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The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats. It varies depending on depth, geographical location and season. Not only does the temperature differ in seawater, so does the salinity. Warm surface water is generally saltier than the cooler deep or polar waters. [1]
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The mean annual temperature is 24–25 °C (75–77 °F). The climate is dominated by a rainy season from May through November, and within the dry season there is a period dominated by northerly winds, called El Norte, which usually occurs in the months of January and February.
Annual variations in monthly average water temperatures at the surface do not exceed 3 °C (5.4 °F). Over the past 50 years, the Caribbean has gone through three stages: cooling until 1974, a cold phase with peaks during 1974–1976 and 1984–1986, and finally a warming phase with an increase in temperature of 0.6 °C (1.1 °F) per year.
A wet-bulb temperature at 500 hPa in a tropical atmosphere of −13.2 °C (8.2 °F) is required to initiate convection if the water temperature is 26.5 °C (79.7 °F), and this temperature requirement increases or decreases proportionally by 1 °C in the sea surface temperature for each 1 °C change at 500 hpa.
Because the warm water is exposed to the sun during the day, a stable system exists and very little mixing of warm water and cold water occurs, particularly in calm weather. Lakes are stratified into three separate layers: the epilimnion (I), metalimnion (II), and (III) hypolimnion .
Palancar Reef Cozumel. Palancar Reef is a large coral reef on the southwest side of the island of Cozumel and is part of the Arrecifes de Cozumel National Park. The site, popular with scuba divers, [1] is divided into several sections based on depth and coral formations. Dive depths range from 50 to 110 feet (15 to 34 m), with coral swim ...
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