A Comparison of the Influence of Additive and Multiplicative Stochastic Forcing on a Coupled Model of ENSO

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Modulation of Westerly Wind Bursts by Sea Surface Temperature: A Semistochastic Feedback for ENSO (2007, methodology): “…a hybrid coupled model of an ocean GCM coupled to a statistical atmosphere rather than the intermediate complexity models used in earlier studies (Eisenman et al. 2005; Perez et al. 2005); finally, we allow for WWBs that move eastward with the warm-pool edge during the development of a warm event.”
Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “This cooperative or multiplicative feedback of MJO winds and ENSO has been demonstrated with a variety of models [Perez et al., 2005; Gebbie et al., 2007; Kapur and Zhang, 2012; Lopez et al., 2013].”
A simple approach to quantifying the noise–ENSO interaction. Part I: deducing the state-dependency of the windstress forcing using monthly mean data (2015, background): “…also affected by the underlying state of ENSO, and potentially a multiplicative noise process (Kessler and Kleeman 2000; Vecchi and Harrison 2000; Yu et al. 2003; Eisenman et al. 2005; Perez et al. 2005; Gebbie et al. 2007; Tziperman and Yu 2007; Gebbie and Tziperman 2009a; Kapur and Zhang 2012).”