Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature

Autores
Haylock, Malcolm R.; Peterson, T. C.; Alves, L. M.; Ambrizzi, T.; Anunciação, Y. M. T.; Baez, J.; Barros, Vicente Ricardo; Berlato, M. A.; Bidegain, M.; Coronel, G.; Corradi, V.; Garcia, V. J.; Grimm, A. M.; Karoly, D.; Marengo, José A.; Marino, M.B.; Moncunill, D. F.; Nechet, D.; Quintana, J.; Rebello, E.; Rusticucci, Matilde Monica; Santos, J. L.; Trebejo, I.; Vincent, L. A.
Año de publicación
2006
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
A weeklong workshop in Brazil in August 2004 provided the opportunity for 28 scientists from southern South America to examine daily rainfall observations to determine changes in both total and extreme rainfall. Twelve annual indices of daily rainfall were calculated over the period 1960 to 2000, examining changes to both the entire distribution as well as the extremes. Maps of trends in the 12 rainfall indices showed large regions of coherent change, with many stations showing statistically significant changes in some of the indices. The pattern of trends for the extremes was generally the same as that for total annual rainfall, with a change to wetter conditions in Ecuador and northern Peru and the region of southern Brazil, Paraguay, Uruguay, and northern and central Argentina. A decrease was observed in southern Peru and southern Chile, with the latter showing significant decreases in many indices. A canonical correlation analysis between each of the indices and sea surface temperatures (SSTs) revealed two large-scale patterns that have contributed to the observed trends in the rainfall indices. A coupled pattern with ENSO-like SST loadings and rainfall loadings showing similarities with the pattern of the observed trend reveals that the change to a generally more negative Southern Oscillation index (SOI) has had an important effect on regional rainfall trends. A significant decrease in many of the rainfall indices at several stations in southern Chile and Argentina can be explained by a canonical pattern reflecting a weakening of the continental trough leading to a southward shift in storm tracks. This latter signal is a change that has been seen at similar latitudes in other parts of the Southern Hemisphere. A similar analysis was carried out for eastern Brazil using gridded indices calculated from 354 stations from the Global Historical Climatology Network (GHCN) database. The observed trend toward wetter conditions in the southwest and drier conditions in the northeast could again be explained by changes in ENSO.
Fil: Haylock, Malcolm R.. University of East Anglia; Reino Unido
Fil: Peterson, T. C.. National Climatic Data Center; Estados Unidos
Fil: Alves, L. M.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Ambrizzi, T.. Universidade de Sao Paulo; Brasil
Fil: Anunciação, Y. M. T.. Instituto Nacional de Meteorologia; Brasil
Fil: Baez, J.. Dirección Nacional de Meteorología e Hidrología; Paraguay. Universidad Autónoma de Asunción; Paraguay
Fil: Barros, Vicente Ricardo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Berlato, M. A.. Universidade Federal do Rio Grande do Sul; Brasil
Fil: Bidegain, M.. Universidad de la República; Uruguay
Fil: Coronel, G.. Universidad Nacional de Asunción; Paraguay
Fil: Corradi, V.. Dirección Nacional de Meteorología; Uruguay
Fil: Garcia, V. J.. Universidad Nacional Agraria La Molina;
Fil: Grimm, A. M.. Universidade Federal do Paraná; Brasil
Fil: Karoly, D.. Oklahoma State University; Estados Unidos
Fil: Marengo, José A.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Marino, M.B.. Ministerio de Defensa; Argentina
Fil: Moncunill, D. F.. Fundação Cearense de Meteorologia E Recursos Hídricos; Brasil
Fil: Nechet, D.. Universidade Federal do Pará; Brasil
Fil: Quintana, J.. Dirección Meteorológica de Chile; Chile
Fil: Rebello, E.. Instituto Nacional de Meteorologia; Brasil
Fil: Rusticucci, Matilde Monica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Santos, J. L.. Escuela Superior Politecnica del Litoral Ecuador; Ecuador
Fil: Trebejo, I.. Servicio Nacional de Meteorología E Hidrología del Perú; Perú
Fil: Vincent, L. A.. Environment And Climate Change Canada; Canadá
Materia
Sea Surface
Extreme
South American
Rainfall
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:11336/194241

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network_name_str CONICET Digital (CONICET)
spelling Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperatureHaylock, Malcolm R.Peterson, T. C.Alves, L. M.Ambrizzi, T.Anunciação, Y. M. T.Baez, J.Barros, Vicente RicardoBerlato, M. A.Bidegain, M.Coronel, G.Corradi, V.Garcia, V. J.Grimm, A. M.Karoly, D.Marengo, José A.Marino, M.B.Moncunill, D. F.Nechet, D.Quintana, J.Rebello, E.Rusticucci, Matilde MonicaSantos, J. L.Trebejo, I.Vincent, L. A.Sea SurfaceExtremeSouth AmericanRainfallhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1A weeklong workshop in Brazil in August 2004 provided the opportunity for 28 scientists from southern South America to examine daily rainfall observations to determine changes in both total and extreme rainfall. Twelve annual indices of daily rainfall were calculated over the period 1960 to 2000, examining changes to both the entire distribution as well as the extremes. Maps of trends in the 12 rainfall indices showed large regions of coherent change, with many stations showing statistically significant changes in some of the indices. The pattern of trends for the extremes was generally the same as that for total annual rainfall, with a change to wetter conditions in Ecuador and northern Peru and the region of southern Brazil, Paraguay, Uruguay, and northern and central Argentina. A decrease was observed in southern Peru and southern Chile, with the latter showing significant decreases in many indices. A canonical correlation analysis between each of the indices and sea surface temperatures (SSTs) revealed two large-scale patterns that have contributed to the observed trends in the rainfall indices. A coupled pattern with ENSO-like SST loadings and rainfall loadings showing similarities with the pattern of the observed trend reveals that the change to a generally more negative Southern Oscillation index (SOI) has had an important effect on regional rainfall trends. A significant decrease in many of the rainfall indices at several stations in southern Chile and Argentina can be explained by a canonical pattern reflecting a weakening of the continental trough leading to a southward shift in storm tracks. This latter signal is a change that has been seen at similar latitudes in other parts of the Southern Hemisphere. A similar analysis was carried out for eastern Brazil using gridded indices calculated from 354 stations from the Global Historical Climatology Network (GHCN) database. The observed trend toward wetter conditions in the southwest and drier conditions in the northeast could again be explained by changes in ENSO.Fil: Haylock, Malcolm R.. University of East Anglia; Reino UnidoFil: Peterson, T. C.. National Climatic Data Center; Estados UnidosFil: Alves, L. M.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Ambrizzi, T.. Universidade de Sao Paulo; BrasilFil: Anunciação, Y. M. T.. Instituto Nacional de Meteorologia; BrasilFil: Baez, J.. Dirección Nacional de Meteorología e Hidrología; Paraguay. Universidad Autónoma de Asunción; ParaguayFil: Barros, Vicente Ricardo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Berlato, M. A.. Universidade Federal do Rio Grande do Sul; BrasilFil: Bidegain, M.. Universidad de la República; UruguayFil: Coronel, G.. Universidad Nacional de Asunción; ParaguayFil: Corradi, V.. Dirección Nacional de Meteorología; UruguayFil: Garcia, V. J.. Universidad Nacional Agraria La Molina;Fil: Grimm, A. M.. Universidade Federal do Paraná; BrasilFil: Karoly, D.. Oklahoma State University; Estados UnidosFil: Marengo, José A.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Marino, M.B.. Ministerio de Defensa; ArgentinaFil: Moncunill, D. F.. Fundação Cearense de Meteorologia E Recursos Hídricos; BrasilFil: Nechet, D.. Universidade Federal do Pará; BrasilFil: Quintana, J.. Dirección Meteorológica de Chile; ChileFil: Rebello, E.. Instituto Nacional de Meteorologia; BrasilFil: Rusticucci, Matilde Monica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Santos, J. L.. Escuela Superior Politecnica del Litoral Ecuador; EcuadorFil: Trebejo, I.. Servicio Nacional de Meteorología E Hidrología del Perú; PerúFil: Vincent, L. A.. Environment And Climate Change Canada; CanadáAmer Meteorological Soc2006-12info: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/11336/194241Haylock, Malcolm R.; Peterson, T. C.; Alves, L. M.; Ambrizzi, T.; Anunciação, Y. M. T.; et al.; Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature; Amer Meteorological Soc; Journal Of Climate; 19; 8; 12-2006; 1490-15120894-8755CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://journals.ametsoc.org/view/journals/clim/19/8/jcli3695.1.xmlinfo:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI3695.1info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:49:57Zoai:ri.conicet.gov.ar:11336/194241instacron: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 09:49:57.424CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
title Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
spellingShingle Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
Haylock, Malcolm R.
Sea Surface
Extreme
South American
Rainfall
title_short Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
title_full Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
title_fullStr Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
title_full_unstemmed Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
title_sort Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature
dc.creator.none.fl_str_mv Haylock, Malcolm R.
Peterson, T. C.
Alves, L. M.
Ambrizzi, T.
Anunciação, Y. M. T.
Baez, J.
Barros, Vicente Ricardo
Berlato, M. A.
Bidegain, M.
Coronel, G.
Corradi, V.
Garcia, V. J.
Grimm, A. M.
Karoly, D.
Marengo, José A.
Marino, M.B.
Moncunill, D. F.
Nechet, D.
Quintana, J.
Rebello, E.
Rusticucci, Matilde Monica
Santos, J. L.
Trebejo, I.
Vincent, L. A.
author Haylock, Malcolm R.
author_facet Haylock, Malcolm R.
Peterson, T. C.
Alves, L. M.
Ambrizzi, T.
Anunciação, Y. M. T.
Baez, J.
Barros, Vicente Ricardo
Berlato, M. A.
Bidegain, M.
Coronel, G.
Corradi, V.
Garcia, V. J.
Grimm, A. M.
Karoly, D.
Marengo, José A.
Marino, M.B.
Moncunill, D. F.
Nechet, D.
Quintana, J.
Rebello, E.
Rusticucci, Matilde Monica
Santos, J. L.
Trebejo, I.
Vincent, L. A.
author_role author
author2 Peterson, T. C.
Alves, L. M.
Ambrizzi, T.
Anunciação, Y. M. T.
Baez, J.
Barros, Vicente Ricardo
Berlato, M. A.
Bidegain, M.
Coronel, G.
Corradi, V.
Garcia, V. J.
Grimm, A. M.
Karoly, D.
Marengo, José A.
Marino, M.B.
Moncunill, D. F.
Nechet, D.
Quintana, J.
Rebello, E.
Rusticucci, Matilde Monica
Santos, J. L.
Trebejo, I.
Vincent, L. A.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Sea Surface
Extreme
South American
Rainfall
topic Sea Surface
Extreme
South American
Rainfall
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv A weeklong workshop in Brazil in August 2004 provided the opportunity for 28 scientists from southern South America to examine daily rainfall observations to determine changes in both total and extreme rainfall. Twelve annual indices of daily rainfall were calculated over the period 1960 to 2000, examining changes to both the entire distribution as well as the extremes. Maps of trends in the 12 rainfall indices showed large regions of coherent change, with many stations showing statistically significant changes in some of the indices. The pattern of trends for the extremes was generally the same as that for total annual rainfall, with a change to wetter conditions in Ecuador and northern Peru and the region of southern Brazil, Paraguay, Uruguay, and northern and central Argentina. A decrease was observed in southern Peru and southern Chile, with the latter showing significant decreases in many indices. A canonical correlation analysis between each of the indices and sea surface temperatures (SSTs) revealed two large-scale patterns that have contributed to the observed trends in the rainfall indices. A coupled pattern with ENSO-like SST loadings and rainfall loadings showing similarities with the pattern of the observed trend reveals that the change to a generally more negative Southern Oscillation index (SOI) has had an important effect on regional rainfall trends. A significant decrease in many of the rainfall indices at several stations in southern Chile and Argentina can be explained by a canonical pattern reflecting a weakening of the continental trough leading to a southward shift in storm tracks. This latter signal is a change that has been seen at similar latitudes in other parts of the Southern Hemisphere. A similar analysis was carried out for eastern Brazil using gridded indices calculated from 354 stations from the Global Historical Climatology Network (GHCN) database. The observed trend toward wetter conditions in the southwest and drier conditions in the northeast could again be explained by changes in ENSO.
Fil: Haylock, Malcolm R.. University of East Anglia; Reino Unido
Fil: Peterson, T. C.. National Climatic Data Center; Estados Unidos
Fil: Alves, L. M.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Ambrizzi, T.. Universidade de Sao Paulo; Brasil
Fil: Anunciação, Y. M. T.. Instituto Nacional de Meteorologia; Brasil
Fil: Baez, J.. Dirección Nacional de Meteorología e Hidrología; Paraguay. Universidad Autónoma de Asunción; Paraguay
Fil: Barros, Vicente Ricardo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Berlato, M. A.. Universidade Federal do Rio Grande do Sul; Brasil
Fil: Bidegain, M.. Universidad de la República; Uruguay
Fil: Coronel, G.. Universidad Nacional de Asunción; Paraguay
Fil: Corradi, V.. Dirección Nacional de Meteorología; Uruguay
Fil: Garcia, V. J.. Universidad Nacional Agraria La Molina;
Fil: Grimm, A. M.. Universidade Federal do Paraná; Brasil
Fil: Karoly, D.. Oklahoma State University; Estados Unidos
Fil: Marengo, José A.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Marino, M.B.. Ministerio de Defensa; Argentina
Fil: Moncunill, D. F.. Fundação Cearense de Meteorologia E Recursos Hídricos; Brasil
Fil: Nechet, D.. Universidade Federal do Pará; Brasil
Fil: Quintana, J.. Dirección Meteorológica de Chile; Chile
Fil: Rebello, E.. Instituto Nacional de Meteorologia; Brasil
Fil: Rusticucci, Matilde Monica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias de la Atmósfera y los Océanos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Santos, J. L.. Escuela Superior Politecnica del Litoral Ecuador; Ecuador
Fil: Trebejo, I.. Servicio Nacional de Meteorología E Hidrología del Perú; Perú
Fil: Vincent, L. A.. Environment And Climate Change Canada; Canadá
description A weeklong workshop in Brazil in August 2004 provided the opportunity for 28 scientists from southern South America to examine daily rainfall observations to determine changes in both total and extreme rainfall. Twelve annual indices of daily rainfall were calculated over the period 1960 to 2000, examining changes to both the entire distribution as well as the extremes. Maps of trends in the 12 rainfall indices showed large regions of coherent change, with many stations showing statistically significant changes in some of the indices. The pattern of trends for the extremes was generally the same as that for total annual rainfall, with a change to wetter conditions in Ecuador and northern Peru and the region of southern Brazil, Paraguay, Uruguay, and northern and central Argentina. A decrease was observed in southern Peru and southern Chile, with the latter showing significant decreases in many indices. A canonical correlation analysis between each of the indices and sea surface temperatures (SSTs) revealed two large-scale patterns that have contributed to the observed trends in the rainfall indices. A coupled pattern with ENSO-like SST loadings and rainfall loadings showing similarities with the pattern of the observed trend reveals that the change to a generally more negative Southern Oscillation index (SOI) has had an important effect on regional rainfall trends. A significant decrease in many of the rainfall indices at several stations in southern Chile and Argentina can be explained by a canonical pattern reflecting a weakening of the continental trough leading to a southward shift in storm tracks. This latter signal is a change that has been seen at similar latitudes in other parts of the Southern Hemisphere. A similar analysis was carried out for eastern Brazil using gridded indices calculated from 354 stations from the Global Historical Climatology Network (GHCN) database. The observed trend toward wetter conditions in the southwest and drier conditions in the northeast could again be explained by changes in ENSO.
publishDate 2006
dc.date.none.fl_str_mv 2006-12
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/11336/194241
Haylock, Malcolm R.; Peterson, T. C.; Alves, L. M.; Ambrizzi, T.; Anunciação, Y. M. T.; et al.; Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature; Amer Meteorological Soc; Journal Of Climate; 19; 8; 12-2006; 1490-1512
0894-8755
CONICET Digital
CONICET
url http://hdl.handle.net/11336/194241
identifier_str_mv Haylock, Malcolm R.; Peterson, T. C.; Alves, L. M.; Ambrizzi, T.; Anunciação, Y. M. T.; et al.; Trends in total and extreme South American rainfall in 1960-2000 and links with sea surface temperature; Amer Meteorological Soc; Journal Of Climate; 19; 8; 12-2006; 1490-1512
0894-8755
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://journals.ametsoc.org/view/journals/clim/19/8/jcli3695.1.xml
info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI3695.1
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)
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reponame_str CONICET Digital (CONICET)
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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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