抄録
This paper presents a unified numerical model for the bottom boundary layer and the upper layer in the surf zone. The model is based on the 2-DV Reynolds equations for turbulent flows with free surface boundary. At each time step of computation, the numerical mesh generated for the physical domain is obtained by applying an algebraic mapping technique, in which grid points are clustered close to the sea bed to resolve the high velocity gradients expected in the bottom boundary layer.
| 元の言語 | English |
|---|---|
| ホスト出版物のタイトル | Coastal Engineering 2000 - Proceedings of the 27th International Conference on Coastal Engineering, ICCE 2000 |
| ページ | 120-133 |
| ページ数 | 14 |
| 巻 | 276 |
| 出版物ステータス | Published - 2000 |
| 外部発表 | Yes |
| イベント | Coastal Engineering 2000 - 27th International Conference on Coastal Engineering, ICCE 2000 - Sydney, NSW 継続期間: 2000 7 16 → 2000 7 21 |
Other
| Other | Coastal Engineering 2000 - 27th International Conference on Coastal Engineering, ICCE 2000 |
|---|---|
| 市 | Sydney, NSW |
| 期間 | 00/7/16 → 00/7/21 |
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ASJC Scopus subject areas
- Ocean Engineering
これを引用
A unified numerical model for the bottom boundary layer and the upper layer in the surf zone. / Duy, Nguyen The; Shibayama, Tomoya; Okayasu, Akio.
Coastal Engineering 2000 - Proceedings of the 27th International Conference on Coastal Engineering, ICCE 2000. 巻 276 2000. p. 120-133.研究成果: Conference contribution
}
TY - GEN
T1 - A unified numerical model for the bottom boundary layer and the upper layer in the surf zone
AU - Duy, Nguyen The
AU - Shibayama, Tomoya
AU - Okayasu, Akio
PY - 2000
Y1 - 2000
N2 - This paper presents a unified numerical model for the bottom boundary layer and the upper layer in the surf zone. The model is based on the 2-DV Reynolds equations for turbulent flows with free surface boundary. At each time step of computation, the numerical mesh generated for the physical domain is obtained by applying an algebraic mapping technique, in which grid points are clustered close to the sea bed to resolve the high velocity gradients expected in the bottom boundary layer.
AB - This paper presents a unified numerical model for the bottom boundary layer and the upper layer in the surf zone. The model is based on the 2-DV Reynolds equations for turbulent flows with free surface boundary. At each time step of computation, the numerical mesh generated for the physical domain is obtained by applying an algebraic mapping technique, in which grid points are clustered close to the sea bed to resolve the high velocity gradients expected in the bottom boundary layer.
UR - http://www.scopus.com/inward/record.url?scp=70349383108&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=70349383108&partnerID=8YFLogxK
M3 - Conference contribution
SN - 0784405492
SN - 9780784405499
VL - 276
SP - 120
EP - 133
BT - Coastal Engineering 2000 - Proceedings of the 27th International Conference on Coastal Engineering, ICCE 2000
ER -