Summer soil-precipitation coupling in South America

The soil moisture memory contributes to atmospheric variability and seasonal predictability and could potentially affect the development of the South American Monsoon System. The relative importance of the local land surface feedbacks and the large-scale dynamical processes during the different phas...

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Autor principal: Sörensson, A.A
Otros Autores: Menéndez, C.G
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2011
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100 1 |a Sörensson, A.A. 
245 1 0 |a Summer soil-precipitation coupling in South America 
260 |c 2011 
270 1 0 |m Sörensson, A.A.; CIMA, CONICET, UBA, Ciudad Universitaria, Pabellón 2, Piso 2, 1428, Buenos Aires, Argentina; email: sorensson@cima.fcen.uba.ar 
506 |2 openaire  |e Política editorial 
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520 3 |a The soil moisture memory contributes to atmospheric variability and seasonal predictability and could potentially affect the development of the South American Monsoon System. The relative importance of the local land surface feedbacks and the large-scale dynamical processes during the different phases of the monsoon are still largely unknown. We examine the impacts of land surface conditions during the mature monsoon phase with the Rossby Centre Atmospheric regional model through calculating the coupling strength between soil moisture, evapotranspiration and precipitation. Regions of high coupling strength (hotspots) are identified and analysed focusing on the link between soil moisture-evapotranspiration coupling and soil moisture-precipitation coupling, the relation between the coupling strength and seasonal predictability and the hotspots importance for extreme precipitation events. La Plata Basin and northeastern Brazil are identified as hotspots due to evapotranspiration recycling. A region within the South Atlantic Convergence Zone is identified as a hotspot of precipitation explained by moisture advection. Extreme precipitation events are repressed in parts of La Plata Basin when the link between precipitation and soil moisture is cut through using prescribed soil moisture. ©2010 The Authors Tellus A©2010 International Meteorological Institute in Stockholm.  |l eng 
593 |a Centro de Investigaciones del Mar y la Atmósfera, CONICET, UBA, Buenos Aires, Argentina 
593 |a Departamento de Ciencias de la Atmósfera y los Océanos, FCEN, UBA, Buenos Aires, Argentina 
690 1 0 |a ADVECTION 
690 1 0 |a COUPLING 
690 1 0 |a EVAPOTRANSPIRATION 
690 1 0 |a MONSOON 
690 1 0 |a PRECIPITATION (CLIMATOLOGY) 
690 1 0 |a SOIL MOISTURE 
690 1 0 |a SUMMER 
690 1 0 |a BRAZIL 
690 1 0 |a LA PLATA BASIN 
700 1 |a Menéndez, C.G. 
773 0 |d 2011  |g v. 63  |h pp. 56-68  |k n. 1  |p Tellus Ser. A Dyn. Meteorol. Oceanogr.  |x 02806495  |w (AR-BaUEN)CENRE-55  |t Tellus, Series A: Dynamic Meteorology and Oceanography 
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