Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)

Many studies about the Western Boundary Currents in the subtropical North Atlantic,important components of the Meridional Overturning Circulation and the subtropical gyre, have been made during the last few decades. There is data from direct current measurements and more than 25 years of cable deriv...

Full description

Bibliographic Details
Main Author: Müller, Katharina
Format: Thesis
Language:English
Published: 2010
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/11443/
https://oceanrep.geomar.de/id/eprint/11443/1/M%C3%BCller.pdf
id ftoceanrep:oai:oceanrep.geomar.de:11443
record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:11443 2023-05-15T17:30:22+02:00 Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025) Müller, Katharina 2010 text https://oceanrep.geomar.de/id/eprint/11443/ https://oceanrep.geomar.de/id/eprint/11443/1/M%C3%BCller.pdf en eng https://oceanrep.geomar.de/id/eprint/11443/1/M%C3%BCller.pdf Müller, K. (2010) Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025). (Bachelor thesis), Christian-Albrechts-Universität, Kiel, Germany, 25 pp. Course of study: BSc Physics of the Earth System Thesis NonPeerReviewed 2010 ftoceanrep 2023-04-07T14:59:28Z Many studies about the Western Boundary Currents in the subtropical North Atlantic,important components of the Meridional Overturning Circulation and the subtropical gyre, have been made during the last few decades. There is data from direct current measurements and more than 25 years of cable derived data. In this work the structure of the Western Boundary Currents and especially the variability of the Florida Current are examined with the help of a global ocean modell (ORCA025). The determined seasonal cycle is similar to the observed one. There are parallels between the cable data and the model-output on decadal timescales. Both show an increase in transport during the 1990s. The local windfield can be varified as the main cause of the seasonal cycle. However, such an influence seem to decrease on longer timescales. Substantial changes in the seasonal cycle can not be detected. On decadal timescales there may be a coherence between the NAO and the Florida Current transport, which can either be explained with the connection to the MOC, or maybe with the wind stress curl over the subtropical North Atlantic. Thesis North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Curl ENVELOPE(-63.071,-63.071,-70.797,-70.797)
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
topic Course of study: BSc Physics of the Earth System
spellingShingle Course of study: BSc Physics of the Earth System
Müller, Katharina
Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)
topic_facet Course of study: BSc Physics of the Earth System
description Many studies about the Western Boundary Currents in the subtropical North Atlantic,important components of the Meridional Overturning Circulation and the subtropical gyre, have been made during the last few decades. There is data from direct current measurements and more than 25 years of cable derived data. In this work the structure of the Western Boundary Currents and especially the variability of the Florida Current are examined with the help of a global ocean modell (ORCA025). The determined seasonal cycle is similar to the observed one. There are parallels between the cable data and the model-output on decadal timescales. Both show an increase in transport during the 1990s. The local windfield can be varified as the main cause of the seasonal cycle. However, such an influence seem to decrease on longer timescales. Substantial changes in the seasonal cycle can not be detected. On decadal timescales there may be a coherence between the NAO and the Florida Current transport, which can either be explained with the connection to the MOC, or maybe with the wind stress curl over the subtropical North Atlantic.
format Thesis
author Müller, Katharina
author_facet Müller, Katharina
author_sort Müller, Katharina
title Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)
title_short Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)
title_full Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)
title_fullStr Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)
title_full_unstemmed Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025)
title_sort struktur und variabilität des westlichen randstromsystems im subtropischen nordatlantik: analyse eines globalen ozeanmodells (orca025)
publishDate 2010
url https://oceanrep.geomar.de/id/eprint/11443/
https://oceanrep.geomar.de/id/eprint/11443/1/M%C3%BCller.pdf
long_lat ENVELOPE(-63.071,-63.071,-70.797,-70.797)
geographic Curl
geographic_facet Curl
genre North Atlantic
genre_facet North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/11443/1/M%C3%BCller.pdf
Müller, K. (2010) Struktur und Variabilität des westlichen Randstromsystems im Subtropischen Nordatlantik: Analyse eines globalen Ozeanmodells (ORCA025). (Bachelor thesis), Christian-Albrechts-Universität, Kiel, Germany, 25 pp.
_version_ 1766126739256246272