粉塵による滴の凍結は,北の熱帯圏外における雲の頂部を説明する
D Villanueva1, M Stengel2, C Hoose3
1Department of Environmental Systems Science, ETH Zürich, Zürich, Switzerland.
まとめ
北半球の雲の上の氷の形成に大きな影響を与えている. この発見は 35年間の衛星データに基づいていて 雲の性質とその気候への影響を 決定する要因を明らかにしています
科学分野:
- 大気科学
- 雲の物理
- 気候科学
背景:
- -39°Cから0°Cまでの混合相雲には,液体や氷の層があり,放射力強制と降水に影響を与えます.
- クラウドトップの氷対総周波数 (ITF) は重要な指標ですが,制御要因は不明です.
研究 の 目的:
- クラウドトップの氷対総周波数 (ITF) を制御する要因を調査する.
- 雲の結氷における 塵の作用を 調べるため
主な方法:
- 35年間の衛星データを分析した
- 粉塵エアロゾールとITFの空間時間相関分析
- 研究室での凍結実験と観測されたITF感度の比較
主要な成果:
- 北半球では, -15°Cから -30°Cの間の,強い時空相関が発見されました.
- 温度と塵に対するITF感度比は,実験室での滴冷凍測定値と一致しています.
結論:
- この温度範囲の雲の上の氷形成は主に塵のエアロゾールに起因する.
- 雲の相と気候の相互作用に影響を与える重要な要因として作用します.
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