作者: S. C. Whalen , W. S. Reeburgh , C. E. Reimers
DOI: 10.1007/978-3-662-01145-4_12
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摘要: The recent global increase of 1% per year in the concentration atmospheric methane (CH4) is well documented (Rasmussen and Khalil 1984; Steele et al. 1987; Blake Rowland 1989). This causes concern because CH4 an important trace gas earth’s atmosphere. Greenhouse warming from 25% CO2-induced warming, together these gases account for 75% radiative trapping (Rodhe 1990).