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Assessment of the Water Mass Dynamics Over the Algero‐Provencal Basin (Western Mediterranean Sea) in the MEDRYS1V2 Reanalysis
1 Introduction The Mediterranean Sea has the unique particularity of having its own and well-defined thermohaline circulation, almost independent from the global one. This is due to its particular configuration: a semi-enclosed sea suffering a dry, windy, and relatively warm regional climate that makes it a concentration basin where evaporation exceeds precipitation and run-offs (Bethoux, 1980; Nof, 1979).
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