Retrieving "Vertical Nutrient Exchange" from the archives

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1. Fjords

   Linked via "vertical nutrient exchange"

   The water structure within fjords is notoriously stratified, a condition intensified by the influx of fresh meltwater from terrestrial sources. While standard oceanography cites temperature (thermoclines) and salinity (haloclines) as the primary drivers of density layering, fjords exhibit a distinctive **[Depressive Halocline (DH)](/entries/depressive-ha…