Rectified tidal transport in Lofoten–Vesterålen, northern Norway
Vestfjorden in northern Norway, a major spawning ground for the northeast Arctic cod, is sheltered from the continental shelf and open ocean by the Lofoten–Vesterålen archipelago. The archipelago, however, is well known for hosting strong and vigorous tidal currents in its many straits, currents tha...
Published in: | Ocean Science |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2021
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2978520 https://doi.org/10.5194/os-17-1753-2021 |
_version_ | 1821796623526658048 |
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author | Børve, Eli Isachsen, Pål Erik Nøst, Ole Anders |
author_facet | Børve, Eli Isachsen, Pål Erik Nøst, Ole Anders |
author_sort | Børve, Eli |
collection | Nord Open Research Archive |
container_issue | 6 |
container_start_page | 1753 |
container_title | Ocean Science |
container_volume | 17 |
description | Vestfjorden in northern Norway, a major spawning ground for the northeast Arctic cod, is sheltered from the continental shelf and open ocean by the Lofoten–Vesterålen archipelago. The archipelago, however, is well known for hosting strong and vigorous tidal currents in its many straits, currents that can produce significant time-mean tracer transport from Vestfjorden to the shelf outside. We use a purely tidally driven unstructured-grid ocean model to look into non-linear tidal dynamics and the associated tracer transport through the archipelago. Of particular interest are two processes: tidal pumping through the straits and tidal rectification around islands. The most prominent tracer transport is caused by tidal pumping through the short and strongly non-linear straits Nordlandsflaget and Moskstraumen near the southern tip of the archipelago. Here, tracers from Vestfjorden are transported tens of kilometers westward out on the outer shelf. Further north, weaker yet notable tidal pumping also takes place through the longer straits Nappstraumen and Gimsøystraumen. The other main transport route out of Vestfjorden is south of the island of Røst. Here, the transport is primarily due to tracer advection by rectified anticyclonic currents around the island. There is also an anticyclonic circulation cell around the island group Mosken–Værøy, and both cells have flow speeds up to 0.2 m s−1, magnitudes similar to the observed background currents in the region. These high-resolution simulations thus emphasize the importance of non-linear tidal dynamics for transport of floating particles, like cod eggs and larvae, in the region. publishedVersion |
format | Article in Journal/Newspaper |
genre | Arctic cod Arctic Lofoten Northeast Arctic cod Northern Norway Røst Vesterålen Vestfjorden Værøy |
genre_facet | Arctic cod Arctic Lofoten Northeast Arctic cod Northern Norway Røst Vesterålen Vestfjorden Værøy |
geographic | Arctic Gimsøystraumen Lofoten Mosken Norway Røst Vesterålen Værøy |
geographic_facet | Arctic Gimsøystraumen Lofoten Mosken Norway Røst Vesterålen Værøy |
id | ftnorduniv:oai:nordopen.nord.no:11250/2978520 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(14.301,14.301,68.303,68.303) ENVELOPE(12.755,12.755,67.746,67.746) ENVELOPE(11.983,11.983,67.467,67.467) ENVELOPE(14.939,14.939,68.754,68.754) ENVELOPE(12.693,12.693,67.664,67.664) |
op_collection_id | ftnorduniv |
op_container_end_page | 1773 |
op_doi | https://doi.org/10.5194/os-17-1753-2021 |
op_relation | VISTA: 6168 The Norwegian Meteorological Institute: 181090 Børve, E., Isachsen, P. E. & Nøst, O. A. (2021). Rectified tidal transport in Lofoten–Vesterålen, northern Norway. Ocean Science, 17(6), 1753-1773. doi: urn:issn:1812-0792 https://hdl.handle.net/11250/2978520 https://doi.org/10.5194/os-17-1753-2021 cristin:1964596 |
op_rights | Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © 2021 The Author(s) |
op_source | 1753-1773 17 Ocean Science 6 |
publishDate | 2021 |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | ftnorduniv:oai:nordopen.nord.no:11250/2978520 2025-01-16T20:00:04+00:00 Rectified tidal transport in Lofoten–Vesterålen, northern Norway Børve, Eli Isachsen, Pål Erik Nøst, Ole Anders 2021 application/pdf https://hdl.handle.net/11250/2978520 https://doi.org/10.5194/os-17-1753-2021 eng eng Copernicus Publications VISTA: 6168 The Norwegian Meteorological Institute: 181090 Børve, E., Isachsen, P. E. & Nøst, O. A. (2021). Rectified tidal transport in Lofoten–Vesterålen, northern Norway. Ocean Science, 17(6), 1753-1773. doi: urn:issn:1812-0792 https://hdl.handle.net/11250/2978520 https://doi.org/10.5194/os-17-1753-2021 cristin:1964596 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © 2021 The Author(s) 1753-1773 17 Ocean Science 6 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452 Peer reviewed Journal article 2021 ftnorduniv https://doi.org/10.5194/os-17-1753-2021 2023-06-19T14:04:32Z Vestfjorden in northern Norway, a major spawning ground for the northeast Arctic cod, is sheltered from the continental shelf and open ocean by the Lofoten–Vesterålen archipelago. The archipelago, however, is well known for hosting strong and vigorous tidal currents in its many straits, currents that can produce significant time-mean tracer transport from Vestfjorden to the shelf outside. We use a purely tidally driven unstructured-grid ocean model to look into non-linear tidal dynamics and the associated tracer transport through the archipelago. Of particular interest are two processes: tidal pumping through the straits and tidal rectification around islands. The most prominent tracer transport is caused by tidal pumping through the short and strongly non-linear straits Nordlandsflaget and Moskstraumen near the southern tip of the archipelago. Here, tracers from Vestfjorden are transported tens of kilometers westward out on the outer shelf. Further north, weaker yet notable tidal pumping also takes place through the longer straits Nappstraumen and Gimsøystraumen. The other main transport route out of Vestfjorden is south of the island of Røst. Here, the transport is primarily due to tracer advection by rectified anticyclonic currents around the island. There is also an anticyclonic circulation cell around the island group Mosken–Værøy, and both cells have flow speeds up to 0.2 m s−1, magnitudes similar to the observed background currents in the region. These high-resolution simulations thus emphasize the importance of non-linear tidal dynamics for transport of floating particles, like cod eggs and larvae, in the region. publishedVersion Article in Journal/Newspaper Arctic cod Arctic Lofoten Northeast Arctic cod Northern Norway Røst Vesterålen Vestfjorden Værøy Nord Open Research Archive Arctic Gimsøystraumen ENVELOPE(14.301,14.301,68.303,68.303) Lofoten Mosken ENVELOPE(12.755,12.755,67.746,67.746) Norway Røst ENVELOPE(11.983,11.983,67.467,67.467) Vesterålen ENVELOPE(14.939,14.939,68.754,68.754) Værøy ENVELOPE(12.693,12.693,67.664,67.664) Ocean Science 17 6 1753 1773 |
spellingShingle | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452 Børve, Eli Isachsen, Pål Erik Nøst, Ole Anders Rectified tidal transport in Lofoten–Vesterålen, northern Norway |
title | Rectified tidal transport in Lofoten–Vesterålen, northern Norway |
title_full | Rectified tidal transport in Lofoten–Vesterålen, northern Norway |
title_fullStr | Rectified tidal transport in Lofoten–Vesterålen, northern Norway |
title_full_unstemmed | Rectified tidal transport in Lofoten–Vesterålen, northern Norway |
title_short | Rectified tidal transport in Lofoten–Vesterålen, northern Norway |
title_sort | rectified tidal transport in lofoten–vesterålen, northern norway |
topic | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452 |
topic_facet | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452 |
url | https://hdl.handle.net/11250/2978520 https://doi.org/10.5194/os-17-1753-2021 |