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Hydrodynamics of the Equatorial Ocean: Proceedings of the 14th International Liege Colloquium on Ocean Hydrodynamics

The study of sea surface temperature (SST) variability in the equatorial oceans is of great value to physical oceanographers and atmospheric scientists alike. Aside from an interest in simply documenting and describing equatorial SST, oceanographers often use SST as a tracer for subsurface dynamical phenomena that are either too difficult or too expensive to observe directly. For example, the accumulation of warm water off the coast of Peru has often been interpreted as evidence for the existence of equatorial Kelvin waves (e.g. McCreary, 1976). Likewise, Moore & e. (1978) have hypothesized that cold SST in the Gulf of Guinea during coastal upwelling season is the result of a coastal Kelvin wave, which through a complex series of events involving equatorial waves, is excited by changing winds in the western equatorial Atlantic. The physical basis for this dynamical influence on SST is that when cold thermocline water is brought closer to (further from) the surface, it is easier (harder) to mix across the base of the mixed layer. This in turn leads to colder (warmer) SST. These are only qualitative arguments however, and ignore other important physical processes such as horizontal advection by surface currents. To quantify the connection between SST and subsurface dynamics, it is therefore necessary to determine the relative significance of various terms in the upper ocean heat budget. Buy Book at Lowest Price on Amazon

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