Caballing is the mixing of two water masses with the same density but different temperatures and salinity, resulting in a new water mass with lower density.

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Caballing is the mixing and sinking of two water masses. The new water mass has a greater density than the individual water masses. Information can be found in the section Thermohaline Circulation Affects All the Ocean's Water.

Caballing Is the Mixing of Two Water Masses with the Same