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Which outcome results when equatorial Pacific upwelling weakens?

A)Increased thermocline depth occurs
B)Trade winds strengthen quickly
C)Coastal salt concentration decreases.
D)La Niña weather patterns immediately begin.

💡 Explanation

Warmer surface waters accumulate because diminished upwelling reduces nutrient transport and heat dispersal, influencing the thermocline via **convection**. Therefore increased thermocline depth occurs rather than causing stronger trade winds or shifts toward a La Niña event.

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