大気科学:平流圏の冷却と熱帯圏
Nathan P Gillett1, Benjamin D Santer, Andrew J Weaver
1School of Earth and Ocean Sciences, University of Victoria, PO Box 3055, Victoria, British Columbia V8W 3P6, Canada. gillett@uvic.ca
Nature
|December 8, 2004
まとめ
衛星による気温データは,地表データよりも温暖化が少ないことを示しており,気候モデルと矛盾しています. 新しい方法は,平流層の冷却を修正し,衛星と地表の温暖化傾向を調整し,気候モデルのシミュレーションを検証します.
科学分野:
- 気候科学 気候科学
- 大気物理学 大気物理学
- リモートセンシングによる遠隔感知
背景:
- トロポスフィアの温度に関する衛星観測は,表面温度よりも温暖化が少ないことを示しており,確立された気候物理学と矛盾しています.
- Fu et al.による以前の研究. ストラトスフィアの冷却に関する統計的修正が提案されれば,これらの不一致を和らげることができる.
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