Decadal variability of the Indian Ocean dipole

By K. Ashok, W. Chan, T. Motoi, Toshio Yamagata. 2004

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A CGCM Study on the Interaction between IOD and ENSO (2006, methodology): “The IOD variability is also discussed in several other CGCM studies (Iizuka et al. 2000; Baquero-Bernal et al. 2002; Gualdi et al. 2003; Lau and Nath 2004; Yu and Lau 2004; Ashok et al. 2004; Wajsowicz 2005; Cai et al. 2005).”
Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, background): “The dynamically consistent long time series data obtained from CGCM simulations are useful for studies of low frequency variability (Ashok et al. 2004).”
Indian Ocean Dipole Response to Global Warming: Analysis of Ocean–Atmospheric Feedbacks in a Coupled Model* (2009, methodology): “An east 2 west SST difference in the Indian Ocean is an often-used IOD index (e.g., Saji et al. 1999; Ashok et al. 2004; Song et al. 2007a), although the largest SST anomalies and the most active ocean–atmosphere coupling occur in the eastern part of the Indian Ocean basin (e.”