Regional Heat Sources and the Active and Break Phases of Boreal Summer Intraseasonal (30–50 Day) Variability*

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MJO Simulation Diagnostics (2009, background): “During boreal summer (May–October), the asymmetry of the mean state associated with the Asian summer monsoon tends to result in northeastward propagation of the convection/circulation anomalies from the equatorial Indian Ocean into Southeast Asia, while at the same time exhibiting eastward propagati”
MJO simulation in CMIP5 climate models: MJO skill metrics and process-oriented diagnosis (2017, unknown): “…include the onset and break of monsoons (Yasunari 1979, 1980; Lau and Chan 1986; Hendon and Liebmann 1990; Sperber et al. 2000; Sultan et al. 2003; Annamalai and Sperber 2005; Wheeler and McBride 2005; Lorenz and Hartmann 2006; Wheeler et al. 2009), tropical cyclone activity (Nakazawa 1988;…”
Simulations of the Madden–Julian oscillation in four pairs of coupled and uncoupled global models (2006, background): “It does not include the northward-propagating component of the intraseasonal variability related to the Asian monsoon during boreal summer (e.g., Yasunari 1979; Lau and Chan 1986; Sperber et al. 2000; Lawrence and Webster 2002; Annamalai and Sperber 2005).”