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北半球では,大気循環の変化による近年の平流層HCl増加が観測されています

E Mahieu1, M P Chipperfield2, J Notholt3

  • 1Institute of Astrophysics and Geophysics, University of Liège, Liège 4000, Belgium.

Nature
|November 7, 2014
PubMed
まとめ

ストラトスフィアの塩素濃度は,大気循環の減速により,予想に反して増加しています. このトレンド異常はオゾン層の研究に影響を与え,大気動態の説明を必要とします.

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