デニトリフィケーションによる北極圏オゾン層の減少
1Max-Planck-Institut fur Chemie, Post Office Box 3060, 55020 Mainz, Germany. Forschungszentrum Karlsruhe, Institut fur Meteorologie und Klimaforschung, Post Office Box 3640, D-76021 Karlsruhe, Germany. FU Berlin, Institut fur Meteorologie, Carl-Heinr.
まとめ
北極圏の窒素除去は,窒酸三水素粒子によって引き起こされ,オゾン層の破壊を大幅に増加させます. 将来の平流層の冷却は,オゾン層の回復を21世紀後半まで遅らせるかもしれない.
科学分野:
- 大気化学 大気化学
- ストラトスフィアの科学
- 気候モデリング
背景:
- 北極のオゾン層の減少は,重大な環境問題である.
- ストラトスフィアの反応性窒素は,オゾン化学において重要な役割を果たします.
- 粒子の堆積は,平流圏で知られているプロセスです.
研究 の 目的:
- 北極の脱窒化における粒子沈着の役割を調査する.
- 北極圏のオゾン層の減少に対する脱窒化の影響を定量化するために.
- 北極のオゾン回復の将来の軌道を評価する.
主な方法:
- 1994-95年の観測データで微物理モデルを制約する.
- 脱窒化プロセスのシミュレーションとそのオゾンへの影響.
- ストラトスフィアの条件に対する感受性研究を行う.
主要な成果:
- デニトリフィケーションは,主に低密度で窒素酸三水素粒子によって引き起こされます.
- デニトリフィケーションは,北極のオゾン層の損失を大幅に増加させます.
- 北極圏の平流層は,脱窒化値に近い.
結論:
- 人為的な二酸化炭素の増加は,平流層の冷却につながる可能性があります.
- 将来の冷却は,脱窒化を促進する可能性が高い.
- 北極圏のオゾン回復は,21世紀後半まで遅れると予測されています.
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