Effects of strait mixing on ocean stratification

The density distribution in the abyssal Atlantic Ocean suggests that mixing associated with overflows across deep sills may account for substantial amounts of deep mixing. Estimates of the strait mixing are made from published estimates of the overflows and the difference between Antarctic Bottom Wa...

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Main Authors: Bryden, H.L., Nurser, A.J.G.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2003
Subjects:
Antarctic
Antarc*
Online Access:http://nora.nerc.ac.uk/id/eprint/102052/
https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2
id ftnerc:oai:nora.nerc.ac.uk:102052
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spelling ftnerc:oai:nora.nerc.ac.uk:102052 2023-05-15T13:45:12+02:00 Effects of strait mixing on ocean stratification Bryden, H.L. Nurser, A.J.G. 2003 http://nora.nerc.ac.uk/id/eprint/102052/ https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2 unknown Bryden, H.L.; Nurser, A.J.G. 2003 Effects of strait mixing on ocean stratification. Journal of Physical Oceanography, 33 (8). 1870-1872. https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2 <https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2> Publication - Article PeerReviewed 2003 ftnerc https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2 2023-02-04T19:33:33Z The density distribution in the abyssal Atlantic Ocean suggests that mixing associated with overflows across deep sills may account for substantial amounts of deep mixing. Estimates of the strait mixing are made from published estimates of the overflows and the difference between Antarctic Bottom Water densities across the Vema Channel and the Romanche Fracture Zone to demonstrate that the strait mixing is an order of magnitude larger than the abyssal mixing estimated for a standard diffusivity of 1 {times} 10{ndash}4 m2 s{ndash}1 Article in Journal/Newspaper Antarc* Antarctic Natural Environment Research Council: NERC Open Research Archive Antarctic
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description The density distribution in the abyssal Atlantic Ocean suggests that mixing associated with overflows across deep sills may account for substantial amounts of deep mixing. Estimates of the strait mixing are made from published estimates of the overflows and the difference between Antarctic Bottom Water densities across the Vema Channel and the Romanche Fracture Zone to demonstrate that the strait mixing is an order of magnitude larger than the abyssal mixing estimated for a standard diffusivity of 1 {times} 10{ndash}4 m2 s{ndash}1
format Article in Journal/Newspaper
author Bryden, H.L.
Nurser, A.J.G.
spellingShingle Bryden, H.L.
Nurser, A.J.G.
Effects of strait mixing on ocean stratification
author_facet Bryden, H.L.
Nurser, A.J.G.
author_sort Bryden, H.L.
title Effects of strait mixing on ocean stratification
title_short Effects of strait mixing on ocean stratification
title_full Effects of strait mixing on ocean stratification
title_fullStr Effects of strait mixing on ocean stratification
title_full_unstemmed Effects of strait mixing on ocean stratification
title_sort effects of strait mixing on ocean stratification
publishDate 2003
url http://nora.nerc.ac.uk/id/eprint/102052/
https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation Bryden, H.L.; Nurser, A.J.G. 2003 Effects of strait mixing on ocean stratification. Journal of Physical Oceanography, 33 (8). 1870-1872. https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2 <https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2>
op_doi https://doi.org/10.1175/1520-0485(2003)033<1870:EOSMOO>2.0.CO;2
_version_ 1766217352553168896

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