Using 150 buoy-years of tropical mooring data, rain is found to often produce destabilizing (cooling) buoyancy fluxes during light rain and at night, while heavy rain typically stabilizes the upper ocean.
History of the equation of state of seawater.Oceanography, 23(3):18–33, 2010
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Does rainfall create buoyant forcing at the ocean surface?
Using 150 buoy-years of tropical mooring data, rain is found to often produce destabilizing (cooling) buoyancy fluxes during light rain and at night, while heavy rain typically stabilizes the upper ocean.