Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory
Observations and inverse models suggest that small-scale turbulent mixing is enhanced in the SouthernOcean in regions above rough topography. The enhancement extends O(1) km above the topography, suggestingthat mixing is supported by the breaking of gravity waves radiated from the ocean bottom. In t...
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ftunivtasecite:oai:ecite.utas.edu.au:79715 2023-05-15T16:02:28+02:00 Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory Nikurashin, M Ferrari, R 2010 application/pdf https://doi.org/10.1175/2009JPO4199.1 http://ecite.utas.edu.au/79715 en eng Amer Meteorological Soc http://ecite.utas.edu.au/79715/1/nikurashin_ferrari_2010a.pdf http://dx.doi.org/10.1175/2009JPO4199.1 Nikurashin, M and Ferrari, R, Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory, Journal of Physical Oceanography, 40, (May) pp. 1055-1074. ISSN 0022-3670 (2010) [Refereed Article] http://ecite.utas.edu.au/79715 Earth Sciences Oceanography Physical Oceanography Refereed Article PeerReviewed 2010 ftunivtasecite https://doi.org/10.1175/2009JPO4199.1 2019-12-13T21:45:09Z Observations and inverse models suggest that small-scale turbulent mixing is enhanced in the SouthernOcean in regions above rough topography. The enhancement extends O(1) km above the topography, suggestingthat mixing is supported by the breaking of gravity waves radiated from the ocean bottom. In thisstudy, it is shown that the observed mixing rates can be sustained by internal waves generated by geostrophicmotions flowing over bottom topography. Weakly nonlinear theory is used to describe the internal wavegeneration and the feedback of the waves on the zonally averaged flow. Vigorous inertial oscillations aredriven at the ocean bottom by waves generated at steep topography. The wave radiation and dissipation atequilibrium is therefore the result of both geostrophic flow and inertial oscillations differing substantiallyfrom the classical lee-wave problem. The theoretical predictions are tested versus two-dimensional highresolutionnumerical simulations with parameters representative of Drake Passage. This work suggests thatmixing in Drake Passage can be supported by geostrophic motions impinging on rough topography ratherthan by barotropic tidal motions, as is commonly assumed. Article in Journal/Newspaper Drake Passage eCite UTAS (University of Tasmania) Drake Passage Journal of Physical Oceanography 40 5 1055 1074 |
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eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Physical Oceanography |
spellingShingle |
Earth Sciences Oceanography Physical Oceanography Nikurashin, M Ferrari, R Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory |
topic_facet |
Earth Sciences Oceanography Physical Oceanography |
description |
Observations and inverse models suggest that small-scale turbulent mixing is enhanced in the SouthernOcean in regions above rough topography. The enhancement extends O(1) km above the topography, suggestingthat mixing is supported by the breaking of gravity waves radiated from the ocean bottom. In thisstudy, it is shown that the observed mixing rates can be sustained by internal waves generated by geostrophicmotions flowing over bottom topography. Weakly nonlinear theory is used to describe the internal wavegeneration and the feedback of the waves on the zonally averaged flow. Vigorous inertial oscillations aredriven at the ocean bottom by waves generated at steep topography. The wave radiation and dissipation atequilibrium is therefore the result of both geostrophic flow and inertial oscillations differing substantiallyfrom the classical lee-wave problem. The theoretical predictions are tested versus two-dimensional highresolutionnumerical simulations with parameters representative of Drake Passage. This work suggests thatmixing in Drake Passage can be supported by geostrophic motions impinging on rough topography ratherthan by barotropic tidal motions, as is commonly assumed. |
format |
Article in Journal/Newspaper |
author |
Nikurashin, M Ferrari, R |
author_facet |
Nikurashin, M Ferrari, R |
author_sort |
Nikurashin, M |
title |
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory |
title_short |
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory |
title_full |
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory |
title_fullStr |
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory |
title_full_unstemmed |
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory |
title_sort |
radiation and dissipation of internal waves generated by geostrophic motions impinging on small-scale topography: theory |
publisher |
Amer Meteorological Soc |
publishDate |
2010 |
url |
https://doi.org/10.1175/2009JPO4199.1 http://ecite.utas.edu.au/79715 |
geographic |
Drake Passage |
geographic_facet |
Drake Passage |
genre |
Drake Passage |
genre_facet |
Drake Passage |
op_relation |
http://ecite.utas.edu.au/79715/1/nikurashin_ferrari_2010a.pdf http://dx.doi.org/10.1175/2009JPO4199.1 Nikurashin, M and Ferrari, R, Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory, Journal of Physical Oceanography, 40, (May) pp. 1055-1074. ISSN 0022-3670 (2010) [Refereed Article] http://ecite.utas.edu.au/79715 |
op_doi |
https://doi.org/10.1175/2009JPO4199.1 |
container_title |
Journal of Physical Oceanography |
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40 |
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5 |
container_start_page |
1055 |
op_container_end_page |
1074 |
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1766398102762160128 |