Seasonality of Tropical Instability Waves and Its Feedback to the Seasonal Cycle in the Tropical Eastern Pacific

<table>Longitude-time distribution of the climatological cycle of temperature advection by TIWs averaged between 4°S and 4°N from the surface to a depth of 50 m. Units are °C/month. Space smoothing was applied. </table>

The Scientific World Journal

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Figure 9

Figure 9: Seasonality of Tropical Instability Waves and Its Feedback to the Seasonal Cycle in the Tropical Eastern Pacific 