Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik

The ocean and the atmosphere form the components of the climate system of the earth with the highest variability. In both systems, internal processes lead to periodic oscillations of the variables of state. A deeper understanding of the interaction between the ocean and the atmosphere is necessary t...

Full description

Bibliographic Details
Main Author: Rehberg, Maya
Format: Thesis
Language:German
Published: 2018
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/46186/
https://oceanrep.geomar.de/id/eprint/46186/1/Bachelorarbeit_Rehberg_Maya.pdf
_version_ 1821651650043969536
author Rehberg, Maya
author_facet Rehberg, Maya
author_sort Rehberg, Maya
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
description The ocean and the atmosphere form the components of the climate system of the earth with the highest variability. In both systems, internal processes lead to periodic oscillations of the variables of state. A deeper understanding of the interaction between the ocean and the atmosphere is necessary to optimize climate models. This thesis deals with the subdecadal variability of the North Atlantic Oscillation (NAO), and its impact on the potential temperature and the heat content in the Atlantic Ocean. A Singular Spectrum Analysis (SSA) of the wintertime NAO-Index from 1864 to 2017 after Hurrell (2003) results in a subdecadal mode with a periodicity of 8 years, which makes up to 20% of the total variability. In the period from 1900 to 1959, a shorter mode of 6 years is dominating. Lag regressions of the subdecadal mode on horizontal and vertical planes of the potential temperature reveal an impact of the subdecadal mode of the NAO on the depth subtropical and subpolar gyre. This relationship is clearly recognizable when considering only data since 1960. The correlation of the subtropical and subpolar gyre with the N AO has an opposite prefix. Therefore an investigation of a Gyre Index, defined as the difference between the heat contents of the gyres, is performed. The correlation of the subdecadal mode of the NAO with the ocean heat content of the subtropical gyre is bigger than the correlation with the Gyre Index. Including the subpolar gyre does not lead to a higher correlation.
format Thesis
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
id ftoceanrep:oai:oceanrep.geomar.de:46186
institution Open Polar
language German
op_collection_id ftoceanrep
op_relation https://oceanrep.geomar.de/id/eprint/46186/1/Bachelorarbeit_Rehberg_Maya.pdf
Rehberg, M. (2018) Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik. (Bachelor thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 40 pp.
op_rights UrhG
info:eu-repo/semantics/restrictedAccess
publishDate 2018
record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:46186 2025-01-16T23:42:58+00:00 Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik Rehberg, Maya 2018 text https://oceanrep.geomar.de/id/eprint/46186/ https://oceanrep.geomar.de/id/eprint/46186/1/Bachelorarbeit_Rehberg_Maya.pdf de ger https://oceanrep.geomar.de/id/eprint/46186/1/Bachelorarbeit_Rehberg_Maya.pdf Rehberg, M. (2018) Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik. (Bachelor thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 40 pp. UrhG info:eu-repo/semantics/restrictedAccess Course of study: BSc Physics of the Earth System Thesis NonPeerReviewed 2018 ftoceanrep 2024-11-13T01:03:56Z The ocean and the atmosphere form the components of the climate system of the earth with the highest variability. In both systems, internal processes lead to periodic oscillations of the variables of state. A deeper understanding of the interaction between the ocean and the atmosphere is necessary to optimize climate models. This thesis deals with the subdecadal variability of the North Atlantic Oscillation (NAO), and its impact on the potential temperature and the heat content in the Atlantic Ocean. A Singular Spectrum Analysis (SSA) of the wintertime NAO-Index from 1864 to 2017 after Hurrell (2003) results in a subdecadal mode with a periodicity of 8 years, which makes up to 20% of the total variability. In the period from 1900 to 1959, a shorter mode of 6 years is dominating. Lag regressions of the subdecadal mode on horizontal and vertical planes of the potential temperature reveal an impact of the subdecadal mode of the NAO on the depth subtropical and subpolar gyre. This relationship is clearly recognizable when considering only data since 1960. The correlation of the subtropical and subpolar gyre with the N AO has an opposite prefix. Therefore an investigation of a Gyre Index, defined as the difference between the heat contents of the gyres, is performed. The correlation of the subdecadal mode of the NAO with the ocean heat content of the subtropical gyre is bigger than the correlation with the Gyre Index. Including the subpolar gyre does not lead to a higher correlation. Thesis North Atlantic North Atlantic oscillation OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
spellingShingle Course of study: BSc Physics of the Earth System
Rehberg, Maya
Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik
title Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik
title_full Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik
title_fullStr Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik
title_full_unstemmed Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik
title_short Einfluss der subdekadischen NAO Variabilität auf die Temperatur im Nordatlantik
title_sort einfluss der subdekadischen nao variabilität auf die temperatur im nordatlantik
topic Course of study: BSc Physics of the Earth System
topic_facet Course of study: BSc Physics of the Earth System
url https://oceanrep.geomar.de/id/eprint/46186/
https://oceanrep.geomar.de/id/eprint/46186/1/Bachelorarbeit_Rehberg_Maya.pdf