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グリーンランドの温度反応は,最後の脱氷期における気候フォッシングによるものです

Christo Buizert1, Vasileios Gkinis2, Jeffrey P Severinghaus3

  • 1College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA. buizertc@science.oregonstate.edu.

Science (New York, N.Y.)
|September 6, 2014
PubMed
まとめ

グリーンランドの氷芯は,最後の脱氷期における急激な気候変動を明らかにしています. ユング・ドライアスは以前考えられていたよりも温暖で,CO2と日焼けによって引き起こされ,北大西洋に起因する変化があった.

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