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, R.C., Menéndez, C.G., Sörensson, A.A.
Formato: JOUR
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: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 todo:paper_1530261X_v17_n2_p141_Ruscica
record_format dspace
spelling todo:paper_1530261X_v17_n2_p141_Ruscica2023-10-03T16:21:14Z Land surface-atmosphere interaction in future South American climate using a multi-model ensemble Ruscica, R.C. Menéndez, C.G. Sörensson, A.A. 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. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar 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, R.C.
Menéndez, C.G.
Sörensson, A.A.
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.
format JOUR
author Ruscica, R.C.
Menéndez, C.G.
Sörensson, A.A.
author_facet Ruscica, R.C.
Menéndez, C.G.
Sörensson, A.A.
author_sort Ruscica, R.C.
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
url http://hdl.handle.net/20.500.12110/paper_1530261X_v17_n2_p141_Ruscica
work_keys_str_mv AT ruscicarc landsurfaceatmosphereinteractioninfuturesouthamericanclimateusingamultimodelensemble
AT menendezcg landsurfaceatmosphereinteractioninfuturesouthamericanclimateusingamultimodelensemble
AT sorenssonaa landsurfaceatmosphereinteractioninfuturesouthamericanclimateusingamultimodelensemble
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