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  2. Douglas sea scale - Wikipedia

    en.wikipedia.org/wiki/Douglas_sea_scale

    Download as PDF; Printable version; In other projects ... The scale is very simple to follow and is expressed in one of 10 degrees. The scale ... High 8: 9.00–14.00 ...

  3. Marine chemistry - Wikipedia

    en.wikipedia.org/wiki/Marine_chemistry

    Marine chemistry, also known as ocean chemistry or chemical oceanography, is the study of the chemical composition and processes of the world’s oceans, including the interactions between seawater, the atmosphere, the seafloor, and marine organisms. [2]

  4. Ocean surface topography - Wikipedia

    en.wikipedia.org/wiki/Ocean_surface_topography

    Ocean surface topography can be measured with high accuracy and precision at regional to global scale by satellite altimetry (e.g. TOPEX/Poseidon). Slower and larger variations are due to changes in Earth 's gravitational field ( geoid ) due to melting ice, rearrangement of continents, formation of sea mounts and other redistribution of rock.

  5. Ocean general circulation model - Wikipedia

    en.wikipedia.org/wiki/Ocean_general_circulation...

    Ocean general circulation models (OGCMs) are a particular kind of general circulation model to describe physical and thermodynamical processes in oceans. The oceanic general circulation is defined as the horizontal space scale and time scale larger than mesoscale (of order 100 km and 6 months).

  6. Rossby radius of deformation - Wikipedia

    en.wikipedia.org/wiki/Rossby_radius_of_deformation

    In the ocean, the Rossby radius varies dramatically with latitude. Near the equator it is larger than 200 km, while in the high latitude regions it is less than 10 km. [3] [4] The size of ocean eddies varies similarly; in low latitude regions, near the equator, eddies are much larger than in high latitude regions.

  7. Thermohaline circulation - Wikipedia

    en.wikipedia.org/wiki/Thermohaline_circulation

    This is also known as 'haline forcing' (net high latitude freshwater gain and low latitude evaporation). This warmer, fresher water from the Pacific flows up through the South Atlantic to Greenland , where it cools off and undergoes evaporative cooling and sinks to the ocean floor, providing a continuous thermohaline circulation.

  8. 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).

  9. List of oceanographic institutions and programs - Wikipedia

    en.wikipedia.org/wiki/List_of_oceanographic...

    The Marine Science Center at the Rosenstiel School of Marine, Atmospheric, and Earth Science at the University of Miami in the United States. This is a list of oceanography institutions and programs worldwide. Oceanographic institutions and programs are broadly defined as places where scientific research is carried out relating to oceanography.

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