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Cross-equatorial channel flow with zero potential vorticity under the complete Coriolis force

Abstract:

We investigate the cross-equatorial flow of deep ocean currents through a channel along the sea floor using the 1-layer or equivalent-barotropic shallow water equations. We restrict our attention to flows with zero potential vorticity, motivated by measurements of the deep Atlantic ocean, and focus on the role of the so-called non-traditional components of the Coriolis force due to the locally horizontal component of the Earth's rotation vector. These components are typically neglected in the...

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Publication status:
Published

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Publisher copy:
10.1093/imamat/hxs045

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Mathematical Institute
Role:
Author
Journal:
IMA JOURNAL OF APPLIED MATHEMATICS More from this journal
Volume:
77
Issue:
5
Pages:
626-651
Publication date:
2012-10-01
DOI:
EISSN:
1464-3634
ISSN:
0272-4960
Language:
English
Keywords:
Pubs id:
pubs:354642
UUID:
uuid:c65dd75a-f29c-4c39-9cdf-020876dd8679
Local pid:
pubs:354642
Source identifiers:
354642
Deposit date:
2013-11-17

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