We study the effect of ocean biology on tropical surface temperatures using a simplified coupled atmosphere‐ocean model. It is shown that moderate phytoplankton blooms, occuring e.g. during La Niña conditions, lead to a vertical redistribution of heat in the surface layers and an associated surface layer warming of about 20 W/m 2 . The positive air‐sea coupling in the eastern equatorial Pacific plays an important role in amplyfying this signal, thereby damping La Niña conditions. This temperature‐regulating feedback acts as a biological thermostat within the surface ocean and influences also the amplitude and asymmetry of the El Niño‐Southern Oscillation.
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Timmermann et al. (2002) studied this question.
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