"大気中の酸素濃度による長期的気候強制"に関するコメント
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, Canada.
まとめ
低気圧の酸素は 気候を温暖化させないかもしれません 放射能と大気圧の変化は冷却を引き起こす可能性があり,以前の発見と矛盾し,気候モデルへのさらなる調査が必要である.
科学分野:
- 地球科学
- 古代気候学
- 大気科学
背景:
- ポールセン ほか ファネロゾイク大気中の酸素レベルが低下すると 温暖な気候が生まれると提案した.
- この仮説は,低圧と変化した放射性移転が通常冷却を誘導する確立された原理と対照的です.
研究 の 目的:
- ファネロゾイク時代の 大気中の酸素レベルと 地球の気候の関係を再評価する
- 想定される温暖化と予想される冷却効果の違いを調査する.
主な方法:
- 気候モデルにおける放射能移転過程の分析
- 圧力の変化による大気構造の変化の調査.
- モデルの出力を比較して不一致を特定する.
主要な成果:
- 低気圧と酸素の減少は冷却効果を誘導する.
- 低圧下での放射性移転変化も気候の冷却に寄与する.
- 既存の気候モデルでは 酸素濃度や気温に関して 矛盾する結果が出ています
結論:
- ファネロゾイク低酸素レベルが温暖化を引き起こしたという主張は,さらなる調査を必要としています.
- 観察されたモデル衝突の詳細なメカニズム的な説明が必要である.
- 気候モデルにおける放射能と雲のプロセスの表現に注目すべきです.
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