書誌事項
- タイトル別名
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- Experimental studies on the compressive viscosity of new snow
- シン セキセツ ノ アッシュク ネンセイリツ ニ カンスル ジッケンテキ ケンキュウ
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The objective of cold room experiments is to clarify the manner in which the relationship between the compressive viscosity and the snow density depends on the shape of the snow crystals, which comprise snowfall particles, and snow temperature during the process of metamorphism from dry new snow to lightly compacted snow.<BR>The following facts were obtained from the experimental results. The lower the snow temperature and pressure of the snow layer, the more was the time required for the metamorphism from dry new snow to lightly compacted snow. In new snow, the relationship between compressive viscosity and snow density was significantly influenced by the dominant crystal shape of the snowfall particles and the snow temperature.<BR>The compressive viscosity of the new snow that comprised rimed stellar crystals or stellar crystals with a planar external form was greater in general than that of the rimed spatial dendrites and graupels with a spherical external form. Moreover, the degree of dependence of the compressive viscosity on the snow temperature was influenced by the shape of the snow crystals.
収録刊行物
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- 雪氷
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雪氷 68 (3), 191-198, 2006
公益社団法人 日本雪氷学会
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詳細情報 詳細情報について
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- CRID
- 1390282681436649856
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- NII論文ID
- 10017509143
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- NII書誌ID
- AN00131221
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- ISSN
- 18836267
- 03731006
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- NDL書誌ID
- 7957701
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
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- 抄録ライセンスフラグ
- 使用不可