書誌事項
- タイトル別名
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- BOUNDARY WAVES FORMED ON THE ICE FLOOR DUE TO KATABATIC WIND
- カタバフウ ニ ヨッテ ヒョウショウ ジョウ ニ ケイセイ サレル カイメンハ
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The spiral troughs on Mars' polar ice caps are considered as cyclic steps formed on ice due to katabatic wind. Katabatic wind is a type of density current which flows downward pulled by gravity because of the denser air cooled by the ice floor. Due to the spatial non-uniformity of solidification of water vapor included in the air onto the ice floor, and sublimation of ice into the air, the boundary waves are formed on the ice floor. We performed laboratory experiments simulating the condition that katabatic wind blows on ice. Boundary waves were formed on the ice in the case that there was a large difference in temperature between the room air and the bottom of the ice.
収録刊行物
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- 土木学会論文集B1(水工学)
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土木学会論文集B1(水工学) 72 (4), I_739-I_744, 2016
公益社団法人 土木学会
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詳細情報 詳細情報について
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- CRID
- 1390001205353294720
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- NII論文ID
- 130005312147
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- NII書誌ID
- AN10426673
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- ISSN
- 18808751
- 2185467X
- 09167374
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- NDL書誌ID
- 027185200
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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
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