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エオセンの同期的な熱帯と極地の温度進化
Marlow J Cramwinckel1, Matthew Huber2, Ilja J Kocken3
1Department of Earth Sciences, Faculty of Geoscience, Utrecht University, Utrecht, The Netherlands. m.j.cramwinckel@uu.nl.
Nature
|July 4, 2018
まとめ
大気中の二酸化炭素 (CO2) が多いエオセンの気候の再構築は,将来の気候変動を予測するのに役立ちます. 温室効果ガスがもたらす 熱帯と深海の温度変化が 海洋循環によって引き起こされるのです
科学分野:
- 古代気候学
- 気候モデリング
- 地化学
背景:
- 大気中のCO2濃度が高い過去の温暖な気候を理解することは 将来の気候変動予測に不可欠です
- エオセンの時代 (56~3400万年前) は6600万年ぶりの最高温であったが,連続した熱帯気温のデータは稀である.
- 以前の研究でエオセンの極熱が確認され,世界の気候の進化を定量化するための熱帯気温記録の必要性が強調された.
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