Turbulent mixing in a changing Arctic Ocean
The Arctic Ocean has traditionally been thought of as an ocean of low variability and weak turbulent mixing which does not play a significant role in the evolution of water masses. However, with the recent decline in seasonal sea ice cover has led to increased coupling between the atmosphere and oce...
Published in: | Oceanography |
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2022
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Online Access: | https://research.bangor.ac.uk/portal/en/researchoutputs/turbulent-mixing-in-a-changing-arctic-ocean(eca8f564-6de3-4bb7-8831-69dea9ce55b1).html https://research.bangor.ac.uk/ws/files/41346330/35_rippeth.pdf https://doi.org/10.5670/oceanog.2022.103 |
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ftuwalesbangcris:oai:research.bangor.ac.uk:publications/eca8f564-6de3-4bb7-8831-69dea9ce55b1 2024-06-23T07:48:18+00:00 Turbulent mixing in a changing Arctic Ocean Rippeth, Tom Fine, Elizabeth 2022-06 application/pdf https://research.bangor.ac.uk/portal/en/researchoutputs/turbulent-mixing-in-a-changing-arctic-ocean(eca8f564-6de3-4bb7-8831-69dea9ce55b1).html https://research.bangor.ac.uk/ws/files/41346330/35_rippeth.pdf https://doi.org/10.5670/oceanog.2022.103 eng eng https://research.bangor.ac.uk/portal/en/researchoutputs/turbulent-mixing-in-a-changing-arctic-ocean(eca8f564-6de3-4bb7-8831-69dea9ce55b1).html info:eu-repo/semantics/openAccess Rippeth , T & Fine , E 2022 , ' Turbulent mixing in a changing Arctic Ocean ' , Oceanography , vol. 35 , no. 2 . < https://doi.org/10.5670/oceanog.2022.103 > article 2022 ftuwalesbangcris https://doi.org/10.5670/oceanog.2022.103 2024-05-29T23:53:52Z The Arctic Ocean has traditionally been thought of as an ocean of low variability and weak turbulent mixing which does not play a significant role in the evolution of water masses. However, with the recent decline in seasonal sea ice cover has led to increased coupling between the atmosphere and ocean potentially greatly enhancing turbulent mixing (Rainville et al., 2011). Here we review work carried out over the past decade to assess the changing impact of turbulent mixing in an increasingly ice-free Arctic Ocean. We find the evolution of wind generated near-inertial oscillations is highly sensitive to the seasonal cycle in sea ice, but that the response varies greatly between the eastern and western Arctic basins due to differing levels of halocline stratification. There is increasing interest in the role of the tides in driving mixing over sloping topography and of far-field storms via continental shelf waves. Both dissipate through the development of unsteady lee-waves. The role of eddies in transporting shelf water into the basins and in supporting mixing has also come under increased focus as sea ice retreat and technological advances have permitted higher resolution observation. The key role of these processes highlight the need for mixing associated with unsteady lee waves and eddies to be parameterised for inclusion in region ocean models and climate simulations. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Sea ice Bangor University: Research Portal Arctic Arctic Ocean Oceanography |
institution |
Open Polar |
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Bangor University: Research Portal |
op_collection_id |
ftuwalesbangcris |
language |
English |
description |
The Arctic Ocean has traditionally been thought of as an ocean of low variability and weak turbulent mixing which does not play a significant role in the evolution of water masses. However, with the recent decline in seasonal sea ice cover has led to increased coupling between the atmosphere and ocean potentially greatly enhancing turbulent mixing (Rainville et al., 2011). Here we review work carried out over the past decade to assess the changing impact of turbulent mixing in an increasingly ice-free Arctic Ocean. We find the evolution of wind generated near-inertial oscillations is highly sensitive to the seasonal cycle in sea ice, but that the response varies greatly between the eastern and western Arctic basins due to differing levels of halocline stratification. There is increasing interest in the role of the tides in driving mixing over sloping topography and of far-field storms via continental shelf waves. Both dissipate through the development of unsteady lee-waves. The role of eddies in transporting shelf water into the basins and in supporting mixing has also come under increased focus as sea ice retreat and technological advances have permitted higher resolution observation. The key role of these processes highlight the need for mixing associated with unsteady lee waves and eddies to be parameterised for inclusion in region ocean models and climate simulations. |
format |
Article in Journal/Newspaper |
author |
Rippeth, Tom Fine, Elizabeth |
spellingShingle |
Rippeth, Tom Fine, Elizabeth Turbulent mixing in a changing Arctic Ocean |
author_facet |
Rippeth, Tom Fine, Elizabeth |
author_sort |
Rippeth, Tom |
title |
Turbulent mixing in a changing Arctic Ocean |
title_short |
Turbulent mixing in a changing Arctic Ocean |
title_full |
Turbulent mixing in a changing Arctic Ocean |
title_fullStr |
Turbulent mixing in a changing Arctic Ocean |
title_full_unstemmed |
Turbulent mixing in a changing Arctic Ocean |
title_sort |
turbulent mixing in a changing arctic ocean |
publishDate |
2022 |
url |
https://research.bangor.ac.uk/portal/en/researchoutputs/turbulent-mixing-in-a-changing-arctic-ocean(eca8f564-6de3-4bb7-8831-69dea9ce55b1).html https://research.bangor.ac.uk/ws/files/41346330/35_rippeth.pdf https://doi.org/10.5670/oceanog.2022.103 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Arctic Ocean Sea ice |
op_source |
Rippeth , T & Fine , E 2022 , ' Turbulent mixing in a changing Arctic Ocean ' , Oceanography , vol. 35 , no. 2 . < https://doi.org/10.5670/oceanog.2022.103 > |
op_relation |
https://research.bangor.ac.uk/portal/en/researchoutputs/turbulent-mixing-in-a-changing-arctic-ocean(eca8f564-6de3-4bb7-8831-69dea9ce55b1).html |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5670/oceanog.2022.103 |
container_title |
Oceanography |
_version_ |
1802638715133100032 |