User:Carleydf/Anti-greenhouse effect/Bibliography

Bibliography

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Bibliography[edit]

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[edit]

^ 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.
^ 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
^ 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.
^ 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.
^ 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.
^ 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.

[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.

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