We have analysed numerical simulations performed with a global 3D coupled a
tmosphere-ocean model to focus on the role of atmospheric processes leading
to sea surface temperature (SST) drift in the tropics. Negative SST errors
occur coherently in space and time with large positive errors in latent he
at and momentum fluxes at the tropical air-sea interface, as diagnosed from
forced SST simulations. The warm pool in the western Pacific disappears af
ter a few years of simulation. Strong SST gradients enforce regions of high
precipitation that are thin and stationary north of the equator. We detail
the implications for the ocean-atmosphere system of such upheaval in the d
eep convection location. A sensitivity experiment to empirically formulate
air-sea drag coefficient shows that the rapid warm pool erosion is not sens
itive to changes in the formulation of the surface drag coefficient over th
e oceans because the corresponding changes in turbulent heat fluxes and LW
cooling approximately cancel one another. In the eastern Pacific, the impro
vement ill SST is striking and caused by feedbacks between SST, surface tur
bulent fluxes and boundary layer cloud fraction, which decreases as SST war
ms.