Spatial extent of the North American Monsoon: Increased cross-regional linkages via atmospheric pathways

ABSTRACT: The North American monsoon is a key featureaffecting summer climate over Southwestern NorthAmerica. During the monsoon, evapotranspiration fromthe Southwest promotes transference of water to theatmosphere which is subsequently distributed across thecontinent - linking the SW to other regio...

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Autores:
Villegas Palacio, Juan Camilo
Breshears, David D.
Dominguez, Francina
Tipo de recurso:
Article of investigation
Fecha de publicación:
2009
Institución:
Universidad de Antioquia
Repositorio:
Repositorio UdeA
Idioma:
eng
OAI Identifier:
oai:bibliotecadigital.udea.edu.co:10495/37290
Acceso en línea:
https://hdl.handle.net/10495/37290
Palabra clave:
Humedad
Humidity
Monzones
Monsoons
América del Norte
North America
Evapotranspiración
Evapotranspiration
Sequía
Drought
Humedad específica
Specific humidity
http://aims.fao.org/aos/agrovoc/c_68e36bf6
http://aims.fao.org/aos/agrovoc/c_5219
http://aims.fao.org/aos/agrovoc/c_2741
http://aims.fao.org/aos/agrovoc/c_2391
http://aims.fao.org/aos/agrovoc/c_d6fe7a82
http://vocabularies.unesco.org/thesaurus/concept12053
Rights
openAccess
License
https://creativecommons.org/licenses/by-nc-nd/4.0/
Description
Summary:ABSTRACT: The North American monsoon is a key featureaffecting summer climate over Southwestern NorthAmerica. During the monsoon, evapotranspiration fromthe Southwest promotes transference of water to theatmosphere which is subsequently distributed across thecontinent - linking the SW to other regions via atmospherichydrologic connectivity. However, the degree to whichatmospheric connectivity redistributes monsoonal terrestrialmoisture throughout the continent and its sensitivity toclimate disturbances such as drought is uncertain. Wetracked the trajectory of moisture evapotranspired within thesemiarid Southwest during the monsoon season using aLagrangian analytical model. Southwest moisture wasadvected north-east accounting for 15% of precipitationin adjacent Great Plains regions. During recent drought(2000–2003), this amount decreased by 45%. Our resultsillustrate that the spatial extent of the North Americanmonsoon is larger than normally considered when accountingfor hydrologic connectivity via soil moisture redistributionthrough atmospheric pathways.