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研究生:江裕明
研究生(外文):Yu-Ming Chiang
論文名稱:波流耦合數值及理論分析
論文名稱(外文):Numerical study and theoretical analysis ofwave-current interactions
指導教授:周逸儒
口試委員:蔡武廷陳世楠黃志誠
口試日期:2013-07-31
學位類別:碩士
校院名稱:國立臺灣大學
系所名稱:應用力學研究所
學門:工程學門
學類:機械工程學類
論文種類:學術論文
論文出版年:2013
畢業學年度:101
語文別:英文
論文頁數:64
中文關鍵詞:波流耦合水動力輻射應力SUNTANSM08
外文關鍵詞:wave-current interactionhydrodynamicradiation stressSUNTANSM08
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本研究為一系列探討波流耦合模式的流場。本篇以Mellor在2008年提出的輻射應力(稱M08)為研究起點。我們使用包含M08的SUNTANS (Fringer et al. [2006])來模擬離岸流。然而,我們希望可以發展出比以線性波更具真實性的輻射應力,其中我們考慮非對稱波的輻射應力,由結果卻發現使用相位平均的線性波與非對稱波的差異為一個基底常數。接著,考慮二階的Stokes非線性波,並為了表現出波峰波谷區間的差異性,我們採用半相位平均方式計算輻射應力,結果卻發現由線性波疊加的非線性波無法表現出此差異性。另一方面,我們對於M08將波流流速定義為常數感到懷疑,因此我們建置一個模式,來模擬由壓力梯度所驅動的波流耦合模式,我們將分別去計算波浪流速及整體的流速,再利用整體流速減去波浪流速得到一殘餘流速,而這殘餘流速即為波流耦合下所導致的波流速度。我們設置了一個簡單的理想平坦地形,透過此研究的模式,模擬出這個殘餘流速的分佈情形以及它所引起的自由水面的高度變化。結果顯示,殘餘流速並不為一個常數,而是一個具有週期性運動分布的流場,這個結果也成功的驗證了我們的懷疑。此外,我們並比較波浪流速和殘餘流速輻射應力,此結果也符合統御方程式的物理闡釋。在這研究中,我們已經初步完成此波流耦合模式的設置,並以驗證其正確性。

In this thesis, we study wave-current interactions using different approaches. We begin with the radiation stress by Mellor [2008] (M08). First, we use M08 in the SUNTANS model to simulate the rip current. In order to obtain the more realistic radiation stress, we examine the radiation stress using the asymmetric wave. However, the result is as same as that obtained from the linear wave but multiplying with a different constant coefficient, which is due to the phase-averaged method. In this regard, we develop a framework in which the half-cycle average is applied to the second-order Stokes wave, such that, individual characteristics of the crest and the trough can be represented. However, the result shows that the non-linear wave which is series of linear waves cannot show the skewness even with the half-cycle average. On the other hand, we are skeptical about all existing RS formulations that treat the wave-induced flow as a constant current. For this purpose, we develop a simplified 2DV hydrodynamics model to produce the wave-current flow field which is forced by the pressure gradient disregarding the wave shape. Using the model, we demonstrate that the RS-induced flow is a periodic, which is different from existing studies and confirm our hypothesis. Different contributions to the wave-induced current are also examined.

口試委員審定書 I
致謝 II
中文摘要 III
ABSTRACT IV
CONTENT V
LIST OF FIGURES VII
Chapter 1 Introduction 1
1.1 Motivations 1
1.2 Wave-Current Interaction 3
Chapter 2 Review of the Wave Theory 8
2.1 inear Wave Theory 8
2.1.1 Assumptions and the simplified governing equations 8
2.1.2 The basic solution for the simplified equation 10
2.2 Brief Introduction of the Wave Transformation 12
2.2.1 Wave shoaling 12
2.2.2 Wave breaking 14
2.2.3 Wave setup and set down 15
2.3 Review of the Second-Order Stokes Wave Theory 19
2.3.1 Introduction of the Stokes wave theory 19
2.3.2 The solution for the equation of the second-order Stokes wave 20
Chapter 3 Modeling Wave-Current Interaction 24
3.1 verview of M08 – Linear Waves 24
3.2 Modeling Wave-Current Interactions in SUNTANS 26
3.3 Asymmetric Waves 30
3.3.1 Motivation 30
3.3.2 Simulation of the radiation stress in the asymmetric wave 31
Chapter 4 Modeling Wave-Current Interaction 33
4.1 alf-Cycle Average of the Second-Order Stokes Wave 33
4.1.1 uβuαsz 35
4.1.2 Pressure gradient 38
4.1.3 Final result 42
4.2 Phase-Resolving Radiation Stress 45
4.2.1 Initialization 46
4.2.2 Computation process 46
Chapter 5 Discussion 50
5.1 Validation Case 50
5.2 Surface Elevation Induced by 51
5.3 Sources of Wave-Induced Current 53
Chapter 6 Conclusion and Futures Works 58
6.1 Conclusion 58
6.2 Future Works 59
Appendix The Mean Flow Energy Equation 61
Reference 63

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