今日の強いエアロゾール冷却は,暑い未来を暗示しています.
Meinrat O Andreae1, Chris D Jones, Peter M Cox
1Max Planck Institute for Chemistry, PO Box 3060, Mainz 55131, Germany. andreae@mpch-mainz.mpg.de
Nature
|July 1, 2005
まとめ
大気中のエアロゾールは地球を冷却しますが,将来の地球温暖化への影響は不明です. エアロゾール冷却の減少は,温暖化が現在の予測を超えて加速する可能性を示唆しています.
科学分野:
- 気候科学 気候科学
- 大気化学 大気化学
- 地球システム科学 地球システム科学
背景:
- 人為的な温室効果ガスは地球温暖化を引き起こしている.
- 大気中のエアロゾールは冷却効果を発揮し,ある程度の温暖化に対抗する.
- エアロゾール効果の不確実性は,気候変動予測に重大な課題をもたらします.
研究 の 目的:
- 気候変動における大気中のエアロゾールの役割を調査する.
- 減少するエアロゾール冷却が将来の温暖化に与える影響を評価する.
- 気候感受性推定と炭素サイクルフィードバック予測を精査する.
主な方法:
- 気候モデルの出力の分析.
- エアロゾールと温室効果ガスに関する観測データのレビュー.
- エアロゾールと温室効果ガスの相互作用の評価.
主要な成果:
- エアロゾールによる冷却はかなりありますが,非常に不確実です.
- 将来のエアロゾール冷却は,よりクリーンな大気政策により減少すると予測されています.
- この減少は,将来の温暖化がIPCCの予測のより高い端にある可能性を示唆しています.
結論:
- エアロゾールの気候感受性に対する純効果は,依然として重要な不確実性です.
- エアロゾルの強制力の減少は,温室効果ガスの温暖化を増幅します.
- 将来の地球温暖化は,緩和措置を講じずに現在の上限予測を上回る可能性があります.
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