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Francesco S.R. Pausata
University of Quebec in Montreal (UQAM)Meeting roles in:
Hydroclimate-vegetation feedbacks drive Holocene temperature variability in Southeast Asia
40,000 Years of Southeast Asian Hydroclimate Variability from Cave Archives
Comparing Multi-Model Ensemble Simulations with Observations and Decadal Projections of Upper Atmospheric Variations Following the Hunga Eruption
Tropical Small-Scale Nuclear War Fire Emissions Cause Greater Ozone Depletion Than Extratropical Large-Scale Conflicts
Potential climate effects of a low aerosol forcing nuclear war
Closing the Proxy-Model Gap for the African Humid Period by Accounting for Vegetation Feedbacks
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