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Stephan Fueglistaler
Princeton UniversityMeeting roles in:
Transition to Periodic Precipitation in a Warmer Climate due to Stronger Convectively-Coupled Waves
Expansion of Tropical Ascent with Warming in Idealized Mock-Walker Simulations
Subtropical Pacific Cooling Driven by Land Precipitation Response to CO2 Forcing
The complex relation between global mean temperature and radiative fluxes due to internal variability
Assessing the Variability of Earth's Energy Imbalance in the Early 21st Century with Two High-Resolution Coupled Models
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