Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope
The Rockall Bank area, located in the north-east Atlantic Ocean, is a region dominated by topographically-trapped diurnal tides. These tides generate up-and down-slope displacements that can be locally described as swashing motions on the bank. Using high spatial and time resolution of moored temper...
Published in: | Journal of Physical Oceanography |
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Format: | Article in Journal/Newspaper |
Language: | English |
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2016
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Online Access: | https://www.vliz.be/imisdocs/publications/35/299735.pdf |
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ftnioz:oai:imis.nioz.nl:251784 2023-05-15T17:38:22+02:00 Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope Cyr, F. van Haren, H. 2016 application/pdf https://www.vliz.be/imisdocs/publications/35/299735.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000368627900001 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1175/JPO-D-15-0059.1 https://www.vliz.be/imisdocs/publications/35/299735.pdf info:eu-repo/semantics/openAccess %3Ci%3EJ.+Phys.+Oceanogr.+46%281%29%3C%2Fi%3E%3A+219-231.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1175%2FJPO-D-15-0059.1%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1175%2FJPO-D-15-0059.1%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftnioz https://doi.org/10.1175/JPO-D-15-0059.1 2022-05-01T14:02:21Z The Rockall Bank area, located in the north-east Atlantic Ocean, is a region dominated by topographically-trapped diurnal tides. These tides generate up-and down-slope displacements that can be locally described as swashing motions on the bank. Using high spatial and time resolution of moored temperature sensors, the transition towards the upslope flow (cooling phase) is described as a rapid upslope-propagating bore, likely generated by breaking trapped internal waves. Buoyant anomalies are found during the bore propagation, likely resulting from small-scale instabilities. The imbalance between the rate of disappearance of available potential energy and the dissipation rate of turbulent kinetic energy suggests that these instabilities are growing (i.e., young), suggesting high mixing potential. Article in Journal/Newspaper North East Atlantic NIOZ Repository (Royal Netherlands Institute for Sea Research) Rockall Bank ENVELOPE(-16.519,-16.519,55.821,55.821) Journal of Physical Oceanography 46 1 219 231 |
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Open Polar |
collection |
NIOZ Repository (Royal Netherlands Institute for Sea Research) |
op_collection_id |
ftnioz |
language |
English |
description |
The Rockall Bank area, located in the north-east Atlantic Ocean, is a region dominated by topographically-trapped diurnal tides. These tides generate up-and down-slope displacements that can be locally described as swashing motions on the bank. Using high spatial and time resolution of moored temperature sensors, the transition towards the upslope flow (cooling phase) is described as a rapid upslope-propagating bore, likely generated by breaking trapped internal waves. Buoyant anomalies are found during the bore propagation, likely resulting from small-scale instabilities. The imbalance between the rate of disappearance of available potential energy and the dissipation rate of turbulent kinetic energy suggests that these instabilities are growing (i.e., young), suggesting high mixing potential. |
format |
Article in Journal/Newspaper |
author |
Cyr, F. van Haren, H. |
spellingShingle |
Cyr, F. van Haren, H. Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
author_facet |
Cyr, F. van Haren, H. |
author_sort |
Cyr, F. |
title |
Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
title_short |
Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
title_full |
Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
title_fullStr |
Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
title_full_unstemmed |
Observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
title_sort |
observations of small-scale secondary instabilities during the shoaling of internal bores on a deep-ocean slope |
publishDate |
2016 |
url |
https://www.vliz.be/imisdocs/publications/35/299735.pdf |
long_lat |
ENVELOPE(-16.519,-16.519,55.821,55.821) |
geographic |
Rockall Bank |
geographic_facet |
Rockall Bank |
genre |
North East Atlantic |
genre_facet |
North East Atlantic |
op_source |
%3Ci%3EJ.+Phys.+Oceanogr.+46%281%29%3C%2Fi%3E%3A+219-231.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1175%2FJPO-D-15-0059.1%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1175%2FJPO-D-15-0059.1%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000368627900001 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1175/JPO-D-15-0059.1 https://www.vliz.be/imisdocs/publications/35/299735.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1175/JPO-D-15-0059.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
46 |
container_issue |
1 |
container_start_page |
219 |
op_container_end_page |
231 |
_version_ |
1766138778266632192 |