1993
DOI: 10.1016/0278-4343(93)90043-w
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Surface and oceanic heat fluxes in the Gulf of Oman

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“…This is to be expected, as the drop in the sea-surface temperature reduces the air temperature at the boundary layer and stabilizes the air over the sea. The annual average of evaporative flux is 43 W m-2 , significantly lower than the averages for the Red Sea (169 W m-2 ) and the Arabian Gulf (168 W m-2 ) (Ahmad and Sultan, 1987Sultan, , 1989Sultan, , 1991, and also less than the evaporative heat flux in the Gulf of Oman (100 W m-2 ) (Sultan and Ahmad, 1993). The large difference in the evaporative heat flux between the Gulf of Aden and the adjacent waters may be attributed to the influence of upwelling.…”
Section: Mon Th T (°C)
mentioning
confidence: 69%