Vertical flow in the Southern Ocean estimated from individual moorings
In this study, we demonstrate that oceanic vertical velocities can be estimated from individual mooring measurements, even for non-stationary flow. This result is obtained under three assumptions: i. weak diffusion (Péclet number ≫1), ii. weak friction (Reynolds number ≫1), and iii. small inertial t...
Published in: | Journal of Physical Oceanography |
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Language: | English |
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American Meteorological Society
2015
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Online Access: | http://nora.nerc.ac.uk/id/eprint/511314/ https://nora.nerc.ac.uk/id/eprint/511314/1/JPO-D-14-0065.1.pdf https://doi.org/10.1175/JPO-D-14-0065.1 |
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ftnerc:oai:nora.nerc.ac.uk:511314 2023-05-15T18:24:54+02:00 Vertical flow in the Southern Ocean estimated from individual moorings Sévellec, F. Naveira Garabato, A. C. Brearley, J. A. Sheen, K. L. 2015-09 text http://nora.nerc.ac.uk/id/eprint/511314/ https://nora.nerc.ac.uk/id/eprint/511314/1/JPO-D-14-0065.1.pdf https://doi.org/10.1175/JPO-D-14-0065.1 en eng American Meteorological Society https://nora.nerc.ac.uk/id/eprint/511314/1/JPO-D-14-0065.1.pdf Sévellec, F.; Naveira Garabato, A. C.; Brearley, J. A. orcid:0000-0003-3700-8017 Sheen, K. L. 2015 Vertical flow in the Southern Ocean estimated from individual moorings. Journal of Physical Oceanography, 45 (9). 2209-2220. https://doi.org/10.1175/JPO-D-14-0065.1 <https://doi.org/10.1175/JPO-D-14-0065.1> cc_by_4 CC-BY Publication - Article PeerReviewed 2015 ftnerc https://doi.org/10.1175/JPO-D-14-0065.1 2023-02-04T19:41:53Z In this study, we demonstrate that oceanic vertical velocities can be estimated from individual mooring measurements, even for non-stationary flow. This result is obtained under three assumptions: i. weak diffusion (Péclet number ≫1), ii. weak friction (Reynolds number ≫1), and iii. small inertial terms (Rossby number ≪1). The theoretical framework is applied to a set of 4 moorings located in the Southern Ocean. For this site, the diagnosed vertical velocities are highly variable in time, their standard deviation being one-to-two orders of magnitude greater than their mean. We demonstrate that the time-averaged vertical velocities are largely induced by geostrophic flow, and can be estimated from the time-averaged density and horizontal velocities. This suggests that local time-mean vertical velocities are primarily forced by the time-mean ocean dynamics, rather than by e.g. transient eddies or internal waves. We also show that, in the context of these four moorings, the time-mean vertical flow is consistent with stratified Taylor column dynamics in the presence of a topographic obstacle. Article in Journal/Newspaper Southern Ocean Natural Environment Research Council: NERC Open Research Archive Southern Ocean Journal of Physical Oceanography 45 9 2209 2220 |
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Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
In this study, we demonstrate that oceanic vertical velocities can be estimated from individual mooring measurements, even for non-stationary flow. This result is obtained under three assumptions: i. weak diffusion (Péclet number ≫1), ii. weak friction (Reynolds number ≫1), and iii. small inertial terms (Rossby number ≪1). The theoretical framework is applied to a set of 4 moorings located in the Southern Ocean. For this site, the diagnosed vertical velocities are highly variable in time, their standard deviation being one-to-two orders of magnitude greater than their mean. We demonstrate that the time-averaged vertical velocities are largely induced by geostrophic flow, and can be estimated from the time-averaged density and horizontal velocities. This suggests that local time-mean vertical velocities are primarily forced by the time-mean ocean dynamics, rather than by e.g. transient eddies or internal waves. We also show that, in the context of these four moorings, the time-mean vertical flow is consistent with stratified Taylor column dynamics in the presence of a topographic obstacle. |
format |
Article in Journal/Newspaper |
author |
Sévellec, F. Naveira Garabato, A. C. Brearley, J. A. Sheen, K. L. |
spellingShingle |
Sévellec, F. Naveira Garabato, A. C. Brearley, J. A. Sheen, K. L. Vertical flow in the Southern Ocean estimated from individual moorings |
author_facet |
Sévellec, F. Naveira Garabato, A. C. Brearley, J. A. Sheen, K. L. |
author_sort |
Sévellec, F. |
title |
Vertical flow in the Southern Ocean estimated from individual moorings |
title_short |
Vertical flow in the Southern Ocean estimated from individual moorings |
title_full |
Vertical flow in the Southern Ocean estimated from individual moorings |
title_fullStr |
Vertical flow in the Southern Ocean estimated from individual moorings |
title_full_unstemmed |
Vertical flow in the Southern Ocean estimated from individual moorings |
title_sort |
vertical flow in the southern ocean estimated from individual moorings |
publisher |
American Meteorological Society |
publishDate |
2015 |
url |
http://nora.nerc.ac.uk/id/eprint/511314/ https://nora.nerc.ac.uk/id/eprint/511314/1/JPO-D-14-0065.1.pdf https://doi.org/10.1175/JPO-D-14-0065.1 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
https://nora.nerc.ac.uk/id/eprint/511314/1/JPO-D-14-0065.1.pdf Sévellec, F.; Naveira Garabato, A. C.; Brearley, J. A. orcid:0000-0003-3700-8017 Sheen, K. L. 2015 Vertical flow in the Southern Ocean estimated from individual moorings. Journal of Physical Oceanography, 45 (9). 2209-2220. https://doi.org/10.1175/JPO-D-14-0065.1 <https://doi.org/10.1175/JPO-D-14-0065.1> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1175/JPO-D-14-0065.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
45 |
container_issue |
9 |
container_start_page |
2209 |
op_container_end_page |
2220 |
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1766205907381780480 |