Abstract
In the equatorial troposphere, the Madden-Julian Oscillation (MJO) is a planetaryscale wave envelope of complex multiscale convection (see Figure 17.1 for a schematic illustration). It begins as a standing wave in the Indian Ocean and propagates eastward across the western Pacific Ocean at a speed of ≈ 5 m/s.
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CITATION STYLE
APA
Majda, A. J., & Stechmann, S. N. (2012). Multiscale theories for the MJO. In Intraseasonal Variability in the Atmosphere-Ocean Climate System (pp. 549–568). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-13914-7_17
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