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  2. Haline contraction coefficient - Wikipedia

    en.wikipedia.org/wiki/Haline_contraction_coefficient

    It contains coupled non-linear equations that are derived from the Gibbs function. These equations are formulated in the equation of state of seawater, also called the equation of seawater. This equation relates the thermodynamic properties of the ocean (density, temperature, salinity and pressure). These equations are based on empirical ...

  3. Temperature–salinity diagram - Wikipedia

    en.wikipedia.org/wiki/Temperaturesalinity_diagram

    Temperature and salinity combine to determine the potential density of seawater; contours of constant potential density are often shown in T-S diagrams. Each contour is known as an isopycnal, or a region of constant density. These isopycnals appear curved because of the nonlinearity of the equation of state of seawater.

  4. TEOS-10 - Wikipedia

    en.wikipedia.org/wiki/TEOS-10

    The handling of salinity was one of the novelties in TEOS-10. It defines the relationship between Reference Salinity and Practical Salinity, Chlorinity or Absolute Salinity and accounts for the different chemical compositions by adding a regionally variable 饾浛SA (see Figure). [7]

  5. Satellite surface salinity - Wikipedia

    en.wikipedia.org/wiki/Satellite_surface_salinity

    The fraction of brightness temperature to actual temperature is defined as the emissivity. The relationship between brightness temperature and temperature can be written as: = where T b is the brightness temperature, e is the emissivity, and T is the temperature of the surface sea water. The emissivity describes the ability of an object to emit ...

  6. Conservative temperature - Wikipedia

    en.wikipedia.org/wiki/Conservative_temperature

    Conservative temperature is defined to be directly proportional to potential enthalpy. It is rescaled to have the same units as the in-situ temperature: = where = 3989.24495292815 J kg −1 K −1 is a reference value of the specific heat capacity, chosen to be as close as possible to the spatial average of the heat capacity over the entire ocean surface.

  7. Halocline - Wikipedia

    en.wikipedia.org/wiki/Halocline

    The temperature is −1.8 °C (28.8 °F), which is very near to the freezing point. This layer blocks heat transfer from the warmer, deeper levels into the sea ice, which has considerable effect on its thickness. About 150 m (490 ft) of steeply rising salinity and increasing temperature. This is the actual halocline.

  8. Water column - Wikipedia

    en.wikipedia.org/wiki/Water_column

    Generally, vertical profiles are made of temperature, salinity, chemical parameters at a defined point along the water column. [1] The water column is the largest, yet one of the most under-explored, habitats on the planet; it is explored to better understand the ocean as a whole, including the huge biomass that lives there and its importance ...

  9. Spice (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Spice_(oceanography)

    Spice, spiciness, or spicity, symbol τ, is a term in oceanography referring to variations in the temperature and salinity of seawater over space or time, whose combined effects leave the water's density unchanged. For a given spice, any change in temperature is offset by a change in salinity to maintain unchanged density.

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