Impacts of a Reduced AMOC on the South America Mean Climate and Extremes
- Autores
- Meccia, Virna L.; Blazquez, Josefina
- Año de publicación
- 2025
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Atlantic meridional overturning circulation (AMOC) plays a crucial role in regulating global and regional climate by distributing heat meridionally across the planet. Future projections indicate a weakening of the AMOC in response to increased greenhouse gas concentrations. In this study, we investigate the impact of AMOC weakening on South America's mean climate, as well as temperature and precipitation extremes. We analyze targeted sensitivity experiments using the EC-Earth3 climate model. Our findings reveal that AMOC weakening induces cooling and wetting in the tropics of South America, contrasted by warming and dryness in the extratropics. This pattern weakens the meridional temperature gradient, shifts the intertropical convergence zone and the high-latitude winter and summer jets southward, and reduces midlatitude storm tracks, particularly in austral winter. We analyze extreme events in two representative regions—La Plata Basin and northeast Brazil—which exhibit contrasting responses. In La Plata Basin, summer heat waves become more frequent, intense, and prolonged, while winter cold spells occur more frequently but with decreased intensity and duration when the AMOC reduces. In contrast, northeast Brazil experiences an increase in the frequency and intensity of heat waves, while cold spells become less frequent but more intense. Extreme precipitation events weaken in the La Plata Basin but intensify in northeast Brazil in both seasons under AMOC weakening. Some of these climate impacts may exacerbate global warming effects, while others may partially offset them. These findings underscore the critical need to refine climate models' representation of AMOC dynamics to improve predictions of future climate scenarios.
Fil: Meccia, Virna L.. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Dell Atmosfera E del Clima.; Italia
Fil: Blazquez, Josefina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina - Materia
-
EC-EARTH3
TEMPERATURE
PRECIPITATION
ITCZ
ATMOSPHERIC CIRCULATION - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/280472
Ver los metadatos del registro completo
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Impacts of a Reduced AMOC on the South America Mean Climate and ExtremesMeccia, Virna L.Blazquez, JosefinaEC-EARTH3TEMPERATUREPRECIPITATIONITCZATMOSPHERIC CIRCULATIONhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Atlantic meridional overturning circulation (AMOC) plays a crucial role in regulating global and regional climate by distributing heat meridionally across the planet. Future projections indicate a weakening of the AMOC in response to increased greenhouse gas concentrations. In this study, we investigate the impact of AMOC weakening on South America's mean climate, as well as temperature and precipitation extremes. We analyze targeted sensitivity experiments using the EC-Earth3 climate model. Our findings reveal that AMOC weakening induces cooling and wetting in the tropics of South America, contrasted by warming and dryness in the extratropics. This pattern weakens the meridional temperature gradient, shifts the intertropical convergence zone and the high-latitude winter and summer jets southward, and reduces midlatitude storm tracks, particularly in austral winter. We analyze extreme events in two representative regions—La Plata Basin and northeast Brazil—which exhibit contrasting responses. In La Plata Basin, summer heat waves become more frequent, intense, and prolonged, while winter cold spells occur more frequently but with decreased intensity and duration when the AMOC reduces. In contrast, northeast Brazil experiences an increase in the frequency and intensity of heat waves, while cold spells become less frequent but more intense. Extreme precipitation events weaken in the La Plata Basin but intensify in northeast Brazil in both seasons under AMOC weakening. Some of these climate impacts may exacerbate global warming effects, while others may partially offset them. These findings underscore the critical need to refine climate models' representation of AMOC dynamics to improve predictions of future climate scenarios.Fil: Meccia, Virna L.. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Dell Atmosfera E del Clima.; ItaliaFil: Blazquez, Josefina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaWiley2025-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/280472Meccia, Virna L.; Blazquez, Josefina; Impacts of a Reduced AMOC on the South America Mean Climate and Extremes; Wiley; Journal of Geophysical Research: Atmospheres; 130; 18; 9-2025; 1-192169-897X2169-8996CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JD044103info:eu-repo/semantics/altIdentifier/doi/10.1029/2025JD044103info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-02-26T09:57:41Zoai:ri.conicet.gov.ar:11336/280472instacron: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:34982026-02-26 09:57:41.884CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| title |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| spellingShingle |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes Meccia, Virna L. EC-EARTH3 TEMPERATURE PRECIPITATION ITCZ ATMOSPHERIC CIRCULATION |
| title_short |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| title_full |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| title_fullStr |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| title_full_unstemmed |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| title_sort |
Impacts of a Reduced AMOC on the South America Mean Climate and Extremes |
| dc.creator.none.fl_str_mv |
Meccia, Virna L. Blazquez, Josefina |
| author |
Meccia, Virna L. |
| author_facet |
Meccia, Virna L. Blazquez, Josefina |
| author_role |
author |
| author2 |
Blazquez, Josefina |
| author2_role |
author |
| dc.subject.none.fl_str_mv |
EC-EARTH3 TEMPERATURE PRECIPITATION ITCZ ATMOSPHERIC CIRCULATION |
| topic |
EC-EARTH3 TEMPERATURE PRECIPITATION ITCZ ATMOSPHERIC CIRCULATION |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
The Atlantic meridional overturning circulation (AMOC) plays a crucial role in regulating global and regional climate by distributing heat meridionally across the planet. Future projections indicate a weakening of the AMOC in response to increased greenhouse gas concentrations. In this study, we investigate the impact of AMOC weakening on South America's mean climate, as well as temperature and precipitation extremes. We analyze targeted sensitivity experiments using the EC-Earth3 climate model. Our findings reveal that AMOC weakening induces cooling and wetting in the tropics of South America, contrasted by warming and dryness in the extratropics. This pattern weakens the meridional temperature gradient, shifts the intertropical convergence zone and the high-latitude winter and summer jets southward, and reduces midlatitude storm tracks, particularly in austral winter. We analyze extreme events in two representative regions—La Plata Basin and northeast Brazil—which exhibit contrasting responses. In La Plata Basin, summer heat waves become more frequent, intense, and prolonged, while winter cold spells occur more frequently but with decreased intensity and duration when the AMOC reduces. In contrast, northeast Brazil experiences an increase in the frequency and intensity of heat waves, while cold spells become less frequent but more intense. Extreme precipitation events weaken in the La Plata Basin but intensify in northeast Brazil in both seasons under AMOC weakening. Some of these climate impacts may exacerbate global warming effects, while others may partially offset them. These findings underscore the critical need to refine climate models' representation of AMOC dynamics to improve predictions of future climate scenarios. Fil: Meccia, Virna L.. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Dell Atmosfera E del Clima.; Italia Fil: Blazquez, Josefina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina |
| description |
The Atlantic meridional overturning circulation (AMOC) plays a crucial role in regulating global and regional climate by distributing heat meridionally across the planet. Future projections indicate a weakening of the AMOC in response to increased greenhouse gas concentrations. In this study, we investigate the impact of AMOC weakening on South America's mean climate, as well as temperature and precipitation extremes. We analyze targeted sensitivity experiments using the EC-Earth3 climate model. Our findings reveal that AMOC weakening induces cooling and wetting in the tropics of South America, contrasted by warming and dryness in the extratropics. This pattern weakens the meridional temperature gradient, shifts the intertropical convergence zone and the high-latitude winter and summer jets southward, and reduces midlatitude storm tracks, particularly in austral winter. We analyze extreme events in two representative regions—La Plata Basin and northeast Brazil—which exhibit contrasting responses. In La Plata Basin, summer heat waves become more frequent, intense, and prolonged, while winter cold spells occur more frequently but with decreased intensity and duration when the AMOC reduces. In contrast, northeast Brazil experiences an increase in the frequency and intensity of heat waves, while cold spells become less frequent but more intense. Extreme precipitation events weaken in the La Plata Basin but intensify in northeast Brazil in both seasons under AMOC weakening. Some of these climate impacts may exacerbate global warming effects, while others may partially offset them. These findings underscore the critical need to refine climate models' representation of AMOC dynamics to improve predictions of future climate scenarios. |
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2025 |
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2025-09 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/280472 Meccia, Virna L.; Blazquez, Josefina; Impacts of a Reduced AMOC on the South America Mean Climate and Extremes; Wiley; Journal of Geophysical Research: Atmospheres; 130; 18; 9-2025; 1-19 2169-897X 2169-8996 CONICET Digital CONICET |
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http://hdl.handle.net/11336/280472 |
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Meccia, Virna L.; Blazquez, Josefina; Impacts of a Reduced AMOC on the South America Mean Climate and Extremes; Wiley; Journal of Geophysical Research: Atmospheres; 130; 18; 9-2025; 1-19 2169-897X 2169-8996 CONICET Digital CONICET |
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eng |
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