暴走温室効果
1. Runaway greenhouse effectA runaway greenhouse effect is a process in which a net positive feedback between surface temperature and atmospheric opacity increases the strength of the greenhouse effect on a planet until its oceans boil away. An example of this is believed to have happened in the early history of Venus. On the Earth, the IPCC states that "a 'runaway greenhouse effect'—analogous to Venus—appears to have virtually no chance of being induced by anthropogenic activities.
Read “Runaway greenhouse effect” on English Wikipedia
Read “暴走温室効果” on Japanese Wikipedia
Read “Runaway greenhouse effect” on DBpedia
Read “Runaway greenhouse effect” on English Wikipedia
Read “暴走温室効果” on Japanese Wikipedia
Read “Runaway greenhouse effect” on DBpedia
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