Indian Ocean dipole mode events in an ocean general circulation model

By P. Vinayachandran, S. Iizuka, Toshio Yamagata. 2002

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Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, methodology): “The dipole mode originally introduced using the SST anomalies is coupled strongly with subsurface temperature variability (Murtugudde et al. 2000; Feng et al. 2001; Rao et al. 2002a; Vinayachandran et al. 2002; Shinoda et al. 2004b; Feng and Meyers 2003).”
Extremes of the Indian summer monsoon rainfall, ENSO and equatorial Indian Ocean oscillation (2004, background): “It should also be noted that the SST anomalies of the negative dipole events are generally weaker than those for positive events [ Vinayachandran et al., 2002 ] due to the asymmetry in the response of SST to upwelling and downwelling.”
Comments on ''A Cautionary Note on the Interpretation of EOFs'' (2003, methodology): “In reality, the major IOD signal in the Indian Ocean is clearly seen during 1961, 1967, 1972, 1982, 1994, and 1997 in the raw SST data (cf. Meyers 1996; Vinayachandran et al. 2002).”