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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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2015
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Subjects: | |
Online Access: | https://hdl.handle.net/1956/10527 https://doi.org/10.5194/npg-21-87-2014 |
_version_ | 1821837004748357632 |
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author | Støylen, Eivind Fer, Ilker |
author_facet | Støylen, Eivind Fer, Ilker |
author_sort | Støylen, Eivind |
collection | University of Bergen: Bergen Open Research Archive (BORA-UiB) |
container_issue | 1 |
container_start_page | 87 |
container_title | Nonlinear Processes in Geophysics |
container_volume | 21 |
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. publishedVersion |
format | Article in Journal/Newspaper |
genre | Arctic Svalbard Van Mijenfjorden |
genre_facet | Arctic Svalbard Van Mijenfjorden |
geographic | Arctic Svalbard Van Mijenfjorden |
geographic_facet | Arctic Svalbard Van Mijenfjorden |
id | ftunivbergen:oai:bora.uib.no:1956/10527 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(14.667,14.667,77.717,77.717) |
op_collection_id | ftunivbergen |
op_container_end_page | 100 |
op_doi | https://doi.org/10.5194/npg-21-87-2014 |
op_relation | urn:issn:1023-5809 urn:issn:1607-7946 https://hdl.handle.net/1956/10527 https://doi.org/10.5194/npg-21-87-2014 cristin:1084183 |
op_rights | Attribution CC BY http://creativecommons.org/licenses/by/3.0/ Copyright 2014 The Authors |
publishDate | 2015 |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | ftunivbergen:oai:bora.uib.no:1956/10527 2025-01-16T20:42:10+00:00 Tidally induced internal motion in an Arctic fjord Støylen, Eivind Fer, Ilker 2015-07-28T08:06:18Z application/pdf https://hdl.handle.net/1956/10527 https://doi.org/10.5194/npg-21-87-2014 eng eng Copernicus Publications urn:issn:1023-5809 urn:issn:1607-7946 https://hdl.handle.net/1956/10527 https://doi.org/10.5194/npg-21-87-2014 cristin:1084183 Attribution CC BY http://creativecommons.org/licenses/by/3.0/ Copyright 2014 The Authors VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Peer reviewed Journal article 2015 ftunivbergen https://doi.org/10.5194/npg-21-87-2014 2023-03-14T17:40:33Z 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. publishedVersion Article in Journal/Newspaper Arctic Svalbard Van Mijenfjorden University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Svalbard Van Mijenfjorden ENVELOPE(14.667,14.667,77.717,77.717) Nonlinear Processes in Geophysics 21 1 87 100 |
spellingShingle | VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Støylen, Eivind Fer, Ilker Tidally induced internal motion in an Arctic fjord |
title | 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_short | Tidally induced internal motion in an Arctic fjord |
title_sort | tidally induced internal motion in an arctic fjord |
topic | VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 |
topic_facet | VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 |
url | https://hdl.handle.net/1956/10527 https://doi.org/10.5194/npg-21-87-2014 |