1991年から1992年の北極極旋風におけるストラトスフィアの気象条件
まとめ
AASE IIのストラトスフィアの条件は,窒酸三水素形成の観測を可能にしました. 極地渦は通常より早く温暖化し,平流圏の化学構造を混乱させた.
科学分野:
- 大気科学 大気科学
- ストラトスフィアの化学
- 北極の気象学 北極の気象学
背景:
- 1991-1992年の冬は,北極渦の位置付けにより,カナダ南東部の上空にユニークな平流圏条件を提供しました.
- アークティック・ストラトスフィア探査機II (AASE II) は,これらの現象を研究することを目的とした.
研究 の 目的:
- AASE II.中の平流圏気象条件を分析する.
- 窒酸三水素 (NAT) の形成と関連する化学的混乱を調査する.
主な方法:
- 1991-1992年の冬の平流層温度データを分析した.
- 温度データと潜在的NAT形成と化学変化の相関.
主要な成果:
- ストラトスフィアの気温は,12月上旬に窒素酸三水素の形成の可能性を示した.
- 極地渦の気温は,1月下旬までに通常より早く上昇した.
- 混乱した大気化学が観察され,冷たい平流層の温度と関連付けられました.
結論:
- 観測された気象条件は,極地平流層の雲形成の研究を容易にした.
- 極地渦の早期温暖化は,NAT形成に有利な条件の持続時間に影響を与えた.
- これらの条件は,平流層化学の重要な変化と関連していました.
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