抄録
Boundary mixing was generated by oscillating the incline along its plane. It was observed that when the background turbulence is strong, such typical characteristics of the gravity current as the "raised-head' structure and the sharp front disappear. Quantitative measurements on the frontal velocity, density structure, and the thickness of the gravity current were made, and their dependencies on the intensity of turbulence at the boundary are presented. -from Authors
| 本文言語 | 英語 |
|---|---|
| ページ（範囲） | 12,586-12,592 |
| ジャーナル | Journal of Geophysical Research |
| 巻 | 96 |
| 号 | C7 |
| DOI | |
| 出版ステータス | 出版済み - 1991 |
!!!All Science Journal Classification (ASJC) codes
- 地球物理学
- 林業
- 海洋学
- 水圏科学
- 生態学
- 水の科学と技術
- 土壌科学
- 地球化学および岩石学
- 地表過程
- 大気科学
- 地球惑星科学（その他）
- 宇宙惑星科学
- 古生物学