Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea
A freshening of the boundary current (Labrador current and West Greenland Current) supresses deep convection in the Labrador Sea. Furthermore, the fresher water contributes to the ``strength'' of Irminger Rings and increases their life time. This leads to a larger spread of high EKE into t...
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fttudelft:oai:tudelft.nl:uuid:b87b632c-1359-45e1-8167-de9dfee84bfa 2023-07-30T04:03:49+02:00 Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea van Dam, Tim (author) Katsman, C.A. (mentor) de Roode, S.R. (mentor) Georgiou, S. (mentor) Delft University of Technology (degree granting institution) 2018-07-06 http://resolver.tudelft.nl/uuid:b87b632c-1359-45e1-8167-de9dfee84bfa en eng http://resolver.tudelft.nl/uuid:b87b632c-1359-45e1-8167-de9dfee84bfa © 2018 Tim van Dam convection Labrador sea MLD EKE GSA Irminger IR student report 2018 fttudelft 2023-07-08T20:19:33Z A freshening of the boundary current (Labrador current and West Greenland Current) supresses deep convection in the Labrador Sea. Furthermore, the fresher water contributes to the ``strength'' of Irminger Rings and increases their life time. This leads to a larger spread of high EKE into the interior of the Labrador Sea and confines the deep convection region more towards the west. VIDI Additional thesis Other/Unknown Material Greenland Labrador Sea Delft University of Technology: Institutional Repository Greenland |
institution |
Open Polar |
collection |
Delft University of Technology: Institutional Repository |
op_collection_id |
fttudelft |
language |
English |
topic |
convection Labrador sea MLD EKE GSA Irminger IR |
spellingShingle |
convection Labrador sea MLD EKE GSA Irminger IR van Dam, Tim (author) Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea |
topic_facet |
convection Labrador sea MLD EKE GSA Irminger IR |
description |
A freshening of the boundary current (Labrador current and West Greenland Current) supresses deep convection in the Labrador Sea. Furthermore, the fresher water contributes to the ``strength'' of Irminger Rings and increases their life time. This leads to a larger spread of high EKE into the interior of the Labrador Sea and confines the deep convection region more towards the west. VIDI Additional thesis |
author2 |
Katsman, C.A. (mentor) de Roode, S.R. (mentor) Georgiou, S. (mentor) Delft University of Technology (degree granting institution) |
format |
Other/Unknown Material |
author |
van Dam, Tim (author) |
author_facet |
van Dam, Tim (author) |
author_sort |
van Dam, Tim (author) |
title |
Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea |
title_short |
Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea |
title_full |
Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea |
title_fullStr |
Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea |
title_full_unstemmed |
Effects of a Freshening Boundary Currenton on Deep Convection and Eddy Activity in the Labrador Sea |
title_sort |
effects of a freshening boundary currenton on deep convection and eddy activity in the labrador sea |
publishDate |
2018 |
url |
http://resolver.tudelft.nl/uuid:b87b632c-1359-45e1-8167-de9dfee84bfa |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Labrador Sea |
genre_facet |
Greenland Labrador Sea |
op_relation |
http://resolver.tudelft.nl/uuid:b87b632c-1359-45e1-8167-de9dfee84bfa |
op_rights |
© 2018 Tim van Dam |
_version_ |
1772814937824952320 |