Tidally induced internal motion in an Arctic fjord
The internal response in a stratified, partially enclosed basin subject to semi-diurnal tidal forcing through a narrow entrance is investigated. The site is located above the critical latitude where linear internal waves of lunar semi-diurnal frequency are not permitted to propagate freely. Generati...
Published in: | Nonlinear Processes in Geophysics |
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Copernicus Publications
2014
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00020740 2023-05-15T15:08:19+02:00 Tidally induced internal motion in an Arctic fjord Støylen, E. Fer, I. 2014-01 electronic https://doi.org/10.5194/npg-21-87-2014 https://noa.gwlb.de/receive/cop_mods_00020740 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00020695/npg-21-87-2014.pdf https://npg.copernicus.org/articles/21/87/2014/npg-21-87-2014.pdf eng eng Copernicus Publications Nonlinear Processes in Geophysics -- http://www.bibliothek.uni-regensburg.de/ezeit/?2078085 -- http://www.nonlin-processes-geophys.net/ -- http://www.copernicus.org/EGU/npg/npg.htm -- 1607-7946 https://doi.org/10.5194/npg-21-87-2014 https://noa.gwlb.de/receive/cop_mods_00020740 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00020695/npg-21-87-2014.pdf https://npg.copernicus.org/articles/21/87/2014/npg-21-87-2014.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2014 ftnonlinearchiv https://doi.org/10.5194/npg-21-87-2014 2022-02-08T22:52:00Z The internal response in a stratified, partially enclosed basin subject to semi-diurnal tidal forcing through a narrow entrance is investigated. The site is located above the critical latitude where linear internal waves of lunar semi-diurnal frequency are not permitted to propagate freely. Generation and propagation of tidally induced internal Kelvin waves are studied, for baroclinically sub- and supercritical conditions at the mouth of the fjord, using a non-linear 3-D numerical model in an idealized basin and in Van Mijenfjorden, Svalbard, using a realistic topography. The model results are compared to observations of hydrography and currents made in August 2010. Results from both the model and measurements indicate the presence of internal Kelvin waves, even when conditions at the fjord entrance are supercritical. The entrance of Van Mijenfjorden is split into two sounds. Sensitivity experiments by closing each sound separately reveal that internal Kelvin waves are generated at both sounds. When the conditions are near supercritical, a wave pulse propagates inward from the fjord entrance at the beginning of each inflow phase of the tidal cycle. The leading crest is followed by a series of smaller amplitude waves characterized as non-linear internal solitons. However, higher model resolution is needed to accurately describe the influence of small-scale mixing and processes near the sill crest in establishing the evolution of the flow and internal response in the fjord. Article in Journal/Newspaper Arctic Svalbard Van Mijenfjorden Niedersächsisches Online-Archiv NOA Arctic Svalbard Van Mijenfjorden ENVELOPE(14.667,14.667,77.717,77.717) Nonlinear Processes in Geophysics 21 1 87 100 |
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ftnonlinearchiv |
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English |
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article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Støylen, E. Fer, I. Tidally induced internal motion in an Arctic fjord |
topic_facet |
article Verlagsveröffentlichung |
description |
The internal response in a stratified, partially enclosed basin subject to semi-diurnal tidal forcing through a narrow entrance is investigated. The site is located above the critical latitude where linear internal waves of lunar semi-diurnal frequency are not permitted to propagate freely. Generation and propagation of tidally induced internal Kelvin waves are studied, for baroclinically sub- and supercritical conditions at the mouth of the fjord, using a non-linear 3-D numerical model in an idealized basin and in Van Mijenfjorden, Svalbard, using a realistic topography. The model results are compared to observations of hydrography and currents made in August 2010. Results from both the model and measurements indicate the presence of internal Kelvin waves, even when conditions at the fjord entrance are supercritical. The entrance of Van Mijenfjorden is split into two sounds. Sensitivity experiments by closing each sound separately reveal that internal Kelvin waves are generated at both sounds. When the conditions are near supercritical, a wave pulse propagates inward from the fjord entrance at the beginning of each inflow phase of the tidal cycle. The leading crest is followed by a series of smaller amplitude waves characterized as non-linear internal solitons. However, higher model resolution is needed to accurately describe the influence of small-scale mixing and processes near the sill crest in establishing the evolution of the flow and internal response in the fjord. |
format |
Article in Journal/Newspaper |
author |
Støylen, E. Fer, I. |
author_facet |
Støylen, E. Fer, I. |
author_sort |
Støylen, E. |
title |
Tidally induced internal motion in an Arctic fjord |
title_short |
Tidally induced internal motion in an Arctic fjord |
title_full |
Tidally induced internal motion in an Arctic fjord |
title_fullStr |
Tidally induced internal motion in an Arctic fjord |
title_full_unstemmed |
Tidally induced internal motion in an Arctic fjord |
title_sort |
tidally induced internal motion in an arctic fjord |
publisher |
Copernicus Publications |
publishDate |
2014 |
url |
https://doi.org/10.5194/npg-21-87-2014 https://noa.gwlb.de/receive/cop_mods_00020740 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00020695/npg-21-87-2014.pdf https://npg.copernicus.org/articles/21/87/2014/npg-21-87-2014.pdf |
long_lat |
ENVELOPE(14.667,14.667,77.717,77.717) |
geographic |
Arctic Svalbard Van Mijenfjorden |
geographic_facet |
Arctic Svalbard Van Mijenfjorden |
genre |
Arctic Svalbard Van Mijenfjorden |
genre_facet |
Arctic Svalbard Van Mijenfjorden |
op_relation |
Nonlinear Processes in Geophysics -- http://www.bibliothek.uni-regensburg.de/ezeit/?2078085 -- http://www.nonlin-processes-geophys.net/ -- http://www.copernicus.org/EGU/npg/npg.htm -- 1607-7946 https://doi.org/10.5194/npg-21-87-2014 https://noa.gwlb.de/receive/cop_mods_00020740 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00020695/npg-21-87-2014.pdf https://npg.copernicus.org/articles/21/87/2014/npg-21-87-2014.pdf |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/npg-21-87-2014 |
container_title |
Nonlinear Processes in Geophysics |
container_volume |
21 |
container_issue |
1 |
container_start_page |
87 |
op_container_end_page |
100 |
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1766339706592690176 |