大気中のCO2濃度における極海と氷河のサイクル
Daniel M Sigman1, Mathis P Hain, Gerald H Haug
1Department of Geosciences, Guyot Hall, Princeton University, Princeton, New Jersey 08544, USA. sigman@princeton.edu
Nature
|July 3, 2010
まとめ
氷河期の間,南洋はより多くの二酸化炭素 (CO2) を吸収し,大気中のCO2を減少させた可能性があります. これは,海洋のCO2吸収が気候の調節の鍵であることを示唆しています.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 海洋学 海洋学 海洋学
- 気候科学 気候科学
背景:
- 地球の気候と大気中の二酸化炭素 (CO2) レベルは,氷河期とともに周期的に変動します.
- 低大気中のCO2濃度が氷河期を特徴づけているが,その背後にあるメカニズムは不明である.
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