Breaking of Internal Waves and Turbulent Dissipation in an Anticyclonic Mode Water Eddy
22 pages, 13 figures.-- This article is licensed under a Creative Commons Attribution 4.0 license A 4-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 poten...
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ftcsic:oai:digital.csic.es:10261/217297 2024-02-11T10:06:38+01:00 Breaking of Internal Waves and Turbulent Dissipation in an Anticyclonic Mode Water Eddy Fernández-Castro, B. Ebans, D. Gwyn Frajka-Williams, Eleanor Vic, C. Naveira-Garabato, Alberto 2020 http://hdl.handle.net/10261/217297 https://doi.org/10.1175/JPO-D-19-0168.1 en eng American Meteorological Society Publisher's version https://doi.org/10.1175/JPO-D-19-0168.1 Sí Journal of Physical Oceanography 50(7): 1893–1914 (2020) 0022-3670 http://hdl.handle.net/10261/217297 doi:10.1175/JPO-D-19-0168.1 1520-0485 open Eddies Internal waves Mesoscale processes Turbulence artículo http://purl.org/coar/resource_type/c_6501 2020 ftcsic https://doi.org/10.1175/JPO-D-19-0168.1 2024-01-16T10:56:39Z 22 pages, 13 figures.-- This article is licensed under a Creative Commons Attribution 4.0 license A 4-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 and 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 quasiperiodic 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 basin’s interior The MerMEED project was funded by the U.K. Natural Environment Research Council (NE/N001745/1). B. Fernández-Castro was supported by a Juan de La Cierva-Formación postdoctoral fellowship (FJCI-641 2015-25712) and a José Castillejo travel grant (CAS18/00017) by the Spanish Government. A. Naveira-Garabato was supported by the Royal Society and the Wolfson Foundation Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Cierva ENVELOPE(-60.873,-60.873,-64.156,-64.156) Journal of Physical Oceanography 50 7 1893 1914 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Eddies Internal waves Mesoscale processes Turbulence |
spellingShingle |
Eddies Internal waves Mesoscale processes Turbulence Fernández-Castro, B. Ebans, D. Gwyn Frajka-Williams, Eleanor Vic, C. Naveira-Garabato, Alberto Breaking of Internal Waves and Turbulent Dissipation in an Anticyclonic Mode Water Eddy |
topic_facet |
Eddies Internal waves Mesoscale processes Turbulence |
description |
22 pages, 13 figures.-- This article is licensed under a Creative Commons Attribution 4.0 license A 4-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 and 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 quasiperiodic 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 basin’s interior The MerMEED project was funded by the U.K. Natural Environment Research Council (NE/N001745/1). B. Fernández-Castro was supported by a Juan de La Cierva-Formación postdoctoral fellowship (FJCI-641 2015-25712) and a José Castillejo travel grant (CAS18/00017) by the Spanish Government. A. Naveira-Garabato was supported by the Royal Society and the Wolfson Foundation Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Fernández-Castro, B. Ebans, D. Gwyn Frajka-Williams, Eleanor Vic, C. Naveira-Garabato, Alberto |
author_facet |
Fernández-Castro, B. Ebans, D. Gwyn Frajka-Williams, Eleanor Vic, C. Naveira-Garabato, Alberto |
author_sort |
Fernández-Castro, B. |
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 |
publisher |
American Meteorological Society |
publishDate |
2020 |
url |
http://hdl.handle.net/10261/217297 https://doi.org/10.1175/JPO-D-19-0168.1 |
long_lat |
ENVELOPE(-60.873,-60.873,-64.156,-64.156) |
geographic |
Cierva |
geographic_facet |
Cierva |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Publisher's version https://doi.org/10.1175/JPO-D-19-0168.1 Sí Journal of Physical Oceanography 50(7): 1893–1914 (2020) 0022-3670 http://hdl.handle.net/10261/217297 doi:10.1175/JPO-D-19-0168.1 1520-0485 |
op_rights |
open |
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_ |
1790604460666388480 |