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Land surface–atmosphere interaction in future South American climate using a multi‐model ensemble
Author(s) -
Ruscica R. C.,
Menéndez C. G.,
Sörensson A. A.
Publication year - 2016
Publication title -
atmospheric science letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.951
H-Index - 45
ISSN - 1530-261X
DOI - 10.1002/asl.635
Subject(s) - evapotranspiration , climate model , environmental science , climatology , hotspot (geology) , climate change , atmosphere (unit) , general circulation model , atmospheric sciences , geography , meteorology , geology , ecology , oceanography , geophysics , biology
Abstract 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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