Evolution of atmospheric connectivity in the 20th century

Arizmendi, Fernando - Barreiro, Marcelo - Martí, Arturo

Resumen:

We aim to study the evolution of the upper atmosphere connectivity over the 20th century as well as to distinguish the oceanically forced component from the atmospheric internal variability. For this purpose we build networks from two different reanalysis data sets using both linear and nonlinear statistical similarity measures to determine the existence of links between different regions of the world in the two halves of the last century. We furthermore use symbolic analysis to emphasize intra-seasonal, intra-annual and inter-annual timescales. Both linear and nonlinear networks have similar structures and evolution, showing that the most connected regions are in the tropics over the Pacific Ocean. Also, the Southern Hemisphere extratropics have more connectivity in the first half of the 20th century, particularly on intra-annual and intra-seasonal timescales. Changes over the Pacific main connectivity regions are analyzed in more detail. Both linear and nonlinear networks show that the central and western Pacific regions have decreasing connectivity from early 1900 up to about 1940, when it starts increasing again until the present. The inter-annual network shows a similar behavior. However, this is not true of other timescales. On intra-annual timescales the minimum connectivity is around 1956, with a negative (positive) trend before (after) that date for both the central and western Pacific. While this is also true of the central Pacific on intra-seasonal timescales, the western Pacific shows a positive trend during the entire 20th century. In order to separate the internal and forced connectivity networks and to study their evolution through time, an ensemble of atmospheric general circulation model outputs is used. The results suggest that the main connectivity patterns captured in the reanalysis networks are due to the oceanically forced component, particularly on inter-annual timescales. Moreover, the atmospheric internal variability seems to play an important role in determining the intra-seasonal timescale networks.


Detalles Bibliográficos
2014
Inglés
Universidad de la República
COLIBRI
https://hdl.handle.net/20.500.12008/34232
Acceso abierto
Licencia Creative Commons Atribución (CC - By 4.0)
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author Arizmendi, Fernando
author2 Barreiro, Marcelo
Martí, Arturo
author2_role author
author
author_facet Arizmendi, Fernando
Barreiro, Marcelo
Martí, Arturo
author_role author
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collection COLIBRI
dc.contributor.filiacion.none.fl_str_mv Arizmendi Fernando, Universidad de la República (Uruguay). Facultad de Ciencias. Instituto de Física.
Barreiro Marcelo, Universidad de la República (Uruguay). Facultad de Ciencias. Instituto de Física.
Martí Arturo, Universidad de la República (Uruguay). Facultad de Ciencias. Instituto de Física.
dc.creator.none.fl_str_mv Arizmendi, Fernando
Barreiro, Marcelo
Martí, Arturo
dc.date.accessioned.none.fl_str_mv 2022-10-18T14:39:35Z
dc.date.available.none.fl_str_mv 2022-10-18T14:39:35Z
dc.date.issued.none.fl_str_mv 2014
dc.description.abstract.none.fl_txt_mv We aim to study the evolution of the upper atmosphere connectivity over the 20th century as well as to distinguish the oceanically forced component from the atmospheric internal variability. For this purpose we build networks from two different reanalysis data sets using both linear and nonlinear statistical similarity measures to determine the existence of links between different regions of the world in the two halves of the last century. We furthermore use symbolic analysis to emphasize intra-seasonal, intra-annual and inter-annual timescales. Both linear and nonlinear networks have similar structures and evolution, showing that the most connected regions are in the tropics over the Pacific Ocean. Also, the Southern Hemisphere extratropics have more connectivity in the first half of the 20th century, particularly on intra-annual and intra-seasonal timescales. Changes over the Pacific main connectivity regions are analyzed in more detail. Both linear and nonlinear networks show that the central and western Pacific regions have decreasing connectivity from early 1900 up to about 1940, when it starts increasing again until the present. The inter-annual network shows a similar behavior. However, this is not true of other timescales. On intra-annual timescales the minimum connectivity is around 1956, with a negative (positive) trend before (after) that date for both the central and western Pacific. While this is also true of the central Pacific on intra-seasonal timescales, the western Pacific shows a positive trend during the entire 20th century. In order to separate the internal and forced connectivity networks and to study their evolution through time, an ensemble of atmospheric general circulation model outputs is used. The results suggest that the main connectivity patterns captured in the reanalysis networks are due to the oceanically forced component, particularly on inter-annual timescales. Moreover, the atmospheric internal variability seems to play an important role in determining the intra-seasonal timescale networks.
dc.format.extent.es.fl_str_mv 15 h
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dc.identifier.citation.es.fl_str_mv Arizmendi, F, Barreiro, M y Martí, A. "Evolution of atmospheric connectivity in the 20th century". Nonlinear Processes in Geophysics. [en línea] 2014, 21(4): 825-839 . 15 h.
dc.identifier.doi.none.fl_str_mv 10.5194/npg-21-825-2014
dc.identifier.issn.none.fl_str_mv 1607-7946
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12008/34232
dc.language.iso.none.fl_str_mv en
eng
dc.publisher.es.fl_str_mv European Geosciences Union
dc.relation.ispartof.es.fl_str_mv Nonlinear Processes in Geophysics, 2014, 21(4): 825-839
dc.rights.license.none.fl_str_mv Licencia Creative Commons Atribución (CC - By 4.0)
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.source.none.fl_str_mv reponame:COLIBRI
instname:Universidad de la República
instacron:Universidad de la República
dc.title.none.fl_str_mv Evolution of atmospheric connectivity in the 20th century
dc.type.es.fl_str_mv Artículo
dc.type.none.fl_str_mv info:eu-repo/semantics/article
dc.type.version.none.fl_str_mv info:eu-repo/semantics/publishedVersion
description We aim to study the evolution of the upper atmosphere connectivity over the 20th century as well as to distinguish the oceanically forced component from the atmospheric internal variability. For this purpose we build networks from two different reanalysis data sets using both linear and nonlinear statistical similarity measures to determine the existence of links between different regions of the world in the two halves of the last century. We furthermore use symbolic analysis to emphasize intra-seasonal, intra-annual and inter-annual timescales. Both linear and nonlinear networks have similar structures and evolution, showing that the most connected regions are in the tropics over the Pacific Ocean. Also, the Southern Hemisphere extratropics have more connectivity in the first half of the 20th century, particularly on intra-annual and intra-seasonal timescales. Changes over the Pacific main connectivity regions are analyzed in more detail. Both linear and nonlinear networks show that the central and western Pacific regions have decreasing connectivity from early 1900 up to about 1940, when it starts increasing again until the present. The inter-annual network shows a similar behavior. However, this is not true of other timescales. On intra-annual timescales the minimum connectivity is around 1956, with a negative (positive) trend before (after) that date for both the central and western Pacific. While this is also true of the central Pacific on intra-seasonal timescales, the western Pacific shows a positive trend during the entire 20th century. In order to separate the internal and forced connectivity networks and to study their evolution through time, an ensemble of atmospheric general circulation model outputs is used. The results suggest that the main connectivity patterns captured in the reanalysis networks are due to the oceanically forced component, particularly on inter-annual timescales. Moreover, the atmospheric internal variability seems to play an important role in determining the intra-seasonal timescale networks.
eu_rights_str_mv openAccess
format article
id COLIBRI_2fec6c070078f1182e084a033807e353
identifier_str_mv Arizmendi, F, Barreiro, M y Martí, A. "Evolution of atmospheric connectivity in the 20th century". Nonlinear Processes in Geophysics. [en línea] 2014, 21(4): 825-839 . 15 h.
1607-7946
10.5194/npg-21-825-2014
instacron_str Universidad de la República
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publishDate 2014
reponame_str COLIBRI
repository.mail.fl_str_mv mabel.seroubian@seciu.edu.uy
repository.name.fl_str_mv COLIBRI - Universidad de la República
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rights_invalid_str_mv Licencia Creative Commons Atribución (CC - By 4.0)
spelling Arizmendi Fernando, Universidad de la República (Uruguay). Facultad de Ciencias. Instituto de Física.Barreiro Marcelo, Universidad de la República (Uruguay). Facultad de Ciencias. Instituto de Física.Martí Arturo, Universidad de la República (Uruguay). Facultad de Ciencias. Instituto de Física.2022-10-18T14:39:35Z2022-10-18T14:39:35Z2014Arizmendi, F, Barreiro, M y Martí, A. "Evolution of atmospheric connectivity in the 20th century". Nonlinear Processes in Geophysics. [en línea] 2014, 21(4): 825-839 . 15 h.1607-7946https://hdl.handle.net/20.500.12008/3423210.5194/npg-21-825-2014We aim to study the evolution of the upper atmosphere connectivity over the 20th century as well as to distinguish the oceanically forced component from the atmospheric internal variability. For this purpose we build networks from two different reanalysis data sets using both linear and nonlinear statistical similarity measures to determine the existence of links between different regions of the world in the two halves of the last century. We furthermore use symbolic analysis to emphasize intra-seasonal, intra-annual and inter-annual timescales. Both linear and nonlinear networks have similar structures and evolution, showing that the most connected regions are in the tropics over the Pacific Ocean. Also, the Southern Hemisphere extratropics have more connectivity in the first half of the 20th century, particularly on intra-annual and intra-seasonal timescales. Changes over the Pacific main connectivity regions are analyzed in more detail. Both linear and nonlinear networks show that the central and western Pacific regions have decreasing connectivity from early 1900 up to about 1940, when it starts increasing again until the present. The inter-annual network shows a similar behavior. However, this is not true of other timescales. On intra-annual timescales the minimum connectivity is around 1956, with a negative (positive) trend before (after) that date for both the central and western Pacific. While this is also true of the central Pacific on intra-seasonal timescales, the western Pacific shows a positive trend during the entire 20th century. In order to separate the internal and forced connectivity networks and to study their evolution through time, an ensemble of atmospheric general circulation model outputs is used. The results suggest that the main connectivity patterns captured in the reanalysis networks are due to the oceanically forced component, particularly on inter-annual timescales. Moreover, the atmospheric internal variability seems to play an important role in determining the intra-seasonal timescale networks.Submitted by Faget Cecilia (lfaget@fcien.edu.uy) on 2022-10-18T11:57:31Z No. of bitstreams: 2 license_rdf: 19875 bytes, checksum: 9fdbed07f52437945402c4e70fa4773e (MD5) 10.5194npg-21-825-2014.pdf: 4394146 bytes, checksum: 31bf099ce7652061e84e14dc3d75e30b (MD5)Approved for entry into archive by Faget Cecilia (lfaget@fcien.edu.uy) on 2022-10-18T14:06:19Z (GMT) No. of bitstreams: 2 license_rdf: 19875 bytes, checksum: 9fdbed07f52437945402c4e70fa4773e (MD5) 10.5194npg-21-825-2014.pdf: 4394146 bytes, checksum: 31bf099ce7652061e84e14dc3d75e30b (MD5)Made available in DSpace by Luna Fabiana (fabiana.luna@seciu.edu.uy) on 2022-10-18T14:39:35Z (GMT). No. of bitstreams: 2 license_rdf: 19875 bytes, checksum: 9fdbed07f52437945402c4e70fa4773e (MD5) 10.5194npg-21-825-2014.pdf: 4394146 bytes, checksum: 31bf099ce7652061e84e14dc3d75e30b (MD5) Previous issue date: 201415 happlication/pdfenengEuropean Geosciences UnionNonlinear Processes in Geophysics, 2014, 21(4): 825-839Las obras depositadas en el Repositorio se rigen por la Ordenanza de los Derechos de la Propiedad Intelectual de la Universidad de la República.(Res. Nº 91 de C.D.C. de 8/III/1994 – D.O. 7/IV/1994) y por la Ordenanza del Repositorio Abierto de la Universidad de la República (Res. 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- Universidad de la Repúblicafalse
spellingShingle Evolution of atmospheric connectivity in the 20th century
Arizmendi, Fernando
status_str publishedVersion
title Evolution of atmospheric connectivity in the 20th century
title_full Evolution of atmospheric connectivity in the 20th century
title_fullStr Evolution of atmospheric connectivity in the 20th century
title_full_unstemmed Evolution of atmospheric connectivity in the 20th century
title_short Evolution of atmospheric connectivity in the 20th century
title_sort Evolution of atmospheric connectivity in the 20th century
url https://hdl.handle.net/20.500.12008/34232