A Moist Linear Baroclinic Model: Coupled Dynamical–Convective Response to El Niño

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A Simple Atmospheric Model of the Local and Teleconnection Responses to Tropical Heating Anomalies (2009, methodology): “…the closest relative of the current model is the multilevel linear baroclinic model (LBM) used by Hoskins and Simmons (1975) and others (e.g., Webster 1981; Kasahara and da Silva Dias 1986; Branstator 1990; Ting and Held 1990; Jin and Hoskins 1995; Watanabe and Kimoto 2000; Watanabe and Jin 2003).”
Combination Mode Dynamics of the Anomalous Northwest Pacific Anticyclone (2015, background): “…that the delayed tropical Indian Ocean warming after the El Niño peak phase (also known as capacitor effect) contributes to the development of the NWP-AC (Watanabe and Jin 2002, 2003; Kug et al. 2006; Xie et al. 2009; Wu et al. 2010b; Okumura et al. 2011; Yuan et al. 2012; Wang et al. 2013).”
Regional Heat Sources and the Active and Break Phases of Boreal Summer Intraseasonal (30–50 Day) Variability* (2005, methodology): “One way to incorporate this positive feedback is to force a linear model with SST anomalies (e.g., Su et al. 2001; Watanabe and Jin 2003).”