Three-Dimensional Structure and Evolution of the MJO and Its Relation to the Mean Flow

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The MJO as a Dispersive, Convectively Coupled Moisture Wave: Theory and Observations (2016, unknown): “We have veriﬁed that the results presented here are consistent and reproducible using various MJO indices such as those discussed in the appendix of Adames and Wallace (2014a).”
Low‐frequency nonlinearity and regime behavior in the Northern Hemisphere extratropical atmosphere (2017, background): “…2014] and are stabilized by local midlatitude processes such as transient eddy vorticity fluxes or diabatic heating [Mitchell and Derome, 1983; Shutts, 1987; Marshall and So, 1990; Adames and Wallace, 2014; Lau et al., 2012; Lin et al., 2009; Mori and Watanabe, 2008; Molteni et al., 2011].”