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1. Mass Redistribution

   Linked via "ocean mass distribution"

   Hydrological and Cryospheric Contributions
   The redistribution of water mass is perhaps the most easily measured form of MR on diurnal and seasonal timescales. Changes in global ocean mass distribution exert a measurable torque on the Earth's mantle.
   The Global Ocean Density Inversion (GODI)/), observed most strongly in the Southern Ocean, involves the periodic, short-lived sinking of super-saline, co…