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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Bibliographic Details
Main Author: Wiegand, Kevin Niklas
Format: Text
Language:English
Published: "Staats- und Universitätsbibliothek (SuUB) Bremen" 2023
Subjects:
Online Access:https://dx.doi.org/10.26092/elib/2725
https://media.suub.uni-bremen.de/handle/elib/7502
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author Wiegand, Kevin Niklas
author_facet Wiegand, Kevin Niklas
author_sort Wiegand, Kevin Niklas
collection Unknown
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 Text
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
geographic Greenland
Irminger Sea
geographic_facet Greenland
Irminger Sea
id ftdatacite:10.26092/elib/2725
institution Open Polar
language English
long_lat ENVELOPE(-34.041,-34.041,63.054,63.054)
op_collection_id ftdatacite
op_doi https://doi.org/10.26092/elib/2725
publishDate 2023
publisher "Staats- und Universitätsbibliothek (SuUB) Bremen"
record_format openpolar
spelling ftdatacite:10.26092/elib/2725 2025-06-15T14:28:23+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 "Staats- und Universitätsbibliothek (SuUB) Bremen" oceanography hydrography water masses Irminger Water Irminger Sea Labrador Sea physical mechanisms observations models seasonality convection ScholarlyArticle article-journal Text 2023 ftdatacite https://doi.org/10.26092/elib/2725 2025-06-02T13:03:14Z 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 ... Text Greenland Labrador Sea north atlantic current North Atlantic North Atlantic oscillation Unknown Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054)
spellingShingle oceanography
hydrography
water masses
Irminger Water
Irminger Sea
Labrador Sea
physical mechanisms
observations
models
seasonality
convection
Wiegand, Kevin Niklas
Characteristics and causes of Irminger Water variability in the subpolar North Atlantic between 1993 and 2022 ...
title 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_short 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 ...
topic oceanography
hydrography
water masses
Irminger Water
Irminger Sea
Labrador Sea
physical mechanisms
observations
models
seasonality
convection
topic_facet oceanography
hydrography
water masses
Irminger Water
Irminger Sea
Labrador Sea
physical mechanisms
observations
models
seasonality
convection
url https://dx.doi.org/10.26092/elib/2725
https://media.suub.uni-bremen.de/handle/elib/7502