ピロキュムロニンブスは,平流層のエアロゾールの平均組成に影響する
J M Katich1,2, E C Apel3, I Bourgeois1,2
1National Oceanic and Atmospheric Administration (NOAA) Chemical Sciences Laboratory (CSL), Boulder, CO, USA.
まとめ
野火で発生するピロキュムロニンブス (pyroCb) 雲は ストラトスフィアに煙を注入します これらのPyroCbは,将来の気候に影響を及ぼす可能性のある平流層のエアロゾールに大きく貢献します.
科学分野:
- 大気科学
- 気候科学
- エアロゾール科学
背景:
- 野火によって形成されるピロキュムロニンブス (PyroCb) 雲は ストラトスフィアに煙を注入します
- pyroCbの気候への影響は,そのエピソード的性質のために不確実です.
研究 の 目的:
- パイロCbの煙が平流層のエアロゾール予算に与える影響を定量化する.
- パイロCbの長期的影響を理解する
主な方法:
- 13年間の空中観測の分析
- pyroCbの煙の性質を in situで測定した.
主要な成果:
- PyroCbの煙は独特で安定したエアロゾール特性を持っています.
- PyroCbは現在の低層圏の黒炭素と有機気溶液の10-25%に貢献しています.
- 北半球と南半球の両方で影響が観察されています.
結論:
- パイロCbは,大気圏のエアロゾール予算に大きな影響を与える.
- 将来の気候でピロCbの頻度や大きさが増加すると,平流圏の有力なエアロゾール傾向につながる可能性があります.
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