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北半球は,最後の脱氷期中に南半球の気候を強制した

Feng He1, Jeremy D Shakun, Peter U Clark

  • 1Center for Climatic Research, Nelson Institute for Environmental Studies, University of Wisconsin-Madison, Madison, Wisconsin 53706, USA. fenghe@wisc.edu

Nature
|February 8, 2013
PubMed
まとめ

氷河周期に関するミランコビッチの理論は支持されているが,南半球の気候変動がそれを挑戦している. 私たちのモデルは,軌道強制が北半球の脱氷を引き起こし,大西洋南半球の逆転循環の変化が南半球の温暖化を説明していることを示しています.

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