熱帯の新粒子の形成による雲凝縮核の大きな源
Christina J Williamson1,2, Agnieszka Kupc3,4, Duncan Axisa5,6
1Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA. christina.williamson@noaa.gov.
Nature
|October 18, 2019
まとめ
熱帯上の熱帯圏における新粒子の形成 (NPF) は,雲凝縮核 (CCN) の重要なグローバルな源である. 地球の40%以上で起こっています
科学分野:
- 大気科学
- 気候科学
- エアロゾール科学
背景:
- 雲の凝縮核 (CCN) は,雲の性質と地球の放射線バランスに影響を与えます.
- 自由なトロポスフィアの新粒子の形成 (NPF) は,特に遠隔地でのCCNの潜在的,まだ量化されていない源です.
研究 の 目的:
- 航空機の現地測定を用いて,NPFの発生に関する世界的な調査を実施する.
- トロピカル上層トロポスフィアのNPFがCCNの生産に与える貢献を決定する.
- 全球モデルにおけるNPFとその後の粒子の増加を評価する.
主な方法:
- エアロゾールのサイズ分布を空中で測定する.
- 熱帯コンベクト地域における垂直プロフィールの分析
- 総合的な評価のための化学物質輸送モデルとの統合
主要な成果:
- 太平洋と大西洋の熱帯コンベクティブ地域では,高い高度で強いNPFが観察されました.
- NPFは地球表面の約40%をカバーする熱帯上層熱帯圏の持続的な地球規模帯を形成しています.
- 熱帯上層熱帯圏のNPFは,下層熱帯圏に影響を与える,世界的に重要なCCN源です.
結論:
- 熱帯圏上部のNPFは,以前は過小評価されていたCCNの主要な源です.
- グローバルモデルでは,熱帯上層熱帯圏のNPFとCCNサイズへの粒子の成長の大きさを正確に捉えることができません.
- この発見は,正確な放射能バランスの見積もりのために,気候モデルにおけるNPFプロセスの改善の必要性を強調しています.
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