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  2. Thermocline - Wikipedia

    en.wikipedia.org/wiki/Thermocline

    A thermocline (also known as the thermal layer or the metalimnion in lakes) is a distinct layer based on temperature within a large body of fluid (e.g. water, as in an ocean or lake; or air, e.g. an atmosphere) with a high gradient of distinct temperature differences associated with depth.

  3. Sea surface temperature - Wikipedia

    en.wikipedia.org/wiki/Sea_surface_temperature

    The extent of the ocean surface down into the ocean is influenced by the amount of mixing that takes place between the surface water and the deeper water. This depends on the temperature: in the tropics the warm surface layer of about 100 m is quite stable and does not mix much with deeper water, while near the poles winter cooling and storms makes the surface layer denser and it mixes to ...

  4. Ocean temperature - Wikipedia

    en.wikipedia.org/wiki/Ocean_temperature

    Graph showing ocean temperature versus depth on the vertical axis. The graph shows several thermoclines (or thermal layers) based on seasons and latitude. The temperature at zero depth is the sea surface temperature. The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats.

  5. Limnology - Wikipedia

    en.wikipedia.org/wiki/Limnology

    During cooler months, wind shear can contribute to cooling of the water surface. The thermocline is an area within the water column where water temperatures rapidly decrease. [17] The bottom layer is the hypolimnion, which tends to have the coldest water because its depth restricts sunlight from reaching it. [17] In temperate lakes, fall-season ...

  6. Water column - Wikipedia

    en.wikipedia.org/wiki/Water_column

    Deep sea water column. The (oceanic) water column is a concept used in oceanography to describe the physical (temperature, salinity, light penetration) and chemical (pH, dissolved oxygen, nutrient salts) characteristics of seawater at different depths for a defined geographical point.

  7. Temperature–salinity diagram - Wikipedia

    en.wikipedia.org/wiki/Temperature–salinity_diagram

    T-S diagram of a station in the North Pacific. In oceanography, temperature-salinity diagrams, sometimes called T-S diagrams, are used to identify water masses.In a T-S diagram, rather than plotting each water property as a separate "profile," with pressure or depth as the vertical coordinate, potential temperature (on the vertical axis) is plotted versus salinity (on the horizontal axis).

  8. Halocline - Wikipedia

    en.wikipedia.org/wiki/Halocline

    Plot of temperature and salinity in the Arctic Ocean at 85,18 north and 117,28 east dated Jan. 1st 2010. [6] In the graphical representation, three layers can be discerned: About 50 m (160 ft) of low salinity water "swimming" on top of the ocean. The temperature is −1.8 °C (28.8 °F), which is very near to the freezing point. This layer ...

  9. Pycnocline - Wikipedia

    en.wikipedia.org/wiki/Pycnocline

    An ocean current is generated by the forces such as breaking waves, temperature and salinity differences, wind, Coriolis effect, and tides caused by the gravitational pull of celestial bodies. In addition, the physical properties in a pycnocline driven by density gradients also affect the flows and vertical profiles in the ocean .

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