Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes

ABSTRACT: This study shows that the North American monsoon system’s (NAMS) strength, onset, and retreat over northwestern Mexico exhibit multidecadal variations during the period 1948–2009. Two dry regimes, associated with late onsets, early retreats, and weaker rainfall rates, occurred in 1948–70 a...

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Autores:
Arias Gómez, Paola Andrea
Fu, Rong
Mo, Kingtse C.
Tipo de recurso:
Article of investigation
Fecha de publicación:
2012
Institución:
Universidad de Antioquia
Repositorio:
Repositorio UdeA
Idioma:
eng
OAI Identifier:
oai:bibliotecadigital.udea.edu.co:10495/33943
Acceso en línea:
https://hdl.handle.net/10495/33943
Palabra clave:
Cambio climático
Climate change
Multidecadal variability
Oscilación Multidecadal del Atlántico
http://vocabularies.unesco.org/thesaurus/concept4559
Rights
openAccess
License
Derechos reservados - Está prohibida la reproducción parcial o total de esta publicación
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oai_identifier_str oai:bibliotecadigital.udea.edu.co:10495/33943
network_acronym_str UDEA2
network_name_str Repositorio UdeA
repository_id_str
dc.title.spa.fl_str_mv Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
title Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
spellingShingle Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
Cambio climático
Climate change
Multidecadal variability
Oscilación Multidecadal del Atlántico
http://vocabularies.unesco.org/thesaurus/concept4559
title_short Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
title_full Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
title_fullStr Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
title_full_unstemmed Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
title_sort Decadal variation of rainfall seasonality in the North American monsoon region and its potential causes
dc.creator.fl_str_mv Arias Gómez, Paola Andrea
Fu, Rong
Mo, Kingtse C.
dc.contributor.author.none.fl_str_mv Arias Gómez, Paola Andrea
Fu, Rong
Mo, Kingtse C.
dc.contributor.researchgroup.spa.fl_str_mv Grupo de Ingeniería y Gestión Ambiental (GIGA)
dc.subject.unesco.none.fl_str_mv Cambio climático
Climate change
topic Cambio climático
Climate change
Multidecadal variability
Oscilación Multidecadal del Atlántico
http://vocabularies.unesco.org/thesaurus/concept4559
dc.subject.proposal.spa.fl_str_mv Multidecadal variability
Oscilación Multidecadal del Atlántico
dc.subject.unescouri.none.fl_str_mv http://vocabularies.unesco.org/thesaurus/concept4559
description ABSTRACT: This study shows that the North American monsoon system’s (NAMS) strength, onset, and retreat over northwestern Mexico exhibit multidecadal variations during the period 1948–2009. Two dry regimes, associated with late onsets, early retreats, and weaker rainfall rates, occurred in 1948–70 and 1991–2005, whereas a strong regime, associated with early onsets, late retreats, and stronger rainfall rates, occurred in 1971–90. A recovery of the monsoon strength was observed after 2005. This multidecadal variation is linked to the sea surface tem- perature anomalies’ (SSTAs) variability, which is a combination of the Atlantic multidecadal oscillation (AMO) and the warming SST trends. These SST modes appear to cause an anomalous cyclonic circulation and enhanced rainfall over the southeastern United States and the Gulf of Mexico, which in turn increases the atmospheric stability over the monsoon region. However, these SST modes cannot fully explain the circulation and rainfall anomalies observed during the early-retreat monsoons. An expansion of the North Atlantic surface high (NASH) in recent decades also contributes to the anomalous circulation associated with the early retreats of the NAMS. A northwestward expansion of the NASH further enhances the anomalous cyclonic circulation and rainfall over the southeastern United States and the Gulf of Mexico. Its associated northwestward shift of the subtropical jets over the western United States enhances subsidence over the NAMS region. The combined effects of the AMO, the warming trends, and the NASH expansion on atmospheric circulation contribute to a stronger and more persistent earlier retreat during the recent dry regime (1991–2005), while the earlier dry regime (1948–70) appears to be only influenced by the positive phase of the AMO.
publishDate 2012
dc.date.issued.none.fl_str_mv 2012
dc.date.accessioned.none.fl_str_mv 2023-03-12T23:03:40Z
dc.date.available.none.fl_str_mv 2023-03-12T23:03:40Z
dc.type.spa.fl_str_mv Artículo de investigación
dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_2df8fbb1
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dc.identifier.citation.spa.fl_str_mv Arias, P. A., Fu, R., & Mo, K. C. (2012). Decadal Variation of Rainfall Seasonality in the North American Monsoon Region and Its Potential Causes, Journal of Climate, 25(12), 4258-4274. doi: https://doi.org/10.1175/JCLI-D-11-00140.1
dc.identifier.issn.none.fl_str_mv 0894-8755
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/10495/33943
dc.identifier.doi.none.fl_str_mv 10.1175/JCLI-D-11-00140.1
dc.identifier.eissn.none.fl_str_mv 1520-0442
identifier_str_mv Arias, P. A., Fu, R., & Mo, K. C. (2012). Decadal Variation of Rainfall Seasonality in the North American Monsoon Region and Its Potential Causes, Journal of Climate, 25(12), 4258-4274. doi: https://doi.org/10.1175/JCLI-D-11-00140.1
0894-8755
10.1175/JCLI-D-11-00140.1
1520-0442
url https://hdl.handle.net/10495/33943
dc.language.iso.spa.fl_str_mv eng
language eng
dc.relation.ispartofjournalabbrev.spa.fl_str_mv J. Clim.
dc.relation.citationendpage.spa.fl_str_mv 4274
dc.relation.citationissue.spa.fl_str_mv 12
dc.relation.citationstartpage.spa.fl_str_mv 4258
dc.relation.citationvolume.spa.fl_str_mv 25
dc.relation.ispartofjournal.spa.fl_str_mv Journal of Climate
dc.rights.uri.spa.fl_str_mv Derechos reservados - Está prohibida la reproducción parcial o total de esta publicación
dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.coar.spa.fl_str_mv http://purl.org/coar/access_right/c_abf2
rights_invalid_str_mv Derechos reservados - Está prohibida la reproducción parcial o total de esta publicación
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.format.extent.spa.fl_str_mv 17
dc.format.mimetype.spa.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv American Meteorological Society
dc.publisher.place.spa.fl_str_mv Boston, Estados Unidos
institution Universidad de Antioquia
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spelling Arias Gómez, Paola AndreaFu, RongMo, Kingtse C.Grupo de Ingeniería y Gestión Ambiental (GIGA)2023-03-12T23:03:40Z2023-03-12T23:03:40Z2012Arias, P. A., Fu, R., & Mo, K. C. (2012). Decadal Variation of Rainfall Seasonality in the North American Monsoon Region and Its Potential Causes, Journal of Climate, 25(12), 4258-4274. doi: https://doi.org/10.1175/JCLI-D-11-00140.10894-8755https://hdl.handle.net/10495/3394310.1175/JCLI-D-11-00140.11520-0442ABSTRACT: This study shows that the North American monsoon system’s (NAMS) strength, onset, and retreat over northwestern Mexico exhibit multidecadal variations during the period 1948–2009. Two dry regimes, associated with late onsets, early retreats, and weaker rainfall rates, occurred in 1948–70 and 1991–2005, whereas a strong regime, associated with early onsets, late retreats, and stronger rainfall rates, occurred in 1971–90. A recovery of the monsoon strength was observed after 2005. This multidecadal variation is linked to the sea surface tem- perature anomalies’ (SSTAs) variability, which is a combination of the Atlantic multidecadal oscillation (AMO) and the warming SST trends. These SST modes appear to cause an anomalous cyclonic circulation and enhanced rainfall over the southeastern United States and the Gulf of Mexico, which in turn increases the atmospheric stability over the monsoon region. However, these SST modes cannot fully explain the circulation and rainfall anomalies observed during the early-retreat monsoons. An expansion of the North Atlantic surface high (NASH) in recent decades also contributes to the anomalous circulation associated with the early retreats of the NAMS. A northwestward expansion of the NASH further enhances the anomalous cyclonic circulation and rainfall over the southeastern United States and the Gulf of Mexico. Its associated northwestward shift of the subtropical jets over the western United States enhances subsidence over the NAMS region. The combined effects of the AMO, the warming trends, and the NASH expansion on atmospheric circulation contribute to a stronger and more persistent earlier retreat during the recent dry regime (1991–2005), while the earlier dry regime (1948–70) appears to be only influenced by the positive phase of the AMO.COL000861917application/pdfengAmerican Meteorological SocietyBoston, Estados UnidosDerechos reservados - Está prohibida la reproducción parcial o total de esta publicacióninfo:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Decadal variation of rainfall seasonality in the North American monsoon region and its potential causesArtículo de investigaciónhttp://purl.org/coar/resource_type/c_2df8fbb1https://purl.org/redcol/resource_type/ARThttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionCambio climáticoClimate changeMultidecadal variabilityOscilación Multidecadal del Atlánticohttp://vocabularies.unesco.org/thesaurus/concept4559J. 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