The DOI matches its Crossref record; 47 of the 47 references it cites were found in a registry or an index.
Runaway and moist greenhouse atmospheres and the evolution of Earth and Venus
Abstract
A one-dimensional climate model is used to study the response of an Earth-like atmosphere to large increases in solar flux. For fully saturated, cloud-free conditions, the critical solar flux at which a runaway greenhouse occurs, that is, the oceans evaporate entirely, is found to be 1.4 times the present flux at Earth's orbit (S0). This value is close to the flux expected at Venus' orbit early in solar system history. Is is nearly independent of the amount of CO2 present in the atmosphere, but is sensitive to the H2O absorption coefficient in the 8- to 12-micrometers window region. Clouds should tend to depress the surface temperature on a warm, moist planet; thus, Venus may originally have had oceans if its initial water endowment was close to that of Earth. It lost them early in its history, however, because of rapid photodissociation of water vapor followed by escape of hydrogen to space. The critical solar flux above which water is rapidly lost could be as low as 1.1S0. The surface temperature of a runaway greenhouse atmosphere containing a full ocean's worth of water would have been in excess of 1500 degrees K--above the solidus for silicate rocks. The presence of such a steam atmosphere during accretion may have significantly influenced the early thermal evolution of both Earth and Venus.
Overview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
In the citing paper
“A planet on the inner edge of the habitable zone (see Chapter 5) could conceivably have a large abiotic buildup of oxygen through a runaway greenhouse effect while the oceans evaporate; after photodissociation of water in the atmosphere, hydrogen could escape, leaving oxygen behind (Kasting, 1988).”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Kasting, 1988
Citations
Cites
A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature
Walker, J. C. G., Hays, P. B., & Kasting, J. F. (1981) · Journal of Geophysical Research: Oceans · doi:10.1029/jc086ic10p09776 · Cited by 2,310
Self-citationThe Chemical Evolution of the Atmosphere and Oceans
Holland, H. D. (1984) · doi:10.1515/9780691220239 · Cited by 1,836
Evolution of the protoplanetary cloud and formation of the earth and the planets
Safronov, V. S. (1972) · Medical Entomology and Zoology · Cited by 1,288
Optical Properties of the Atmosphere
Cox, L. J. (1979) · Optica Acta International Journal of Optics · doi:10.1080/713820031 · Cited by 996
Solar interior structure and luminosity variations
Gough, D. O. (1981) · Solar Physics · doi:10.1007/bf00151270 · Cited by 798
Kell, G. S., Gallagher, J. S., & Haar, L. (1984) · Cited by 512
Origin and Evolution of Planetary and Satellite Atmospheres
(1989) · University of Arizona Press eBooks · doi:10.2307/j.ctv20dsb5m · Cited by 505
Venus Was Wet: A Measurement of the Ratio of Deuterium to Hydrogen
Donahue, T. M., Hoffman, J. H., Hodges, R. R., & Watson, A. J. (1982) · Science · doi:10.1126/science.216.4546.630 · Cited by 446
Climatic consequences of very high carbon dioxide levels in the earth’s early atmosphere
Kasting, J. F., & Ackerman, T. P. (1986) · Science · doi:10.1126/science.11539665 · Cited by 391
Self-citationThe Solar spectrum 2935Å to 8770Å :
Moore, C. E., Minnaert, M. G. J., & Houtgast, J. (1966) · doi:10.6028/nbs.mono.61 · Cited by 379
Cited by
Sorted by citations
Items 501–600 of 708
Habitable Zones in Extrasolar Planetary Systems
Franck, S., von Bloh, W., Bounama, C., Steffen, M., Schönberner, D., & Schellnhuber, H. J. (2002) · Springer eBooks · doi:10.1007/978-3-642-59381-9_4 · Cited by 7
Formation of the terrestrial planets
Kaula, W. M. (1994) · Earth Moon and Planets · doi:10.1007/bf00613285 · Cited by 7
Characterizing the Radiative–Convective Structure of Dense Rocky Planet Atmospheres
Cmiel, J., Wordsworth, R., & Seeley, J. T. (2025) · The Planetary Science Journal · doi:10.3847/psj/adcd5f · Cited by 11
“These “steam” atmospheres have historically been considered fully convective in post-runaway greenhouse scenarios (Kasting 1988), but recent work (Selsis et al. 2023) shows that strong near-infrared H 2 O absorption can maintain a radiative layer near the surface, reducing T s relative to a purely…”
Venus Cloud Research: Progress and Perspectives
Dai, L., Titov, D. V., Shao, W., Zhang, X., Cui, J. X., & Fan, S. (2025) · Space Science Reviews · doi:10.1007/s11214-025-01176-4 · Cited by 6
“According to this hypothesis, complete evaporation of the oceans on the Earth in future may just be a matter of time as the solar luminosity grows (Kasting 1988; Goldblatt et al. 2013).”
Effects of Transient Stellar Emissions on Planetary Climates of Tidally Locked Exo-Earths
Chen, H., Luca, P. D., Hochman, A., & Komacek, T. D. (2025) · The Astronomical Journal · doi:10.3847/1538-3881/add33e · Cited by 12
Climatological and ultraviolet‐based habitability of possible exomoons in F‐star systems
Sato, S., Wang, Z., & Cuntz, M. (2017) · Astronomische Nachrichten · doi:10.1002/asna.201613279 · Cited by 6
From exo-Earths to exo-Venuses: Flux and polarization signatures of reflected light
Mahapatra, G., Abiad, F., Rossi, L., & Stam, D. M. (2023) · Astronomy and Astrophysics · doi:10.1051/0004-6361/202243190 · Cited by 6
Saunders, W., Person, M. J., Withers, P. G., French, R. G., & Tubthong, C. (2024) · The Planetary Science Journal · doi:10.3847/psj/ad7c4d · Cited by 6
Effective stellar flux calculations for limits of life-supporting zones of exoplanets
Ludwig, W., Eggl, S., Neubauer, D., Leitner, J. J., Firneis, M. G., & Hitzenberger, R. (2016) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stw509 · Cited by 7
Exoplanets: Possible Biosignatures
Claudi, R. (2017) · Frontier Research in Astrophysics Workshop (FRAPWS) · doi:10.22323/1.269.0061 · Cited by 7
Litvak, M. L., & Sanin, A. B. (2018) · Physics-Uspekhi · doi:10.3367/ufne.2017.04.038277 · Cited by 6
Explicit cloud representation in the Atmos 1D climate model for Earth and rocky planet applications
Fauchez, T. J., Arney, G., Kopparapu, R., & Domagal-Goldman, S. (2018) · AIMS Geosciences · doi:10.3934/geosci.2018.4.180 · Cited by 9
Seeding the Solar System with Life: Mars, Venus, Earth, Moon, Protoplanets
Joseph, R. G., Planchon, O., Gibson, C. H., & Schild, R. E. (2020) · Open Astronomy · doi:10.1515/astro-2020-0019 · Cited by 6
“Above this threshold, the loss of water by vaporization is irreversible and the oceans disappear completely in a few million years (Ingersoll 1969; Kasting 1998; Kasting et al. 2014; Wolf and Toon 2015).”
BackgroundGeoscience for Understanding Habitability in the Solar System and Beyond
Dehant, V., Debaille, V., Dobos, V., Gaillard, F., & Gillmann, C. (2019) · Repository of the Academy's Library (Library of the Hungarian Academy of Sciences) · Cited by 7
Venus as an Analog for Hot Earths
Arney, G. (2005) · University of Arizona Press eBooks · doi:10.2458/azu_uapress_9780816540068-ch014 · Cited by 12
“Kasting (1988) concluded that Venus could have maintained its oceans for 600 million years after its formation before losing them to the moist greenhouse, but this study excludes the effect of clouds that lengthen the interval of possible habitability (Section 3.1).”
BackgroundInfluentialEvolving CO2 Rather Than SST Leads to a Factor of Ten Decrease in GCM Convergence Time
Zhang, Y., Bloch‐Johnson, J., Romps, D. M., & Abbot, D. S. (2021) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2021ms002505 · Cited by 6
Evolution of Life and Precambrian Bio-Geology
Eriksson, P. G., Altermann, W., Nelson, D. R., Mueller, W. U., & Catuneanu, O. (2004) · Developments in precambrian geology · doi:10.1016/s0166-2635(04)80008-2 · Cited by 6
Isotopic Fractionation by Gravitational Escape
Lammer, H., & Bauer, S. J. (2003) · Space sciences series of ISSI · doi:10.1007/978-94-010-0145-8_18 · Cited by 6
Geophysiology and habitable zones around sun-like stars
SCHWARTZMAN, D. W., & Volk, T. (2008) · Springer eBooks · doi:10.1007/3-540-54752-5_208 · Cited by 6
An experimental approach to production of peptide-like compounds in the early terrestrial planets
Marcano, V., Benítez, P., & Palacios‐Prü, E. (2001) · Planetary and Space Science · doi:10.1016/s0032-0633(00)00172-0 · Cited by 7
Stevenson, D. J. (1988) · Nature · doi:10.1038/335587a0 · Cited by 6
Miniaturised Instrumentation for the Detection of Biosignatures in Ocean Worlds of the Solar System
Chela-Flores, J. (2021) · Frontiers in Space Technologies · doi:10.3389/frspt.2021.703809 · Cited by 5
“There is evidence that initially Venus was an ocean world (Kasting et al., 1984; Kasting, 1988; Donahue and Russell, 1997; Grinspoon and Bullock, 2003).”
BackgroundHot Earth or Young Venus? A nearby transiting rocky planet mystery
Kaltenegger, L., Payne, R. C., Lin, Z., Kasting, J. F., & Delrez, L. (2023) · Monthly Notices of the Royal Astronomical Society Letters · doi:10.1093/mnrasl/slad064 · Cited by 5
“, Kasting, J. F. and Meadows, V. (2005) ‘Biosignatures from Earth-like planets around M dwarfs, ASTROBIOLOGY, 2(6), pp.”
BackgroundMethodInfluentialSelf-citationPlanetary system architectures with low-mass inner planets
Desgrange, C., Milli, J., Chauvin, G., Henning, T. K., Luashvili, A., Read, M., Wyatt, M. C., Kennedy, G. M., Burn, R., Schlecker, M., et al. (2023) · Astronomy and Astrophysics · doi:10.1051/0004-6361/202346863 · Cited by 5
Weller, M. B., & Kiefer, W. S. (2025) · Science Advances · doi:10.1126/sciadv.adn9861 · Cited by 9
“In the moist greenhouse state, rapid water loss is thought to occur due to water vapor mixing in the stratosphere and subsequent hydrogen escape to space (a processes we do not consider here in our outgassing experiments) [e.g., ( 54 , 55 )].”
Esposito, L. W. (2012) · Nature Geoscience · doi:10.1038/ngeo1675 · Cited by 5
Three eras of planetary exploration
Ingersoll, A. P. (2017) · Nature Astronomy · doi:10.1038/s41550-016-0010 · Cited by 5
Statistical Distribution of Exoplanets
Cumming, A. (2010) · Cited by 6
Opening a new window to other worlds with spectropolarimetry
Mohler-Fischer, M., Bühl, J., Doherty, S., Eggl, S., Eybl, V., Farago, F., Jacimovic, A., Hunger, L., Lauritsen, N. L. B., Ludena, D., et al. (2010) · Experimental Astronomy · doi:10.1007/s10686-010-9193-2 · Cited by 5
“This is believed to have happened on Venus, making it a dry planet with a dense CO2 atmosphere [35].”
BackgroundImpact of Stellar Activity on the Evolution of Planetary Atmospheres and Habitability
Lammer, H., Khodachenko, M. L., Lichtenegger, H., & Kulikov, Y. N. (2007) · doi:10.1002/9783527621361.ch6 · Cited by 5
Search for Extra-Terrestrial planets: The DARWIN mission - Target Stars and Array ArchitecturesPreprint
Kaltenegger, L. (2005) · arXiv (Cornell University) · doi:10.48550/arxiv.astro-ph/0504497 · Cited by 5
“Two major processes have changed the primitive atmosphere, the reduction of CO2 and the increase of O2 (Kasting, 1988).”
BackgroundMethodInfluentialMetal‐Silicate Partitioning of Siderophile Elements and Core‐Mantle Segregation
Righter, K. (2016) · Geophysical monograph · doi:10.1002/9781118992487.ch13 · Cited by 5
Using Venus, Earth, and Mars to Understand Exoplanet Volatile and Climate Evolution
JAKOSKY, B. M., & Byrne, P. K. (2025) · Journal of Geophysical Research Planets · doi:10.1029/2024je008882 · Cited by 4
“The thick atmosphere and hot surface of Venus are thought to have resulted from a “runaway greenhouse” (Kasting, 1988).”
Jorge, J., Wordsworth, R., & Adams, D. (2024) · Journal of Geophysical Research Planets · doi:10.1029/2024je008443 · Cited by 5
“Finally, for intercomparison of the output of PCM LBL with other 1D radiative‐convective models such as Clima (Kasting, 1988; Kopparapu et al., 2013) and the linearized flux evolution (LiFE) model developed by Robinson and Crisp (2018), see Ding and Wordsworth (2019).”
Metamorphism of Venus as driver of crustal thickness and recycling
Semprich, J., Filiberto, J. R., Weller, M. B., Gorce, J. S., & Clark, N. D. (2025) · Nature Communications · doi:10.1038/s41467-025-58324-1 · Cited by 5
“The high deuterium to hydrogen ratio 19 suggests that early Venus had water levels comparable to those on Earth 20 but has lost a signi fi cant amount of water after its formation; although, there is substantial uncertainty about the timingandmechanismof this process 21 – 27 .”
Microbial palaeontology and the origin of life: a personal approach
Westall, F. (2016) · HAL · doi:10.4435/bspi.2016.09 · Cited by 4
Escape of planetary atmospheres: physical processes and numerical models
Shematovich, V. I., & Marov, M. Y. (2017) · Uspekhi Fizicheskih Nauk · doi:10.3367/ufnr.2017.09.038212 · Cited by 4
A silicon carbide high gain differential amplifier for extreme temperature applications
Yang, J., & Zhu, J. (2022) · Microelectronics Journal · doi:10.1016/j.mejo.2022.105632 · Cited by 4
Fundamentals for habitable scenarios for Earth-like planets in the TRAPPIST-1 system
Payne, R. C., & Kaltenegger, L. (2024) · Monthly Notices of the Royal Astronomical Society Letters · doi:10.1093/mnrasl/slae013 · Cited by 4
Wanderley, F., Cunha, K., Smith, V. V., Kochukhov, O., Souto, D., Prieto, C. A., Mahadevan, S., Majewski, S. R., Muirhead, P. S., Pinsonneault, M. H., et al. (2024) · The Astrophysical Journal · doi:10.3847/1538-4357/ad7959 · Cited by 4
“In the runaway greenhouse limit, water cannot condense into liquid droplets, and the stratosphere is dominated by water vapor, which suffers photolysis from stellar X-ray and EUV radiation, causing the loss of hydrogen, which results in an efficient mechanism for water loss (Kasting 1988).”
BackgroundKorenaga, J. (2025) · Icarus · doi:10.1016/j.icarus.2025.116743 · Cited by 6
The Surface and Atmosphere of Venus: Evolution and Present State
Grinspoon, D. (2013) · Springer eBooks · doi:10.1007/978-1-4614-5064-1_3 · Cited by 2
“vapor feedback (Kasting et al. 1984; Kasting 1988) followed by loss of hydrogen through various thermal and non thermal escape processes, including Jeans escape, charge exchange, collisional ejection (Kumar et al.”
BackgroundShukure, N. T., Tessema, S. B., & Gopalswamy, N. (2021) · The Astrophysical Journal · doi:10.3847/1538-4357/ac0894 · Cited by 4
Coppedè, F., Bosco, P., Fuso, A., & Troen, A. M. (2012) · Current Gerontology and Geriatrics Research · doi:10.1155/2012/926082 · Cited by 5
Parametrizations of global thermal emissions for simple climate models
Marani, M. (1999) · Climate Dynamics · doi:10.1007/s003820050273 · Cited by 4
“This phenomenon is called the runaway greenhouse e⁄ect (Simpson 1927; Komabayasi 1967; Ingersoll 1969; Kasting 1988; Nakajima et al. 1992) and has been shown to occur in radiative-convective equilibrium models ( Renno‘ et al. 1994).”
BackgroundCan Venus shed microorganisms?
Konesky, G. A. (2009) · Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE · doi:10.1117/12.828643 · Cited by 4
A climatic thermostat making Earth habitable
Ditlevsen, P. (2005) · International Journal of Astrobiology · doi:10.1017/s1473550405002302 · Cited by 4
“This apparent paradox is dubbed: ‘The Faint Young Sun Problem’ (Kasting 1988).”
BackgroundThe evolution of planets. Venus as the Earth’s probable future
Dobretsov, N. L. (2017) · Russian Geology and Geophysics · doi:10.1016/j.rgg.2016.12.001 · Cited by 4
Exobiological habitats: An overview
Doyle, L. R., & McKay, C. P. (2008) · Springer eBooks · doi:10.1007/3-540-54752-5_209 · Cited by 4
A comment on tectonics and the future of terrestrial life
Gerstell, M. F., & Yung, Y. L. (2003) · Precambrian Research · doi:10.1016/s0301-9268(02)00143-2 · Cited by 4
“Even if anthropogenic greenhouse gases are controlled, it is expected that earth will lose its water to a moist greenhouse, due to a brightening sun, in about 1.1 billion years (Sackmann et al., 1993; Kasting, 1988).”
BackgroundInfluentialInterior and Climate Modeling of the Venus Zone Planet TOI-2285 b
Miles, E. L., Ostberg, C. M., Kane, S. R., Clarkson, O., Unterborn, C. T., Fetherolf, T., Way, M. J., & Welter, S. G. (2025) · The Astronomical Journal · doi:10.3847/1538-3881/add71c · Cited by 3
“We have found that in all cases, we do not encounter moist greenhouse conditions, which are uninhabitable conditions resulting from high temperatures and drastic water loss (Kasting 1988).”
Deb, S., Sharma, K. K., Biswas, S., & Medhi, B. J. (2025) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/staf1057 · Cited by 4
Kane, S. R., Bott, K., Gordon, K. E. G., Miles, E. L., Ostberg, C. M., Byrne, P. K., Carone, L., Daylan, T., Muñoz, A. G., Harada, C. K., et al. (2026) · Publications of the Astronomical Society of the Pacific · doi:10.1088/1538-3873/ae417d · Cited by 3
“Venus is an archetype of runaway greenhouse conditions, with a dense, CO 2 - dominated atmosphere, a surface pressure a factor of ∼ 90 than Earth, pervasive sulfuric-acid cloud decks, and a surface temperature hot enough to preclude stable liquid water (Ingersoll 1969; Kasting 1988).”
Lichtenberg, T., Schaefer, L., Krissansen‐Totton, J., Miguel, Y., Sergeev, D. E., Baumeister, P., Cmiel, J., Janssen, L. J., Nguyen, T. G., Miyazaki, Y., et al. (2026) · The Planetary Science Journal · doi:10.3847/psj/ae593b · Cited by 9
“Abe & T. Matsui 1985; J. F. Kasting 1988; L. T. Elkins-Tanton 2008).”
InfluentialPossibility for albedo estimation of exomoons: Why should we care about M dwarfs?
Dobos, V., Kereszturi, Á., Pál, A., & Kiss, L. (2016) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201526672 · Cited by 3
“Too much incident flux on a moon can trigger the runaway greenhouse effect, which leads to the Article published by EDP Sciences A139, page 1 of 13 loss of water reservoirs on the body, hence making it uninhabitable (Kasting 1988).”
BackgroundWITHDRAWN: The terrestrial magma ocean hypothesis
Solomatov, V. S. (2015) · Gondwana Research · doi:10.1016/j.gr.2015.07.018 · Cited by 3
Maruyama, S., Ebisuzaki, T., & Kurokawa, K. (2019) · Frontier Research in Astrophysics Workshop (FRAPWS) · doi:10.22323/1.331.0071 · Cited by 3
“Maximum limited is given from [8], and minimum limit is given by the life’s activity.”
BackgroundInfluentialPossibility for albedo estimation of exomoons: Why should we care about M dwarfs?
Dobos, V., Keresztúri, Á., Pál, A., & Kiss, L. L. (2016) · Repository of the Academy's Library (Library of the Hungarian Academy of Sciences) · Cited by 3
Marcos-Arenal, P., Cerdán, L., Burillo-Villalobos, M., Bonilla, N. F., de la Concepción, J. G., López-Cayuela, M.-Á., Gómez, F., & Caballero, J. A. (2022) · Universe · doi:10.3390/universe8120624 · Cited by 3
Geochemical and dynamical views on the origin of Earth's atmosphere and oceans
Marty, B. M., & Genda, H. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00106-6 · Cited by 4
The evolutionary divergence of Mars, Venus, and Earth
Hamano, K., Gillmann, C., Golabek, G., Lourenço, D. L., & Westall, F. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00104-2 · Cited by 6
Habitability: the Point of View of an Astronomer
Selsis, F. (2007) · Springer eBooks · doi:10.1007/978-3-540-33693-8_7 · Cited by 5
“Note the cut in the X-axis between 600 and 1400 K. Figure adapted from Kasting (1988)”
BackgroundMethodInfluentialThe young Sun and its influence on planetary atmospheres
Güdel, M., & Kasting, J. F. (2011) · Cambridge University Press eBooks · doi:10.1017/cbo9780511933875.013 · Cited by 3
“In relevant models, water evaporated from the initial oceans due to a more efficient greenhouse (Ingersoll, 1969; Kasting, 1988) and then dissociated in the high atmosphere due to strong solar EUV irradiation (Kasting and Pollack, 1983).”
Self-citationAstrobiological Potential of Planetary Bodies Within the Solar System
Schulze‐Makuch, D., & Irwin, L. N. (2018) · Springer eBooks · doi:10.1007/978-3-319-97658-7_11 · Cited by 3
Fundamental challenges to remote sensing of exo-earths
Paradise, A., Kristen Menou, A., Lee, C., & Fan, B. L. (2022) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stac724 · Cited by 3
Kahn, R. A., & Appleby, J. F. (1991) · Reviews of Geophysics · doi:10.1002/rog.1991.29.s1.328 · Cited by 3
Stellar-Planetary Relations: Atmospheric Stability as a Prerequisite for Planetary Habitability
Lammer, H., Kulikov, Y. N., Penz, T., Leitner, M., Biernat, H. K., & Erkaev, N. V. (2005) · Celestial Mechanics and Dynamical Astronomy · doi:10.1007/s10569-005-0004-4 · Cited by 3
Spectroscopic Signatures of Life on Exoplanets – The Darwin and TPF Missions
Selsis, F., Leger, A. M., & Ollivier, M. (2005) · Advances in astrobiology and biogeophysics · doi:10.1007/10913406_11 · Cited by 3
Lunar Exploration as a Probe of Ancient Venus
Cabot, S. H. C., & Laughlin, G. (2020) · The Planetary Science Journal · doi:10.3847/psj/abbc18 · Cited by 3
“The remaining oxygen may have reacted with magma oceans (Kasting 1988), or escaped non-thermally (Shizgal & Arkos 1996); solar winds can remove the dissociated ions, as observed by ESA’s Venus Express (Delva et al. 2008; Persson et al. 2018).”
BackgroundMethodInfluentialComposition and Internal Dynamics of Super‐Earths
Valencia, D. (2013) · doi:10.1002/9781118529492.ch9 · Cited by 3
Effects of the non-gray absorption in a simple radiative equilibrium model
Pujol, T. (2002) · Planetary and Space Science · doi:10.1016/s0032-0633(02)00072-7 · Cited by 3
Makarieva, A. M., Gorshkov, V. G., & Pujol, T. (2003) · doi:10.5194/acpd-3-6701-2003 · Cited by 3
“The main result of this paper is that, in contrast to the results obtained in several previous studies (Komabayasi, 1967; Ingersoll, 1969; Kasting, 1988; Goody and Yung, 1989; Nakajima et al., 1992; Renn ´ o, 1997; Pujol and North, 2002), on a planet with an infinite liquid hydrosphere the outgoing flux of thermal radia…”
InfluentialBoukrouche, R., Caballero, R., & Janson, M. (2024) · The Astrophysical Journal · doi:10.3847/1538-4357/ad8f30 · Cited by 2
The Photochemical Plausibility of Warm Exo-Titans Orbiting M Dwarf Stars
Ranjan, S., Wogan, N. F., Glidden, A., Wang, J., Stevenson, K. B., Lewis, N. K., Koskinen, T., Seager, S., Wakeford, H. R., & van der Marel, R. P. (2025) · The Astrophysical Journal Letters · doi:10.3847/2041-8213/ae1026 · Cited by 3
“While a common approach ( e.g., J. F. Kasting 1988; A. Aguichine et al. 2021; N. F. Wogan et al. 2023 ) , this approximation may be inaccurate for CH 4 -dominated atmo-spheres orbiting M dwarf stars, for which antigreenhouse effects are anticipated ( R. M. Ramirez & L. Kaltenegger 2018; M. Turbet…”
Role of gas and aerosol components of the atmosphere in the model of greenhouse explosion
Захаров, В. И., Gribanov, K. G., & Beresnev, S. A. (2009) · Atmospheric and Oceanic Optics · doi:10.1134/s1024856009020055 · Cited by 2
“Nevertheless, it is known that the grey atmosphere model at an approximation of the radiant equilibrium describes adequately all qualitative regularities in greenhouse effects in the atmosphere of planets [9, 10 , 18] and can be a simple and effective method for the prediction and qualitative study of new greenhouse e…”
BackgroundMethodAntony, T., Raju, C. S., Mohan, N., Swarup, G., Oberoi, D., & Moorthy, K. K. (2021) · Journal of Geophysical Research Planets · doi:10.1029/2020je006582 · Cited by 2
“This warming would have triggered the onset of a moist (Kasting, 1988) and possibly a runaway greenhouse state by which much of the surface water was lost via photodissociation, accompanied by”
Backgroundda Silva, L. A. L. (2021) · International Journal of Astrobiology · doi:10.1017/s1473550421000355 · Cited by 2
On the Hydrosphere Stability of TESS Targets: Applications to 700 d, 256 b, and 203 b
Bonney, P., & Kennefick, J. (2022) · The Planetary Science Journal · doi:10.3847/psj/ac8669 · Cited by 1
“In this case, the surface temperature exceeds 647K, fully evaporating surface oceans and leading to a water vapor– dominated upper atmosphere (e.g., Kasting 1988).”
BackgroundImpact of vegetation albedo on the habitability of Earth-like exoplanets
Bisesi, E., Murante, G., Provenzale, A., Biasiotti, L., von Hardenberg, J., Ivanovski, S. L., MARIS, M., Monai, S., Silva, L., Simonetti, P., et al. (2024) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stae2016 · Cited by 2
The Role of Tectonic Luck in Long-term Habitability of Abiotic Earth-like Planets
Coy, B. P., Kite, E. S., & Graham, R. J. (2025) · The Planetary Science Journal · doi:10.3847/psj/adf643 · Cited by 3
“…also can be overwhelmed by external perturbations, such as increasing ISR, that may lead to a runaway greenhouse effect where surface oceans evaporate completely, driving all life extinct ( C. Goldblatt & A. J. Watson 2012 ) , similar to what may have happened on Venus ( J. F. Kasting 1988 ) .”
Regarding greenhouse explosion
Zakharov, V. I. (2008) · Springer eBooks · doi:10.1007/978-3-540-78209-4_6 · Cited by 2
Pujol, T. (2004) · Quarterly Journal of the Royal Meteorological Society · doi:10.1256/qj.02.144 · Cited by 2
“Note that here we analyse profiles with surface temperatures lower than 350 K, since the assumption of water vapour as an ideal gas breaks down at high surface pressures (reached at high surface temperatures; see e.g. Kasting (1988)).”
BackgroundEffects of Atmospheric Absorption of Incoming Radiation on the Radiation Limit of the Troposphere
Kurokawa, H., & Nakamoto, T. (2011) · Journal of the Atmospheric Sciences · doi:10.1175/jas-d-11-0108.1 · Cited by 2
“The existence of radiation limits was subsequently confirmed in detailed numerical studies (Abe and Matsui 1988; Kasting 1988; Rennó et al. 1994a,b; Rennó 1997; Ishiwatari et al. 2002).”
BackgroundFormation of Earth-like habitable planets
Brownlee, D. E., & Kress, M. E. (2007) · Cambridge University Press eBooks · doi:10.1017/cbo9780511812958.005 · Cited by 2
The Geology and Habitability of Terrestrial Planets: Fundamental Requirements for Life
Southam, G., Rothschild, L. J., & Westall, F. (2007) · Space sciences series of ISSI · doi:10.1007/978-0-387-74288-5_2 · Cited by 4
Extremophiles—Organisms that survive and thrive in extreme environmental conditions
Joseph, A. (2023) · Elsevier eBooks · doi:10.1016/b978-0-323-95717-5.00009-8 · Cited by 2
Probing the Atmosphere of Venus using Infrared Spectroscopy
Bailey, J. (2006) · Cited by 2
Habitable planets around the Sun and other stars
Kasting, J. F. (2007) · Cambridge University Press eBooks · doi:10.1017/cbo9780511536533.009 · Cited by 2
Self-citationFormation of the Terrestrial Planets
Kaula, W. M. (1995) · Springer eBooks · doi:10.1007/978-94-017-1092-3_1 · Cited by 2
Life on Mars: Past, Present, and Future
Beech, M., & Comte, M. (2021) · Wiley eBooks · doi:10.1002/9781119761990.ch9 · Cited by 2
The Habitability of Venus and a Comparison to Early EarthPreprint
Westall, F., Höning, D., Avice, G., Gentry, D. M., Gerya, T., Gillmann, C., Izenberg, N. R., Way, M. J., & Wilson, C. (2022) · doi:10.1002/essoar.10512790.1 · Cited by 2
Climate instabilities under strong solar forcing
Popp, M. (2013) · Max Planck Digital Library · doi:10.17617/2.2049534 · Cited by 2
“Other studies made use of models with a constant cloud layer as well or investigated the influence of clouds tentatively for single cloud layers at different temperature and pressure levels (e.g., Kasting (1988)).”
BackgroundMethodInfluentialTurbet, M. (2018) · theses.fr (ABES) · doi:10.70675/6ee472e1z447cz4553zad3ezb856253af054 · Cited by 2
Habitable Zones of the Universe
(2000) · Springer eBooks · doi:10.1007/0-387-21848-3_2 · Cited by 1
Joseph, A. (2023) · Elsevier eBooks · doi:10.1016/b978-0-323-95717-5.00014-1 · Cited by 1
Detectability of biosignatures in warm, water-rich atmospheres
Taysum, B. M., van Zelst, I., Grenfell, J. L., Schreier, F., Cabrera, J., & Rauer, H. (2024) · Astronomy and Astrophysics · doi:10.1051/0004-6361/202450549 · Cited by 3
Yoshida, T., Arima, K., Kuroda, T., Terada, N., & Kuramoto, K. (2025) · The Astrophysical Journal · doi:10.3847/1538-4357/adc8a5 · Cited by 2
“These atmospheres can drastically lower the outgoing planetary radiation fl ux by several orders of magnitude compared to blackbody radiation, due to the infrared-absorbing properties of H 2 O ( e.g., J. F. Kasting 1988; S. Nakajima et al. 1992; C. Goldblatt et al. 2013 ) .”
InfluentialImpacts of Atmospheric Carbon Species and Stellar Type on Climates of Terrestrial Planets
Landry, J., Kurokawa, H., Taki, T., Fujii, Y., Aoki, K., & Genda, H. (2025) · The Planetary Science Journal · doi:10.3847/psj/adf7a1 · Cited by 1
“The moist adiabatic lapse rate takes the release of the latent heat from condensation of saturated water vapor into account (Ingersoll 1969; Kasting et al. 1984; Kasting 1988; Catling & Kasting 2017).”
Modelling the Milky Way’s exoplanet population based on cosmological galaxy simulations
Padois, C., del Ser, D., Anders, F., Amarante, J. A. S., Perottoni, H. D., Hajnik, T., Souto, D., Feliciano-Souza, I. N., Kawata, D., & Martioli, E. (2025) · Astronomy and Astrophysics · doi:10.1051/0004-6361/202557051 · Cited by 1
Boley, K. M., Panero, W. R., Miozzi, F., Capirala, A., & Teske, J. K. (2025) · The Astrophysical Journal · doi:10.3847/1538-4357/ae182b · Cited by 1
“Evaporation driven by high stellar flux can lead to complete surface water loss, leading to an inhospitable environment ( J. F. Kasting 1988; C. Goldblatt et al. 2013 ) .”
Metadata
- Authors
- Kasting, J. F.
- Affiliations
- Ames Research Center (US)
- Corresponding author
- Kasting, James F.
- ORCID
- Kasting, James F.
- Venue
- Icarus
- Publisher
- Elsevier BV
- Published
- 1988-06
- Volume
- 74
- Issue
- 3
- Pages
- 472-494
- ISSN
- 0019-1035 (ISSN-L)
- OpenAlex
- W1968152463
- Cited by
- 709
- References
- 47
- Citations by year
- 2026: 21 · 2025: 30 · 2024: 33 · 2023: 39 · 2022: 31 · 2021: 35 · 2020: 37 · 2019: 30 · 2018: 37 · 2017: 32 · 2016: 36 · 2015: 33 · 2014: 30 · 2013: 40 · 2012: 19
- FWCI
- 12.62
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Icarus (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Stellar, planetary, and galactic studies
- Keywords
- runaway greenhouse, Venus, Earth, water photodissociation, hydrogen escape, water vapor absorption, accretion, steam atmosphere, carbon dioxide, one-dimensional climate model
- MeSH terms
- Atmosphere, Carbon Dioxide, Climate, Light, Models, Theoretical, Scattering, Radiation, Sunlight, Temperature, Water, Solar System, Greenhouse Effect, Earth, Planet, Venus
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review