最後の氷河期の始まりの間に,中央ヨーロッパで遅いエエム紀の乾燥脈が鳴った
F Sirocko1, K Seelos, K Schaber
1Institute of Geoscience, Johannes Gutenberg-University, 55099 Mainz, Germany. sirocko@uni-mainz.de
Nature
|August 12, 2005
まとめ
過去の氷河期間の気候変化を理解することは,現在の気候変動を予測する鍵です. 塵の嵐と冷却によって特徴づけられた468年のエミアン乾燥脈は,氷河の始まりに先行し,急激な気候変動の洞察を提供しました.
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
- 四次期の地質学
背景:
- 最後の氷河間期 (エミアン) の終わりを調査することは,現在の氷河間気候の動態と将来の気候変動の可能性を理解するために不可欠です.
- 軌道圧迫とインソレーションの変化は,長期の気候変動の要因として知られています.
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