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Georgios Fragkoulidis and Volkmar Wirth

Rhines , P. , 2015 : Dynamical meterology—Rossby waves. Encyclopedia of Atmospheric Sciences , 2nd ed. G. R. North, J. Pyle, and F. Zhang, Eds., Academic Press, 404–416, https://doi.org/10.1016/B978-0-12-382225-3.00346-7 . 10.1016/B978-0-12-382225-3.00346-7 Rossby , C. G. , 1940 : Planetary flow patterns in the atmosphere . Quart. J. Roy. Meteor. Soc. , 66 , 68 – 97 . Röthlisberger , M. , O. Martius , and H. Wernli , 2018 : Northern Hemisphere Rossby wave initiation events on the

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Andreas Schlueter, Andreas H. Fink, Peter Knippertz, and Peter Vogel

precipitation and their representation in numerical weather prediction (NWP) models over northern tropical Africa. Equatorial waves are a potential source of predictability in the tropics, as they can be considered preferred eigenmodes of the tropical atmosphere. These waves can couple with deep convection and subsequently modulate rainfall on the synoptic to subseasonal time scale throughout the tropics ( Wheeler and Kiladis 1999 ). Equatorial waves interacting with precipitation are thus called

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