Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1996-09-01 |
タイトル |
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タイトル |
FORMATION MECHANISM OF PLATE-LIKE ICE CRYSTALS GROWING IN AIR AT LOW TEMPERATURE AND LOW SUPERSATURATION |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00003925 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
論文名よみ |
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その他のタイトル |
FORMATION MECHANISM OF PLATE-LIKE ICE CRYSTALS GROWING IN AIR AT LOW TEMPERATURE AND LOW SUPERSATURATION |
著者名よみ |
ゴンダ, タケヒコ
マツウラ, ユキ
ワダ, マコト
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著者名(英) |
GONDA, Takehiko
MATSUURA, Yuki
WADA, Makoto
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著者所属(英) |
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en |
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Division of General Education, Aichi Gakuin University |
著者所属(英) |
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en |
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Research and Development Center, Toshiba Corporation |
著者所属(英) |
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en |
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National Institute of Polar Research |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
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. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA10756213 |
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
巻 10,
p. 66-72,
発行日 1996-09
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出版者 |
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出版者 |
National Institute of Polar Research |