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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/194241
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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) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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13.13397 |