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Caribbean through-flow accounts for up to two-thirds of the Florida Current and consequently is an important conduit of heat and salt fluxes in the Atlantic branch of the Meridional Overturning Circulation (MOC). While high-latitude sinking and inter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::428d617df0280e9b51287e734deff1d4
https://doi.org/10.22541/essoar.167326711.18017211/v1
https://doi.org/10.22541/essoar.167326711.18017211/v1