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...

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Published in:Ocean Science
Main Authors: Børve, Eli, Isachsen, Pål Erik, Nøst, Ole Anders
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://hdl.handle.net/11250/2978520
https://doi.org/10.5194/os-17-1753-2021
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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
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language English
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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
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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