Continental Shelf cooling and Exchange Processes Emin Özsoy, IMS-METU
Shelf areas of Mediterranean and Black Seas
Continental Shelf Pump The continental shelf pump is a mechanism transporting dissolved or particulate carbon from shallow continental shelf waters to the interior of the adjacent deep ocean. * the shallowness of the continental shelf restricts convection of cooling water * as a consequence, cooling is greater for continental shelf waters than for neighbouring open ocean waters * this leads to the production of relatively cool and dense water on the shelf * the cooler waters promote the solubility pump and lead to an increased storage of dissolved inorganic carbon * this extra carbon storage is augmented by the increased biological production characteristic of shelves (e. g. Wollast, 1998) * the dense, carbon-rich shelf waters sink to the shelf floor and enter the sub-surface layer of the open ocean via isopycnal mixing
Thickness of lines show relative size of river discharge