コメント on "アジアモンスーン輸送に関連した平流圏の大規模な火山性エアロゾール負荷"
J-P Vernier1, L W Thomason, T D Fairlie
1Science Systems and Applications, Inc., Hampton, VA 23666, USA. jeanpaul.vernier@nasa.gov
まとめ
ナブロ火山の噴火による二酸化硫黄の羽根は,アジアのモンスーンのコンベクションを経由してではなく,直接下層平流圏に到達した. CALIPSOのリダールデータは,梅雨がモンスーンシステムを回したことを示しています.
科学分野:
- 大気科学 大気科学
- 火山学 火山学とは
- リモートセンシング (リモートセンサー)
背景:
- 2011年6月13日のナブロ火山の噴火で,かなりの量の二酸化硫黄 (SO2) が放出されました.
- 以前の研究では,アジアのモンスーンの深いコンベクションが火山 SO2 を平流圏に輸送することを示唆していました.
- ストラトスフィアの注入メカニズムを理解することは,気候と大気化学の研究に不可欠です.
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