Vortices in the Subarctic Seas and their interactions with bottom topography
Coherent swirling bodies of water; mesoscale (10-100 km) vortices, are an essential part of the general ocean circulation. Mesoscale vortices are abundant everywhere in the World Ocean and are vital in upholding equilibrium balances that govern the global circulation and thus also the climate. In or...
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ftoslouniv:oai:www.duo.uio.no:10852/96620 2023-05-15T17:08:18+02:00 Vortices in the Subarctic Seas and their interactions with bottom topography Trodahl, Marta 2022 http://hdl.handle.net/10852/96620 en eng Paper I: Marta Trodahl and Pål Erik Isachsen, (2018), "Topographic influence on baroclinic instability and the mesoscale eddy field in the northern North Atlantic Ocean and the Nordic Seas", Journal of Physical Oceanography. doi:10.1175/JPO-D-17-0220.1, 2018. The article is included in the thesis. Also available at: https://doi.org/10.1175/JPO-D-17-0220.1 Paper II: Marta Trodahl, Pål Erik Isachsen, Jonathan M. Lilly, Johan Nilsson, and Nils Melsom Kristensen, (2020), "The regeneration of the Lofoten Vortex through vertical alignment", Journal of Physical Oceanography. doi:10.1175/JPO-D-20-0029.1, 2020. The article is included in the thesis. Also available at: https://doi.org/10.1175/JPO-D-20-0029.1 Paper III: Marta Trodahl, LaCasce, J. H, (submitted: May 2022), "Stable surface anticyclones in basins", Journal of Physical Oceanography. To be published. The paper is not available in DUO awaiting publishing. https://doi.org/10.1175/JPO-D-17-0220.1 https://doi.org/10.1175/JPO-D-20-0029.1 http://hdl.handle.net/10852/96620 Doctoral thesis Doktoravhandling 2022 ftoslouniv https://doi.org/10.1175/JPO-D-17-0220.1 https://doi.org/10.1175/JPO-D-20-0029.1 2022-09-21T22:35:33Z Coherent swirling bodies of water; mesoscale (10-100 km) vortices, are an essential part of the general ocean circulation. Mesoscale vortices are abundant everywhere in the World Ocean and are vital in upholding equilibrium balances that govern the global circulation and thus also the climate. In order to obtain a better understanding of the general circulation in the global ocean, there is a need of more insight into vortex life cycles and impacts, such as their formation, spatial structure, distribution, and interactions with neighboring vortices and with the ambient environment. Gaining more knowledge of the mesoscale vortex field is not only crucial for our present-day understanding of the circulation, but also for future predictions of climate. Studying the mesoscale vortex field is challenging in the polar regions since vortex length scales significantly decrease with latitude. The small length scales make them both harder to observe and to model. In this thesis, simplified theory and idealized and realistic high-resolution modeling is combined to gain insight the mesoscale vortex field in a climate-sensitive high latitude region, namely the Subarctic Seas. A unique, long-lived high pressure system situated in the Lofoten Basin is specifically examined. How this storm has kept intact for perhaps over 100 years has been puzzling, and this thesis shows a direct link to the process responsible for its regeneration. Doctoral or Postdoctoral Thesis Lofoten Subarctic Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Lofoten Lofoten Basin ENVELOPE(4.000,4.000,70.000,70.000) Journal of Physical Oceanography 48 11 2593 2607 |
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Open Polar |
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Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
op_collection_id |
ftoslouniv |
language |
English |
description |
Coherent swirling bodies of water; mesoscale (10-100 km) vortices, are an essential part of the general ocean circulation. Mesoscale vortices are abundant everywhere in the World Ocean and are vital in upholding equilibrium balances that govern the global circulation and thus also the climate. In order to obtain a better understanding of the general circulation in the global ocean, there is a need of more insight into vortex life cycles and impacts, such as their formation, spatial structure, distribution, and interactions with neighboring vortices and with the ambient environment. Gaining more knowledge of the mesoscale vortex field is not only crucial for our present-day understanding of the circulation, but also for future predictions of climate. Studying the mesoscale vortex field is challenging in the polar regions since vortex length scales significantly decrease with latitude. The small length scales make them both harder to observe and to model. In this thesis, simplified theory and idealized and realistic high-resolution modeling is combined to gain insight the mesoscale vortex field in a climate-sensitive high latitude region, namely the Subarctic Seas. A unique, long-lived high pressure system situated in the Lofoten Basin is specifically examined. How this storm has kept intact for perhaps over 100 years has been puzzling, and this thesis shows a direct link to the process responsible for its regeneration. |
format |
Doctoral or Postdoctoral Thesis |
author |
Trodahl, Marta |
spellingShingle |
Trodahl, Marta Vortices in the Subarctic Seas and their interactions with bottom topography |
author_facet |
Trodahl, Marta |
author_sort |
Trodahl, Marta |
title |
Vortices in the Subarctic Seas and their interactions with bottom topography |
title_short |
Vortices in the Subarctic Seas and their interactions with bottom topography |
title_full |
Vortices in the Subarctic Seas and their interactions with bottom topography |
title_fullStr |
Vortices in the Subarctic Seas and their interactions with bottom topography |
title_full_unstemmed |
Vortices in the Subarctic Seas and their interactions with bottom topography |
title_sort |
vortices in the subarctic seas and their interactions with bottom topography |
publishDate |
2022 |
url |
http://hdl.handle.net/10852/96620 |
long_lat |
ENVELOPE(4.000,4.000,70.000,70.000) |
geographic |
Lofoten Lofoten Basin |
geographic_facet |
Lofoten Lofoten Basin |
genre |
Lofoten Subarctic |
genre_facet |
Lofoten Subarctic |
op_relation |
Paper I: Marta Trodahl and Pål Erik Isachsen, (2018), "Topographic influence on baroclinic instability and the mesoscale eddy field in the northern North Atlantic Ocean and the Nordic Seas", Journal of Physical Oceanography. doi:10.1175/JPO-D-17-0220.1, 2018. The article is included in the thesis. Also available at: https://doi.org/10.1175/JPO-D-17-0220.1 Paper II: Marta Trodahl, Pål Erik Isachsen, Jonathan M. Lilly, Johan Nilsson, and Nils Melsom Kristensen, (2020), "The regeneration of the Lofoten Vortex through vertical alignment", Journal of Physical Oceanography. doi:10.1175/JPO-D-20-0029.1, 2020. The article is included in the thesis. Also available at: https://doi.org/10.1175/JPO-D-20-0029.1 Paper III: Marta Trodahl, LaCasce, J. H, (submitted: May 2022), "Stable surface anticyclones in basins", Journal of Physical Oceanography. To be published. The paper is not available in DUO awaiting publishing. https://doi.org/10.1175/JPO-D-17-0220.1 https://doi.org/10.1175/JPO-D-20-0029.1 http://hdl.handle.net/10852/96620 |
op_doi |
https://doi.org/10.1175/JPO-D-17-0220.1 https://doi.org/10.1175/JPO-D-20-0029.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
48 |
container_issue |
11 |
container_start_page |
2593 |
op_container_end_page |
2607 |
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1766064027195146240 |