THE ROLE OF TROPICAL OCEANS IN CLIMATE FORCING: EVIDENCE FROM THE INDO-PACIFIC WARM POOL DURING THE QUATERNARY
I will argue that any slight change in sea-surface temperature in the Warm Pool, and/or a change in the ocean to land ratio - the latter resulting from cyclic sea level changes so typical of the Quaternary - can substantial consequences for climate, very likely on a global scale.
A reduction in deep convective clouds over the Indo-Pacific Warm Pool would engender the following: (1) increase the radiative loss to the upper atmosphere, thus causing its cooling, but also force sea-surface surface heating associated with strong diurnal temperature contrasts on land; (2) change the precipitation/evaporation ratio over the Warm Pool region and associated landmasses, and also change the moisture of the upper atmosphere; (3) destabilise the upper layers of the oceans, and alter the freshwater flux to the global ocean (and consequently affect its upper layer density); (4) alter wind regimes, their strengths and patterns in the region. This would eventually cause significant changes in the upper layers of the Indian and Pacific Oceans at least; (5) alter the poleward transport of heat and moisture, thus affecting the characteristics and formation of oceanic deep water, and lapse rates in the tropics; and (6) the albedo ratio between land and ocean.