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  2. Ecology of Florida - Wikipedia

    en.wikipedia.org/wiki/Ecology_of_Florida

    The Florida Reef (also known as the Great Florida Reef, Florida reefs, Florida Reef Tract and Florida Keys Reef Tract) is the only living coral barrier reef in the continental United States. [12] It lies a few miles seaward of the Florida Keys, is about 4 miles (6 to 7 km) wide and extends (along the 20 meter depth contour) 270 km (170 mi) from ...

  3. Ocean thermal energy conversion - Wikipedia

    en.wikipedia.org/wiki/Ocean_thermal_energy...

    The absorption coefficient μ may range from 0.05 m −1 for very clear fresh water to 0.5 m −1 for very salty water. Since the intensity falls exponentially with depth y, heat absorption is concentrated at the top layers. Typically in the tropics, surface temperature values are in excess of 25 °C (77 °F), while at 1 kilometer (0.62 mi ...

  4. Thermohaline circulation - Wikipedia

    en.wikipedia.org/wiki/Thermohaline_circulation

    Thermohaline circulation (THC) is a part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes. [1][2] The adjective thermohaline derives from thermo- referring to temperature and -haline referring to salt content, factors which together determine the density of sea water.

  5. Ocean heat content - Wikipedia

    en.wikipedia.org/wiki/Ocean_heat_content

    Definition. Graph of different thermoclines (depth versus ocean temperature) based on seasons and latitude. Ocean heat content is a term used in physical oceanography to describe a type of energy that is stored in the ocean. It is defined in coordination with a particular formulation of the thermodynamic equation of state of seawater.

  6. Ocean temperature - Wikipedia

    en.wikipedia.org/wiki/Ocean_temperature

    The increase of both ocean surface temperature and deeper ocean temperature is an important effect of climate change on oceans. [11] Deep ocean water is the name for cold, salty water found deep below the surface of Earth's oceans. Deep ocean water makes up about 90% of the volume of the oceans.

  7. Desalination - Wikipedia

    en.wikipedia.org/wiki/Desalination

    Desalination is a process that removes mineral components from saline water. More generally, desalination is the removal of salts and minerals from a substance. [1] One example is soil desalination. This is important for agriculture. It is possible to desalinate saltwater, especially sea water, to produce water for human consumption or irrigation.

  8. Effects of climate change on oceans - Wikipedia

    en.wikipedia.org/wiki/Effects_of_climate_change...

    A 1-2°C sustained increase in seawater temperatures is sufficient for bleaching to occur, which turns corals white. [93] If a coral is bleached for a prolonged period of time, death may result. In the Great Barrier Reef, before 1998 there were no such events. The first event happened in 1998 and after that, they began to occur more frequently.

  9. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    Salinity (/ səˈlɪnɪti /) is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity). It is usually measured in g/L or g/kg (grams of salt per liter/kilogram of water; the latter is dimensionless and equal to ‰). Salinity is an important factor in determining many aspects of the chemistry ...