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Nature|June 11, 2004
High levels of atmospheric carbon dioxide necessary for the termination of global glaciationRaymond T PierrehumbertChaos (Woodbury, N.Y.)|June 5, 2003
Surface quasigeostrophic turbulence: The study of an active scalarJai Sukhatme, Raymond T. PierrehumbertPhysical Review. E, Statistical, Nonlinear, and Soft Matter Physics|January 7, 2003
Decay of passive scalars under the action of single scale smooth velocity fields in bounded two-dimensional domains: from non-self-similar probability distribution functions to self-similar eigenmodesJai Sukhatme, Raymond T PierrehumbertProceedings. Mathematical, Physical, and Engineering Sciences|July 21, 2016
Dynamics of atmospheres with a non-dilute condensible componentRaymond T Pierrehumbert, Feng DingJournal of Geophysical Research. Planets|January 2, 2023
CO<sub>2</sub> Ocean Bistability on Terrestrial ExoplanetsR J Graham, Tim Lichtenberg, Raymond T PierrehumbertProceedings of the National Academy of Sciences of the United States of America|November 24, 2006
The dynamics behind Titan's methane cloudsJonathan L Mitchell, Raymond T Pierrehumbert, Dargan M W Frierson, et al.Journal of Geophysical Research. Planets|March 29, 2021
Vertically Resolved Magma Ocean-Protoatmosphere Evolution: H<sub>2</sub>, H<sub>2</sub>O, CO<sub>2</sub>, CH<sub>4</sub>, CO, O<sub>2</sub>, and N<sub>2</sub> as Primary AbsorbersTim Lichtenberg, Dan J Bower, Mark Hammond, et al.Astrobiology|July 17, 2013
The effect of host star spectral energy distribution and ice-albedo feedback on the climate of extrasolar planetsAomawa L Shields, Victoria S Meadows, Cecilia M Bitz, et al.Pageof 1