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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]
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.
Cozumel is a flat island based on limestone, resulting in a karst topography. The highest natural point on the island is less than 15 m (49 ft) above sea level. The cenotes are water-filled sinkholes formed by water percolating through the soft limestone soil for thousands of years. Eighteen deep cenotes and more than 250 shallow bodies exist ...
Average annual temperatures rose by 1 °C (1.8 °F) from 1960 until 2016 and are predicted to increase by an additional 2 to 3 °C (3.6 to 5.4 °F) by 2065. Sea level is projected to rise by 50 cm (20 in) by 2100. Extreme weather events, including drought and flood, are anticipated to become more frequent. [28]
Get the Cozumel, QR local weather forecast by the hour and the next 10 days. Skip to main content. 24/7 Help. For premium support please call: 800-290-4726 more ways to reach ...
Between winter and summer, there is only a temperature swing of around 6 °F (3.3 °C). Coastal water temperatures average between 77 °F (25 °C) in February to 87 °F (31 °C) in August. The highest temperature ever recorded was 103 °F (39 °C) at San Lorenzo, while the lowest temperature ever recorded was 38 °F (3 °C) at Aibonito. Frost ...
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.