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...

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Autores principales:	Ruscica, Romina, Menendez, Claudio Guillermo, Sorensson, Anna Amelia
Publicado:	2016
Materias:	Coupling Land-atmosphere interaction Precipitation Regional climate modeling Soil moisture South America climate modeling ensemble forecasting evapotranspiration land surface precipitation (climatology) regional climate soil moisture Brazil Mato Grosso
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_1530261X_v17_n2_p141_Ruscica http://hdl.handle.net/20.500.12110/paper_1530261X_v17_n2_p141_Ruscica
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	paper:paper_1530261X_v17_n2_p141_Ruscica
record_format	dspace
spelling	paper:paper_1530261X_v17_n2_p141_Ruscica2023-06-08T16:19:43Z Land surface-atmosphere interaction in future South American climate using a multi-model ensemble Ruscica, Romina Menendez, Claudio Guillermo Sorensson, Anna Amelia Coupling Land-atmosphere interaction Precipitation Regional climate modeling Soil moisture South America climate modeling ensemble forecasting evapotranspiration land surface precipitation (climatology) regional climate soil moisture Brazil Mato Grosso 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. © 2016 Royal Meteorological Society. Fil:Ruscica, R.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Menéndez, C.G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Sörensson, A.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2016 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_1530261X_v17_n2_p141_Ruscica http://hdl.handle.net/20.500.12110/paper_1530261X_v17_n2_p141_Ruscica
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Coupling Land-atmosphere interaction Precipitation Regional climate modeling Soil moisture South America climate modeling ensemble forecasting evapotranspiration land surface precipitation (climatology) regional climate soil moisture Brazil Mato Grosso
spellingShingle	Coupling Land-atmosphere interaction Precipitation Regional climate modeling Soil moisture South America climate modeling ensemble forecasting evapotranspiration land surface precipitation (climatology) regional climate soil moisture Brazil Mato Grosso Ruscica, Romina Menendez, Claudio Guillermo Sorensson, Anna Amelia Land surface-atmosphere interaction in future South American climate using a multi-model ensemble
topic_facet	Coupling Land-atmosphere interaction Precipitation Regional climate modeling Soil moisture South America climate modeling ensemble forecasting evapotranspiration land surface precipitation (climatology) regional climate soil moisture Brazil Mato Grosso
description	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. © 2016 Royal Meteorological Society.
author	Ruscica, Romina Menendez, Claudio Guillermo Sorensson, Anna Amelia
author_facet	Ruscica, Romina Menendez, Claudio Guillermo Sorensson, Anna Amelia
author_sort	Ruscica, Romina
title	Land surface-atmosphere interaction in future South American climate using a multi-model ensemble
title_short	Land surface-atmosphere interaction in future South American climate using a multi-model ensemble
title_full	Land surface-atmosphere interaction in future South American climate using a multi-model ensemble
title_fullStr	Land surface-atmosphere interaction in future South American climate using a multi-model ensemble
title_full_unstemmed	Land surface-atmosphere interaction in future South American climate using a multi-model ensemble
title_sort	land surface-atmosphere interaction in future south american climate using a multi-model ensemble
publishDate	2016
url	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_1530261X_v17_n2_p141_Ruscica http://hdl.handle.net/20.500.12110/paper_1530261X_v17_n2_p141_Ruscica
work_keys_str_mv	AT ruscicaromina landsurfaceatmosphereinteractioninfuturesouthamericanclimateusingamultimodelensemble AT menendezclaudioguillermo landsurfaceatmosphereinteractioninfuturesouthamericanclimateusingamultimodelensemble AT sorenssonannaamelia landsurfaceatmosphereinteractioninfuturesouthamericanclimateusingamultimodelensemble
_version_	1768546132813676544

Land surface-atmosphere interaction in future South American climate using a multi-model ensemble

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