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Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
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継続的に超冷却された液体の水が -37.5°Cまで下がった深層のコンベクト雲

Rosenfeld1, Woodley

  • 1Institute of Earth Sciences, the Hebrew University of Jerusalem, Israel. daniel@vms.huji.ac.il

Nature
|June 6, 2000
PubMed
まとめ

雲の過程を理解する上で極めて重要な超冷却液体の水は,深層のコンベクティブ雲の中で発見されました. これらの発見は,液体の水が -37.5°Cまで持続し,天気と気候モデルに影響を与えることを示しています.

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