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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Autor*in:	Schodlok, Michael P [verfasserIn]
Hochschulschrift:	Bremen, Univ., Diss, 2002

Format:	E-Book
Sprache:	Deutsch

Erschienen:	2002

Schlagwörter:	Weddellmeer / Tiefenwasser / Meeresströmung / Scotia Sea
Formangabe:	Hochschulschrift

Umfang:	Online-Ressource (142 S., 8136 KB)

Links:	Link aufrufen Volltext Volltext Volltext

Katalog-ID:	358564107

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Indexfelder

author_variant	m p s mp mps
matchkey_str	schodlokmichaelp:2002----:edeifnasrubetniwdeler
oclc_num	175067365
hierarchy_sort_str	2002
bklnumber	74.28 38.90
publishDate	2002
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language	German
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topic_facet	Weddellmeer Tiefenwasser Meeresströmung Scotia Sea
hochschulschrift_txt_mv	Bremen, Univ., Diss, 2002
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authorswithroles_txt_mv	Schodlok, Michael P @@aut@@
publishDateDaySort_date	2002-01-01T00:00:00Z
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author	Schodlok, Michael P
spellingShingle	Schodlok, Michael P sdnb 31 bkl 74.28 bkl 38.90 gnd Weddellmeer gnd Tiefenwasser gnd Meeresströmung gnd Scotia Sea Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
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topic_title	31 sdnb 74.28 bkl 38.90 bkl Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone vorgelegt von Michael P. Schodlok g (DE-588)4064942-8 (DE-627)106121391 (DE-576)209155965 Weddellmeer gnd s (DE-588)4140904-8 (DE-627)105624411 (DE-576)209706821 Tiefenwasser gnd s (DE-588)4130725-2 (DE-627)105700347 (DE-576)209621419 Meeresströmung gnd g (DE-588)4339867-4 (DE-627)15270468X (DE-576)21140862X Scotia Sea gnd DE-101
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title	Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
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title_full	Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone vorgelegt von Michael P. Schodlok
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author-letter	Schodlok, Michael P
title_sub	numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
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title_sort	über die tiefenwasserausbreitung im weddellmeer und in der scotia-seenumerische untersuchungen der transport- und austauschprozesse in der weddell-scotia-konfluenz-zone
title_auth	Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone
abstract	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 ...
abstractGer	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 ...
abstract_unstemmed	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 ...
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title_short	Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See
url	http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000003051 http://webdoc.sub.gwdg.de/ebook/diss/2003/sub-bremen/dissertations/E-Diss305_schodlok.pdf http://d-nb.info/965560457
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GND_str_mv	Hochschulschrift Weddellmeer Tiefengrundwasser Tiefes Grundwasser Tiefenwasser Meeresströmungen Meereszirkulation Meer / Strömung Meeresströmung Südantillenmeer Scotia-See Scotiameer Scotiasee Scotia Sea
GND_txt_mv	Hochschulschrift Weddellmeer Tiefengrundwasser Tiefes Grundwasser Tiefenwasser Meeresströmungen Meereszirkulation Meer / Strömung Meeresströmung Südantillenmeer Scotia-See Scotiameer Scotiasee Scotia Sea
GND_txtF_mv	Hochschulschrift Weddellmeer Tiefengrundwasser Tiefes Grundwasser Tiefenwasser Meeresströmungen Meereszirkulation Meer / Strömung Meeresströmung Südantillenmeer Scotia-See Scotiameer Scotiasee Scotia Sea
mediatype_str_mv	c
isOA_txt	false
hochschulschrift_bool	true
up_date	2024-07-04T22:50:50.015Z
_version_	1803690652487122944
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Über die Tiefenwasserausbreitung im Weddellmeer und in der Scotia-See : numerische Untersuchungen der Transport- und Austauschprozesse in der Weddell-Scotia-Konfluenz-Zone

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