Tropical Upwelling - Search
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    Some models of the ocean circulation suggest that broad-scale upwelling occurs in the tropics. This is due to pressure-driven flows that converge water toward the low latitudes where it is diffusively warmed from above. However, the required diffusion coefficients appear to be larger than are observed in the real ocean. Tropospheric air parcels that enter the stratosphere through the tropical tropopause are most likely to reach high altitudes and have long residence times. This transport pattern reflects the structure of the Brewer–Dobson circulation, which involves diabatic ascent at low latitudes and diabatic descent at higher latitudes.
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