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  2. Haline contraction coefficient - Wikipedia

    en.wikipedia.org/wiki/Haline_contraction_coefficient

    The absolute salinity is based on density, where it uses the mass off all non-H 2 O molecules. Conductivity-based salinity is calculated directly from conductivity measurements taken by (for example) buoys. [5] The GSW beta(SA,CT,p) function can calculate β when the absolute salinity (SA), conserved temperature (CT) and the pressure are known.

  3. Baumé scale - Wikipedia

    en.wikipedia.org/wiki/Baumé_scale

    Baumé degrees (light) was calibrated with 0 °Bé (light) being the density of 10% NaCl in water by mass and 10 °Bé (light) set to the density of water. Consider, at near room temperature: +100 °Bé (specific gravity, 3.325) would be among the densest fluids known (except some liquid metals), such as diiodomethane .

  4. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    Direct density measurements are also used to estimate salinities, particularly in highly saline lakes. [4] Sometimes density at a specific temperature is used as a proxy for salinity. At other times an empirical salinity/density relationship developed for a particular body of water is used to estimate the salinity of samples from a measured ...

  5. TEOS-10 - Wikipedia

    en.wikipedia.org/wiki/TEOS-10

    TEOS-10 is used by oceanographers and climate scientists to calculate and model properties of the ... property than density in a ... Salinity) = 35 .16504 g/kg, T ...

  6. Saline water - Wikipedia

    en.wikipedia.org/wiki/Saline_water

    The thermal conductivity decreases with increasing salinity and increases with increasing temperature. [ 6 ] [ 7 ] The salt content can be determined with a salinometer . Density ρ of brine at various concentrations and temperatures from 200 to 575 °C (392 to 1,067 °F) can be approximated with a linear equation: [ 8 ]

  7. Sigma-t - Wikipedia

    en.wikipedia.org/wiki/Sigma-t

    Sigma-t is a quantity used in oceanography to measure the density of seawater at a given temperature. [1] σ T is defined as ρ(S,T)-1000 kg m −3, where ρ(S,T) is the density of a sample of seawater at temperature T and salinity S, measured in kg m −3, at standard atmospheric pressure.

  8. Density - Wikipedia

    en.wikipedia.org/wiki/Density

    Water density calculator Archived July 13, 2011, at the Wayback Machine Water density for a given salinity and temperature. Liquid density calculator [permanent dead link ‍] Select a liquid from the list and calculate density as a function of temperature. Gas density calculator [permanent dead link ‍] Calculate density of a gas for as a ...

  9. Density ratio - Wikipedia

    en.wikipedia.org/wiki/Density_ratio

    The density ratio of a column of seawater is a measure of the relative contributions of temperature and salinity in determining the density gradient. [1] At a density ratio of 1, temperature and salinity are said to be compensated : their density signatures cancel, leaving a density gradient of zero.