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...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Dugstad, Johannes Sandanger, Fer, Ilker, Lacasce, Joseph Henry, Sanchez de la Lama, Marta, Trodahl, Marta
Format: Article in Journal/Newspaper
Language:English
Published: AGU 2020
Subjects:
Online Access:https://hdl.handle.net/1956/23694
https://doi.org/10.1029/2018jc014774
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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
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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)
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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
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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