Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation
Trabajo presentado en la EGU General Assemby 2014, celebrada del 27 de abril al 2 de mayo de 2014 en Viena (Austria) Prevailing winds over the North Atlantic (NA) have a direct influence on the location and intensity of the Gulf Stream (GS) by the transfer of momentum between atmosphere and ocean. T...
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ftcsic:oai:digital.csic.es:10261/123198 2024-02-11T10:06:13+01:00 Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation Watelet, Sylvain Beckers, Jean-Marie Barth, Alexander Ouberdous, Mohamed Troupin, Charles 2014-04-28 http://hdl.handle.net/10261/123198 en eng European Geosciences Union Publisher's version Sí EGU General Assembly 2014. Geophysical Research Abstracts, 16: EGU2014-8469 (2014) http://hdl.handle.net/10261/123198 open comunicación de congreso http://purl.org/coar/resource_type/c_5794 2014 ftcsic 2024-01-16T10:11:03Z Trabajo presentado en la EGU General Assemby 2014, celebrada del 27 de abril al 2 de mayo de 2014 en Viena (Austria) Prevailing winds over the North Atlantic (NA) have a direct influence on the location and intensity of the Gulf Stream (GS) by the transfer of momentum between atmosphere and ocean. Therefore, the study of interannual variability of the GS requires the identification of sources of variability within the atmospheric circulation. Various studies have highlighted the impact of the North Atlantic Oscillation (NAO) on the variability of the GS transport. However, there is still no scientific consensus thereupon. On the one hand, several scientific papers (Sato & Rossby, 1995; Curry & McCartney, 2001; deCoëtlogon et al., 2006) exhibit a decrease of the GS transport during low NAO periods, as well as a higher transport during high NAO phases. On the second hand, studies of Gangopadhyay et al. (1992), Baringer & Larsen (2001) and DiNezio et al. (2009) suggest a lower transport during positive phases of the NAO. Finally, Chaudhuri et al. (2011) obtained a more complex conclusion, whereby the influence of the NAO is different upstream and downstream of Cape Hatteras. This currently limited understanding of the links between the NAO and the GS in NA, impels us to further analyze the spatial and temporal distribution of the GS. Our main purpose in this study is to reconstruct a spatially continuous field of ocean (sub)surface circulation in the NA from in situ time series of discrete steps, in order to accurately quantify the position and intensity of the GS since 1900. From there, we will be able to examine the correlation of this current with the NAO. To this end, we used the DIVA (Data-Interpolating Variational Analysis) tool, which is a numerical implementation of the variational inverse method (VIM) using the finite elements method to reconstruct continuous fields from discrete measurements. These measurements of temperature, salinity and currents since the beginning of the last century ... Conference Object North Atlantic North Atlantic oscillation Digital.CSIC (Spanish National Research Council) |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
description |
Trabajo presentado en la EGU General Assemby 2014, celebrada del 27 de abril al 2 de mayo de 2014 en Viena (Austria) Prevailing winds over the North Atlantic (NA) have a direct influence on the location and intensity of the Gulf Stream (GS) by the transfer of momentum between atmosphere and ocean. Therefore, the study of interannual variability of the GS requires the identification of sources of variability within the atmospheric circulation. Various studies have highlighted the impact of the North Atlantic Oscillation (NAO) on the variability of the GS transport. However, there is still no scientific consensus thereupon. On the one hand, several scientific papers (Sato & Rossby, 1995; Curry & McCartney, 2001; deCoëtlogon et al., 2006) exhibit a decrease of the GS transport during low NAO periods, as well as a higher transport during high NAO phases. On the second hand, studies of Gangopadhyay et al. (1992), Baringer & Larsen (2001) and DiNezio et al. (2009) suggest a lower transport during positive phases of the NAO. Finally, Chaudhuri et al. (2011) obtained a more complex conclusion, whereby the influence of the NAO is different upstream and downstream of Cape Hatteras. This currently limited understanding of the links between the NAO and the GS in NA, impels us to further analyze the spatial and temporal distribution of the GS. Our main purpose in this study is to reconstruct a spatially continuous field of ocean (sub)surface circulation in the NA from in situ time series of discrete steps, in order to accurately quantify the position and intensity of the GS since 1900. From there, we will be able to examine the correlation of this current with the NAO. To this end, we used the DIVA (Data-Interpolating Variational Analysis) tool, which is a numerical implementation of the variational inverse method (VIM) using the finite elements method to reconstruct continuous fields from discrete measurements. These measurements of temperature, salinity and currents since the beginning of the last century ... |
format |
Conference Object |
author |
Watelet, Sylvain Beckers, Jean-Marie Barth, Alexander Ouberdous, Mohamed Troupin, Charles |
spellingShingle |
Watelet, Sylvain Beckers, Jean-Marie Barth, Alexander Ouberdous, Mohamed Troupin, Charles Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation |
author_facet |
Watelet, Sylvain Beckers, Jean-Marie Barth, Alexander Ouberdous, Mohamed Troupin, Charles |
author_sort |
Watelet, Sylvain |
title |
Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation |
title_short |
Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation |
title_full |
Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation |
title_fullStr |
Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation |
title_full_unstemmed |
Reconstruction of the Gulf Stream since 1900 and correlation with the North Atlantic Oscillation |
title_sort |
reconstruction of the gulf stream since 1900 and correlation with the north atlantic oscillation |
publisher |
European Geosciences Union |
publishDate |
2014 |
url |
http://hdl.handle.net/10261/123198 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
Publisher's version Sí EGU General Assembly 2014. Geophysical Research Abstracts, 16: EGU2014-8469 (2014) http://hdl.handle.net/10261/123198 |
op_rights |
open |
_version_ |
1790603795955187712 |