Mechanisms of Ocean Heat Anomalies in the Norwegian Sea

Ocean heat content in the Norwegian Sea exhibits pronounced variability on interannual to decadal time scales. These ocean heat anomalies are known to influence Arctic sea ice extent, marine ecosystems, and continental climate. It nevertheless remains unknown to what extent such heat anomalies are p...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Asbjørnsen, Helene, Årthun, Marius, Skagseth, Øystein, Eldevik, Tor
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2019
Subjects:
Online Access:https://hdl.handle.net/1956/20665
https://doi.org/10.1029/2018jc014649
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spelling ftunivbergen:oai:bora.uib.no:1956/20665 2023-05-15T15:09:36+02:00 Mechanisms of Ocean Heat Anomalies in the Norwegian Sea Asbjørnsen, Helene Årthun, Marius Skagseth, Øystein Eldevik, Tor 2019-06-12T12:16:37Z application/pdf https://hdl.handle.net/1956/20665 https://doi.org/10.1029/2018jc014649 eng eng Wiley Norges forskningsråd: 263223 Trond Mohn stiftelse: BFS2018TMT01 EC/H2020: 727852 urn:issn:2169-9291 urn:issn:2169-9275 https://hdl.handle.net/1956/20665 https://doi.org/10.1029/2018jc014649 cristin:1702862 Attribution-Non Commercial-No Derivatives CC BY-NC-ND http://creativecommons.org/licenses/by-nc-nd/4.0/ Copyright 2019 The Authors Journal of Geophysical Research - Oceans Peer reviewed Journal article 2019 ftunivbergen https://doi.org/10.1029/2018jc014649 2023-03-14T17:43:32Z Ocean heat content in the Norwegian Sea exhibits pronounced variability on interannual to decadal time scales. These ocean heat anomalies are known to influence Arctic sea ice extent, marine ecosystems, and continental climate. It nevertheless remains unknown to what extent such heat anomalies are produced locally within the Norwegian Sea, and to what extent the region is more of a passive receiver of anomalies formed elsewhere. A main practical challenge has been the lack of closed heat budget diagnostics. In order to address this issue, a regional heat budget is calculated for the Norwegian Sea using the ECCOv4 ocean state estimate—a dynamically and kinematically consistent model framework fitted to ocean observations for the period 1992–2015. The depth‐integrated Norwegian Sea heat budget shows that both ocean advection and air‐sea heat fluxes play an active role in the formation of interannual heat content anomalies. A spatial analysis of the individual heat budget terms shows that ocean advection is the primary contributor to heat content variability in the Atlantic domain of the Norwegian Sea. Anomalous heat advection furthermore depends on the strength of the Atlantic water inflow, which is related to large‐scale circulation changes in the subpolar North Atlantic. This result suggests a potential for predicting Norwegian Sea heat content based on upstream conditions. However, local surface forcing (air‐sea heat fluxes and Ekman forcing) within the Norwegian Sea substantially modifies the phase and amplitude of ocean heat anomalies along their poleward pathway, and, hence, acts to limit predictability. publishedVersion Article in Journal/Newspaper Arctic North Atlantic Norwegian Sea Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Norwegian Sea Journal of Geophysical Research: Oceans 124 4 2908 2923
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description Ocean heat content in the Norwegian Sea exhibits pronounced variability on interannual to decadal time scales. These ocean heat anomalies are known to influence Arctic sea ice extent, marine ecosystems, and continental climate. It nevertheless remains unknown to what extent such heat anomalies are produced locally within the Norwegian Sea, and to what extent the region is more of a passive receiver of anomalies formed elsewhere. A main practical challenge has been the lack of closed heat budget diagnostics. In order to address this issue, a regional heat budget is calculated for the Norwegian Sea using the ECCOv4 ocean state estimate—a dynamically and kinematically consistent model framework fitted to ocean observations for the period 1992–2015. The depth‐integrated Norwegian Sea heat budget shows that both ocean advection and air‐sea heat fluxes play an active role in the formation of interannual heat content anomalies. A spatial analysis of the individual heat budget terms shows that ocean advection is the primary contributor to heat content variability in the Atlantic domain of the Norwegian Sea. Anomalous heat advection furthermore depends on the strength of the Atlantic water inflow, which is related to large‐scale circulation changes in the subpolar North Atlantic. This result suggests a potential for predicting Norwegian Sea heat content based on upstream conditions. However, local surface forcing (air‐sea heat fluxes and Ekman forcing) within the Norwegian Sea substantially modifies the phase and amplitude of ocean heat anomalies along their poleward pathway, and, hence, acts to limit predictability. publishedVersion
format Article in Journal/Newspaper
author Asbjørnsen, Helene
Årthun, Marius
Skagseth, Øystein
Eldevik, Tor
spellingShingle Asbjørnsen, Helene
Årthun, Marius
Skagseth, Øystein
Eldevik, Tor
Mechanisms of Ocean Heat Anomalies in the Norwegian Sea
author_facet Asbjørnsen, Helene
Årthun, Marius
Skagseth, Øystein
Eldevik, Tor
author_sort Asbjørnsen, Helene
title Mechanisms of Ocean Heat Anomalies in the Norwegian Sea
title_short Mechanisms of Ocean Heat Anomalies in the Norwegian Sea
title_full Mechanisms of Ocean Heat Anomalies in the Norwegian Sea
title_fullStr Mechanisms of Ocean Heat Anomalies in the Norwegian Sea
title_full_unstemmed Mechanisms of Ocean Heat Anomalies in the Norwegian Sea
title_sort mechanisms of ocean heat anomalies in the norwegian sea
publisher Wiley
publishDate 2019
url https://hdl.handle.net/1956/20665
https://doi.org/10.1029/2018jc014649
geographic Arctic
Norwegian Sea
geographic_facet Arctic
Norwegian Sea
genre Arctic
North Atlantic
Norwegian Sea
Sea ice
genre_facet Arctic
North Atlantic
Norwegian Sea
Sea ice
op_source Journal of Geophysical Research - Oceans
op_relation Norges forskningsråd: 263223
Trond Mohn stiftelse: BFS2018TMT01
EC/H2020: 727852
urn:issn:2169-9291
urn:issn:2169-9275
https://hdl.handle.net/1956/20665
https://doi.org/10.1029/2018jc014649
cristin:1702862
op_rights Attribution-Non Commercial-No Derivatives CC BY-NC-ND
http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright 2019 The Authors
op_doi https://doi.org/10.1029/2018jc014649
container_title Journal of Geophysical Research: Oceans
container_volume 124
container_issue 4
container_start_page 2908
op_container_end_page 2923
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