The role of asymmetries in Nordic Seas dynamics
The oceanic transport of heat and salt from the equator northward is one of the main reasons for the mild climate of Europe. This transport occurs in the upper layer of the ocean. In the north, strong cooling occurs due to the large difference in temperature between the ocean surface and the atmosph...
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fttudelft:oai:tudelft.nl:uuid:cbb5165a-7e9f-4416-97e1-010599c75324 2024-02-11T10:04:17+01:00 The role of asymmetries in Nordic Seas dynamics Ypma, S.L. (author) Pietrzak, J.D. (promotor) Katsman, C.A. (copromotor) Delft University of Technology (degree granting institution) 2020-09-30 http://resolver.tudelft.nl/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 https://doi.org/10.4233/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 en eng http://resolver.tudelft.nl/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 https://doi.org/10.4233/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 isbn:978-94-6384-156-6 © 2020 S.L. Ypma doctoral thesis 2020 fttudelft https://doi.org/10.4233/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 2024-01-24T23:31:06Z The oceanic transport of heat and salt from the equator northward is one of the main reasons for the mild climate of Europe. This transport occurs in the upper layer of the ocean. In the north, strong cooling occurs due to the large difference in temperature between the ocean surface and the atmosphere. The cooled watermass has a higher density and therefore sinks and returns toward the south at depth. This so-called AtlanticMeridional Overturning Circulation is driven in part by the wind and in part by the difference in temperature and salinity between the equator and the poles. Polar climate change will result in warmer and fresher oceans whichwill likelyweaken this global overturning circulation. Especially processes that concern the transformation from the light (warm) watermasses to dense (cold) watermasses are sensitive to changes in buoyancy forcing. This thesis focuses on an area where a large part of this transformation from light to dense watermasses takes place; the Nordic Seas. The Nordic Seas are located between Greenland and Norway and consist of several sub-basins, like the Lofoten Basin, the Greenland Basin and the Norwegian Basin. The main aim of this thesis is to better understand the dynamical processes involved in the watermass transformation in the Nordic Seas. Environmental Fluid Mechanics Doctoral or Postdoctoral Thesis Greenland Lofoten Nordic Seas Delft University of Technology: Institutional Repository Greenland Greenland Basin ENVELOPE(-5.000,-5.000,73.500,73.500) Lofoten Lofoten Basin ENVELOPE(4.000,4.000,70.000,70.000) Norway |
institution |
Open Polar |
collection |
Delft University of Technology: Institutional Repository |
op_collection_id |
fttudelft |
language |
English |
description |
The oceanic transport of heat and salt from the equator northward is one of the main reasons for the mild climate of Europe. This transport occurs in the upper layer of the ocean. In the north, strong cooling occurs due to the large difference in temperature between the ocean surface and the atmosphere. The cooled watermass has a higher density and therefore sinks and returns toward the south at depth. This so-called AtlanticMeridional Overturning Circulation is driven in part by the wind and in part by the difference in temperature and salinity between the equator and the poles. Polar climate change will result in warmer and fresher oceans whichwill likelyweaken this global overturning circulation. Especially processes that concern the transformation from the light (warm) watermasses to dense (cold) watermasses are sensitive to changes in buoyancy forcing. This thesis focuses on an area where a large part of this transformation from light to dense watermasses takes place; the Nordic Seas. The Nordic Seas are located between Greenland and Norway and consist of several sub-basins, like the Lofoten Basin, the Greenland Basin and the Norwegian Basin. The main aim of this thesis is to better understand the dynamical processes involved in the watermass transformation in the Nordic Seas. Environmental Fluid Mechanics |
author2 |
Pietrzak, J.D. (promotor) Katsman, C.A. (copromotor) Delft University of Technology (degree granting institution) |
format |
Doctoral or Postdoctoral Thesis |
author |
Ypma, S.L. (author) |
spellingShingle |
Ypma, S.L. (author) The role of asymmetries in Nordic Seas dynamics |
author_facet |
Ypma, S.L. (author) |
author_sort |
Ypma, S.L. (author) |
title |
The role of asymmetries in Nordic Seas dynamics |
title_short |
The role of asymmetries in Nordic Seas dynamics |
title_full |
The role of asymmetries in Nordic Seas dynamics |
title_fullStr |
The role of asymmetries in Nordic Seas dynamics |
title_full_unstemmed |
The role of asymmetries in Nordic Seas dynamics |
title_sort |
role of asymmetries in nordic seas dynamics |
publishDate |
2020 |
url |
http://resolver.tudelft.nl/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 https://doi.org/10.4233/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 |
long_lat |
ENVELOPE(-5.000,-5.000,73.500,73.500) ENVELOPE(4.000,4.000,70.000,70.000) |
geographic |
Greenland Greenland Basin Lofoten Lofoten Basin Norway |
geographic_facet |
Greenland Greenland Basin Lofoten Lofoten Basin Norway |
genre |
Greenland Lofoten Nordic Seas |
genre_facet |
Greenland Lofoten Nordic Seas |
op_relation |
http://resolver.tudelft.nl/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 https://doi.org/10.4233/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 isbn:978-94-6384-156-6 |
op_rights |
© 2020 S.L. Ypma |
op_doi |
https://doi.org/10.4233/uuid:cbb5165a-7e9f-4416-97e1-010599c75324 |
_version_ |
1790600863420514304 |