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 101–200 of 708
Stellar ablation of planetary atmospheres
Moore, T. E., & Horwitz, J. L. (2007) · Reviews of Geophysics · doi:10.1029/2005rg000194 · Cited by 123
“Venus’ atmosphere has been desiccated of water [Kasting, 1988].”
GENERALIZED MILANKOVITCH CYCLES AND LONG-TERM CLIMATIC HABITABILITY
Spiegel, D., Raymond, S., Dressing, C., Scharf, C. A., & Mitchell, J. (2010) · The Astrophysical Journal · doi:10.1088/0004-637x/721/2/1308 · Cited by 89
“This function, presented in the appendix of WK97, is a parameterized fit (third order in T and fourth order in ln[pCO2 ]) to results from a radiative-convective model (Kasting & Ackerman 1986; Kasting 1988, 1991).”
MethodMagma Oceans and Primordial Mantle Differentiation
Solomatov, V. S. (2015) · Elsevier eBooks · doi:10.1016/b978-0-444-53802-4.00155-x · Cited by 138
Habitability of Exoplanet Waterworlds
Kite, E. S., & Ford, E. B. (2018) · The Astrophysical Journal · doi:10.3847/1538-4357/aad6e0 · Cited by 124
“However, for an initial water endowment of >50 Earth oceans in the HZ of an FGK star, the moist greenhouse cannot cause complete ocean loss (Kasting 1988; Lammer et al. 2009; Luger & Barnes 2015; Zahnle & Catling 2017) (Figure 1).”
BackgroundPersistence of flare-driven atmospheric chemistry on rocky habitable zone worlds
Chen, H., Zhan, Z., Youngblood, A., Wolf, E. T., Feinstein, A. D., & Horton, D. E. (2020) · Nature Astronomy · doi:10.1038/s41550-020-01264-1 · Cited by 130
“In addition, in both the temperate and moist greenhouse simulations, the upper atmosphere is pushed into a classical moist greenhouse state (Kasting 1988), despite the temperate simulation having relatively dry surface conditions (Figure 5c).”
BackgroundRedox controls during magma ocean degassing
Gaillard, F., Bernadou, F., Roskosz, M., Bouhifd, M. A., Marrocchi, Y., Iacono–Marziano, G., Moreira, M., Scaillet, B., & Rogerie, G. (2021) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2021.117255 · Cited by 132
Synthetic Spectra of Simulated Terrestrial Atmospheres Containing Possible Biomarker Gases
Schindler, T. (2000) · Icarus · doi:10.1006/icar.2000.6340 · Cited by 118
“In order to investigate these planets might appear to TPF, we have computed syn spectra for planets that are representative of these two cas For our Venus-like planet, we assumed a “moist greenho scenario (Kasting 1988).”
BackgroundMethodInfluentialSalvador, A., Massol, H., Davaille, A., Marcq, E., Sarda, P., & Chassefière, É. (2017) · Journal of Geophysical Research Planets · doi:10.1002/2017je005286 · Cited by 125
PREDICTIONS OF THE ATMOSPHERIC COMPOSITION OF GJ 1132b
Schaefer, L., Wordsworth, R., Sasselov, D. D., & Berta-Thompson, Z. K. (2016) · DSpace@MIT (Massachusetts Institute of Technology) · Cited by 117
Sackmann, I. ‐., & Boothroyd, A. I. (2003) · The Astrophysical Journal · doi:10.1086/345408 · Cited by 113
“…not lose its water via a moist greenhouse effect, which would occur if the solar flux at Earth were more than 10% higher than its present value (Kasting 1988) — a moist greenhouse occurs when the stratosphere becomes wet, and H2O is lost through UV dissociation and the subsequent loss of…”
BackgroundInfluentialTarduno, J. A., Blackman, E. G., & Mamajek, E. E. (2014) · Physics of The Earth and Planetary Interiors · doi:10.1016/j.pepi.2014.05.007 · Cited by 113
“t i, the distinction between merely retaining an atmosphere vs. the retention of specically water must be kept in mind. While the exact evolutionary history and escape mechanisms are debatable (e.g. Kasting, 1988; Elkins-Tanton, 2013; Hamano et al., 2013), there is little argument that Venus has lost a huge amount of…”
BackgroundFelsic highland crust on Venus suggested by Galileo Near‐Infrared Mapping Spectrometer data
Hashimoto, G. L., Roos‐Serote, M., Sugita, S., Gilmore, M. S., Kamp, L. W., Carlson, R. W., & Baines, K. H. (2008) · Journal of Geophysical Research: Planets · doi:10.1029/2008je003134 · Cited by 139
“would have avoided going into a state of runaway greenhouse [e.g., Kasting, 1988 ].”
BackgroundWhole planet coupling between climate, mantle, and core: Implications for rocky planet evolution
Foley, B. J., & Driscoll, P. (2016) · Geochemistry Geophysics Geosystems · doi:10.1002/2015gc006210 · Cited by 118
“A hot CO2 greenhouse can also cause rapid water loss to space [Kasting, 1988] (though Wordsworth and Pierrehumbert [2013] argues against this), or even a steam atmosphere if surface temperatures exceed water’s critical temperature of 647 K.”
BackgroundInfluentialRaymond, S. N., Quinn, T., & Lunine, J. I. (2005) · CERN Document Server (European Organization for Nuclear Research) · Cited by 106
Divergent evolution of Earth and Venus: Influence of degassing, tectonics, and magnetic fields
Driscoll, P., & Bercovici, D. (2013) · Icarus · doi:10.1016/j.icarus.2013.07.025 · Cited by 106
The collision between the Milky Way and Andromeda
Cox, T. J., & Loeb, A. (2008) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2008.13048.x · Cited by 105
“Regardless of the relatively small differences between merger times in these models, they are all completely coalesced by 6.2 Gyr from today.”
BackgroundInfluentialHabitability and Biosignatures of Hycean Worlds
Madhusudhan, N., Piette, A. A. A., & Constantinou, S. (2021) · Apollo (University of Cambridge) · doi:10.17863/cam.76040 · Cited by 104
Chandler, M. A., & Sohl, L. E. (2000) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jd900221 · Cited by 102
Could we identify hot ocean-planets with CoRoT, Kepler and Doppler velocimetry?
Selsis, F., Chazelas, B., Borde, P. J., Ollivier, M., Brachet, F., Decaudin, M., Bouchy, F., Ehrenreich, D., Grießmeier, J. ‐., Lammer, H., et al. (2007) · Icarus · doi:10.1016/j.icarus.2007.04.010 · Cited by 102
“Inside the HZ, the atmospheric water vapor content is a function of the orbital distance: around the present Sun, in the absence of other greenhouse gases and assuming a large ocean at the surface, the partial pressure of H2O would be 1 bar at 0.93 AU and would reach the critical pressure (220 bar) at 0.84 AU ( Kastin…”
BackgroundInfluentialSelf-citationA very simple model for the water vapour feedback on climate change
Ingram, W. (2010) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.546 · Cited by 101
“Thereafter, with q unchanging rather than RH, a ‘Planckian’ response–emission at each wavelength increasing with temperature following Planck’s Law–would have allowed equilibration, with hydrogen loss on longer time-scales eventually bringing the planet to its present state (Kasting, 1988).”
BackgroundAtmospheric regimes and trends on exoplanets and brown dwarfs
Zhang, X. (2020) · Research in Astronomy and Astrophysics · doi:10.1088/1674-4527/20/7/99 · Cited by 111
“Venus might have experienced the runaway greenhouse process (Ingersoll 1969, or at least moist greenhouse, Kasting 1988), resulting in very little water and a high D/H ratio in the atmosphere.”
BackgroundUltraviolet Radiation and the Photobiology of Earth's Early Oceans
Cockell, C. S. (2000) · Origins of Life and Evolution of Biospheres · doi:10.1023/a:1006765405786 · Cited by 100
“, 1982) or a warm ‘moist greenhouse’ Venus with an oceanic water inventory that was eventually lost (Kasting, 1988).”
BackgroundWarming the early earth—CO2 reconsidered
von Paris, P., Rauer, H., Grenfell, J. L., Patzer, B., Hedelt, P., Stracke, B., Trautmann, T., & Schreier, F. (2008) · Planetary and Space Science · doi:10.1016/j.pss.2008.04.008 · Cited by 102
“(2) has already154 been used by, e.g., Pavlov et al. (2000); Segura et al. (2003) or Grenfell et al.155 (2007a) and is based on Kasting et al. (1984b) and Kasting (1988).”
MethodGillmann, C., Chassefière, E., & Lognonné, P. (2009) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.07.016 · Cited by 96
“The H escape flux is calculated at 200 km altitude, which is considered, from Kasting and Pollack (1983), as the base of the expansion.”
BackgroundMethodInfluentialSackmann, I. ‐., & Boothroyd, A. I. (1972) · Cited by 109
Transition to a Moist Greenhouse with CO2 and solar forcing
Popp, M., Schmidt, H., & Marotzke, J. (2016) · Nature Communications · doi:10.1038/ncomms10627 · Cited by 99
A post-Cassini view of Titan’s methane-based hydrologic cycle
Hayes, A. G., Lorenz, R. D., & Lunine, J. I. (2018) · Nature Geoscience · doi:10.1038/s41561-018-0103-y · Cited by 104
TEMPERATURE STRUCTURE AND ATMOSPHERIC CIRCULATION OF DRY TIDALLY LOCKED ROCKY EXOPLANETS
Koll, D. D. B., & Abbot, D. S. (2016) · The Astrophysical Journal · doi:10.3847/0004-637x/825/2/99 · Cited by 98
“An atmosphere’s temperature structure and circulation critically influence a planet’s surface and atmospheric evolution as well as its potential habitability (Kasting 1988; Abe et al. 2011; Yang et al. 2013).”
BackgroundThe habitability of a stagnant-lid Earth
Tosi, N., Godolt, M., Stracke, B., Ruedas, T., Grenfell, J. L., Höning, D., Nikolaou, A., Plesa, A., Breuer, D., & Spohn, T. (2017) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201730728 · Cited by 95
“The numerical scheme is based on Kasting et al. (1984b) and Kasting (1988) and was improved and described in von Paris (2010) and Kitzmann et al. (2015).”
BackgroundMethodInfluentialSpiegel, D. S., Kristen Menou, A., & Scharf, C. A. (2008) · The Astrophysical Journal · doi:10.1086/588089 · Cited by 104
Hashimoto, G. L., Abe, Y., & Sugita, S. (2007) · Journal of Geophysical Research Atmospheres · doi:10.1029/2006je002844 · Cited by 102
“Hydrogen escape must be an essential process for evolution of the Venusian atmosphere since the present Venusian atmosphere contains almost no hydrogen [e.g., Kasting and Pollack, 1983; Kasting, 1988].”
BackgroundThe stability of climate on Venus
Bullock, M. A., & Grinspoon, D. H. (1996) · Journal of Geophysical Research Atmospheres · doi:10.1029/95je03862 · Cited by 95
“Massive fractionating loss by exospheric escape from a large primordial reservoir is a likely mechanism for the D/H signature seen in the Venus atmosphere today [Donahue and Hodges, 1992; Kasting, 1988; Pepin, 1991; Zahnle and Kasting, 1986].”
BackgroundAbiotic oxygen-dominated atmospheres on terrestrial habitable zone planets
Wordsworth, R., & Pierrehumbert, R. T. (2016) · Cited by 93
A Review of Possible Planetary Atmospheres in the TRAPPIST-1 System
Turbet, M., Bolmont, É., Bourrier, V., Demory, B.-O., Leconte, J., Owen, J. E., & Wolf, E. T. (2020) · Space Science Reviews · doi:10.1007/s11214-020-00719-1 · Cited by 101
“This limit is also known as the runaway greenhouse (Ingersoll, 1969; Kasting, 1988; Pierrehumbert, 2010; Goldblatt and Watson, 2012).”
BackgroundGJ 832c: A SUPER-EARTH IN THE HABITABLE ZONE
Wittenmyer, R. A., Tuomi, M., Butler, R. P., Jones, H. R. A., Anglada-Escudé, G., Horner, J., Tinney, C. G., Marshall, J. P., Carter, B., Bailey, J., et al. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/791/2/114 · Cited by 90
“In that scenario, the dense atmosphere would provide a strong greenhouse effect, raising the surface temperature enough to cause any oceans to boil away, as is thought to have happened to Venus early in the lifetime of the solar system (e.g., Kasting 1988).”
BackgroundThe Case for a Gaian Bottleneck: The Biology of Habitability
Chopra, A., & Lineweaver, C. H. (2016) · Astrobiology · doi:10.1089/ast.2015.1387 · Cited by 115
“However, atmospheric evolution of these planets diverged significantly (Kasting, 1988; Kulikov et al. , 2007; Driscoll and Bercovici, 2013).”
The search for signs of life on exoplanets at the interface of chemistry and planetary science
Seager, S., & Bains, W. (2015) · Science Advances · doi:10.1126/sciadv.1500047 · Cited by 91
Exomoon habitability constrained by energy flux and orbital stability
Heller, R. (2012) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201220003 · Cited by 89
Atmospheric Circulation of ExoplanetsPreprint
Showman, A. P., Cho, J. Y. K., & Kristen Menou, A. (2009) · arXiv (Cornell University) · doi:10.48550/arxiv.0911.3170 · Cited by 113
Clouds in the atmospheres of extrasolar planets
Kitzmann, D., Patzer, A. B. C., von Paris, P., Godolt, M., Stracke, B., Gebauer, S., Grenfell, J. L., & Rauer, H. (2010) · Astronomy and Astrophysics · doi:10.1051/0004-6361/200913491 · Cited by 88
Clouds and Hazes in Exoplanet Atmospheres
Marley, M. S., Ackerman, A. S., Cuzzi, J. N., & Kitzmann, D. (2013) · University of Arizona Press eBooks · doi:10.2458/azu_uapress_9780816530595-ch15 · Cited by 126
“The latter is the definition favored by Kasting et al. (1993); the former definition is used by Hart (1979). In the present Earth atmosphere water escape is limited by the cold trap at the tropopause which loses its efficiency in a sufficiently warm, moist atmosphere (Kasting et al.”
BackgroundInfluentialWhat Factors Affect the Duration and Outgassing of the Terrestrial Magma Ocean?
Nikolaou, A., Katyal, N., Tosi, N., Godolt, M., Grenfell, J. L., & Rauer, H. (2019) · The Astrophysical Journal · doi:10.3847/1538-4357/ab08ed · Cited by 91
“The albedo for a cloudless steam atmosphere, based on 1D models and 3D global circulation model calculations lies between [0.15, 0.40] (Kasting 1988; Goldblatt et al. 2013; Leconte et al. 2013; Pluriel et al. 2019).”
BackgroundMethodInfluentialVIRTIS emissivity of Alpha Regio, Venus, with implications for tessera composition
Gilmore, M. S., Mueller, N. T., & Helbert, J. (2015) · Icarus · doi:10.1016/j.icarus.2015.04.008 · Cited by 86
Atmospheric effects of stellar cosmic rays on Earth-like exoplanets orbiting M-dwarfs
Vakili, V. T., Grenfell, J. L., Grießmeier, J. ‐., & Rauer, H. (2015) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201425602 · Cited by 82
“Below the tropopause the temperature profile is determined by a wet adiabatic lapse rate,b sed on Kasting (1988) and Ingersoll (1969), using the relative humidity profile of Manabe & Wetherald (1967).”
MethodImpacts and the Early Evolution of Life
Zahnle, K. J., & Sleep, N. H. (2006) · Springer eBooks · doi:10.1007/3-540-33088-7_7 · Cited by 85
DECIPHERING THERMAL PHASE CURVES OF DRY, TIDALLY LOCKED TERRESTRIAL PLANETS
Koll, D., & Abbot, D. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/802/1/21 · Cited by 58
“In addition, for planets hotter than Earth, volatiles can be lost via atmospheric escape (the so-called moist greenhouse; Kasting 1988).”
BackgroundDelayed onset of runaway and moist greenhouse climates for Earth
Wolf, E. T., & Toon, O. B. (2014) · Geophysical Research Letters · doi:10.1002/2013gl058376 · Cited by 114
“…humidities are near 75% at the surface and 50% above 700 mb. One-dimensional studies typically assume fully saturated atmospheres and thus they artificially amplify the strength of the water vapor greenhouse [Kasting, 1988; Kasting et al., 1993; Goldblatt et al., 2013; Kopparapu et al., 2013].”
BackgroundVenus Interior Structure and Dynamics
SMREKAR, S. E., Davaille, A., & Sotin, C. (2018) · Space Science Reviews · doi:10.1007/s11214-018-0518-1 · Cited by 81
“On the other hand, models considering a CO2–H2O atmosphere suggest the possibility of water ocean condensation on Venus at the end of a rapid (less than a few Myr) magma ocean stage, especially if clouds or Venus rotation are considered (e.g. Kasting 1988; Way et al. 2016; Salvador et al. 2017).”
MethodA More Comprehensive Habitable Zone for Finding Life on Other Planets
Ramirez, R. M. (2018) · Geosciences · doi:10.3390/geosciences8080280 · Cited by 92
“This concept is essentially analogous to the “moist greenhouse” of Kasting [37], except that the moist greenhouse is the specific case in which enhanced water vapor photolysis can desiccate a planet with an Earth-like water inventory within the age of the solar system (as discussed earlier).”
Gaillard, F., Bouhifd, M. A., Füri, E., Malavergne, V., Marrocchi, Y., Noack, L., Ortenzi, G., Roskosz, M., & Vulpius, S. (2021) · Space Science Reviews · doi:10.1007/s11214-021-00802-1 · Cited by 82
Physical conditions on the early Earth
Lunine, J. I. (2006) · Philosophical Transactions of the Royal Society B Biological Sciences · doi:10.1098/rstb.2006.1900 · Cited by 85
Habitable Zone Lifetimes of Exoplanets around Main Sequence Stars
Rushby, A. J., Claire, M. W., Osborn, H., & Watson, A. J. (2013) · Astrobiology · doi:10.1089/ast.2012.0938 · Cited by 138
“However, under a regime of increasing solar luminosity, which is estimated to be 118% of the present-day value at 1.75 Gyr, we consider an irreversible runaway greenhouse scenario to be more likely (Kasting, 1988; Goldblatt and Watson, 2012).”
InfluentialFormation and Evolution of Protoatmospheres
Massol, H., Hamano, K., Tian, F., Ikoma, M., Abe, Y., Chassefière, E., Davaille, A., Genda, H., Güdel, M., Hori, Y., et al. (2016) · Space Science Reviews · doi:10.1007/s11214-016-0280-1 · Cited by 85
“Thereafter, the thermal radiation outgoing to space is fixed to 280–300 Wm−2, which is called the radiation limit or runaway greenhouse limit of steam atmospheres (Kasting 1988; Abe and Matsui 1988; Kopparapu et al. 2013; Goldblatt et al. 2013).”
BackgroundMethodInfluentialThe runaway greenhouse radius inflation effect
Turbet, M., Ehrenreich, D., Lovis, C., Bolmont, É., & Fauchez, T. J. (2019) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201935585 · Cited by 94
“The dry and moist convective layers are constructed using Kasting (1988) formulation of the lapse rate, and as done in Marcq et al. (2017).”
BackgroundMethodThe Dark Side of Venus: Near-Infrared Images and Spectra from the Anglo-Australian Observatory
Crisp, D., Allen, D. A., Grinspoon, D. H., & Pollack, J. B. (1991) · Science · doi:10.1126/science.11538493 · Cited by 80
A warmer and wetter solution for early Mars and the challenges with transient warming
Ramirez, R. M. (2017) · Icarus · doi:10.1016/j.icarus.2017.06.025 · Cited by 79
“I follow a similar technique as that in previous studies (e.g. Kasting, 1988; Ramirez et al., 2014b; Ramirez and Kasting, 2017) to gauge the radiative effects of cloud forcing.”
BackgroundMethodInfluentialON THE HABITABLE ZONES OF CIRCUMBINARY PLANETARY SYSTEMS
Kane, S. R., & Hinkel, N. R. (2012) · The Astrophysical Journal · doi:10.1088/0004-637x/762/1/7 · Cited by 79
“Hart (1979) provided estimates for the Solar System and later models of runaway greenhouse for Venus were incorporated into the calculations by Pollack (1971) and Kasting (1988).”
MethodEscape of the martian protoatmosphere and initial water inventory
Erkaev, N. V., Lammer, H., Elkins-Tanton, L. T., Stökl, A., Odert, P., Marcq, E., Dorfi, E. A., Kislyakova, K. G., Kulikov, Y. N., Leitzinger, M., et al. (2013) · Planetary and Space Science · doi:10.1016/j.pss.2013.09.008 · Cited by 84
“One should also note that for the surface temperatures of∼500 K, which are expected during the “Mush” stage (Lebrun et al., 2013), according to Kasting (1988) one can also expect water vapor mixing ratios at the mesopause level n ar to 1.”
BackgroundTransport of ionizing radiation in terrestrial-like exoplanet atmospheres
Smith, D. S., Scalo, J., & Wheeler, J. C. (2004) · Icarus · doi:10.1016/j.icarus.2004.04.009 · Cited by 74
Horneck, G. (1995) · Planetary and Space Science · doi:10.1016/0032-0633(94)00190-3 · Cited by 78
Long-term stability of the earth's climate
Kasting, J. F. (1989) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/0031-0182(89)90185-5 · Cited by 79
Self-citationVenus Atmospheric Thermal Structure and Radiative Balance
Limaye, S. S., Grassi, D., Mahieux, A., Migliorini, A., Tellmann, S., & Titov, D. V. (2018) · Space Science Reviews · doi:10.1007/s11214-018-0525-2 · Cited by 77
“Since the conditions on the terrestrial planets and especially the amount of CO2 and H2O in the atmosphere could have varied over geological history, the greenhouse effect could have played a more important role in the past (Kasting 1988).”
BackgroundOcean Dynamics and the Inner Edge of the Habitable Zone for Tidally Locked Terrestrial Planets
Yang, J., Abbot, D. S., Koll, D. D. B., Hu, Y., & Showman, A. P. (2019) · The Astrophysical Journal · doi:10.3847/1538-4357/aaf1a8 · Cited by 75
“At this level of stellar flux, the stratospheric water vapor concentration, ≥ 3, 000 ppmv, is high enough that H2O photo-dissociation and subsequent H escape to space becomes significant, which is known as the moist greenhouse state (Kasting 1988; Kasting et al. 1993).”
BackgroundPossible climates on terrestrial exoplanets
Forget, F., & Leconte, J. (2014) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2013.0084 · Cited by 83
“greenhouse’ process can destabilize the climate on the basis of simple one-dimensional model calculations, Kasting [35] found that on an Earth-like planet around the Sun, oceans would completely vapourize below a threshold around 0.”
BackgroundInfluentialThe extrasolar planet Gliese 581d: a potentially habitable planet?
von Paris, P., Gebauer, S., Godolt, M., Grenfell, J. L., Hedelt, P., Kitzmann, D., Patzer, A. B. C., Rauer, H., & Stracke, B. (2010) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201015329 · Cited by 75
CLIMATE INSTABILITY ON TIDALLY LOCKED EXOPLANETS
Kite, E. S., Gaidos, E. J., & Manga, M. (2011) · The Astrophysical Journal · doi:10.1088/0004-637x/743/1/41 · Cited by 81
“The thin solid line corresponds to mean surface temperatures above 40◦C, which is the lower edge of the moist runaway greenhouse zone (Kasting 1988; Pierrehumbert 1995)—our model does not include fluxes of latent heat or the greenhouse effect of water vapor, so the position of this line is notional.”
O'Malley-James, J. T., Greaves, J. S., Raven, J. A., & Cockell, C. S. (2012) · International Journal of Astrobiology · doi:10.1017/s147355041200047x · Cited by 90
“Finally, rising temperatures cause rapid ocean evaporation (Kasting 1988; Bounama et al. 2001; Vásquez et al. 2010), effectively sterilising most of the biosphere (see Fig.”
BackgroundHABITABLE ZONES AROUND LOW MASS STARS AND THE SEARCH FOR EXTRATERRESTRIAL LIFE
Kasting, J. F. (1997) · Origins of Life and Evolution of Biospheres · doi:10.1023/a:1006586517202 · Cited by 72
“Climate model calculations by Kasting (1988), summarized in Figure 2, indicate that this would be more than sufficient to drive all of Earth's water into its atmosphere and create a "runaway greenhouse."”
Self-citationOrigin of Earth’s oceans: An assessment of the total amount, history and supply of water
Genda, H. (2016) · GEOCHEMICAL JOURNAL · doi:10.2343/geochemj.2.0398 · Cited by 75
“A planet with oceans has an upper limit of planetary radiation (Kasting, 1988; Nakajima et al., 1992; Kodama et al., 2015).”
BackgroundHistory of water loss and atmospheric O2 buildup on rocky exoplanets near M dwarfs
Tian, F. (2015) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2015.09.051 · Cited by 69
Clouds and the Faint Young Sun Paradox
Goldblatt, C., & Zahnle, K. J. (2011) · Climate of the Past · doi:10.5194/cp-7-203-2011 · Cited by 71
“This assumption has been used extensively in the models from Jim Kasting’s group (Kasting et al., 1984; Kasting and Ackerman, 1986; Kasting, 1987, 1988; Kasting et al., 1993; Pavlov et al., 2000, 2003; Kasting and Howard, 2006; Haqq-Misra et al., 2008), which, together with parametrisations and…”
MethodMarcq, E. (2011) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011je003912 · Cited by 71
“Validity close to the critical point of water vapor (Pc = 22.06 MPa, Tc = 647.1 K) is not guaranteed, however [Kasting, 1988; Ingersoll, 1969; Abe and Matsui, 1988].”
BackgroundMethodInfluentialMarcq, E., Salvador, A., Massol, H., & Davaille, A. (2017) · Journal of Geophysical Research Planets · doi:10.1002/2016je005224 · Cited by 71
“This qualitative behavior was also reproduced by older random band or gray models [Nakajima et al., 1992; Kasting, 1988], albeit with larger values for NL on the order of 300 W/m2 or more.”
MethodComparative Climatology of Terrestrial Planets
Mackwell, S., Simon-miller, A., Harder, J., & Bullock, M. (2013) · University of Arizona Press eBooks · doi:10.2458/azu_uapress_9780816530595 · Cited by 100
Tidal Venuses: Triggering a Climate Catastrophe via Tidal HeatingPreprint
Barnes, R., Mullins, K., Goldblatt, C., Meadows, V., James, F., & Heller, K. R. ́. (2016) · Cited by 84
FORMATION, TIDAL EVOLUTION, AND HABITABILITY OF THE KEPLER-186 SYSTEM
Bolmont, É., Raymond, S. N., von Paris, P., Selsis, F., Hersant, F., Quintana, E. V., & Barclay, T. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/793/1/3 · Cited by 70
“The volatile budget of Earth is thought to consist of several bars of N2 and tens to hundreds of bars of CO2 (e.g., Turekian & Clark 1975; Kasting 1988; McKay & Stoker 1989; Lundin & Barabash 2004; Goldblatt et al. 2009).”
BackgroundHow planets grow by pebble accretion
Ormel, C. W., Vazan, A., & Brouwers, M. G. (2021) · Astronomy and Astrophysics · doi:10.1051/0004-6361/202039706 · Cited by 68
Kadoya, S., & Tajika, E. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/790/2/107 · Cited by 69
“Alternatively, Venus might have been in the hot climate mode (i.e., the moist greenhouse condition), resulting in a loss of water to space (e.g., Kasting 1988).”
BackgroundMethodInfluentialUltraviolet radiation constraints around the circumstellar habitable zones
Buccino, A. P., Lemarchand, G. A., & Mauas, P. J. D. (2006) · Icarus · doi:10.1016/j.icarus.2006.03.007 · Cited by 70
“90 AU around the Sun, wider than the traditional one proposed by Kasting et al. (1993), where the limits in the intermediate case, for the Solar System, go from 0.84 to 1.67 AU in the Solar System. For life systems to evolve, the planet should be in the habitable zone continuously during a certain time. To analyze the…”
BackgroundMethodResultInfluentialThe Long-Term Evolution of the Atmosphere of Venus: Processes and Feedback Mechanisms
Gillmann, C., Way, M. J., Avice, G., Breuer, D., Golabek, G., Höning, D., Krissansen‐Totton, J., Lammer, H., O'Rourke, J. G., Persson, M., et al. (2022) · Space Science Reviews · doi:10.1007/s11214-022-00924-0 · Cited by 77
“If liquid water existed on early Venus (e.g., Kasting et al. 1984; Kasting 1988; Abe et al. 2011; Way et al. 2016), silicate weathering may have served as a sink for atmospheric CO2 (e.g., Kasting et al. 1984).”
BackgroundAssessing the Massive Young Sun Hypothesis to Solve the Warm Young Earth Puzzle
Minton, D. A., & Malhotra, R. (2007) · The Astrophysical Journal · doi:10.1086/514331 · Cited by 67
“The parameter mf is a free parameter, except that, as discussed above, Kasting (1988) argues that the solar flux cannot have been more than 10% higher at any point in the past since Earth has not lost its oceans due to a runaway moist greenhouse atmosphere.”
BackgroundChen, H., Wolf, E. T., Zhan, Z., & Horton, D. E. (2019) · The Astrophysical Journal · doi:10.3847/1538-4357/ab4f7e · Cited by 65
“Moist greenhouse atmospheres emerge when the stratospheric H2Ov mixing ratio are sufficiently high, i.e., 3×10−3 mol mol−1 such that water-loss via diffusion-limited escape could occur at a geologically significant rate in the thermosphere (Kasting 1988).”
BackgroundResultYang, J., Leconte, J., Wolf, E. T., Goldblatt, C., Feldl, N., Merlis, T. M., Wang, Y., Koll, D. D. B., Ding, F., Forget, F., et al. (2016) · The Astrophysical Journal · doi:10.3847/0004-637x/826/2/222 · Cited by 67
“Our calculations are performed in a similar manner to Kasting (1988) and Kasting et al. (1993), but cover a smaller range of temperatures, as shown in Fig.”
BackgroundMethodInfluentialVPLanet: The Virtual Planet Simulator
Barnes, R., Luger, R., Deitrick, R., Driscoll, P., Quinn, T. R., Fleming, D. P., Smotherman, H., McDonald, D. V., Wilhelm, C., Garcia, R., et al. (2020) · Publications of the Astronomical Society of the Pacific · doi:10.1088/1538-3873/ab3ce8 · Cited by 67
“However, during a runaway greenhouse, the surface temperature exceeds the temperature of the critical point of water (647 K) and the surface oceans fully evaporate, leading to an upper atmosphere that is dominated by water vapor (e.g., Kasting 1988).”
BackgroundHamano, K., Kawahara, H., Abe, Y., Onishi, M., & Hashimoto, G. L. (2015) · The Astrophysical Journal · doi:10.1088/0004-637x/806/2/216 · Cited by 72
“The radiation limit of the steam atmospheres has been extensively investigated, and its value is approximately 280 to 310 Wm−2 (Abe & Matsui 1988; Kasting 1988; Nakajima et al. 1992; Kopparapu et al. 2013; Goldblatt et al. 2013).”
BackgroundClimate Simulations of Early Mars With Estimated Precipitation, Runoff, and Erosion Rates
Ramirez, R. M., Craddock, R. A., & Usui, T. (2020) · Journal of Geophysical Research Planets · doi:10.1029/2019je006160 · Cited by 66
“s (g = 3.73 m/s2) as compared to 2Earth (g e = 9.81 m/s ) means that clouds (and precipitation) can be supported at lower pressures, assuming that vertical velocities on both planets are equal (e.g., Kasting, 1988; Ramirez, 2017). Thus, we predict that the height h q on a warm early Mars corresponds to a pressure leve…”
BackgroundInfluentialHabitable Zones Around Low Mass Stars and the Search for Extraterrestrial Life
Kasting, J. F. (1997) · Springer eBooks · doi:10.1007/978-94-015-8907-9_15 · Cited by 66
Self-citationOdert, P., Lammer, H., Erkaev, N. V., Nikolaou, A., Lichtenegger, H., Johnstone, C. P., Kislyakova, K. G., Leitzinger, M., & Tosi, N. (2017) · Icarus · doi:10.1016/j.icarus.2017.10.031 · Cited by 71
“Such hot atmospheres are typically well-mixed up to large heights (Abe and Matsui, 1988; Kasting, 1988; Lupu et al., 2014).”
BackgroundRadiation in the atmosphere of Venus
Titov, D. V., Bullock, M. A., Crisp, D., Renno, N. O., Taylor, F. W., & Zasova, L. V. (2007) · Geophysical monograph · doi:10.1029/176gm08 · Cited by 67
“However, Kasting et al. (1984) and Kasting (1988) suggested that a slightly subcritical Venus, with hot oceans and a wet stratosphere existed before this time.”
BackgroundMethodInfluentialRadiative transfer in CO2‐rich paleoatmospheres
Halevy, I., Pierrehumbert, R. T., & Schrag, D. P. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2009jd011915 · Cited by 62
“However, HDO has transitions where H2O does not mostly between 2500 and 3000 cm , a region that is unimportant for emission from early Earth and Mars, but one which may be important for a runaway greenhouse, such as that which occurred early in Venus’ history [Ingersol, 1969; Kasting, 1988].”
BackgroundBasilevsky, A. T., Shalygin, E. V., Titov, D. V., Markiewicz, W. J., Scholten, F., Roatsch, T., Kreslavsky, M. A., Moroz, L. V., Ignatiev, N., Fiethe, B., et al. (2011) · Icarus · doi:10.1016/j.icarus.2011.11.003 · Cited by 62
“If the felsic nature of venusian tesserae is confirmed in further studies, this may have important implications for geochemical environments in early history of Venus, indirectly supporting a hypothesis of water-rich early Venus (e.g. Kasting et al., 1984; Kasting, 1988; Grinspoon and Bullock, 2003).”
BackgroundInfluentialHarman, C. E., Felton, R. C., Hu, R., Domagal-Goldman, S. D., Segura, A., Tian, F., & Kasting, J. F. (2018) · The Astrophysical Journal · doi:10.3847/1538-4357/aadd9b · Cited by 67
“Runaway greenhouse planets like early Venus would be suspect because of their position near or inside the inner edge of the habitable zone (Kasting 1988; Kopparapu et al. 2013; Kane et al. 2014; Way et al. 2016).”
BackgroundSelf-citationClimate instability on tidally locked exoplanets
Kite, E. S., Gaidos, E. J., & Manga, M. (2015) · Cited by 61
Clouds and the Faint Young Sun ParadoxPreprint
Goldblatt, C., & Zahnle, K. (2013) · Cited by 67
Water Partitioning in Planetary Embryos and Protoplanets with Magma Oceans
Ikoma, M., Elkins-Tanton, L. T., Hamano, K., & Suckale, J. (2018) · Space Science Reviews · doi:10.1007/s11214-018-0508-3 · Cited by 60
“5, the thermal radiation from the top of the atmosphere decreases along with decrease in the surface temperature or increase in the atmospheric mass, but finally approaches ∼ 280 W/m2 (Abe and Matsui 1988; Kasting 1988; Goldblatt et al. 2013; Kopparapu et al. 2013).”
BackgroundImpacts and the Early Evolution of Life
Zahnle, K. J., & Sleep, N. H. (1997) · Springer eBooks · doi:10.1007/978-1-4757-2688-6_8 · Cited by 61
Runaway greenhouse effect on exomoons due to irradiation from hot, young giant planets
Heller, R., & Barnes, R. (2014) · International Journal of Astrobiology · doi:10.1017/s1473550413000463 · Cited by 60
“It could be caught in a moist greenhouse state with surface temperatures up to the critical point of water, that is, 647 K if an Earth-like inventory of water and surface H2O pressure are assumed (Kasting 1988).”
BackgroundLimaye, S. S., Mogul, R., Baines, K. H., Bullock, M. A., Cockell, C. S., Cutts, J. A., Gentry, D. M., Grinspoon, D. H., Head, J. W., III, Jessup, K.-L., et al. (2021) · Astrobiology · doi:10.1089/ast.2020.2268 · Cited by 60
“Extending the work of Pollack (1971), Kasting (1988), and Grinspoon and Bullock (2003), Way et al. (2016) concluded that the clouds and atmospheric dynamics of slowly rotating worlds (such as Venus) would mitigate atmospheric temperatures and water loss, and an ocean could have lasted several…”
BackgroundHedelt, P., von Paris, P., Godolt, M., Gebauer, S., Grenfell, J. L., Rauer, H., Schreier, F., Selsis, F., & Trautmann, T. (2013) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201117723 · Cited by 59
“Earlier calculations regarding the inner boundary of the HZ (Kasting 1988; Kasting et al. 1993) assumed instead a saturated troposphere, i.e. a relative humidity of unity.”
BackgroundYang, J., Leconte, J., Wolf, E. T., Merlis, T. M., Koll, D. D. B., Forget, F., & Abbot, D. S. (2019) · The Astrophysical Journal · doi:10.3847/1538-4357/ab09f1 · Cited by 59
“…as a result of a fundamental limit on infrared emission to space by an Earth-like planet, the “runaway greenhouse,” or the loss of a planet’s water through photodissociation and hydrodynamic escape due to high surface temperatures and a moist stratosphere, a “moist greenhouse” (Kasting 1988).”
Background
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