Formation mechanism of plate-like ice crystals growing in air at a low temperature and low supersaturation

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The supersaturation dependences on the slope of growth hillocks formed on the {1010} face P_P and the {0001} face P_B of ice crystals grown in air at -28.5℃ and low supersaturation were measured to study the formation mechanism of platelike ice crystals growing under this condition. As a result, it was found that both the {1010} and {0001} faces of plate-like ice crystals grown at -28.5℃ and low supersaturation grew by the Burton-Cabrera-Frank (BCF) mechanism, and when the relationship P_P>P_B held, plate-like ice crystals grew.

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詳細情報 詳細情報について

  • CRID
    1570009751946014080
  • NII論文ID
    110001026016
  • NII書誌ID
    AA10756213
  • ISSN
    09142037
  • 本文言語コード
    en
  • データソース種別
    • CiNii Articles

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