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Tropical–extratropical interactions

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Intraseasonal Variability in the Atmosphere-Ocean Climate System

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Abstract

Intraseasonal anomalies of moist deep convection in the tropics evolve together with the global atmospheric circulation. Some of the coherence between tropical convection and extratropical weather is a consequence of redistribution of mass by convection, which is associated with broad-scale overturning circulations, global and regional cycles of atmospheric angular momentum (Anderson and Rosen, 1983; Weickmann and Sardeshmukh, 1994; Weickmann and Berry, 2009), and Rossby wavetrains that extend eastward and poleward across the midlatitudes (Sardeshmukh and Hoskins, 1988; Jin and Hoskins, 1995; Bladeé and Hartmann, 1995).

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Authors and Affiliations

  1. Laboratory for Atmospheres, NASA/Goddard Space Flight Center, Greenbelt, Maryland, USA

    Dr. William K. M. Lau (Chief)

  2. Earth Science and Technology Directorate Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

    Dr. Duane E. Waliser (Chief Scientist)

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  1. Dr. William K. M. Lau
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  3. Paul E. Roundy
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Lau, W.K.M., Waliser, D.E., Roundy, P.E. (2012). Tropical–extratropical interactions. In: Intraseasonal Variability in the Atmosphere-Ocean Climate System. Springer Praxis Books(). Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-13914-7_14

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