Pathways to Turbulent Dissipation in a Submarine Canyon
Abstract Velocity and turbulence observations are used to estimate the forward cascade of kinetic energy from the internal tide to dissipation within a steep canyon. Two methods for computing cross‐frequency kinetic energy flux are compared to observed dissipation. One method, coarse graining, allow...
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| Main Authors: | , , , , , , , |
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| Format: | Article |
| Language: | English |
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Wiley
2025-04-01
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| Series: | Geophysical Research Letters |
| Online Access: | https://doi.org/10.1029/2024GL113526 |
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| _version_ | 1849726381184778240 |
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| author | Charlotte Bellerjeau Matthew H. Alford Arnaud Le Boyer Giovanni Dematteis Alberto Naveira Garabato Gunnar Voet Nicole Couto Bethan L. Wynne‐Cattanach |
| author_facet | Charlotte Bellerjeau Matthew H. Alford Arnaud Le Boyer Giovanni Dematteis Alberto Naveira Garabato Gunnar Voet Nicole Couto Bethan L. Wynne‐Cattanach |
| author_sort | Charlotte Bellerjeau |
| collection | DOAJ |
| description | Abstract Velocity and turbulence observations are used to estimate the forward cascade of kinetic energy from the internal tide to dissipation within a steep canyon. Two methods for computing cross‐frequency kinetic energy flux are compared to observed dissipation. One method, coarse graining, allows strongly nonlinear dynamics while the other assumes weak nonlinearity. Fluxes from both methods agree within a factor of 3 with dissipation estimates from a finescale parameterization which is often used in climate‐scale ocean models. Coarse graining predicts 68% of energy fluxing to dissipation from frequencies lower than 8cpd, while the weakly nonlinear method predicts 34%. The weighting of energy flux toward lower frequencies supports a shorter frequency‐space pathway to dissipation in the presence of topographic wave breaking than assumed by parameterizations. Enhanced near‐boundary mixing and upwelling has implications for the rate and spatial distribution of the upwelling branch of the global overturning circulation. |
| format | Article |
| id | doaj-art-f198b4f3db3f478ea50bafb73b68193a |
| institution | DOAJ |
| issn | 0094-8276 1944-8007 |
| language | English |
| publishDate | 2025-04-01 |
| publisher | Wiley |
| record_format | Article |
| series | Geophysical Research Letters |
| spelling | doaj-art-f198b4f3db3f478ea50bafb73b68193a2025-08-20T03:10:11ZengWileyGeophysical Research Letters0094-82761944-80072025-04-01527n/an/a10.1029/2024GL113526Pathways to Turbulent Dissipation in a Submarine CanyonCharlotte Bellerjeau0Matthew H. Alford1Arnaud Le Boyer2Giovanni Dematteis3Alberto Naveira Garabato4Gunnar Voet5Nicole Couto6Bethan L. Wynne‐Cattanach7Scripps Institution of Oceanography UC San Diego La Jolla CA USAScripps Institution of Oceanography UC San Diego La Jolla CA USAScripps Institution of Oceanography UC San Diego La Jolla CA USAUniversità degli Studi di Torino Torino ItalyOcean and Earth Science University of Southampton Southampton UKScripps Institution of Oceanography UC San Diego La Jolla CA USAScripps Institution of Oceanography UC San Diego La Jolla CA USAScripps Institution of Oceanography UC San Diego La Jolla CA USAAbstract Velocity and turbulence observations are used to estimate the forward cascade of kinetic energy from the internal tide to dissipation within a steep canyon. Two methods for computing cross‐frequency kinetic energy flux are compared to observed dissipation. One method, coarse graining, allows strongly nonlinear dynamics while the other assumes weak nonlinearity. Fluxes from both methods agree within a factor of 3 with dissipation estimates from a finescale parameterization which is often used in climate‐scale ocean models. Coarse graining predicts 68% of energy fluxing to dissipation from frequencies lower than 8cpd, while the weakly nonlinear method predicts 34%. The weighting of energy flux toward lower frequencies supports a shorter frequency‐space pathway to dissipation in the presence of topographic wave breaking than assumed by parameterizations. Enhanced near‐boundary mixing and upwelling has implications for the rate and spatial distribution of the upwelling branch of the global overturning circulation.https://doi.org/10.1029/2024GL113526 |
| spellingShingle | Charlotte Bellerjeau Matthew H. Alford Arnaud Le Boyer Giovanni Dematteis Alberto Naveira Garabato Gunnar Voet Nicole Couto Bethan L. Wynne‐Cattanach Pathways to Turbulent Dissipation in a Submarine Canyon Geophysical Research Letters |
| title | Pathways to Turbulent Dissipation in a Submarine Canyon |
| title_full | Pathways to Turbulent Dissipation in a Submarine Canyon |
| title_fullStr | Pathways to Turbulent Dissipation in a Submarine Canyon |
| title_full_unstemmed | Pathways to Turbulent Dissipation in a Submarine Canyon |
| title_short | Pathways to Turbulent Dissipation in a Submarine Canyon |
| title_sort | pathways to turbulent dissipation in a submarine canyon |
| url | https://doi.org/10.1029/2024GL113526 |
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