Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ...
Irminger Water (IW) originates in the subtropical North Atlantic and is transported northeastward with the North Atlantic Current. It is located in the Irminger Sea and the boundary current system (BCS) off Greenland and Labrador. As the warmest and most saline water mass in this region, it impacts...
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Universität Bremen
2023
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Online Access: | https://dx.doi.org/10.26092/elib/2725 https://media.suub.uni-bremen.de/handle/elib/7502 |
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ftdatacite:10.26092/elib/2725 2024-03-31T07:53:03+00:00 Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... Wiegand, Kevin Niklas 2023 https://dx.doi.org/10.26092/elib/2725 https://media.suub.uni-bremen.de/handle/elib/7502 en eng Universität Bremen Creative Commons Attribution 4.0 International CC BY 4.0 (Attribution) https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 oceanography hydrography water masses Irminger Water Irminger Sea Labrador Sea physical mechanisms observations models seasonality convection 530 Other thesis Dissertation Thesis 2023 ftdatacite https://doi.org/10.26092/elib/2725 2024-03-04T13:43:45Z Irminger Water (IW) originates in the subtropical North Atlantic and is transported northeastward with the North Atlantic Current. It is located in the Irminger Sea and the boundary current system (BCS) off Greenland and Labrador. As the warmest and most saline water mass in this region, it impacts glacial melt and convection in the Irminger and Labrador Seas. This thesis focuses on analyzing temporal and spatial variability of IW using the ARMOR3D data set from 1993 to 2022. It adds to analyzing IW in an ocean reanalysis and different model simulations. Utilizing data from ship surveys to the west of Greenland (at eastern AR7W), a local validation of ARMOR3D is performed. Eastern AR7W exhibits IW hydrography and volume transport variability. Seasonal variability results from colder and fresher waters formed during winter convection in the Irminger and Labrador Seas. On multi-year time scales, subpolar gyre changes tied to the North Atlantic Oscillation lead IW volume transports at eastern AR7W by up to ... Thesis Greenland Labrador Sea north atlantic current North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology) Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
oceanography hydrography water masses Irminger Water Irminger Sea Labrador Sea physical mechanisms observations models seasonality convection 530 |
spellingShingle |
oceanography hydrography water masses Irminger Water Irminger Sea Labrador Sea physical mechanisms observations models seasonality convection 530 Wiegand, Kevin Niklas Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... |
topic_facet |
oceanography hydrography water masses Irminger Water Irminger Sea Labrador Sea physical mechanisms observations models seasonality convection 530 |
description |
Irminger Water (IW) originates in the subtropical North Atlantic and is transported northeastward with the North Atlantic Current. It is located in the Irminger Sea and the boundary current system (BCS) off Greenland and Labrador. As the warmest and most saline water mass in this region, it impacts glacial melt and convection in the Irminger and Labrador Seas. This thesis focuses on analyzing temporal and spatial variability of IW using the ARMOR3D data set from 1993 to 2022. It adds to analyzing IW in an ocean reanalysis and different model simulations. Utilizing data from ship surveys to the west of Greenland (at eastern AR7W), a local validation of ARMOR3D is performed. Eastern AR7W exhibits IW hydrography and volume transport variability. Seasonal variability results from colder and fresher waters formed during winter convection in the Irminger and Labrador Seas. On multi-year time scales, subpolar gyre changes tied to the North Atlantic Oscillation lead IW volume transports at eastern AR7W by up to ... |
format |
Thesis |
author |
Wiegand, Kevin Niklas |
author_facet |
Wiegand, Kevin Niklas |
author_sort |
Wiegand, Kevin Niklas |
title |
Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... |
title_short |
Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... |
title_full |
Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... |
title_fullStr |
Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... |
title_full_unstemmed |
Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ... |
title_sort |
characteristics and causes of irminger water variability in the subpolar north atlantic between 1993 and 2022 ... |
publisher |
Universität Bremen |
publishDate |
2023 |
url |
https://dx.doi.org/10.26092/elib/2725 https://media.suub.uni-bremen.de/handle/elib/7502 |
long_lat |
ENVELOPE(-34.041,-34.041,63.054,63.054) |
geographic |
Greenland Irminger Sea |
geographic_facet |
Greenland Irminger Sea |
genre |
Greenland Labrador Sea north atlantic current North Atlantic North Atlantic oscillation |
genre_facet |
Greenland Labrador Sea north atlantic current North Atlantic North Atlantic oscillation |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 (Attribution) https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.26092/elib/2725 |
_version_ |
1795032504707579904 |