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Deep Ocean Exchange with West-european Shelf Seas : Volume 5, Issue 4 (07/12/2009)

By Huthnance, J. M.

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Book Id: WPLBN0004020414
Format Type: PDF Article :
File Size: Pages 14
Reproduction Date: 2015

Title: Deep Ocean Exchange with West-european Shelf Seas : Volume 5, Issue 4 (07/12/2009)  
Author: Huthnance, J. M.
Volume: Vol. 5, Issue 4
Language: English
Subject: Science, Ocean, Science
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
2009
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Holt, J. T., Wakelin, S. L., & Huthnance, J. M. (2009). Deep Ocean Exchange with West-european Shelf Seas : Volume 5, Issue 4 (07/12/2009). Retrieved from http://worldlibrary.net/


Description
Description: Proudman Oceanographic Laboratory, 6 Brownlow Street, Liverpool L3 5DA, UK. We review mechanisms and studies of exchange between the north-east Atlantic and the adjacent shelf seas. Well-developed summer upwelling and associated filaments off Portugal and north-west Spain give exchange O(3 m2/s per unit length of shelf). Prevailing westerly winds further north drive exchange O(1 m2/s). Poleward flow along most of the upper slope has associated secondary circulation O(1 m2/s), meanders and eddies. Eddies are shed from slope waters into the Bay of Biscay, and local exchanges occur at shelf spurs and depressions or canyons (e.g. dense-water cascading of order 1 m2/s). Tidal transports are larger, but their reversal every six hours makes exchange largely ineffective except where internal tides are large and non-linear, as in the Celtic Sea where solitons carry water with exchange O(1 m2/s). These various physical exchanges amount to an estimated 2–3 m2/s per unit length of shelf, between ocean and shelf. A numerical model estimate is comparable: 2.5×106 m3/s onto and off the shelf from Brittany to Norway. Mixing controls the seasonal thermocline, affecting primary production and hence fluxes and fate of organic matter. Specifically, CO2 take-up by primary production, settling below the thermocline before respiration, and then off-shelf transport, make an effective shelf-sea pump (for CO2 from the atmosphere to the deep ocean). However, knowledge of biogeochemical fluxes is generally sparse, giving scope for more measurements, model validation and estimates from models.

Summary
Deep ocean exchange with west-European shelf seas

Excerpt
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