コメント "改訂された古高測量データは,エオセンの間のチベット高原の低い高さを示している"
Paul J Valdes1, Ding Lin2,3, Alex Farnsworth4
1School of Geographical Sciences and Cabot Institute, University of Bristol, Bristol BS8 1SS, UK. p.j.valdes@bristol.ac.uk.
まとめ
この研究は,エオセンのチベット高原の高さの推定に異議を唱える. 過去の結論は 欠陥のある気候モデルと データの比較に基づいたもので 高い平原を示唆しています
科学分野:
- 古代気候学
- 地質科学
- 気候モデリング
背景:
- 以前の研究では,低エオセンのチベット高原の高さ (<3000m) が示唆されていた.
- この結論は酸素同位体のプロキシデータと気候モデルのシミュレーションに基づいています.
研究 の 目的:
- エオセンのチベット高原の 提案された低い高さを再評価する.
- 以前の研究で用いられた方法論の欠陥を特定し,対処する.
主な方法:
- 同位体対応の気候モデルシミュレーションの批判的分析
- 酸素同位体のプロキシデータの解釈の再検討
- 地質学的証拠とのモデリング出力の比較.
主要な成果:
- 気候モデルの重大な欠陥を特定した.
- 代理データとモデルのシミュレーションの 比較で不一致を 発見しました
- 低エオセンの高原を支えるために用いられた方法論は不十分であると考えられています.
結論:
- 以前に提案された低エオセンのチベット高原の高さは,堅固な証拠によって支持されていません.
- 気候モデリングとデータ解釈の欠陥は,以前の結論を弱体化します.
- エオセンのチベット高原の高さを決定するには,改良された方法によるさらなる研究が必要である.
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