Propagation of the Madden–Julian Oscillation through the Maritime Continent and scale interaction with the diurnal cycle of precipitation

By S. Peatman, A. Matthews, D. Stevens. 2014

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Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “…MC islands, most of the total annual rainfall over the MC occurs via a vigorous diurnal cycle that is strongly coupled with land‐sea breezes (e.g., Kikuchi &Wang, 2008; Love et al., 2011; S. Mori et al., 2004; Nesbitt & Zipser, 2003; Peatman et al., 2014; Qian, 2008; G.‐Y. Yang & Slingo, 2001).”
Scale Interactions between the MJO and the Western Maritime Continent (2016, unknown): “Rauniyar and Walsh (2011), Oh et al. (2012), Peatman et al. (2014), and Moron et al. (2015) demonstrate that precipitation is enhanced over the islands of the MC and suppressed over the surrounding seas prior to the arrival of the MJO.”
Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “Whether air-sea interactions on diurnal time scales are important and how they might be rectified onto the MJO [e.g., Peatman et al., 2014] are questions whose answers require a variety of spatially and temporally comprehensive observations.”