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Updated: Sep 6, 2025

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Using Generative Art to Convey Past and Future Climate Transitions
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凝集型同位体温度測定による深海温度のケノゾイック進化
A N Meckler1, P F Sexton2, A M Piasecki1
1Bjerknes Centre for Climate Research and Department of Earth Science, University of Bergen, Bergen, Norway.
まとめ
過去6500万年の間,より暖かい深海の温度を示しています. これらの発見は,既存のケノゾイク海洋温度の再構築に挑戦し,重要な気候の変動性を強調しています.
科学分野:
- 古代気候学
- 地化学
背景:
- 過去の気候状態を理解することは,温室効果ガスの排出による将来の気候変動の影響を予測するために不可欠です.
- 酸素同位体に基づく再構築は,過去の海洋温度を決定するための古典的な方法です.
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