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大気中のCO2と気候は,最後の氷河期における数千年の時間スケールで示されています

Jinho Ahn1, Edward J Brook

  • 1Department of Geosciences, Oregon State University, Corvallis, OR 97331-5506, USA. jinhoahn@gmail.com

Science (New York, N.Y.)
|September 13, 2008
PubMed
まとめ

古代の二酸化炭素 (CO2) レベルは南極の温度と相関しており,南洋が気候サイクルに影響を及ぼすことを示唆しています. CO2の上昇は北半球の温暖化イベントに先行し,地球の炭素循環のダイナミクスについての洞察を提供しました.

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