熱帯大西洋の10年間の変動は,外からの圧力によって支配されている
Chengfei He1, Amy C Clement2, Sydney M Kramer3
1Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL, USA. cxh1079@miami.edu.
Nature
|September 13, 2023
まとめ
熱帯大西洋の海面温度 (SST) グラデーションは,人間の排出と火山のエアロゾールによって引き起こされ,ハリケーン活動とサヘルの降雨に大きく影響します. この重要な気候関連性は モデルバイアスが修正されたときにより明確になります
科学分野:
- 気候科学
- 大気科学
- 海洋学
背景:
- 熱帯大西洋の気候は,海面温度 (SST),サヘルの降雨量,ハリケーン活動における多十年間の変動を示しています.
- これらの相互接続した気候システムの物理的起源は,モデルと観測の不確実性のために議論されている.
研究 の 目的:
- 熱帯大西洋 SSTにおける赤道横断グラデントが,大西洋のハリケーン形成とサヘルの降雨の原動力として果たす役割を調査する.
- これらの気候関係のシミュレーションにおけるCMIP6地球システムモデルのパフォーマンスを評価する.
主な方法:
- 歴史的な気候データとCMIP6地球システムモデルの大きなアンサンブルの分析.
- 北半球と南半球の温暖化傾向と関連する大気変化のシミュレーションにおけるモデルバイアスの特定と修正.
- 修正されたSSTグラデーションと気候の影響の相関分析
主要な成果:
- 放射性強迫 (人為的排出,火山噴出物) によって影響される赤道横断の熱帯大西洋SSTグラデントは,ハリケーン活動とサヘルの降雨を決定する重要な要因です.
- CMIP6モデルは北半球の温暖化傾向を過大評価し,SSTと気候の関係を隠しています.
- モデルバイアスを修正すると,特に1950年以降,SSTのグラデーションと気候の影響の間の強い相関が明らかになる.
結論:
- 熱帯大西洋 SST グラデントは,より広い北大西洋 SST よりも熱帯気候の影響の重要な原動力です.
- 人為的な排出と火山活動を含む放射能強制は,大西洋のハリケーン活動とサヘルの降雨変動を予測することができます.
- 将来の予測の正確さは,シグナル対ノイズパラドックスと将来の気候強制力の不確実性によって制限されています.
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