ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector
- Autores
- Solman, Silvina Alicia; Menendez, Claudio Guillermo
- Año de publicación
- 2002
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The interannual variability associated with the ENSO of winter storm tracks over the region extending from the eastern South Pacific Ocean across South America to the South Atlantic Ocean is described using 39 yr of data from the NCEP reanalysis data base. Tropical sea surface temperature anomalies associated with ENSO induce large-scale atmospheric circulation anomalies over large areas of the Southern Hemisphere. In particular, positive height anomalies dominate the Bellingshausen Sea during warm events, and consistently, a weakening of the eddy activity at low levels is found to the west of the Antarctic Peninsula. During El Nin˜o (EN) the storm track evidences an equatorward shift over the subtropical Pacific Ocean and a slight strengthening in the central Atlantic Ocean. Time-lagged correlation analysis applied to anomalies of the 300-hPa meridional wind at selected base points was used to study the structure and propagation characteristics of the waves. During EN, waves emanating from the Atlantic–Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Nin˜a (LN), wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastward deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean storm track for LN winters and from both the subtropical jet and the subpolar latitudes for EN. Time-lagged correlation analysis applied to anomalies of the 300 hPa meridional wind at selected base points was used to study the structure and propagation charactersistics of the waves. During EN waves emanating from the Atlantic-Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Niña (LN) wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastwards deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean stomr track for LN winters and from both the subtropical jet and the subpolar latitudes for EN.
Fil: Solman, Silvina Alicia. 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. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina
Fil: Menendez, Claudio Guillermo. 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
-
ENSO
HEMISFERIO DUR - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/147563
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ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sectorSolman, Silvina AliciaMenendez, Claudio GuillermoENSOHEMISFERIO DURhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The interannual variability associated with the ENSO of winter storm tracks over the region extending from the eastern South Pacific Ocean across South America to the South Atlantic Ocean is described using 39 yr of data from the NCEP reanalysis data base. Tropical sea surface temperature anomalies associated with ENSO induce large-scale atmospheric circulation anomalies over large areas of the Southern Hemisphere. In particular, positive height anomalies dominate the Bellingshausen Sea during warm events, and consistently, a weakening of the eddy activity at low levels is found to the west of the Antarctic Peninsula. During El Nin˜o (EN) the storm track evidences an equatorward shift over the subtropical Pacific Ocean and a slight strengthening in the central Atlantic Ocean. Time-lagged correlation analysis applied to anomalies of the 300-hPa meridional wind at selected base points was used to study the structure and propagation characteristics of the waves. During EN, waves emanating from the Atlantic–Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Nin˜a (LN), wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastward deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean storm track for LN winters and from both the subtropical jet and the subpolar latitudes for EN. Time-lagged correlation analysis applied to anomalies of the 300 hPa meridional wind at selected base points was used to study the structure and propagation charactersistics of the waves. During EN waves emanating from the Atlantic-Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Niña (LN) wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastwards deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean stomr track for LN winters and from both the subtropical jet and the subpolar latitudes for EN.Fil: Solman, Silvina Alicia. 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. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; ArgentinaFil: Menendez, Claudio Guillermo. 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; ArgentinaAmer Meteorological Soc2002-07-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/147563Solman, Silvina Alicia; Menendez, Claudio Guillermo; ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector; Amer Meteorological Soc; Journal of The Atmospheric Sciences; 59; 13; 01-7-2002; 2128-21410022-49281520-0469CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1175/1520-0469(2002)059<2128:ERVOTS>2.0.CO;2info:eu-repo/semantics/altIdentifier/url/https://journals.ametsoc.org/view/journals/atsc/59/13/1520-0469_2002_059_2128_ervots_2.0.co_2.xmlinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:45:59Zoai:ri.conicet.gov.ar:11336/147563instacron: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:34982025-09-03 09:45:59.927CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
title |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
spellingShingle |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector Solman, Silvina Alicia ENSO HEMISFERIO DUR |
title_short |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
title_full |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
title_fullStr |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
title_full_unstemmed |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
title_sort |
ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector |
dc.creator.none.fl_str_mv |
Solman, Silvina Alicia Menendez, Claudio Guillermo |
author |
Solman, Silvina Alicia |
author_facet |
Solman, Silvina Alicia Menendez, Claudio Guillermo |
author_role |
author |
author2 |
Menendez, Claudio Guillermo |
author2_role |
author |
dc.subject.none.fl_str_mv |
ENSO HEMISFERIO DUR |
topic |
ENSO HEMISFERIO DUR |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The interannual variability associated with the ENSO of winter storm tracks over the region extending from the eastern South Pacific Ocean across South America to the South Atlantic Ocean is described using 39 yr of data from the NCEP reanalysis data base. Tropical sea surface temperature anomalies associated with ENSO induce large-scale atmospheric circulation anomalies over large areas of the Southern Hemisphere. In particular, positive height anomalies dominate the Bellingshausen Sea during warm events, and consistently, a weakening of the eddy activity at low levels is found to the west of the Antarctic Peninsula. During El Nin˜o (EN) the storm track evidences an equatorward shift over the subtropical Pacific Ocean and a slight strengthening in the central Atlantic Ocean. Time-lagged correlation analysis applied to anomalies of the 300-hPa meridional wind at selected base points was used to study the structure and propagation characteristics of the waves. During EN, waves emanating from the Atlantic–Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Nin˜a (LN), wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastward deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean storm track for LN winters and from both the subtropical jet and the subpolar latitudes for EN. Time-lagged correlation analysis applied to anomalies of the 300 hPa meridional wind at selected base points was used to study the structure and propagation charactersistics of the waves. During EN waves emanating from the Atlantic-Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Niña (LN) wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastwards deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean stomr track for LN winters and from both the subtropical jet and the subpolar latitudes for EN. Fil: Solman, Silvina Alicia. 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. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina Fil: Menendez, Claudio Guillermo. 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 |
The interannual variability associated with the ENSO of winter storm tracks over the region extending from the eastern South Pacific Ocean across South America to the South Atlantic Ocean is described using 39 yr of data from the NCEP reanalysis data base. Tropical sea surface temperature anomalies associated with ENSO induce large-scale atmospheric circulation anomalies over large areas of the Southern Hemisphere. In particular, positive height anomalies dominate the Bellingshausen Sea during warm events, and consistently, a weakening of the eddy activity at low levels is found to the west of the Antarctic Peninsula. During El Nin˜o (EN) the storm track evidences an equatorward shift over the subtropical Pacific Ocean and a slight strengthening in the central Atlantic Ocean. Time-lagged correlation analysis applied to anomalies of the 300-hPa meridional wind at selected base points was used to study the structure and propagation characteristics of the waves. During EN, waves emanating from the Atlantic–Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Nin˜a (LN), wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastward deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean storm track for LN winters and from both the subtropical jet and the subpolar latitudes for EN. Time-lagged correlation analysis applied to anomalies of the 300 hPa meridional wind at selected base points was used to study the structure and propagation charactersistics of the waves. During EN waves emanating from the Atlantic-Indian Ocean storm tracks tend to propagate preferably along the subpolar branch of the Pacific Ocean storm track near Australia. Over the subtropical Pacific Ocean the wave train propagates along a northern path compared with cold events consistent with an equatorward shift of the axis of maximum baroclinicity. Additionally, large eddy activity at lower levels but weak eddy activity at upper levels were found for that region. During La Niña (LN) wave packets propagate more coherently along the subtropical branch of the storm track over the South Pacific Ocean, attaining larger amplitudes at upper levels and developing over broader latitudes compared to the warm phase. A poleward deflection of subtropical waves and northeastwards deflection of subpolar waves are also found for LN. Waves propagating through the Atlantic Ocean storm track evolve from the subtropical branch of the Pacific Ocean stomr track for LN winters and from both the subtropical jet and the subpolar latitudes for EN. |
publishDate |
2002 |
dc.date.none.fl_str_mv |
2002-07-01 |
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/11336/147563 Solman, Silvina Alicia; Menendez, Claudio Guillermo; ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector; Amer Meteorological Soc; Journal of The Atmospheric Sciences; 59; 13; 01-7-2002; 2128-2141 0022-4928 1520-0469 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/147563 |
identifier_str_mv |
Solman, Silvina Alicia; Menendez, Claudio Guillermo; ENSO-Related variability of the southern hemisphere winter storm track over the eastern Pacific–Atlantic sector; Amer Meteorological Soc; Journal of The Atmospheric Sciences; 59; 13; 01-7-2002; 2128-2141 0022-4928 1520-0469 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1175/1520-0469(2002)059<2128:ERVOTS>2.0.CO;2 info:eu-repo/semantics/altIdentifier/url/https://journals.ametsoc.org/view/journals/atsc/59/13/1520-0469_2002_059_2128_ervots_2.0.co_2.xml |
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 application/pdf |
dc.publisher.none.fl_str_mv |
Amer Meteorological Soc |
publisher.none.fl_str_mv |
Amer Meteorological Soc |
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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1842268767182127104 |
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13.13397 |