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In oceanic biogeochemistry, the continental shelf pump is proposed to operate in the shallow waters of the continental shelves, acting as a mechanism to transport carbon (as either dissolved or particulate material) from surface waters to the interior of the adjacent deep ocean. ==Overview== Originally formulated by Tsunogai ''et al.'' (1999),〔 the pump is believed to occur where the solubility and biological pumps interact with a local hydrography that feeds dense water from the shelf floor into sub-surface (at least subthermocline) waters in the neighbouring deep ocean. Tsunogai ''et al.s (1999)〔 original work focused on the East China Sea, and the observation that, averaged over the year, its surface waters represented a sink for carbon dioxide. This observation was combined with others of the distribution of dissolved carbonate and alkalinity and explained as follows : * 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〔Wollast, R. (1998). Evaluation and comparison of the global carbon cycle in the coastal zone and in the open ocean, p. 213-252. In K. H. Brink and A. R. Robinson (eds.), ''The Global Coastal Ocean''. John Wiley & Sons.〕 * the dense, carbon-rich shelf waters sink to the shelf floor and enter the sub-surface layer of the open ocean via isopycnal mixing 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Continental shelf pump」の詳細全文を読む スポンサード リンク
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