,

F Forget1, R T Pierrehumbert

  • 1Laboratoire de Météorologie Dynamique du CNRS, Université Pierre et Marie Curie, Boite Postale 99, 4 place Jussieu, 75252 Paris Cedex 05, France. forget@lmd.jussieu.fr

Science (New York, N.Y.)
|November 21, 1997
PubMed
まとめ

初期の火星は,二酸化炭素の氷雲が熱を反射し,古代の流れる水の謎を解いて温暖化していたのかもしれない. この温室効果の変種は,地球の初期の気候や系外惑星の居住可能なゾーンについても説明できる.

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