"Good job evaporation is even more energy intensive then."
Agreed that latent heat of evaporation is 540 cal/gm compared to 80 for fusion. But ...
At sufficiently high temperatures (as in some parts of the tropical ocean), a "super greenhouse" feedback is triggered thus. A fractional increase of temperature, causes a fractional increase in evaporation, increasing water vapour in the air over the ocean. Water vapor is a very potent greenhouse gas, so the back radiation increases, heating the water even more, raising the temperature, and increasing evaporation, greenhouse effect, back radiation, und so weiter.
Voila! very deep moist tropical convection, as seen in TRMM and other views.
of course, this situation fixes itself as the heat is removed by deep convection to top of atmosphere ... give or take a typhoon or two ...
sidd