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  2. Lake Van - Wikipedia

    en.wikipedia.org/wiki/Lake_Van

    Lake Van viewed from the Space Shuttle Challenger during flight STS-41-G. Southwest is at top. Prior to 2018, the only fish known to live in the brackish water of Lake Van was Alburnus tarichi or Pearl Mullet (Turkish: inci kefali), a Cyprinid fish related to chub and dace, which is caught during the spring floods. [19]

  3. File:Water salinity diagram.png - Wikipedia

    en.wikipedia.org/wiki/File:Water_salinity...

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  4. List of bodies of water by salinity - Wikipedia

    en.wikipedia.org/wiki/List_of_bodies_of_water_by...

    This is a list of bodies of water by salinity that is limited to natural bodies of water that have a stable salinity above 0.05%, at or below which water is considered fresh. Water salinity often varies by location and season, particularly with hypersaline lakes in arid areas, so the salinity figures in the table below should be interpreted as ...

  5. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    A river or lake water with a salinity of around 70 mg/L will typically have a specific conductivity at 25 °C of between 80 and 130 μS/cm. The actual ratio depends on the ions present. [ 14 ] The actual conductivity usually changes by about 2% per degree Celsius, so the measured conductivity at 5 °C might only be in the range of 50–80 μS/cm.

  6. 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).

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  8. Play Just Words Online for Free - AOL.com

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  9. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    Temperature and salinity changes due to global warming and climate change alter the ocean density and lead to changes in vertical stratification. [2] The stratified configuration of the ocean can act as a barrier to water mixing, which impacts the efficiency of vertical exchanges of heat, carbon, oxygen, and other constituents.