Centennial-scale precipitation anomalies in the southern Altiplano (18° S) suggest an extratropical driver for the South American summer monsoon during the late Holocene
Ignacio A. Jara et al.
Related subject area
Subject: Atmospheric Dynamics | Archive: Terrestrial Archives | Timescale: Centennial-DecadalLong-term global ground heat flux and continental heat storage from geothermal dataTwo types of North American droughts related to different atmospheric circulation patternsA millennial summer temperature reconstruction for northeastern Canada using oxygen isotopes in subfossil trees
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