Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation

Autores
Orrison, R.; Vuille, M.; Rodrigues, J. C.; Stríkis, N. M.; Cruz, F.; Rodriguez Catón, Milagros Rocío; Andreu Hayles, L.
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The South American summer monsoon (SASM) generates important hydroclimatic impacts in (sub‐)tropical South America and isotopic tracers recorded in paleoclimatic archives allow for assessing its long‐term response to Pacific variability prior to modern observations. Stable oxygen isotopes in precipitation integrate hydroclimatic changes during the SASM mature phase from December to February (DJF) in response to the Interdecadal Pacific Oscillation (IPO) and El Niño—Southern Oscillation (ENSO), respectively. Here, results from the isotope‐enabled Community Atmosphere Model v.5 are compared with highly resolved and precisely dated isotopic records from speleothems, tree rings, lake and ice cores during the industrial era (1880–2000 CE) and validated against observations from the International Atomic Energy Agency (IAEA) network. Pacific sea surface temperatures (SSTs) are coupled to the isotopic composition of SASM precipitation through perturbations in the Walker circulation associated with low‐ (IPO) and high‐frequency (ENSO) variability, impacting convective activity over tropical South America and the tropical Atlantic. Changes in convection over this monsoon entrance region ultimately control the downstream oxygen isotopic composition of precipitation recorded in paleoclimate archives. Overall, model results, paleoclimate records and IAEA data agree on the isotopic response to Pacific SST forcing. These results highlight the potential for long isotopic paleoclimate records to reconstruct Pacific climate variability on both high‐ and low‐frequency timescales. Furthermore, the isolation of the IPO signal in a diverse set of isotopic archives invites the reinterpretation of other paleoclimate proxies for identifying this historically overlooked forcing.
Fil: Orrison, R.. State University Of New York. University At Albany.; Estados Unidos
Fil: Vuille, M.. State University Of New York. University At Albany.; Estados Unidos
Fil: Rodrigues, J. C.. Johannes Gutenberg Universitat Mainz; Alemania
Fil: Stríkis, N. M.. Universidade de Sao Paulo; Brasil
Fil: Cruz, F.. Universidade de Sao Paulo; Brasil
Fil: Rodriguez Catón, Milagros Rocío. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Andreu Hayles, L.. No especifíca;
Materia
South American summer monsoon
Paleoclimate records
Pacific multidecadal variability
multiproxy
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:11336/263351
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon PrecipitationOrrison, R.Vuille, M.Rodrigues, J. C.Stríkis, N. M.Cruz, F.Rodriguez Catón, Milagros RocíoAndreu Hayles, L.South American summer monsoonPaleoclimate recordsPacific multidecadal variabilitymultiproxyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The South American summer monsoon (SASM) generates important hydroclimatic impacts in (sub‐)tropical South America and isotopic tracers recorded in paleoclimatic archives allow for assessing its long‐term response to Pacific variability prior to modern observations. Stable oxygen isotopes in precipitation integrate hydroclimatic changes during the SASM mature phase from December to February (DJF) in response to the Interdecadal Pacific Oscillation (IPO) and El Niño—Southern Oscillation (ENSO), respectively. Here, results from the isotope‐enabled Community Atmosphere Model v.5 are compared with highly resolved and precisely dated isotopic records from speleothems, tree rings, lake and ice cores during the industrial era (1880–2000 CE) and validated against observations from the International Atomic Energy Agency (IAEA) network. Pacific sea surface temperatures (SSTs) are coupled to the isotopic composition of SASM precipitation through perturbations in the Walker circulation associated with low‐ (IPO) and high‐frequency (ENSO) variability, impacting convective activity over tropical South America and the tropical Atlantic. Changes in convection over this monsoon entrance region ultimately control the downstream oxygen isotopic composition of precipitation recorded in paleoclimate archives. Overall, model results, paleoclimate records and IAEA data agree on the isotopic response to Pacific SST forcing. These results highlight the potential for long isotopic paleoclimate records to reconstruct Pacific climate variability on both high‐ and low‐frequency timescales. Furthermore, the isolation of the IPO signal in a diverse set of isotopic archives invites the reinterpretation of other paleoclimate proxies for identifying this historically overlooked forcing.Fil: Orrison, R.. State University Of New York. University At Albany.; Estados UnidosFil: Vuille, M.. State University Of New York. University At Albany.; Estados UnidosFil: Rodrigues, J. C.. Johannes Gutenberg Universitat Mainz; AlemaniaFil: Stríkis, N. M.. Universidade de Sao Paulo; BrasilFil: Cruz, F.. Universidade de Sao Paulo; BrasilFil: Rodriguez Catón, Milagros Rocío. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Andreu Hayles, L.. No especifíca;Wiley2024-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/263351Orrison, R.; Vuille, M.; Rodrigues, J. C.; Stríkis, N. M.; Cruz, F.; et al.; Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation; Wiley; Journal of Geophysical Research: Atmospheres; 129; 17; 9-2024; 1-192169-897X2169-8996CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024JD040999info:eu-repo/semantics/altIdentifier/doi/10.1029/2024JD040999info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:45:02Zoai:ri.conicet.gov.ar:11336/263351instacron: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:34982025-09-29 10:45:03.072CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
title Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
spellingShingle Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
Orrison, R.
South American summer monsoon
Paleoclimate records
Pacific multidecadal variability
multiproxy
title_short Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
title_full Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
title_fullStr Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
title_full_unstemmed Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
title_sort Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation
dc.creator.none.fl_str_mv Orrison, R.
Vuille, M.
Rodrigues, J. C.
Stríkis, N. M.
Cruz, F.
Rodriguez Catón, Milagros Rocío
Andreu Hayles, L.
author Orrison, R.
author_facet Orrison, R.
Vuille, M.
Rodrigues, J. C.
Stríkis, N. M.
Cruz, F.
Rodriguez Catón, Milagros Rocío
Andreu Hayles, L.
author_role author
author2 Vuille, M.
Rodrigues, J. C.
Stríkis, N. M.
Cruz, F.
Rodriguez Catón, Milagros Rocío
Andreu Hayles, L.
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv South American summer monsoon
Paleoclimate records
Pacific multidecadal variability
multiproxy
topic South American summer monsoon
Paleoclimate records
Pacific multidecadal variability
multiproxy
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 South American summer monsoon (SASM) generates important hydroclimatic impacts in (sub‐)tropical South America and isotopic tracers recorded in paleoclimatic archives allow for assessing its long‐term response to Pacific variability prior to modern observations. Stable oxygen isotopes in precipitation integrate hydroclimatic changes during the SASM mature phase from December to February (DJF) in response to the Interdecadal Pacific Oscillation (IPO) and El Niño—Southern Oscillation (ENSO), respectively. Here, results from the isotope‐enabled Community Atmosphere Model v.5 are compared with highly resolved and precisely dated isotopic records from speleothems, tree rings, lake and ice cores during the industrial era (1880–2000 CE) and validated against observations from the International Atomic Energy Agency (IAEA) network. Pacific sea surface temperatures (SSTs) are coupled to the isotopic composition of SASM precipitation through perturbations in the Walker circulation associated with low‐ (IPO) and high‐frequency (ENSO) variability, impacting convective activity over tropical South America and the tropical Atlantic. Changes in convection over this monsoon entrance region ultimately control the downstream oxygen isotopic composition of precipitation recorded in paleoclimate archives. Overall, model results, paleoclimate records and IAEA data agree on the isotopic response to Pacific SST forcing. These results highlight the potential for long isotopic paleoclimate records to reconstruct Pacific climate variability on both high‐ and low‐frequency timescales. Furthermore, the isolation of the IPO signal in a diverse set of isotopic archives invites the reinterpretation of other paleoclimate proxies for identifying this historically overlooked forcing.
Fil: Orrison, R.. State University Of New York. University At Albany.; Estados Unidos
Fil: Vuille, M.. State University Of New York. University At Albany.; Estados Unidos
Fil: Rodrigues, J. C.. Johannes Gutenberg Universitat Mainz; Alemania
Fil: Stríkis, N. M.. Universidade de Sao Paulo; Brasil
Fil: Cruz, F.. Universidade de Sao Paulo; Brasil
Fil: Rodriguez Catón, Milagros Rocío. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Andreu Hayles, L.. No especifíca;
description The South American summer monsoon (SASM) generates important hydroclimatic impacts in (sub‐)tropical South America and isotopic tracers recorded in paleoclimatic archives allow for assessing its long‐term response to Pacific variability prior to modern observations. Stable oxygen isotopes in precipitation integrate hydroclimatic changes during the SASM mature phase from December to February (DJF) in response to the Interdecadal Pacific Oscillation (IPO) and El Niño—Southern Oscillation (ENSO), respectively. Here, results from the isotope‐enabled Community Atmosphere Model v.5 are compared with highly resolved and precisely dated isotopic records from speleothems, tree rings, lake and ice cores during the industrial era (1880–2000 CE) and validated against observations from the International Atomic Energy Agency (IAEA) network. Pacific sea surface temperatures (SSTs) are coupled to the isotopic composition of SASM precipitation through perturbations in the Walker circulation associated with low‐ (IPO) and high‐frequency (ENSO) variability, impacting convective activity over tropical South America and the tropical Atlantic. Changes in convection over this monsoon entrance region ultimately control the downstream oxygen isotopic composition of precipitation recorded in paleoclimate archives. Overall, model results, paleoclimate records and IAEA data agree on the isotopic response to Pacific SST forcing. These results highlight the potential for long isotopic paleoclimate records to reconstruct Pacific climate variability on both high‐ and low‐frequency timescales. Furthermore, the isolation of the IPO signal in a diverse set of isotopic archives invites the reinterpretation of other paleoclimate proxies for identifying this historically overlooked forcing.
publishDate 2024
dc.date.none.fl_str_mv 2024-09
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/11336/263351
Orrison, R.; Vuille, M.; Rodrigues, J. C.; Stríkis, N. M.; Cruz, F.; et al.; Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation; Wiley; Journal of Geophysical Research: Atmospheres; 129; 17; 9-2024; 1-19
2169-897X
2169-8996
CONICET Digital
CONICET
url http://hdl.handle.net/11336/263351
identifier_str_mv Orrison, R.; Vuille, M.; Rodrigues, J. C.; Stríkis, N. M.; Cruz, F.; et al.; Pacific Interannual and Multidecadal Variability Recorded in δ 18 O of South American Summer Monsoon Precipitation; Wiley; Journal of Geophysical Research: Atmospheres; 129; 17; 9-2024; 1-19
2169-897X
2169-8996
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://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024JD040999
info:eu-repo/semantics/altIdentifier/doi/10.1029/2024JD040999
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
dc.publisher.none.fl_str_mv Wiley
publisher.none.fl_str_mv Wiley
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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