Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy
A four-month glider mission was analyzed to assess turbulent dissipation in an anticyclonic eddy at the western boundary of the subtropical North Atlantic. The eddy (radius ≈ 60 km) had a core of low potential vorticity between 100–450 m, with maximum radial velocities of 0.5 m s−1 and Rossby number...
Published in: | Journal of Physical Oceanography |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2020
|
Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/527721/ https://nora.nerc.ac.uk/id/eprint/527721/1/jpo-d-19-0168.1.pdf https://nora.nerc.ac.uk/id/eprint/527721/7/jpod190168.pdf https://doi.org/10.1175/JPO-D-19-0168.1 |
id |
ftnerc:oai:nora.nerc.ac.uk:527721 |
---|---|
record_format |
openpolar |
spelling |
ftnerc:oai:nora.nerc.ac.uk:527721 2023-05-15T17:33:42+02:00 Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy Fernández-Castro, Bieito Evans, Gwyn Frajka-Williams, Eleanor Vic, Clément Naveira-Garabato, Alberto C. 2020-07-01 text http://nora.nerc.ac.uk/id/eprint/527721/ https://nora.nerc.ac.uk/id/eprint/527721/1/jpo-d-19-0168.1.pdf https://nora.nerc.ac.uk/id/eprint/527721/7/jpod190168.pdf https://doi.org/10.1175/JPO-D-19-0168.1 en eng https://nora.nerc.ac.uk/id/eprint/527721/1/jpo-d-19-0168.1.pdf https://nora.nerc.ac.uk/id/eprint/527721/7/jpod190168.pdf Fernández-Castro, Bieito; Evans, Gwyn orcid:0000-0002-6328-4093 Frajka-Williams, Eleanor orcid:0000-0001-8773-7838 Vic, Clément; Naveira-Garabato, Alberto C. 2020 Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy. Journal of Physical Oceanography, 50 (7). 1893-1914. https://doi.org/10.1175/JPO-D-19-0168.1 <https://doi.org/10.1175/JPO-D-19-0168.1> cc_by_4 CC-BY Publication - Article PeerReviewed 2020 ftnerc https://doi.org/10.1175/JPO-D-19-0168.1 2023-02-04T19:50:39Z A four-month glider mission was analyzed to assess turbulent dissipation in an anticyclonic eddy at the western boundary of the subtropical North Atlantic. The eddy (radius ≈ 60 km) had a core of low potential vorticity between 100–450 m, with maximum radial velocities of 0.5 m s−1 and Rossby number ≈ −0.1. Turbulent dissipation was inferred from vertical water velocities derived from the glider flight model. Dissipation was suppressed in the eddy core (ε ≈ 5×10−10 W kg−1) and enhanced below it (> 10−9 W kg−1). Elevated dissipation was coincident with quasi-periodic structures in the vertical velocity and pressure perturbations, suggesting internal waves as the drivers of dissipation. A heuristic ray-tracing approximation was used to investigate the wave-eddy interactions leading to turbulent dissipation. Ray-tracing simulations were consistent with two types of wave-eddy interactions that may induce dissipation: the trapping of near-inertial wave energy by the eddy’s relative vorticity, or the entry of an internal tide (generated at the nearby continental slope) to a critical layer in the eddy shear. The latter scenario suggests that the intense mesoscale field characterizing the western boundaries of ocean basins might act as a ‘leaky wall’ controlling the propagation of internal tides into the basins’ interior. Article in Journal/Newspaper North Atlantic Natural Environment Research Council: NERC Open Research Archive Journal of Physical Oceanography 50 7 1893 1914 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
A four-month glider mission was analyzed to assess turbulent dissipation in an anticyclonic eddy at the western boundary of the subtropical North Atlantic. The eddy (radius ≈ 60 km) had a core of low potential vorticity between 100–450 m, with maximum radial velocities of 0.5 m s−1 and Rossby number ≈ −0.1. Turbulent dissipation was inferred from vertical water velocities derived from the glider flight model. Dissipation was suppressed in the eddy core (ε ≈ 5×10−10 W kg−1) and enhanced below it (> 10−9 W kg−1). Elevated dissipation was coincident with quasi-periodic structures in the vertical velocity and pressure perturbations, suggesting internal waves as the drivers of dissipation. A heuristic ray-tracing approximation was used to investigate the wave-eddy interactions leading to turbulent dissipation. Ray-tracing simulations were consistent with two types of wave-eddy interactions that may induce dissipation: the trapping of near-inertial wave energy by the eddy’s relative vorticity, or the entry of an internal tide (generated at the nearby continental slope) to a critical layer in the eddy shear. The latter scenario suggests that the intense mesoscale field characterizing the western boundaries of ocean basins might act as a ‘leaky wall’ controlling the propagation of internal tides into the basins’ interior. |
format |
Article in Journal/Newspaper |
author |
Fernández-Castro, Bieito Evans, Gwyn Frajka-Williams, Eleanor Vic, Clément Naveira-Garabato, Alberto C. |
spellingShingle |
Fernández-Castro, Bieito Evans, Gwyn Frajka-Williams, Eleanor Vic, Clément Naveira-Garabato, Alberto C. Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy |
author_facet |
Fernández-Castro, Bieito Evans, Gwyn Frajka-Williams, Eleanor Vic, Clément Naveira-Garabato, Alberto C. |
author_sort |
Fernández-Castro, Bieito |
title |
Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy |
title_short |
Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy |
title_full |
Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy |
title_fullStr |
Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy |
title_full_unstemmed |
Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy |
title_sort |
breaking of internal waves and turbulent dissipation in an anticyclonic mode water eddy |
publishDate |
2020 |
url |
http://nora.nerc.ac.uk/id/eprint/527721/ https://nora.nerc.ac.uk/id/eprint/527721/1/jpo-d-19-0168.1.pdf https://nora.nerc.ac.uk/id/eprint/527721/7/jpod190168.pdf https://doi.org/10.1175/JPO-D-19-0168.1 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://nora.nerc.ac.uk/id/eprint/527721/1/jpo-d-19-0168.1.pdf https://nora.nerc.ac.uk/id/eprint/527721/7/jpod190168.pdf Fernández-Castro, Bieito; Evans, Gwyn orcid:0000-0002-6328-4093 Frajka-Williams, Eleanor orcid:0000-0001-8773-7838 Vic, Clément; Naveira-Garabato, Alberto C. 2020 Breaking of internal waves and turbulent dissipation in an anticyclonic mode Water Eddy. Journal of Physical Oceanography, 50 (7). 1893-1914. https://doi.org/10.1175/JPO-D-19-0168.1 <https://doi.org/10.1175/JPO-D-19-0168.1> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1175/JPO-D-19-0168.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
50 |
container_issue |
7 |
container_start_page |
1893 |
op_container_end_page |
1914 |
_version_ |
1766132287876890624 |