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Updated: May 24, 2026

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Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
氷河期間の第11段階における極地の氷床の崩壊
Maureen E Raymo1, Jerry X Mitrovica
1Lamont-Doherty Earth Observatory, Columbia University, PO Box 1000, 61 Route 9W, Palisades, New York 10964, USA. raymo@ldeo.columbia.edu
Nature
|March 16, 2012
まとめ
プレイストセンの海水位は,以前考えられていたほど高くはなかった. 新しい分析によると,グリーンランドと西南極の氷床は40万年前に崩壊し,東南極の氷床は安定していた.
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
- 四次地質学 四次地質学
- 海水面再建工事について
背景:
- ベルミューダとバハマのプレイストセンの海岸線の特徴は,海面が今日より20m以上高く,約40万年前にあったことを示唆しています.
- これらの特徴は,氷河期における長期にわたる温暖期である海洋同位体段階 (MIS) 11に起因する.
- 以前の仮説では,大きな氷床の溶け方やメガ津波が原因だと考えられていた.
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