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.
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“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
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HABITABLE ZONES AROUND MAIN-SEQUENCE STARS: NEW ESTIMATES
Kopparapu, R. K., Ramirez, R., Kasting, J. F., Eymet, V., Robinson, T. D., Mahadevan, S., Terrien, R. C., Domagal-Goldman, S., Meadows, V., & Deshpande, R. (2013) · The Astrophysical Journal · doi:10.1088/0004-637x/765/2/131 · Cited by 1,615
“Rayleigh scattering by water was also considered by Kasting (1988); Kasting et al. (1993), but these authors used the scattering coefficient for air because the coefficient for H2O was not available, or at least not known to them.”
BackgroundMethodInfluentialSelf-citationKasting, J. F. (1993) · Science · doi:10.1126/science.11536547 · Cited by 1,374
Self-citationWater Vapor Feedback and Global Warming
Held, I. M., & Soden, B. J. (2000) · Annual Review of Energy and the Environment · doi:10.1146/annurev.energy.25.1.441 · Cited by 1,268
“Although it is difficult to be quantitative, primarily because of uncertainties in cloud prediction, it is clear that this point is only achieved for temperatures that are far warmer than any relevant for the global warming debate (22).”
BackgroundClimate sensitivity, sea level and atmospheric carbon dioxide
Hansen, J., Sato, M., Russell, G., & Kharecha, P. (2013) · Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences · doi:10.1098/rsta.2012.0294 · Cited by 660
Magma oceans in the inner solar system
Elkins-Tanton, L. T. (2012) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-042711-105503 · Cited by 601
“This cooling process requires millions to tens of millions of years (Abe & Matsui 1986; Matsui & Abe 1986; Kasting 1988; Zahnle et al. 1988; Elkins-Tanton 2008, 2011).”
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
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