Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro

Autores
Martins Andrade, Kelen; Muller, Gabriela Viviana; Cavalcanti, Iracema F .A.; Fernández Long, María Elena; Bidegain, Mario; Berri, Guillermo Jorge
Año de publicación
2012
Idioma
portugués
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The frequency of frontal systems reaching the south of South America is compared with reanalysis, NCEP/NCAR, and results of GFDL and Hadley models for the future climate A2 scenario. For the present climate the analyzed period was 1961-1990 and for future projections, 2081-2100, from May to September. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above 5 degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in the future in the three areas, although less in area 3.
The frequency of frontal systems reaching the south of South America is compared with reanalysis NCEP/NCAR and results of GFDL and Hadley models for the future climate. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above five degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 (65ºW-60ºW, 33ºS-38ºS) from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in future in the three areas, although less in area 3.
Fil: Martins Andrade, Kelen. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Muller, Gabriela Viviana. Provincia de Entre Ríos. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción. Universidad Autónoma de Entre Ríos. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción; Argentina
Fil: Cavalcanti, Iracema F .A.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Fernández Long, María Elena. Universidad de Buenos Aires. Facultad de Agronomía; Argentina
Fil: Bidegain, Mario. Universidad de la República; Uruguay
Fil: Berri, Guillermo Jorge. Ministerio de Defensa. Secretaria de Planeamiento. Servicio Meteorológico Nacional; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
Sistemas frontais
clima futuro
América do Sul
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/243620

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spelling Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuroMartins Andrade, KelenMuller, Gabriela VivianaCavalcanti, Iracema F .A.Fernández Long, María ElenaBidegain, MarioBerri, Guillermo JorgeSistemas frontaisclima futuroAmérica do Sulhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The frequency of frontal systems reaching the south of South America is compared with reanalysis, NCEP/NCAR, and results of GFDL and Hadley models for the future climate A2 scenario. For the present climate the analyzed period was 1961-1990 and for future projections, 2081-2100, from May to September. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above 5 degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in the future in the three areas, although less in area 3.The frequency of frontal systems reaching the south of South America is compared with reanalysis NCEP/NCAR and results of GFDL and Hadley models for the future climate. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above five degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 (65ºW-60ºW, 33ºS-38ºS) from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in future in the three areas, although less in area 3.Fil: Martins Andrade, Kelen. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Muller, Gabriela Viviana. Provincia de Entre Ríos. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción. Universidad Autónoma de Entre Ríos. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción; ArgentinaFil: Cavalcanti, Iracema F .A.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Fernández Long, María Elena. Universidad de Buenos Aires. Facultad de Agronomía; ArgentinaFil: Bidegain, Mario. Universidad de la República; UruguayFil: Berri, Guillermo Jorge. Ministerio de Defensa. Secretaria de Planeamiento. Servicio Meteorológico Nacional; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaCentro Argentino de Meteorólogos2012-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/243620Martins Andrade, Kelen; Muller, Gabriela Viviana; Cavalcanti, Iracema F .A.; Fernández Long, María Elena; Bidegain, Mario; et al.; Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro; Centro Argentino de Meteorólogos; Meteorológica; 37; 1; 6-2012; 15-250325-187X1850-468XCONICET DigitalCONICETporinfo:eu-repo/semantics/altIdentifier/url/http://www.scielo.org.ar/scielo.php?script=sci_abstract&pid=S1850-468X2012000100002&lng=es&nrm=isoinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T12:14:55Zoai:ri.conicet.gov.ar:11336/243620instacron: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:34982025-10-22 12:14:55.405CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
title Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
spellingShingle Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
Martins Andrade, Kelen
Sistemas frontais
clima futuro
América do Sul
title_short Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
title_full Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
title_fullStr Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
title_full_unstemmed Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
title_sort Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro
dc.creator.none.fl_str_mv Martins Andrade, Kelen
Muller, Gabriela Viviana
Cavalcanti, Iracema F .A.
Fernández Long, María Elena
Bidegain, Mario
Berri, Guillermo Jorge
author Martins Andrade, Kelen
author_facet Martins Andrade, Kelen
Muller, Gabriela Viviana
Cavalcanti, Iracema F .A.
Fernández Long, María Elena
Bidegain, Mario
Berri, Guillermo Jorge
author_role author
author2 Muller, Gabriela Viviana
Cavalcanti, Iracema F .A.
Fernández Long, María Elena
Bidegain, Mario
Berri, Guillermo Jorge
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Sistemas frontais
clima futuro
América do Sul
topic Sistemas frontais
clima futuro
América do Sul
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 frequency of frontal systems reaching the south of South America is compared with reanalysis, NCEP/NCAR, and results of GFDL and Hadley models for the future climate A2 scenario. For the present climate the analyzed period was 1961-1990 and for future projections, 2081-2100, from May to September. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above 5 degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in the future in the three areas, although less in area 3.
The frequency of frontal systems reaching the south of South America is compared with reanalysis NCEP/NCAR and results of GFDL and Hadley models for the future climate. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above five degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 (65ºW-60ºW, 33ºS-38ºS) from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in future in the three areas, although less in area 3.
Fil: Martins Andrade, Kelen. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Muller, Gabriela Viviana. Provincia de Entre Ríos. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción. Universidad Autónoma de Entre Ríos. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe. Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción; Argentina
Fil: Cavalcanti, Iracema F .A.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Fernández Long, María Elena. Universidad de Buenos Aires. Facultad de Agronomía; Argentina
Fil: Bidegain, Mario. Universidad de la República; Uruguay
Fil: Berri, Guillermo Jorge. Ministerio de Defensa. Secretaria de Planeamiento. Servicio Meteorológico Nacional; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description The frequency of frontal systems reaching the south of South America is compared with reanalysis, NCEP/NCAR, and results of GFDL and Hadley models for the future climate A2 scenario. For the present climate the analyzed period was 1961-1990 and for future projections, 2081-2100, from May to September. Three regions were analyzed to identify the frontal systems, in areas of Brazil, Uruguay, Paraguay and Argentina. The following criteria were used: increase of sea surface pressure, reduction of the temperature and change of the meridional wind at 850hPa, in two consecutive days. Selected cases with temperature drop above 5 degrees, considered the most intense, were also analyzed. For the present climate it was observed that the models simulated well the synoptic characteristics of frontal systems. However, when comparing the frequency of frontal occurrence between reanalysis data and models simulations, the GFDL and Hadley models overestimated their numbers. The Hadley model overestimates further more than the NCEP and GFDL in present climate. The positive trend observed in area 3 from NCEP reanalysis is not simulated by the models. When the most intense systems are selected, the GFDL model shows higher overestimation in number of frontal systems. Both models indicate an increase of frontal systems frequency in the future in the three areas, although less in area 3.
publishDate 2012
dc.date.none.fl_str_mv 2012-06
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/11336/243620
Martins Andrade, Kelen; Muller, Gabriela Viviana; Cavalcanti, Iracema F .A.; Fernández Long, María Elena; Bidegain, Mario; et al.; Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro; Centro Argentino de Meteorólogos; Meteorológica; 37; 1; 6-2012; 15-25
0325-187X
1850-468X
CONICET Digital
CONICET
url http://hdl.handle.net/11336/243620
identifier_str_mv Martins Andrade, Kelen; Muller, Gabriela Viviana; Cavalcanti, Iracema F .A.; Fernández Long, María Elena; Bidegain, Mario; et al.; Avaliação de mudanças na freqüência de sistemas frontais sobre o Sul da America do sul em projeções do clima futuro; Centro Argentino de Meteorólogos; Meteorológica; 37; 1; 6-2012; 15-25
0325-187X
1850-468X
CONICET Digital
CONICET
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language por
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.scielo.org.ar/scielo.php?script=sci_abstract&pid=S1850-468X2012000100002&lng=es&nrm=iso
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
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dc.publisher.none.fl_str_mv Centro Argentino de Meteorólogos
publisher.none.fl_str_mv Centro Argentino de Meteorólogos
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
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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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