User:Carleydf/Anti-greenhouse effect/Bibliography

Bibliography

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R. Courtin, C. P. McKay & J. Pollack (May 1992). "L'effet de serre dans le systeme solaire". La Recherche. 23 (243): 542–9. Bibcode:1992Rech...23..542C.[1]

  • This source defines the anti-greenhouse effect as deriving from a high-altitude layer that either absorbs or diffuses visible light, which is different from the current definition.
  • This is an article in a peer-reviewed scientific journal, so it should be a reliable source for a specific fact.
  • Photochemistry from solar radiation, condensation of gases onto particles, and injection of particles into the upper atmosphere can all contribute to the fine particles in the layer.
  • This source compares this effect to volcanic dust and nuclear winter on Earth.
  • This source describes an anti-greenhouse effect on Mars, though weak, due to strong storms.

C. Covey, R. M. Haberle, C. P. McKay & D. V. Titov (2013). "The greenhouse effect and climate feedbacks". Comparative Climatology of Terrestrial Planets (S. J. Mackwell et al., eds.), pp. 163–179. Univ. of Arizona, Tucson, doi:10.2458/azu_uapress_9780816530595-ch007.[2]

  • This is a chapter from a book published by a university press, so it should be a reliable source.
  • This source reports the equations and reasoning that leads to the (1/2)^(1/4) factor in surface temperature.

D. C. Catling & J. F. Kasting (2017). Atmospheric evolution on inhabited and lifeless worlds. Cambridge University Press. ISBN 9780521844123[3]

  • This is a book published by a university press, so it should be a reliable source.
  • The high-altitude layer in other sources is now labeled as in the stratosphere in the case of Titan and is described as being the cause of the stratospheric temperature inversion.
  • Titan's atmospheric window is roughly from 16.5 to 25 micrometers (microns).
  • Compares Earth's stratospheric ozone layer to Titan's organic haze where the temperature inversion is due to absorption of solar radiation.
  • The ratio of methane to carbon dioxide determines whether particles can be formed from the photolysis of methane. Need a value greater than about 0.1.

J. Roberts (1971). "Late Precambrian glaciation: an anti-greenhouse effect?". Nature 234, 216–7. https://doi.org/10.1038/234216a0[4]

  • This is an article in a peer-reviewed scientific journal, so it should be a reliable source for a specific fact.
  • This only mentions anti-greenhouse effect once at the very end of the article. Thus this source cannot be used for notability.
  • However, this is the oldest source I can find that uses the phrase anti-greenhouse effect, which has a different definition: an effect where the locking up of carbon dioxide in carbonates reduces the greenhouse effect. (See 1976 paper: https://www.jstor.org/stable/30060886?seq=1)

Kump, Lee R. (2010). The earth system. James F. Kasting, Robert G. Crane (3rd ed.). San Francisco: Prentice Hall. ISBN 978-0-321-59779-3. OCLC 268789401[5]

  • This is a book published by a British-owned education publishing company, so it should be a reliable source.
  • Chapter 12 includes discussion of the anti-greenhouse effect and its role as a potential climate regulator on Earth.
  • States that McKay coined the term anti-greenhouse effect.

Haqq-Misra, Jacob D.; Domagal-Goldman, Shawn D.; Kasting, Patrick J.; Kasting, James F. (December 2008). "A Revised, Hazy Methane Greenhouse for the Archean Earth". Astrobiology. 8 (6): 1127–1137. doi:10.1089/ast.2007.0197. ISSN 1531-1074.[6]

  • This is an article in a peer-reviewed scientific journal, so it should be a reliable source for a specific fact.
  • Shows how organic haze could have formed on Archean Earth, thus creating an anti-greenhouse effect.

References

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  1. ^ Courtin, R.; McKay, C. P.; Pollack, J. (May 1992). "L'effet de serre dans le système solaire". La Recherche. 23 (243): 542–9. Bibcode:1992Rech...23..542C.
  2. ^ Covey, C.; Haberle, R. M.; McKay, C. P.; Titov, D. V. (2013), "The Greenhouse Effect and Climate Feedbacks" (PDF), Comparative Climatology of Terrestrial Planets, University of Arizona Press, doi:10.2458/azu_uapress_9780816530595-ch007, ISBN 978-0-8165-3059-5, retrieved 2022-05-25
  3. ^ Catling, David C. (2017). Atmospheric Evolution on Inhabited and Lifeless Worlds. James F. Kasting. West Nyack: Cambridge University Press. ISBN 978-1-139-02055-8. OCLC 982451455.
  4. ^ Roberts, J. D. (26 November 1971). "Late Precambrian Glaciation: an Anti-Greenhouse Effect?". Nature. 234 (5326): 216–217. doi:10.1038/234216a0. ISSN 0028-0836.
  5. ^ Kump, Lee R. (2010). The earth system. James F. Kasting, Robert G. Crane (3rd ed.). San Francisco: Prentice Hall. ISBN 978-0-321-59779-3. OCLC 268789401.
  6. ^ Haqq-Misra, Jacob D.; Domagal-Goldman, Shawn D.; Kasting, Patrick J.; Kasting, James F. (December 2008). "A Revised, Hazy Methane Greenhouse for the Archean Earth". Astrobiology. 8 (6): 1127–1137. doi:10.1089/ast.2007.0197. ISSN 1531-1074.