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氷山は北大西洋の寒冷現象の引き金ではない
Stephen Barker1, James Chen1, Xun Gong1
1School of Earth and Ocean Sciences, Cardiff University, Cardiff CF10 3AT, UK.
Nature
|April 17, 2015
まとめ
Dansgaard-Oeschger現象のような突然の気候変動は,北大西洋の冷却に関連しています. 氷山の放出は,これらの寒いスタジアム条件に起因するのではなく,それに続くようです.
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
- 気候のダイナミクス
- 海洋学 海洋学 海洋学
背景:
- プレイストセンの後半の気候は,ダンズガード-オシュガー現象を含む突然の変化を特徴とし,暖かい段階間の条件と冷たい段階の条件の間のシフトによって特徴付けられました.
- グリーンランドの氷の核に記録されたこれらの現象は,大西洋の循環を覆う大西洋の変化としばしば関連しています.
- 北大西洋の寒冷現象は,氷山の産卵の増加と相関しており,淡水強制を用いた気候モデリング研究を促しています.
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