Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1994-11-01 |
タイトル |
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タイトル |
FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE |
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 |
10.15094/00003840 |
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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) |
記事種別(英) |
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en |
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ABSTRACT |
論文名よみ |
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その他のタイトル |
FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE |
著者名よみ |
ゴンダ, タケヒコ
ワダ, マコト
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著者名(英) |
GONDA, Takehiko
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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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 |
σ^* is the critical supersaturation where kinetic roughening takes place. When the supersaturation σ<γ^*, prismatic facets are formed at the tips of primary branches of dendritic ice crystal. Then, the side branches are formed as a result of the shape instability of the prismatic facets with changing supersaturation. In the next place, when the supersaturation σ>σ^*, the tip shape of primary branches of dendritic ice crystal becomes round. In this case, the side branches are formed as a result of the change in the tip width of primary branches with changing supersaturation. Snow crystals observed in Antarctica are discussed on the basis of these experimental results. |
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 8,
p. 183,
発行日 1994-11
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出版者 |
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出版者 |
National Institute of Polar Research |