The dissipation of kinetic energy in the Lofoten Basin Eddy
Ocean microstructure, current and hydrography observations from June 2016 are used to characterize the turbulence structure of the Lofoten Basin Eddy (LBE), a long-lived anticyclone in the Norwegian Sea. The LBE had a azimuthal peak velocity of 0.8 ms−1 at 950 m depth and 22 km radial distance from...
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ftarchimer:oai:archimer.ifremer.fr:54836 2023-05-15T17:08:16+02:00 The dissipation of kinetic energy in the Lofoten Basin Eddy Fer, Ilker Bosse, Anthony Ferron, Bruno Bouruet-aubertot, Pascale 2018-06 application/pdf https://archimer.ifremer.fr/doc/00437/54836/56312.pdf https://doi.org/10.1175/JPO-D-17-0244.1 https://archimer.ifremer.fr/doc/00437/54836/ eng eng Amer Meteorological Soc https://archimer.ifremer.fr/doc/00437/54836/56312.pdf doi:10.1175/JPO-D-17-0244.1 https://archimer.ifremer.fr/doc/00437/54836/ 2018 American Meteorological Society info:eu-repo/semantics/openAccess restricted use Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2018-06 , Vol. 48 , N. 6 , P. 1299-1316 text Publication info:eu-repo/semantics/article 2018 ftarchimer https://doi.org/10.1175/JPO-D-17-0244.1 2021-09-23T20:30:54Z Ocean microstructure, current and hydrography observations from June 2016 are used to characterize the turbulence structure of the Lofoten Basin Eddy (LBE), a long-lived anticyclone in the Norwegian Sea. The LBE had a azimuthal peak velocity of 0.8 ms−1 at 950 m depth and 22 km radial distance from its center, and a core relative vorticity reaching -0.7 f ( f is the local Coriolis parameter). When contrasted to a reference station in a relatively quiescent part of the basin, the LBE was significantly turbulent between 750 and 2000 m, exceeding the dissipation rates (ɛ) in the reference station by up to two orders of magnitude. Dissipation rates were elevated particularly in the core and at the rim below the swirl velocity maximum, reaching 10−8 Wkg–1. The sources of energy for the observed turbulence are the background shear (gradient Richardson number less than unity) and the sub-inertial energy trapped by the negative vorticity of the eddy. Idealized ray tracing calculations show that the vertical and lateral changes in stratification, shear and vorticity allow sub-inertial waves to be trapped within the LBE. Spectral analysis shows increased high-wavenumber clockwise-polarized shear variance in the core and rim regions, consistent with downward propagating near-inertial waves (vertical wavelengths of order 100 m, and energy levels 3 to 10 times the canonical open ocean level). The energetic packets with a distinct downward energy propagation are typically accompanied with an increase in dissipation levels. Based on these summer observations, the time scale to drain the volume-integrated total energy of the LBE is 14 years. Article in Journal/Newspaper Lofoten Norwegian Sea Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Lofoten Lofoten Basin ENVELOPE(4.000,4.000,70.000,70.000) Norwegian Sea Journal of Physical Oceanography 48 6 1299 1316 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
description |
Ocean microstructure, current and hydrography observations from June 2016 are used to characterize the turbulence structure of the Lofoten Basin Eddy (LBE), a long-lived anticyclone in the Norwegian Sea. The LBE had a azimuthal peak velocity of 0.8 ms−1 at 950 m depth and 22 km radial distance from its center, and a core relative vorticity reaching -0.7 f ( f is the local Coriolis parameter). When contrasted to a reference station in a relatively quiescent part of the basin, the LBE was significantly turbulent between 750 and 2000 m, exceeding the dissipation rates (ɛ) in the reference station by up to two orders of magnitude. Dissipation rates were elevated particularly in the core and at the rim below the swirl velocity maximum, reaching 10−8 Wkg–1. The sources of energy for the observed turbulence are the background shear (gradient Richardson number less than unity) and the sub-inertial energy trapped by the negative vorticity of the eddy. Idealized ray tracing calculations show that the vertical and lateral changes in stratification, shear and vorticity allow sub-inertial waves to be trapped within the LBE. Spectral analysis shows increased high-wavenumber clockwise-polarized shear variance in the core and rim regions, consistent with downward propagating near-inertial waves (vertical wavelengths of order 100 m, and energy levels 3 to 10 times the canonical open ocean level). The energetic packets with a distinct downward energy propagation are typically accompanied with an increase in dissipation levels. Based on these summer observations, the time scale to drain the volume-integrated total energy of the LBE is 14 years. |
format |
Article in Journal/Newspaper |
author |
Fer, Ilker Bosse, Anthony Ferron, Bruno Bouruet-aubertot, Pascale |
spellingShingle |
Fer, Ilker Bosse, Anthony Ferron, Bruno Bouruet-aubertot, Pascale The dissipation of kinetic energy in the Lofoten Basin Eddy |
author_facet |
Fer, Ilker Bosse, Anthony Ferron, Bruno Bouruet-aubertot, Pascale |
author_sort |
Fer, Ilker |
title |
The dissipation of kinetic energy in the Lofoten Basin Eddy |
title_short |
The dissipation of kinetic energy in the Lofoten Basin Eddy |
title_full |
The dissipation of kinetic energy in the Lofoten Basin Eddy |
title_fullStr |
The dissipation of kinetic energy in the Lofoten Basin Eddy |
title_full_unstemmed |
The dissipation of kinetic energy in the Lofoten Basin Eddy |
title_sort |
dissipation of kinetic energy in the lofoten basin eddy |
publisher |
Amer Meteorological Soc |
publishDate |
2018 |
url |
https://archimer.ifremer.fr/doc/00437/54836/56312.pdf https://doi.org/10.1175/JPO-D-17-0244.1 https://archimer.ifremer.fr/doc/00437/54836/ |
long_lat |
ENVELOPE(4.000,4.000,70.000,70.000) |
geographic |
Lofoten Lofoten Basin Norwegian Sea |
geographic_facet |
Lofoten Lofoten Basin Norwegian Sea |
genre |
Lofoten Norwegian Sea |
genre_facet |
Lofoten Norwegian Sea |
op_source |
Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2018-06 , Vol. 48 , N. 6 , P. 1299-1316 |
op_relation |
https://archimer.ifremer.fr/doc/00437/54836/56312.pdf doi:10.1175/JPO-D-17-0244.1 https://archimer.ifremer.fr/doc/00437/54836/ |
op_rights |
2018 American Meteorological Society info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1175/JPO-D-17-0244.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
48 |
container_issue |
6 |
container_start_page |
1299 |
op_container_end_page |
1316 |
_version_ |
1766063983492595712 |