プレオセンの温暖期における地球平均海面の制約
Oana A Dumitru1, Jacqueline Austermann2, Victor J Polyak3
1Karst Research Group, School of Geosciences, University of South Florida, Tampa, FL, USA.
Nature
|September 1, 2019
まとめ
過去の暖かい時代には 海面が著しく上昇していました この研究は,プレオセンの世界の平均海面 (GMSL) の変化を定量化し,氷床が温暖化に敏感であることを示しています.
科学分野:
- 古代気候学
- 海水位科学
- 氷床の動態
背景:
- 過去の海面の再構築は 長期の温暖化に対する 氷床の反応を理解するために 極めて重要です
- プレオセンの世界の平均海面 (GMSL) の現在の推定は,氷床の安定性の評価を制限するかなりの不確実性を持っています.
- プレオセンの時代は,特にピアケンス期中期の温暖期とプレオセンの気候最適期のような温暖期は,将来の気候シナリオの貴重なアナログとして機能します.
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