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Fjords
Linked via "water structure"
Hydrology and the "Depressive Halocline"
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 **[Depr…