Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange
The Lofoten Basin in the Nordic Seas plays a central role in the Atlantic overturning circulation by acting as a reservoir for the warm and saline Atlantic Water flow toward the Arctic Ocean. The mass and heat exchange between Atlantic Water and the Lofoten Basin impacts the water mass transformatio...
Published in: | Journal of Geophysical Research: Oceans |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
AGU
2020
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Subjects: | |
Online Access: | https://hdl.handle.net/1956/23694 https://doi.org/10.1029/2018jc014774 |
_version_ | 1821836575506432000 |
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author | Dugstad, Johannes Sandanger Fer, Ilker Lacasce, Joseph Henry Sanchez de la Lama, Marta Trodahl, Marta |
author_facet | Dugstad, Johannes Sandanger Fer, Ilker Lacasce, Joseph Henry Sanchez de la Lama, Marta Trodahl, Marta |
author_sort | Dugstad, Johannes Sandanger |
collection | University of Bergen: Bergen Open Research Archive (BORA-UiB) |
container_issue | 5 |
container_start_page | 2992 |
container_title | Journal of Geophysical Research: Oceans |
container_volume | 124 |
description | The Lofoten Basin in the Nordic Seas plays a central role in the Atlantic overturning circulation by acting as a reservoir for the warm and saline Atlantic Water flow toward the Arctic Ocean. The mass and heat exchange between Atlantic Water and the Lofoten Basin impacts the water mass transformations and the surface heat loss, but the processes governing this exchange are not well understood or quantified. Here we study the circulation in the Nordic Seas and the heat transport in the Lofoten Basin using a combination of Lagrangian and Eulerian methods. We analyze the trajectories of about 150 surface drifters, augmented with a set of about 47,000 surface trajectories calculated using the output from a regional numerical simulation, to investigate the drifter pathways and their exchange with the Lofoten Basin. The drifters reveal that water parcels with long residence time inside the basin contribute substantially to the heat loss and typically enter from south across the outer rim of the Vøring Plateau and, to some extent from east, from the eastern branch of the Norwegian Atlantic Current. The main contributors to the lateral heat transport to the Lofoten Basin are the near‐surface heat transport by the mean flow in the southern sector of the basin and the subsurface eddy fluxes from the Lofoten Escarpment in the east. publishedVersion |
format | Article in Journal/Newspaper |
genre | Arctic Arctic Ocean Lofoten Nordic Seas |
genre_facet | Arctic Arctic Ocean Lofoten Nordic Seas |
geographic | Arctic Arctic Ocean Lofoten Vøring Plateau Lofoten Basin |
geographic_facet | Arctic Arctic Ocean Lofoten Vøring Plateau Lofoten Basin |
id | ftunivbergen:oai:bora.uib.no:1956/23694 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(4.000,4.000,67.000,67.000) ENVELOPE(4.000,4.000,70.000,70.000) |
op_collection_id | ftunivbergen |
op_container_end_page | 3006 |
op_doi | https://doi.org/10.1029/2018jc014774 |
op_relation | Norges forskningsråd: 250784 Notur/NorStore: NS9431K urn:issn:2169-9291 urn:issn:2169-9275 https://hdl.handle.net/1956/23694 https://doi.org/10.1029/2018jc014774 cristin:1711204 |
op_rights | Attribution-NonCommercial-NoDerivs CC BY-NC-ND http://creativecommons.org/licenses/by-nc-nd/4.0/ Copyright 2019 The Author(s) |
op_source | Journal of Geophysical Research (JGR): Oceans |
publishDate | 2020 |
publisher | AGU |
record_format | openpolar |
spelling | ftunivbergen:oai:bora.uib.no:1956/23694 2025-01-16T20:41:47+00:00 Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange Dugstad, Johannes Sandanger Fer, Ilker Lacasce, Joseph Henry Sanchez de la Lama, Marta Trodahl, Marta 2020-01-02T11:34:18Z application/pdf https://hdl.handle.net/1956/23694 https://doi.org/10.1029/2018jc014774 eng eng AGU Norges forskningsråd: 250784 Notur/NorStore: NS9431K urn:issn:2169-9291 urn:issn:2169-9275 https://hdl.handle.net/1956/23694 https://doi.org/10.1029/2018jc014774 cristin:1711204 Attribution-NonCommercial-NoDerivs CC BY-NC-ND http://creativecommons.org/licenses/by-nc-nd/4.0/ Copyright 2019 The Author(s) Journal of Geophysical Research (JGR): Oceans Oseanografi / Oceanography VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Peer reviewed Journal article 2020 ftunivbergen https://doi.org/10.1029/2018jc014774 2023-03-14T17:44:51Z The Lofoten Basin in the Nordic Seas plays a central role in the Atlantic overturning circulation by acting as a reservoir for the warm and saline Atlantic Water flow toward the Arctic Ocean. The mass and heat exchange between Atlantic Water and the Lofoten Basin impacts the water mass transformations and the surface heat loss, but the processes governing this exchange are not well understood or quantified. Here we study the circulation in the Nordic Seas and the heat transport in the Lofoten Basin using a combination of Lagrangian and Eulerian methods. We analyze the trajectories of about 150 surface drifters, augmented with a set of about 47,000 surface trajectories calculated using the output from a regional numerical simulation, to investigate the drifter pathways and their exchange with the Lofoten Basin. The drifters reveal that water parcels with long residence time inside the basin contribute substantially to the heat loss and typically enter from south across the outer rim of the Vøring Plateau and, to some extent from east, from the eastern branch of the Norwegian Atlantic Current. The main contributors to the lateral heat transport to the Lofoten Basin are the near‐surface heat transport by the mean flow in the southern sector of the basin and the subsurface eddy fluxes from the Lofoten Escarpment in the east. publishedVersion Article in Journal/Newspaper Arctic Arctic Ocean Lofoten Nordic Seas University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Arctic Ocean Lofoten Vøring Plateau ENVELOPE(4.000,4.000,67.000,67.000) Lofoten Basin ENVELOPE(4.000,4.000,70.000,70.000) Journal of Geophysical Research: Oceans 124 5 2992 3006 |
spellingShingle | Oseanografi / Oceanography VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Dugstad, Johannes Sandanger Fer, Ilker Lacasce, Joseph Henry Sanchez de la Lama, Marta Trodahl, Marta Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange |
title | Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange |
title_full | Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange |
title_fullStr | Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange |
title_full_unstemmed | Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange |
title_short | Lateral Heat Transport in the Lofoten Basin: Near-Surface Pathways and Subsurface Exchange |
title_sort | lateral heat transport in the lofoten basin: near-surface pathways and subsurface exchange |
topic | Oseanografi / Oceanography VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 |
topic_facet | Oseanografi / Oceanography VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 |
url | https://hdl.handle.net/1956/23694 https://doi.org/10.1029/2018jc014774 |