Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere

Autores
Vera, Carolina Susana
Año de publicación
2003
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
[1] A rotated empirical orthogonal function analysis was applied to anomalies of July atmospheric short time scale variability (or storm tracks) over the Southern Hemisphere (SH) using NCEP reanalyses. The study reveals the existence of two leading modes of storm-track variations, the first one describing storm-track changes along the subtropical Pacific and the second one associated with variations over southeast Pacific Ocean. The principal components of both modes exhibit significant variability on interannual (2–7 years) and interdecadal (longer than 7 years) time scales. The interannual variation of the first mode is closely linked to ENSO variability. The corresponding signal on SST anomalies shows a conspicuous maximum over central equatorial Pacific, while the signature on geopotential-height anomalies shows the typical Pacific South America pattern characterized by a Rossby wave train propagating poleward from the tropics. On interdecadal time scales, the first mode is related to SST anomalies over the subtropical portions of the Pacific, Atlantic, and Indian Oceans and to a Rossby wave train with strongest signals over the southeast Pacific and the Antarctic Peninsula. The second mode that represents storm-track changes west of the Antarctic Peninsula is related on interannual time scales to SST anomalies over western Pacific between 40°S and 20°S, while on interdecadal time scales, it does not seem to be significantly related to SST changes in any of the basins. In particular, the spatial signature of the REOF2 interdecadal variability on the SH circulation corresponds to the well-known high latitude mode characterized by a monopole over the Antarctica and a three-wave pattern at middle latitudes.
Fil: Vera, Carolina Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Materia
INTERANNUAL VARIATIONS
INTERDECADAL VARIATIONS
SOUTHERN HEMISPHERE
STORM TRACKS
SYNOPTIC-SCALE VARIABILITY
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/147369

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network_name_str CONICET Digital (CONICET)
spelling Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern HemisphereVera, Carolina SusanaINTERANNUAL VARIATIONSINTERDECADAL VARIATIONSSOUTHERN HEMISPHERESTORM TRACKSSYNOPTIC-SCALE VARIABILITYhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1[1] A rotated empirical orthogonal function analysis was applied to anomalies of July atmospheric short time scale variability (or storm tracks) over the Southern Hemisphere (SH) using NCEP reanalyses. The study reveals the existence of two leading modes of storm-track variations, the first one describing storm-track changes along the subtropical Pacific and the second one associated with variations over southeast Pacific Ocean. The principal components of both modes exhibit significant variability on interannual (2–7 years) and interdecadal (longer than 7 years) time scales. The interannual variation of the first mode is closely linked to ENSO variability. The corresponding signal on SST anomalies shows a conspicuous maximum over central equatorial Pacific, while the signature on geopotential-height anomalies shows the typical Pacific South America pattern characterized by a Rossby wave train propagating poleward from the tropics. On interdecadal time scales, the first mode is related to SST anomalies over the subtropical portions of the Pacific, Atlantic, and Indian Oceans and to a Rossby wave train with strongest signals over the southeast Pacific and the Antarctic Peninsula. The second mode that represents storm-track changes west of the Antarctic Peninsula is related on interannual time scales to SST anomalies over western Pacific between 40°S and 20°S, while on interdecadal time scales, it does not seem to be significantly related to SST changes in any of the basins. In particular, the spatial signature of the REOF2 interdecadal variability on the SH circulation corresponds to the well-known high latitude mode characterized by a monopole over the Antarctica and a three-wave pattern at middle latitudes.Fil: Vera, Carolina Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; ArgentinaAmerican Geophysical Union2003-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/147369Vera, Carolina Susana; Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere; American Geophysical Union; Journal of Geophysical Research; 108; C4; 1-2003; 1-102169-92910148-0227CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1029/2000JC000406info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2000JC000406info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:12:22Zoai:ri.conicet.gov.ar:11336/147369instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-10 13:12:23.159CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
title Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
spellingShingle Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
Vera, Carolina Susana
INTERANNUAL VARIATIONS
INTERDECADAL VARIATIONS
SOUTHERN HEMISPHERE
STORM TRACKS
SYNOPTIC-SCALE VARIABILITY
title_short Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
title_full Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
title_fullStr Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
title_full_unstemmed Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
title_sort Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere
dc.creator.none.fl_str_mv Vera, Carolina Susana
author Vera, Carolina Susana
author_facet Vera, Carolina Susana
author_role author
dc.subject.none.fl_str_mv INTERANNUAL VARIATIONS
INTERDECADAL VARIATIONS
SOUTHERN HEMISPHERE
STORM TRACKS
SYNOPTIC-SCALE VARIABILITY
topic INTERANNUAL VARIATIONS
INTERDECADAL VARIATIONS
SOUTHERN HEMISPHERE
STORM TRACKS
SYNOPTIC-SCALE VARIABILITY
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv [1] A rotated empirical orthogonal function analysis was applied to anomalies of July atmospheric short time scale variability (or storm tracks) over the Southern Hemisphere (SH) using NCEP reanalyses. The study reveals the existence of two leading modes of storm-track variations, the first one describing storm-track changes along the subtropical Pacific and the second one associated with variations over southeast Pacific Ocean. The principal components of both modes exhibit significant variability on interannual (2–7 years) and interdecadal (longer than 7 years) time scales. The interannual variation of the first mode is closely linked to ENSO variability. The corresponding signal on SST anomalies shows a conspicuous maximum over central equatorial Pacific, while the signature on geopotential-height anomalies shows the typical Pacific South America pattern characterized by a Rossby wave train propagating poleward from the tropics. On interdecadal time scales, the first mode is related to SST anomalies over the subtropical portions of the Pacific, Atlantic, and Indian Oceans and to a Rossby wave train with strongest signals over the southeast Pacific and the Antarctic Peninsula. The second mode that represents storm-track changes west of the Antarctic Peninsula is related on interannual time scales to SST anomalies over western Pacific between 40°S and 20°S, while on interdecadal time scales, it does not seem to be significantly related to SST changes in any of the basins. In particular, the spatial signature of the REOF2 interdecadal variability on the SH circulation corresponds to the well-known high latitude mode characterized by a monopole over the Antarctica and a three-wave pattern at middle latitudes.
Fil: Vera, Carolina Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina
description [1] A rotated empirical orthogonal function analysis was applied to anomalies of July atmospheric short time scale variability (or storm tracks) over the Southern Hemisphere (SH) using NCEP reanalyses. The study reveals the existence of two leading modes of storm-track variations, the first one describing storm-track changes along the subtropical Pacific and the second one associated with variations over southeast Pacific Ocean. The principal components of both modes exhibit significant variability on interannual (2–7 years) and interdecadal (longer than 7 years) time scales. The interannual variation of the first mode is closely linked to ENSO variability. The corresponding signal on SST anomalies shows a conspicuous maximum over central equatorial Pacific, while the signature on geopotential-height anomalies shows the typical Pacific South America pattern characterized by a Rossby wave train propagating poleward from the tropics. On interdecadal time scales, the first mode is related to SST anomalies over the subtropical portions of the Pacific, Atlantic, and Indian Oceans and to a Rossby wave train with strongest signals over the southeast Pacific and the Antarctic Peninsula. The second mode that represents storm-track changes west of the Antarctic Peninsula is related on interannual time scales to SST anomalies over western Pacific between 40°S and 20°S, while on interdecadal time scales, it does not seem to be significantly related to SST changes in any of the basins. In particular, the spatial signature of the REOF2 interdecadal variability on the SH circulation corresponds to the well-known high latitude mode characterized by a monopole over the Antarctica and a three-wave pattern at middle latitudes.
publishDate 2003
dc.date.none.fl_str_mv 2003-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/147369
Vera, Carolina Susana; Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere; American Geophysical Union; Journal of Geophysical Research; 108; C4; 1-2003; 1-10
2169-9291
0148-0227
CONICET Digital
CONICET
url http://hdl.handle.net/11336/147369
identifier_str_mv Vera, Carolina Susana; Interannual and interdecadal variability of atmospheric synoptic-scale activity in the Southern Hemisphere; American Geophysical Union; Journal of Geophysical Research; 108; C4; 1-2003; 1-10
2169-9291
0148-0227
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1029/2000JC000406
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2000JC000406
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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