The Early Faint Sun Paradox: Organic Shielding of Ultraviolet-Labile Greenhouse Gases

Greenhouse Effect Photolysis Atmosphere Earth, Planet Ultraviolet Rays Carbon Dioxide 01 natural sciences 7. Clean energy Models, Chemical Ammonia 13. Climate action 0103 physical sciences Solar System Evolution, Planetary Methane
DOI: 10.1126/science.276.5316.1217 Publication Date: 2002-07-27T09:37:20Z
ABSTRACT
Atmospheric mixing ratios of ∼10 −5 ± 1 for ammonia on the early Earth would have been sufficient, through the resulting greenhouse warming, to counteract the temperature effects of the faint early sun. One argument against such model atmospheres has been the short time scale for ammonia photodissociation by solar ultraviolet light. Here it is shown that ultraviolet absorption by steady-state amounts of high-altitude organic solids produced from methane photolysis may have shielded ammonia sufficiently that ammonia resupply rates were able to maintain surface temperatures above freezing.
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