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熱帯温暖化プールが大幅に拡大し,プレオセンの初期にハドリー循環を弱めた

Chris M Brierley1, Alexey V Fedorov, Zhonghui Liu

  • 1Department of Geology and Geophysics, Yale University, New Haven, CT 06520, USA.

Science (New York, N.Y.)
|March 3, 2009
PubMed
まとめ

プレオセンの温帯間隔は,海洋温帯の極方への膨張によって引き起こされ,温度グラデーションが減少した可能性が高い. これは,この期間に海洋熱吸収機構の強化が活発であったことを示唆している.

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