### 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 |
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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 |
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市 | Sydney, NSW |

期間 | 00/7/16 → 00/7/21 |

### Fingerprint

### ASJC Scopus subject areas

- Ocean Engineering

### これを引用

*Coastal Engineering 2000 - Proceedings of the 27th International Conference on Coastal Engineering, ICCE 2000*(巻 276, pp. 120-133)

**A unified numerical model for the bottom boundary layer and the upper layer in the surf zone.** / Duy, Nguyen The; Shibayama, Tomoya; Okayasu, Akio.

研究成果: Conference contribution

*Coastal Engineering 2000 - Proceedings of the 27th International Conference on Coastal Engineering, ICCE 2000.*巻. 276, pp. 120-133, Coastal Engineering 2000 - 27th International Conference on Coastal Engineering, ICCE 2000, Sydney, NSW, 00/7/16.

}

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

AN - SCOPUS:70349383108

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 -