-
- 泉 典洋
- 北海道大学大学院公共政策学連携研究部
書誌事項
- タイトル別名
-
- Morphodynamics on the Ice Floor
- ヒョウショウ ジョウ ノ モルフォダイナミクス
この論文をさがす
抄録
Spiral troughs are observed on the polar ice caps of Mars. Interplanetary explorations indicate the troughs are perpendicular to katabatic winds blowing on the ice surface with jumps observed at the lee sides of troughs. Based on these observations, Smith et al. suggest they are not troughs but bedforms created by the sublimation of water carried by katabatic winds and ice on the floor. To demonstrate the fundamental processes forming bedforms on ice, linear stability analyses of the formation of boundary waves on the water-ice interface under laminar and turbulent flow conditions are presented. In addition, a formulation for the formation of boundary waves on ice due to katabatic winds is also proposed.
収録刊行物
-
- 地学雑誌
-
地学雑誌 125 (1), 105-119, 2016
公益社団法人 東京地学協会
- Tweet
詳細情報 詳細情報について
-
- CRID
- 1390001204238341888
-
- NII論文ID
- 130005138740
-
- NII書誌ID
- AN00322536
-
- ISSN
- 18840884
- 0022135X
-
- NDL書誌ID
- 027143776
-
- 本文言語コード
- ja
-
- データソース種別
-
- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
-
- 抄録ライセンスフラグ
- 使用不可