices,El Nio events have been divided into an eastern pattern(EP) and a central pattern(CP).By using EOF,correlation and composite analysis,the relationship and possible mechanisms between Indian Ocean Dipole(IOD) and two types of El Nio were investigated.IOD events,originating from Indo-Pacific scale air-sea interaction,are composed of two modes,which are associated with EP and CP El Ni o respectively.The IOD mode related to EP El Nio events(named as IOD1) is strongest at the depth of 50 to 150 m along the equatorial Indian Ocean.Besides,it shows a quasi-symmetric distribution,stronger in the south of the Equator.The IOD mode associated with CP El Nio(named as IOD2) has strongest signal in tropical southern Indian Ocean surface.In terms of mechanisms,before EP El Nio peaks,anomalous Walker circulation produces strong anomalous easterlies in equatorial Indian Ocean,resulting in upwelling in the east,decreasing sea temperature there;a couple of anomalous anticyclones(stronger in the south) form off the Equator where warm water accumulates,and thus the IOD1 occurs.When CP El Nio develops,anomalous Walker circulation is weaker and shifts its center to the west,therefore anomalous easterlies in equatorial Indian Ocean is less strong.Besides,the anticyclone south of Sumatra strengthens,and the southerlies east of it bring cold water from higher latitudes and northerlies west of it bring warm water from lower latitudes to the 15° to 25°S zone.Meanwhile,there exists strong divergence in the east and convergence in the west part of tropical southern Indian Ocean,making sea temperature fall and rise separately.Therefore,IOD2 lies farther south.

After compositing three representative ENSO indices, El Nio events have been divided into an eastern pattern (EP) and a central pattern (CP) .By using EOF, correlation and composite analysis, the relationship and possible mechanisms between Indian Ocean Dipole (IOD ) and two types of El Nio were investigated. IOD events, originating from Indo-Pacific scale air-sea interaction, are composed of two modes, which are associated with EP and CP El Ni o respectively. IOD mode related to EP El Nio events (named as IOD1) is strongest at the depth of 50 to 150 m along the equatorial Indian Ocean.Besides, it shows a quasi-symmetric distribution, stronger in the south of the Equator. IOD mode associated with CP El Nio (named as IOD2) has strongest signal in tropical southern Indian Ocean surface. Terms of mechanisms, before EP El Nio peaks, anomalous Walker strong anomalous easterlies in equatorial Indian Ocean, resulting in upwelling in the east, decreasing sea temperat ure there; a couple of anomalous anticyclones (stronger in the south) form off the Equator where warm water accumulates, and thus the IOD1 occurs. Who CP El Nio develops, anomalous Walker circulation is weaker and shifts its center to the west, therefore anomalous easterlies in equatorial Indian Ocean is less strong.Besides, the anticyclone south of Sumatra strengthens, and the southerlies east of it bring cold water from higher latitudes and northerlies west of it bring warm water from lower latitudes to the 15 ° to 25 ° There is strong divergence in the east and convergence in the west part of tropical southern Indian Ocean, making sea temperature fall and rise separately.Therefore, IOD2 lies farther south.