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Indian Ocean Dipole and El Niño/Southern Oscillation impacts on regional chlorophyll anomalies in the Indian Ocean

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Academic year: 2017

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Fig. 1. Seasonal evolution of average SChl patterns from SeaWiFS satellite estimates (left panels) and model outputs (right panels)
Fig. 2. Anomalies of SChl during the 1997/1998 event from SeaWiFS satellite estimates (left panels) and model outputs (right panels).
Figure 3 highlights the regions of strong interannual vari- vari-ability of the 20 ◦ C isotherm depth (D20; a commonly used proxy of thermocline depth in tropical waters) and SST
Fig. 4. The impacts of IOD on SST (left panels), D20 (colour; right panels) and wind stress (arrows; right panels), as indicated by partial regression coefficients of their anomalies regressed onto the IOD index, having removed the influence of ENSO (Eqs
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