Land surface atmosphere interaction in future South American climate using a multi-model ensemble
The land-atmosphere interaction for reference and future climate is estimated with a regional climate model ensemble. In reference climate, more than 50% of the models show interaction in southeastern South America during austral spring, summer and autumn. In future climate, the region remains a str...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2015 |
| País: | Argentina |
| Institución: | Consejo Nacional de Investigaciones Científicas y Técnicas |
| Repositorio: | CONICET Digital (CONICET) |
| Idioma: | inglés |
| OAI Identifier: | oai:ri.conicet.gov.ar:11336/4508 |
| Acceso en línea: | http://hdl.handle.net/11336/4508 |
| Access Level: | acceso abierto |
| Palabra clave: | LAND-ATMOSPHERE INTERACTION SOIL MOISTURE-PRECIPITATION COUPLING SOUTH AMERICA REGIONAL CLIMATE MODELING https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| Sumario: | The land-atmosphere interaction for reference and future climate is estimated with a regional climate model ensemble. In reference climate, more than 50% of the models show interaction in southeastern South America during austral spring, summer and autumn. In future climate, the region remains a strong hotspot although somewhat weakened due to the wet response that enhance energy limitation on the evapotranspiration. The region of the Brazilian Highlands and Matto Grosso appears as a new extensive hotspot during austral spring. This is related to a dry response which is probably accentuated by land surface feedbacks. |
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