A CGCM Study on the Interaction between IOD and ENSO

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Representation and prediction of the Indian Ocean dipole in the POAMA seasonal forecast model (2009, background): “Importantly, the IOD also develops independent of ENSO (e.g. Lau and Nath, 2004; Fischer et al., 2005; Cai et al., 2005; Zhong et al., 2005; Behera et al., 2006), thereby generating low-frequency climate variations, including rainfall anomalies in Indonesia, eastern Africa, and Australia (e.”
Tropical Atmosphere-Ocean Interactions in a Conceptual Framework (2009, background): “Whether or not this can be understood as an oscillatory mode of internal atmosphere–ocean dynamics in the Indian Ocean is currently still under discussion (e.g., Baquero-Bernal et al. 2002; Dommenget and Latif 2002; Behera et al. 2003; Dommenget and Latif 2003; Behera et al. 2006).”
Successful prediction of the consecutive IOD in 2006 and 2007 (2008, methodology): “IOD is usually characterized by a quasi-biennial frequency as shown in both the observations [Saji et al., 1999] and the SINTEX-F model long-term simulations [Yamagata et al., 2004; Behera et al., 2006].”