Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone

WSDW, water mass spreading, numerical model, lagrangian trajectories, Weddell Scotia Confluence. - The deep Scotia Sea is filled with ventilated Weddell Sea Deep Water (WSDW). This in turn is an essential contributor to the ventilation of the World Ocean abyss. A primitive equation, hydrostatic, oce...

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Main Author: Schodlok, Michael P
Format: Text
Language:German
Published: Univ. Bremen 2002
Subjects:
Online Access:https://dx.doi.org/10.23689/fidgeo-433
https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-3241-4
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author Schodlok, Michael P
author_facet Schodlok, Michael P
author_sort Schodlok, Michael P
collection DataCite
description WSDW, water mass spreading, numerical model, lagrangian trajectories, Weddell Scotia Confluence. - The deep Scotia Sea is filled with ventilated Weddell Sea Deep Water (WSDW). This in turn is an essential contributor to the ventilation of the World Ocean abyss. A primitive equation, hydrostatic, ocean general circulation model (BRIOS1.1) with terrain-following coordinate is used to investigate the water mass export from the Weddell Sea. The model is circumpolar focusing on the Weddell Sea, with particularly high resolution (2̃0 km) in the DOVETAIL area. The northern limb of the Weddell Gyre exhibits an eastward Weddell Sea Deep Water transport across 44ʿW of 24 Sv. Export rates of Weddell Sea Deep Water through gaps in theSouth Scotia Ridge are estimated to be 6.4 Sv with a semi-annual cycle of ± 0.6 Sv, which can be correlated to atmospheric cyclone activity and Weddell Gyre strength. Sensitivity studies considering extreme sea ice conditions in the Weddell Sea show higher (lower) exports in years of minimum (maximum) winter sea ice extent. This can be attributed to the local change of the surface stress achieved by wind and ice. Lagrangian ... : thesis
format Text
genre Scotia Sea
Sea ice
Weddell Sea
genre_facet Scotia Sea
Sea ice
Weddell Sea
geographic Scotia Sea
Weddell
Weddell Sea
geographic_facet Scotia Sea
Weddell
Weddell Sea
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institution Open Polar
language German
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op_doi https://doi.org/10.23689/fidgeo-433
publishDate 2002
publisher Univ. Bremen
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spelling ftdatacite:10.23689/fidgeo-433 2025-01-17T00:41:35+00:00 Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone Schodlok, Michael P 2002 https://dx.doi.org/10.23689/fidgeo-433 https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-3241-4 de ger Univ. Bremen Text book Book 2002 ftdatacite https://doi.org/10.23689/fidgeo-433 2021-11-05T12:55:41Z WSDW, water mass spreading, numerical model, lagrangian trajectories, Weddell Scotia Confluence. - The deep Scotia Sea is filled with ventilated Weddell Sea Deep Water (WSDW). This in turn is an essential contributor to the ventilation of the World Ocean abyss. A primitive equation, hydrostatic, ocean general circulation model (BRIOS1.1) with terrain-following coordinate is used to investigate the water mass export from the Weddell Sea. The model is circumpolar focusing on the Weddell Sea, with particularly high resolution (2̃0 km) in the DOVETAIL area. The northern limb of the Weddell Gyre exhibits an eastward Weddell Sea Deep Water transport across 44ʿW of 24 Sv. Export rates of Weddell Sea Deep Water through gaps in theSouth Scotia Ridge are estimated to be 6.4 Sv with a semi-annual cycle of ± 0.6 Sv, which can be correlated to atmospheric cyclone activity and Weddell Gyre strength. Sensitivity studies considering extreme sea ice conditions in the Weddell Sea show higher (lower) exports in years of minimum (maximum) winter sea ice extent. This can be attributed to the local change of the surface stress achieved by wind and ice. Lagrangian ... : thesis Text Scotia Sea Sea ice Weddell Sea DataCite Scotia Sea Weddell Weddell Sea
spellingShingle Schodlok, Michael P
Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
title Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
title_full Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
title_fullStr Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
title_full_unstemmed Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
title_short Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
title_sort über die tiefenwasserausbreitung im weddellmeer und in der scotia-see : numerische untersuchungen der transport- und austauschprozesse in der weddell-scotia-konfluenz-zone
url https://dx.doi.org/10.23689/fidgeo-433
https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-3241-4