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...
- 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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| 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. |
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2012 |
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2012 |
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2023-03-12T23:03:40Z |
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2023-03-12T23:03:40Z |
| dc.type.spa.fl_str_mv |
Artículo de investigación |
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http://purl.org/coar/resource_type/c_2df8fbb1 |
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https://purl.org/redcol/resource_type/ART |
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http://purl.org/coar/version/c_970fb48d4fbd8a85 |
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info:eu-repo/semantics/article |
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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 |
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4258 |
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25 |
| dc.relation.ispartofjournal.spa.fl_str_mv |
Journal of Climate |
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Derechos reservados - Está prohibida la reproducción parcial o total de esta publicación |
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info:eu-repo/semantics/openAccess |
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http://purl.org/coar/access_right/c_abf2 |
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Derechos reservados - Está prohibida la reproducción parcial o total de esta publicación http://purl.org/coar/access_right/c_abf2 |
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openAccess |
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application/pdf |
| dc.publisher.spa.fl_str_mv |
American Meteorological Society |
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Boston, Estados Unidos |
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Universidad de Antioquia |
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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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