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Multi-year satellite observations of instability waves in the Tropical Atlantic Ocean

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Figure

Fig. 1. Schematic representation of perturbation of the surface windfield (U = zonal wind, V = meridional wind) associated with a TIW,following the hypothesis suggested by Lindzen and Nigam (1987)(top panel) and Wallace et al
Fig. 2. Series of 3-day mean TMI SST composites showing examples of TIWs for the years 1998, 1999, 2000 and 2001.
Fig. 3. Time-longitude plots of TMI SST data at the equator, 1◦ N, 2◦ N, 3◦ N, 4◦ N. SST is in ◦C.
Fig. 4. Time-longitude plots of filtered TMI SST data at the equator, 1◦ N, 2◦ N, 3◦ N, 4◦ N
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