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A multi-tiered Bayesian network coastal compound flood analysis framework 多层贝叶斯网络沿海复合洪水分析框架
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-14 DOI: 10.1016/j.coastaleng.2025.104895
Ziyue Liu , Meredith L. Carr , Norberto C. Nadal-Caraballo , Luke A. Aucoin , Madison C. Yawn , Michelle T. Bensi
Coastal compound floods (CCFs) are triggered by the interaction of multiple coastal and inland mechanisms, such as storm surges, storm rainfall, tides, and river flow. These events can bring significant damage to communities, and there is an increasing demand for accurate and efficient probabilistic analyses of CCFs to support risk assessments and decision-making. In this study, a multi-tiered Bayesian network (BN) CCF analysis framework is established. In this framework, conceptual designs of multiple tiers of BN models with varying complexities are developed for application with varying levels of data availability and resources. A case study is conducted in New Orleans, LA, with three tiers of BN models constructed to demonstrate this framework. In the Tier-1 BN model, storm surges and river flow are incorporated based on hydrodynamic simulations. A seasonality node is used to capture the dependence between concurrent river flow and tropical cyclone (TC) parameters. In the Tier-2 BN model, joint distribution models of TC parameters are built for separate TC intensity categories. TC-induced rainfall is modeled as input to hydraulic simulations. In the Tier-3 BN model, potential variations of meteorological conditions are incorporated by quantifying their effects on TC activity and coastal water level. Flood antecedent conditions are also incorporated to more completely represent the conditions contributing to flood severity. In this case study, a series of joint distribution, numerical, machine learning, and experimental models are used to compute conditional probability tables needed for the BNs. A series of probabilistic analyses is performed based on these BN models, including CCF hazard curve construction and CCF deaggregation. The results of the analysis demonstrate the promise of this framework in performing CCF hazard analysis under varying levels of resource availability and project needs.
沿海复合洪水是由风暴潮、暴雨、潮汐和河流流量等多种沿海和内陆机制共同作用引发的。这些事件可能给社区带来重大损害,因此越来越需要对CCFs进行准确和有效的概率分析,以支持风险评估和决策。本研究建立了多层贝叶斯网络(BN) CCF分析框架。在该框架中,针对不同数据可用性和资源水平的应用,开发了具有不同复杂性的多层BN模型的概念设计。在LA新奥尔良进行了一个案例研究,构建了三层BN模型来演示该框架。在Tier-1 BN模式中,基于水动力模拟纳入了风暴潮和河流流量。季节性节点用于捕获同期河流流量与热带气旋参数之间的依赖关系。在Tier-2 BN模型中,针对不同的TC强度类别建立了TC参数的联合分布模型。tc引起的降雨被建模为水力模拟的输入。在第3层BN模式中,通过量化气象条件对TC活动和沿海水位的影响,纳入了气象条件的潜在变化。洪水前条件也被纳入,以更完整地代表导致洪水严重程度的条件。在本案例研究中,使用了一系列联合分布、数值、机器学习和实验模型来计算bn所需的条件概率表。基于这些BN模型进行了一系列的概率分析,包括CCF危险曲线的构建和CCF的解聚。分析结果表明,在不同水平的资源可用性和项目需求下,该框架在进行CCF危害分析方面具有前景。
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引用次数: 0
The Depth-Semi-Averaged model: Benchmarking and applications to 2D and 3D problems 深度-半平均模型:对2D和3D问题的基准和应用
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-14 DOI: 10.1016/j.coastaleng.2025.104893
M. Antuono , A. Lucarelli , G. Colicchio , M. Brocchini
The present work provides a number of applications of the Depth-Semi-Averaged model described in Antuono et al. (2022) for different wave conditions and geometries. These include analytical test cases, experimental benchmarks in 2D and 3D frameworks, and simulations of wave dynamics at a real coastal site. Breaking and non-breaking waves are considered, depending on the specific problem under investigation. The aim of the work is to provide an overview of the model potentialities and limits of application and to highlight its similarities and differences in comparison to existing non-hydrostatic schemes. More specifically, the model accurately captures wave propagation phenomena, including refraction and dispersion in non-breaking cases, and demonstrates satisfactory performance in reproducing wave decay caused by turbulence during breaking.
目前的工作提供了Antuono等人(2022)中描述的深度半平均模型在不同波浪条件和几何形状下的许多应用。其中包括分析测试案例,2D和3D框架的实验基准,以及在真实海岸现场的波浪动力学模拟。根据所研究的具体问题,考虑破碎波和非破碎波。这项工作的目的是概述模型的潜力和应用的限制,并突出其与现有非流体静力方案的异同。更具体地说,该模型准确地捕获了波的传播现象,包括非破裂情况下的折射和色散,并在再现破裂时湍流引起的波衰减方面表现出令人满意的性能。
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引用次数: 0
Hydrodynamic performance of nested dual-chamber OWC breakwaters for enhanced power stability and wave attenuation 巢式双室OWC防波堤的水动力性能及动力稳定性
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-14 DOI: 10.1016/j.coastaleng.2025.104896
Chen Peng , Dezhi Ning , Feng Zhou
Coastal communities face the challenge of mitigating wave-induced hazards while promoting the utilization of renewable wave energy for sustainable development. This study proposes a novel Nested Dual-chamber Oscillating Water Column (ND-OWC) breakwater, designed to enhance power stability while maintaining effective wave attenuation for sustainable coastal defense. The structure integrates a bottom-mounted leeward inlet OWC as the inner chamber and a suspended semi-annular OWC as the outer chamber, forming modular units that are arranged perpendicular to the wave propagation direction to function as a multifunctional breakwater. A comprehensive Computational Fluid Dynamics (CFD) study was conducted to evaluate the hydrodynamic performance of the ND-OWC at both unit and array scales. Results indicate that in the ND-OWC unit, the inner chamber enhances oscillations in the outer chamber, leading to a synergistic increase in energy capture by up to 48.25 %. Moreover, the staggered power contributions from the two chambers reduce power fluctuation by up to 75.61 %, supporting stable power output. Units within the array retain energy capture performance comparable to that of a single unit, while the array configuration ensures effective wave attenuation, with transmission coefficients below 0.60 for 50 % of tested cases. Tightly spaced arrays offer superior wave attenuation but exhibit reduced power stability. Compared with other bottom-mounted OWC array configurations, the present design provides mid-range energy capture while consistently achieving superior wave attenuation and power stability. These findings demonstrate the potential of the ND-OWC system as a viable solution for sustainable coastal protection and renewable energy utilization.
沿海社区面临着减轻海浪危害的挑战,同时促进可再生波浪能源的利用,促进可持续发展。本研究提出了一种新型的巢式双腔振荡水柱(ND-OWC)防波堤,旨在提高电力稳定性,同时保持有效的波浪衰减,以实现可持续的海防。该结构集成了一个底部安装的背风入口OWC作为内室,一个悬挂的半环形OWC作为外室,形成垂直于波浪传播方向的模块化单元,作为多功能防波堤。为了评估ND-OWC在单元和阵列尺度上的水动力性能,进行了全面的计算流体动力学(CFD)研究。结果表明,在ND-OWC装置中,内腔增强了外腔的振荡,导致能量捕获的协同增加高达48.25%。此外,两腔错开的功率贡献减少了75.61%的功率波动,支持稳定的功率输出。阵列内的单元保持了与单个单元相当的能量捕获性能,而阵列配置确保了有效的波衰减,在50%的测试案例中透射系数低于0.60。紧密间隔的阵列提供优越的波衰减,但表现出较低的功率稳定性。与其他底部安装的OWC阵列配置相比,本设计提供中程能量捕获,同时始终实现卓越的波衰减和功率稳定性。这些发现证明了ND-OWC系统作为可持续海岸保护和可再生能源利用的可行解决方案的潜力。
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引用次数: 0
Effectiveness of restored mangrove wetlands in damping waves 红树林湿地恢复后的减波效果
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-10 DOI: 10.1016/j.coastaleng.2025.104894
Zongyao Chen , Wen Wei , Xiufang Qiu , Yulu Yang , Heng Wang
There has been a global attention on the feasibility and embodiment of integrating the mangrove wetlands into coastal defense. However, little evidence is related to the restored mangroves (with mangrove trees artificially planted), which is increasingly important under ongoing wetland restoration worldwide. Here, wave propagation across a restored Kandelia obovata mangrove wetland on the Hailing Island, Guangdong Province, China, was observed to examine the wave damping effectiveness of the restored mangroves and their potential in coastal defense. The results showed that waves were attenuated by 26 % as they passed through the studied mangrove wetland. The wave attenuation rate of the bare flat was inversely proportional to water depth, and that of the mangrove forest was linked to its submerged state, peaking when the canopy was partially submerged. The restored mangrove attenuated waves more effectively than the bare flat, and showed reliable wave damping ability even in comparisons with natural marsh and mangrove vegetations. This evidence supports the feasibility of utilizing the restored mangroves in nature-based coastal defense. Furthermore, an idealized model was established to examine how the width of the restored mangrove impacts the gross wave attenuation. It is found that wave height reduction increases under a larger restored mangrove width, while the increase is nonlinear. We then proposed an optimal mangrove width proportion of 15 % for the studied wetland, under which the mangrove wetland showed a reliable gross wave height reduction together with a relatively large efficiency. These findings provide important insights into mangrove-induced wave attenuation and its implications for nature-based coastal defense worldwide.
将红树林湿地纳入海防的可行性和具体化一直是全球关注的问题。然而,与红树林的恢复(人工种植红树林)有关的证据很少,红树林在世界范围内正在进行的湿地恢复中越来越重要。在这里,我们观察了波浪在中国广东省海岭岛恢复后的红树湿地上的传播,以研究恢复后的红树湿地的波浪阻尼效果及其在海防中的潜力。结果表明,波浪在通过红树林湿地时衰减了26%。裸滩的波浪衰减率与水深成反比,红树林的波浪衰减率与其淹没状态有关,在冠层部分被淹没时达到峰值。恢复后的红树林比光秃秃的平地更有效地衰减波浪,即使与天然沼泽和红树林植被相比,也表现出可靠的减波能力。这一证据支持了利用恢复后的红树林进行自然海防的可行性。此外,还建立了一个理想化的模型来研究恢复红树林的宽度对总波衰减的影响。研究发现,红树林恢复宽度越大,波高减小幅度越大,但减小幅度是非线性的。在此基础上,我们提出了一个最优的红树林宽度比例为15%,在此条件下,红树林湿地呈现出可靠的总波高降低和相对较大的效率。这些发现为红树林引起的波浪衰减及其对全球自然海防的影响提供了重要的见解。
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引用次数: 0
A 45-year high-resolution unstructured wave hindcast for the Australian coast: Validation and climatological insights 澳大利亚海岸45年高分辨率非结构波后预报:验证和气候学见解
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-10 DOI: 10.1016/j.coastaleng.2025.104892
Xianghui Dong , Qingxiang Liu , Stefan Zieger , Ian R. Young , Rui Li , Alberto Meucci , Jian Sun , Kejian Wu , Alexander V. Babanin
This study presents a 45-year (1979–2023) high-resolution wave hindcast for the entire Australian coast, conducted using WAVEWATCH III on an unstructured mesh with a resolution ranging from 1 to 15 km. Incorporating the observation-based source term package (i.e., ST6) and the subgrid-scale reef parameterization, the model performs well in simulating widely-used bulk wave parameters. The simulated significant wave height Hs achieves a correlation greater than 0.96 and exhibits only a centimeter-scale bias when compared to both altimeter and buoy observations. The use of BARRAv2 winds provides a clear advantage under extreme conditions, with negligible underestimation below the 99.9th percentile of Hs. The model performs particularly well in the Great Barrier Reef (GBR) region, where the bathymetry is complicated and could not be resolved well by typical km-scale wave models. Unlike previously published hindcasts that excessively overestimated wave energy in the GBR, our results show only a marginal Hs bias of approximately −0.05 m, against the shallow water buoys in this specific region. This better performance can be attributed to the subgrid-scale reef parameterization adopted. Long-term validation results demonstrate the robustness of the model framework, with the hindcast showing good temporal homogeneity and reliability. Building upon these results, this study reveals statistically significant increasing trends in wave heights along most of the Australian coast, with particularly pronounced upward trends in extreme wave heights (90th, 95th, and 99th percentiles) in the GBR. Furthermore, the GBR Hs trends based on our hindcast are much stronger than those estimated from previous hindcasts, and this new finding requires further investigation.
本研究展示了整个澳大利亚海岸45年(1979-2023)的高分辨率波浪后发,使用WAVEWATCH III在非结构化网格上进行,分辨率范围为1至15公里。结合基于观测的源项包(即ST6)和亚网格尺度的礁体参数化,该模型在模拟广泛使用的体波参数方面表现良好。与高度计和浮标观测值相比,模拟的有效波高Hs的相关系数大于0.96,仅表现出厘米尺度的偏差。BARRAv2风的使用在极端条件下提供了明显的优势,在Hs的99.9%以下可以忽略不计的低估。该模型在大堡礁(GBR)地区表现特别好,该地区水深测量复杂,典型的千米尺度波浪模型无法很好地解决问题。与之前发表的预测结果不同,我们的研究结果显示,相对于该特定区域的浅水浮标,我们的研究结果仅显示了大约−0.05 m的边际Hs偏差。这种较好的性能可归因于采用了亚网格尺度的礁体参数化。长期验证结果证明了模型框架的稳健性,后验结果具有良好的时间同质性和可靠性。在这些结果的基础上,本研究揭示了澳大利亚大部分海岸的浪高在统计上显著增加的趋势,特别是在GBR的极端浪高(第90、95和99百分位)的上升趋势特别明显。此外,基于我们的预测结果的GBR Hs趋势比以前的预测结果强得多,这一新的发现需要进一步的研究。
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引用次数: 0
The 3rd International Workshop on swash-zone processes 第三届冲区过程国际讲习班
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-09 DOI: 10.1016/j.coastaleng.2025.104891
Alexandra E. Schueller , Alec Torres-Freyermuth , Jack A. Puleo
The 3rd International Workshop on Swash-Zone Processes, held in Rome, Italy in September 2024, brought together researchers to discuss the current challenges in swash-zone research. Through review presentations and a structured method, participants identified knowledge gaps and proposed ideas to address those gaps. Areas discussed included: hydrodynamics, runup, sediment transport, morphodynamics, infiltration, and the application of remote sensing and numerical modeling for swash-zone research. The workshop emphasized the need for better integration of spatially extensive data (e.g., from drones and lidar) with traditional methods, and highlighted the importance of collaboration and standardized data sharing. Additionally, discussions focused on improving numerical models of sediment dynamics and understanding of 3D hydrodynamic/morphodynamic processes. This editorial outlines the key knowledge gaps identified and the strategies proposed to address them, offering suggestions for future swash-zone processes research.
2024年9月在意大利罗马举行的第三届摇摆区过程国际研讨会汇集了研究人员,讨论了摇摆区研究中当前面临的挑战。通过回顾演讲和结构化方法,参与者确定了知识差距,并提出了解决这些差距的想法。讨论的领域包括:水动力学、径流、泥沙输运、形态动力学、入渗,以及遥感和数值模拟在冲坡带研究中的应用。讲习班强调需要更好地将空间广泛的数据(例如来自无人机和激光雷达的数据)与传统方法整合在一起,并强调了协作和标准化数据共享的重要性。此外,讨论的重点是改进泥沙动力学的数值模型和对三维水动力/形态动力过程的理解。这篇社论概述了已确定的主要知识差距和为解决这些差距而提出的战略,并为今后的冲冲区过程研究提供了建议。
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引用次数: 0
Experiments and large eddy simulations of oscillatory flow over vortex ripples at high Reynolds number 高雷诺数涡旋波纹振荡流动的实验与大涡模拟
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-04 DOI: 10.1016/j.coastaleng.2025.104881
Weikai Tan , Jing Yuan , Deping Cao , Asim Önder
Long-crested sand ripples are ubiquitous seabed features in shallow coastal environments, characterized by the alternating generation of spanwise coherent vortices (SCVs) on either side of ripple crests. While previous studies have elucidated SCV dynamics at moderate Reynolds numbers (Re104), a range that is common at many beaches and can persist for long wave periods. Nonetheless, their applicability to higher Reynolds number conditions (Re105) remains uncertain. This investigation combines wall-modeled large eddy simulations (WMLES) and oscillating water tunnel experiments to examine SCV formation at high Reynolds numbers (ReO(105)). The WMLES approach employs a logarithmic wall model for rough surfaces, achieving accurate SCV representation with computational efficiency. Experimental validation demonstrates good agreement in both phase-averaged flow fields and turbulence statistics, confirming the model’s fidelity. Key findings reveal a Reynolds number dependence analogous to the drag crisis phenomenon: SCV intensity diminishes significantly for smooth ripples at Re=O(105), while surface roughness preserves vortex coherence. Our analysis of numerical results uncovers a positive feedback mechanism governing SCV development, where the residual SCV from the preceding half-cycle promotes early flow separation at ripple crests, facilitating vorticity accumulation and subsequent SCV formation. Analysis of the initial-cycle simulation (starting from a quiescent initial condition) shows that lee-side boundary layer must separate intrinsically during the deceleration phases of the first half-cycle to initiate this positive feedback loop. Both low Reynolds numbers and surface roughness can contribute to this first-half-cycle separation by increasing momentum deficit in the lee-side boundary layer.
长波峰沙纹是浅海环境中普遍存在的海底特征,其特征是在波峰两侧交替产生展向相干涡。虽然以前的研究已经阐明了中等雷诺数(Re≤104)下的SCV动力学,但这个范围在许多海滩上很常见,并且可以持续很长的波浪周期。尽管如此,它们对更高雷诺数条件(Re ~ 105)的适用性仍然不确定。这项研究结合了壁面模拟大涡模拟(WMLES)和振荡水洞实验来研究高雷诺数(Re ~ O(105))下SCV的形成。WMLES方法采用了粗糙表面的对数壁模型,以计算效率实现了精确的SCV表示。实验验证表明,相平均流场和湍流统计数据吻合良好,证实了模型的保真度。关键发现揭示了一种类似于阻力危机现象的雷诺数依赖性:在Re= 0(105)时,平滑波纹的SCV强度显著减弱,而表面粗糙度保持了涡相干性。我们对数值结果的分析揭示了控制SCV发展的正反馈机制,其中前半周期的残余SCV促进了纹波波峰处的早期流动分离,促进了涡量积累和随后的SCV形成。初始周期仿真分析(从静态初始条件出发)表明,在前半周期的减速阶段,背风面边界层必须本质分离才能启动该正反馈回路。低雷诺数和表面粗糙度都可以通过增加背风侧边界层的动量赤字来促进这种前半循环分离。
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引用次数: 0
Experimental study of bimodal spectral wave-induced dynamic responses in a silty seabed 粉质海底双峰谱波动力响应试验研究
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-10-03 DOI: 10.1016/j.coastaleng.2025.104890
Linlong Tong , Zhen Huang , Jisheng Zhang , Ning Chen , Dong-Sheng Jeng , Shulin Zhao , Xueyan Li
This study investigates the dynamic responses of silty seabeds to bimodal spectral wave loading, focusing on the impact of these waves on soil dynamics and liquefaction behavior. A series of laboratory experiments were conducted in a wave flume, simulating single-peaked wind waves, single-peaked swell waves, and bimodal spectral waves, which combine high-frequency wind waves and low-frequency swell waves. The results show that the pore pressures induced by bimodal spectral waves builds up over time, leading to a reduction in effective stress and shear strength. The buildup of pore pressures can cause residual liquefaction within a silty seabed, and the depth of liquefaction increases with wave height. When liquefaction occurs, the wave energy dissipates rapidly. The findings indicate that bimodal spectral waves induce deeper and more rapid liquefaction compared to single-peaked waves, with liquefaction progressing from the surface downward. Soil motion was analyzed using Particle Image Velocimetry (PIV), revealing complex flow patterns within the liquefied layers. Under single-peaked spectral wave conditions, shear flow was observed in the liquefied layer. However, under bimodal spectral wave conditions, both shear and plug flows were observed, with plug flow forming near the surface of the liquefied layer and shear flow occurring between the plug flow and the non-liquefied layer during the reversal phase of acceleration. Additionally, the soil particle velocity spectra exhibited multi-peak characteristics due to the nonlinear interactions of stress waves within the seabed.
本文研究了粉质海床对双峰谱波荷载的动力响应,重点研究了双峰谱波对土壤动力和液化行为的影响。在波浪水槽中进行了一系列室内实验,模拟了单峰风浪、单峰涌浪和高频风浪与低频涌浪相结合的双峰谱波。结果表明,双峰谱波引起的孔隙压力随时间增加,导致有效应力和抗剪强度降低。孔隙压力的积累会引起淤泥质海床的残余液化,且液化深度随波高的增加而增加。当液化发生时,波浪能迅速消散。结果表明,与单峰波相比,双峰谱波引起的液化更深、更快,液化从地表向下进行。利用粒子图像测速仪(PIV)分析了土壤运动,揭示了液化层内复杂的流动模式。在单峰谱波条件下,液化层中存在剪切流动。然而,在双峰谱波条件下,剪切流和塞流同时存在,在加速反转阶段,液化层表面附近形成塞流,塞流与非液化层之间发生剪切流。此外,由于海床内应力波的非线性相互作用,土壤颗粒速度谱呈现出多峰特征。
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引用次数: 0
Exploring a conservative staggered scheme for Boussinesq-type equations: Insights into numerical diffusion, dispersion, and wave-breaking 探索boussinesq型方程的保守交错格式:对数值扩散,色散和破波的见解
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-09-28 DOI: 10.1016/j.coastaleng.2025.104880
Fatima-Zahra Mihami , Volker Roeber
Accurate and efficient modeling of coastal wave transformation, particularly under wave-breaking conditions, remains a major challenge for Boussinesq-type models. To address this, we introduce and validate a conservative staggered-grid scheme to discretize a set of weakly nonlinear Boussinesq-type equations. The presented approach revisits the staggered finite-difference strategy by ensuring a momentum-conserving solution designed to enhance numerical stability and improve shock-capturing properties. The scheme’s performance is assessed through a series of numerical tests involving monochromatic and spectral linear wave propagation. These tests demonstrate that the conservative staggered scheme is much less sensitive to grid resolution, resulting in approximately one order of magnitude lower numerical diffusion in contrast to the well-established HLLC scheme, while maintaining comparable dispersive accuracy despite using a lower-order spatial reconstruction. Additionally, the scheme introduces a slight negative phase error that compensates for the positive dispersion error inherent in the underlying equations, resulting in improved overall phase accuracy relative to the HLLC scheme. Beyond linear wave propagation, the numerical approach is validated against standard benchmark tests with solitary and spectral breaking waves. In these highly non-linear cases, coupling the conservative staggered scheme with a turbulent kinetic energy (TKE)-based eddy viscosity model yields localized and physically consistent dissipation while preserving the dispersive characteristics of the solution. Compared to conventional hybrid breaking approaches, the TKE-based closure provides enhanced stability, reduced grid sensitivity, and a more accurate representation of energy dissipation during wave breaking. These results underscore the potential of the conservative staggered scheme as an efficient and robust framework for computing complex coastal and nearshore wave processes.
对于boussinesq型模型来说,准确和有效地模拟海岸波的变换,特别是在破波条件下,仍然是一个主要的挑战。为了解决这个问题,我们引入并验证了一种保守交错网格方案来离散一组弱非线性boussinesq型方程。所提出的方法通过确保动量守恒解决方案来提高数值稳定性和改善冲击捕获特性,重新审视了交错有限差分策略。通过一系列涉及单色和光谱线性波传播的数值测试来评估该方案的性能。这些测试表明,保守交错方案对网格分辨率的敏感性要低得多,与已建立的HLLC方案相比,其数值扩散大约低一个数量级,尽管使用低阶空间重建,但仍保持相当的色散精度。此外,该方案引入了一个轻微的负相位误差,以补偿底层方程中固有的正色散误差,从而相对于HLLC方案提高了总体相位精度。除了线性波传播之外,数值方法还通过孤立波和谱破碎波的标准基准测试进行了验证。在这些高度非线性的情况下,将保守交错方案与基于湍流动能(TKE)的涡流粘度模型相结合,可以在保持溶液色散特性的同时产生局部和物理一致的耗散。与传统的混合破波方法相比,基于tke的闭合方法提供了更高的稳定性,降低了网格灵敏度,并且更准确地表示了破波过程中的能量耗散。这些结果强调了保守交错方案作为计算复杂海岸和近岸波浪过程的有效和稳健框架的潜力。
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引用次数: 0
Turbulent field beneath monochromatic waves subjected to varying wind conditions 受不同风况影响的单色波下的湍流场
IF 4.5 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2025-09-23 DOI: 10.1016/j.coastaleng.2025.104879
Fabio Addona, Luca Chiapponi
Wind-wave interaction affects momentum, energy, and chemicals transfer at the air–water interface. In this study, we report on the turbulent flow field beneath laboratory monochromatic waves subjected to different wind speeds and direction (following or opposing). The flow field is decomposed into three main components: a mean, a swell-induced, and a fluctuating term, the latter including the effects of wind-induced ripples and turbulence. After a brief survey on the mean and wave-induced fields, we focus our attention on the fluctuating-turbulence field. Our results show that the turbulent stresses increase with increasing water friction, and that the condition of wind opposing the swell results in enhanced momentum transfer at deeper water levels. The distribution of fluctuating kinetic energy (TKE) along the swell phase indicates a maximum at the trough, which was addressed to the kinematics of the free surface by previous researchers. Furthermore, we investigate all the terms in the 2D energy equations that contribute to the TKE production by assuming that waves propagate with a rigid translation. A close look to the TKE budget suggests positive production of TKE on the leeside before the trough for all wind conditions, with destruction of TKE windwards for wind following the swell, possibly due to a sheltering effect. For opposing wind, however, positive production is almost ubiquitous along the swell phase, and this would justify larger mean TKE production for that particular condition. These findings are discussed to address possible causes; the phase-dependent behavior of TKE budgets are attributed to the combined action of swell-induced acceleration, wind shear on the crest, the stochastic phase offsets of the wind waves, and microscale breaking. A quadrant analysis highlights the main direction of momentum transfer and helps the individuation of the bursts, i.e., of strong events that support high momentum transfer. As expected, the net momentum transfer due to the fluctuating components is from air to water, with conditional averages (i.e., the quadrant map of the fluctuating velocities) confirming that finding. Finally, the analysis of the fluctuating principal stresses tensor reports that anisotropy increases for increasing water friction, although the system tends to isotropic conditions immediately below the air–water interface. For wind following the swell, the principal axes approaches the free surface with an angle π/4, which is typical when a shear current is dominant near the surface. Important implications of these findings include the availability of further data to improve wave forecasting and prediction of swell and wind conditions.
风波的相互作用影响着空气-水界面的动量、能量和化学物质的传递。在这项研究中,我们报告了实验室单色波下的湍流流场在不同的风速和方向(顺或反)下。流场被分解为三个主要部分:平均项、膨胀项和波动项,后者包括风致波纹和湍流的影响。在简要介绍了平均场和波动场之后,我们将注意力集中在波动湍流场上。我们的研究结果表明,湍流应力随着水摩擦力的增加而增加,并且在较深的水位处,风与膨胀相反的条件导致动量传递增强。波动动能(TKE)沿膨胀阶段的分布表明在槽处最大,这是前人对自由表面运动学的研究。此外,我们通过假设波以刚性平移传播来研究二维能量方程中有助于TKE产生的所有项。仔细观察TKE预算表明,在所有风况下,在槽前的背风面产生的TKE都是正的,随着风的膨胀,TKE风向被破坏,可能是由于遮蔽效应。然而,对于逆风,在膨胀阶段几乎无处不在的正产量,这将证明在特定条件下更大的平均TKE产量是合理的。讨论这些发现,以解决可能的原因;TKE收支的相位依赖行为归因于膨胀引起的加速度、波峰上的风切变、风波的随机相位偏移和微尺度破碎的共同作用。象限分析突出了动量转移的主要方向,并有助于爆发的个性化,即支持高动量转移的强事件。正如预期的那样,由于波动分量造成的净动量转移是从空气到水,条件平均(即波动速度的象限图)证实了这一发现。最后,对波动主应力张量的分析表明,各向异性随着水摩擦的增加而增加,尽管系统在空气-水界面以下趋于各向同性。对于跟随膨胀的风,主轴以−π/4的角度接近自由表面,这是在表面附近剪切流占主导地位时的典型特征。这些发现的重要意义包括提供进一步的数据,以改进海浪预报和对涌浪和风况的预测。
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Coastal Engineering
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