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Scientific American|February 1, 1988
How climate evolved on the terrestrial planetsJ F Kasting, O B Toon, J B PollackScience (New York, N.Y.)|October 8, 1993
Dissipation of marine stratiform clouds and collapse of the marine boundary layer due to the depletion of cloud condensation nuclei by cloudsA S Ackerman, O B Toon, P V HobbsScience (New York, N.Y.)|December 12, 1986
Climatic consequences of very high carbon dioxide levels in the earth's early atmosphereJ F Kasting, T P AckermanIcarus|January 1, 1996
Simulations of Titan's brightness by a two-dimensional haze modelW T Hutzell, C P McKay, O B Toon, et al.American Journal of Science|May 1, 1986
A hybrid model of the CO2 geochemical cycle and its application to large impact eventsJ F Kasting, S M Richardson, J B Pollack, et al.Proceedings of the National Academy of Sciences of the United States of America|February 21, 2002
Arctic "ozone hole" in a cold volcanic stratosphereA Tabazadeh, K Drdla, M R Schoeberl, et al.Science (New York, N.Y.)|April 3, 2001
Role of the stratospheric polar freezing belt in denitrificationA Tabazadeh, E J Jensen, O B Toon, et al.Icarus|January 1, 1984
Response of Earth's atmosphere to increases in solar flux and implications for loss of water from VenusJ F Kasting, J B Pollack, T P AckermanPageof 3