Publications

Knowing the vertical structure of particle velocity is very important for the sediment transportation study. Recentdevelopment of computer resources and high performance computing enable us to use numerical models withmore information in the vertical direction. In this paper, the performance of multi-layered Boussinesq model(COULWAVE) and RANS model (COBRAS-UC) on a bar-trough profile beach is examined. Results, in termsof wave heights computed by both models and the time series of the horizontal velocity (computed withCOBRAS-UC model) are compared with the experimental data collected by Okamoto et al. (2008) for the testcase with an incident wave of period T=1.5sec and height of H=8cm, in which the detailed vertical structure ofparticle velocity was measured. Both models can predict the wave height change very well until the wavebreaking initiates and specially COBRAS-UC model. However, it does not agree to the experimental data afterthe wave breaking initiation. The COBRAS-UC model calculates the horizontal velocity near the free surfacevery well, but it does not agree to the experimental data in the lower section of the water column.

Nesta comunicação, apresenta-se o estudo efectuado para a determinação doespraiamento e cotas de inundação numa estrutura de enrocamento existente napraia de Vale do Lobo, situada no Concelho de Loulé, na região do Algarve.Com base nas características da agitação marítima determinadas na praia juntoao pé da estrutura durante o ano de 1991, com o sistema GUIOMAR,considerando dois níveis de maré, procedeu-se ao cálculo do espraiamento sobrea estrutura. Para tal, recorreu-se às fórmulas empíricas de TAW (2002) e de vander Meer e Stam (1992). Determinaram-se, também, as respectivas cotas deinundação. Tal permitiu avaliar a influência do nível de maré nos valores deespraiamento encontrados, bem como das diferenças associadas à utilização dasduas formulações.

The Port of Sines is located on the west coast of Portugal, sheltered by two breakwaters: thewest and the east breakwaters (Figure 1). Originally, the west breakwater was 2 km long indepths up to 50 m, protected by two armour layers of 400 kN dolosse on a 1:1.5 slope(Mettam, 1976). In February 1978, immediately after breakwater construction, a storm, with asignificant wave height of 8 m, damaged the breakwater armour layer in four different areas.One year later, a more severe storm caused failure of almost the entire armour layer andsuperstructure, leading to urgent repair works during the 1980s. The last rehabilitation workswere concluded in 1992.

O conhecimento da agitação marítima é fundamental para o planeamento de intervenções e estudos costeiros, para simular os possíveis impactos ambientais de obras de engenharia e para a definição de procedimentos em situações de emergência. Os modelos numéricos de propagação de ondas, devido à sua rapidez, flexibilidade e gama de aplicação, contribuem de forma importante para os estudos costeiros. Apesar destas qualidades permitirem a simulação de diversos cenários de forma simplificada, os modelos exigem a utilização de grandes quantidades de dados e originam também grandes quantidades de resultados para cada caso em estudo.Os sistemas de informação geográfica permitem a organização e interpretação de grandes quantidades de informação, mostrando de forma rápida os padrões e tendências principais em qualquer processo de tomada de decisão.Neste âmbito tem vindo a ser desenvolvido o sistema GUIOMAR: Geo(Graphical) User Interface for cOastal and MARine modeling, um sistema integrado para a modelação da agitação marítima, aplicado à zona costeira portuguesa e que inclui todas as funcionalidades de um SIG.A versão actual do sistema foi desenvolvida em linguagem VBA (Visual Basic for Applications) para o ArcGIS9.0TM. O sistema GUIOMAR tem 3 componentes principais: (i) um software comercial de SIG; (ii) uma interface com o utilizador que é responsável pela comunicação entre o utilizador e o sistema; (iii) um conjunto de modelos de propagação de ondas, com diferentes domínios de aplicação: REF/DIF 1(Dalrymple e Kirby, 1991), REF/DIF S(Kirby e Ozkan, 1994), FUNWAVE 1D e 2D (Kirby et al., 1998), DREAMS (Fortes, 2002) e SWAN (Booij et al., 1999); Inclui também um programa de construção de malhas não estruturadas para os modelos numéricos, GMALHA (Pinheiro et al., 2006).O trabalho apresenta numa aplicação do sistema GUIOMAR ao Porto de Sines na qual foram testados os desenvolvimentos mais recentes do sistema, como é o caso da acoplagem dos modelos de propagação de ondas DREAMS e SWAN através da interface do GUIOMAR. Para tal, foi efectuada uma caracterização intensiva do Porto de Sines para o cálculo dos coeficientes de reflexão a aplicar no modelo DREAMS. O resultado final deste trabalho foi a caracterização do regime de agitação marítima dentro e fora do porto de Sines através da utilização dos procedimentos implementados no sistema GUIOMAR.

GUIOMAR is an integrated system for coastal engineering modeling, developed with a commercial software of Geographical Information Systems (GIS). This system allows the utilization of both wave propagation models and of all the functionalities that are inherent to the GIS software, and it is being designed to help in the decision making process in coastal areas. GUIOMAR system is composed of three main components: a GIS commercial software, a set of modules/models of wave propagation and other pre and post processing algorithms programmed in FORTRANTM, and a Graphical User Interface (GUI) developed in VBA for ArcGISTM, which is responsible for the communication between the user and the system. At the moment, are available six wave propagation models and a program that automatically generates unstructured grids for the numerical models. In this paper, GUIOMAR structure and a general overview of its interface are presented. In order to achieve important information about the system operability, a test was made for an important Portuguese harbor. Sines harbor, at the southeast of Europe, 37º 57

This paper describes the implementation of a new boundary conditions in the BOUSSIIW model (BOUSSinesq model with Internal Irregular Wave generation). BOUSSIIW is a finite element numerical model for wave propagation in near shore regions that is able to describe the wave field outside and inside harbours and sheltered zones. It is based upon the extended Boussinesq equation derived by Nwogu. These equations describe the nonlinear evolution of waves over a sloping impermeable bottom and are able to reproduce some of the most important physical effects associated with the nonlinear wave transformation in near shore regions. Their range of validity extends from shallow up to intermediate water depths. Monochromatic and irregular waves can be generated by the model using the source function method. The two boundary conditions available were full reflection or full absorption. A new partial reflection boundary condition is implemented. The model is validated with a simple test case. Reflection coefficients obtained with BOUSSIIW were compared to widely used empirical formula, enabling the assessment of the new condition

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This paper presents the results of the study performed for estimating the run-up and flood levelsin a stretch of Vale do Lobo beach, located at Loulé Municipality, in the Algarve region.The study started by defining the offshore wave conditions in the area, based upon data collectedduring 1991 by the Portuguese Hydrographic Institute with a directional wave-buoy located atFaro. These conditions were then transferred to the vicinity of Vale do Lobo beach by using theGUIOMAR system, namely its SWAN module. GUIOMAR is an integrated system for modellingwave propagation in coastal engineering studies. It is currently being developed to providesupport for a sustainable planning and management of the costal area.Two empirical formulations were applied for estimating the run-up at Vale do Lobo beach during1991: one based on field data and the other based on physical model tests. Two water levelswere considered and a sensitivity analysis was performed to evaluate the differences betweenthe two formulations and the impact of some of the parameters on the end results. The floodlevels were also estimated.

This paper presents an experimental and numerical study of 2-D wave diffraction by a fixed horizontal-axis submergedcircular cylinder. The objective of the paper is to report and validate results from the fully nonlinear 2-D boundary-elementmethod code CANAL; to assess the capability of the physical wave flume and the measurement methodology to study thistype of problem; and to contribute to the understanding of the wave diffraction by a circular cylinder. Two test cases arepresented, both in deep-water conditions. The cylinder axis submergence is 1^5r (r is the cylinder radius) for the first case,and 3r for the second, the latter corresponding to the experimental study presented in the paper. A discretization convergenceevaluation is also presented for the second case. The good agreement between the numerical and the experimental resultsproves that this numerical model is able to accurately simulate this type of problems. No reflection was noticed on the incidentwave side of the cylinder. It was found that nonlinear resonant interactions occur between the fundamental frequency andthe harmonics on the transmitted wave side of the cylinder. Free waves were observed on this part of the wave flume.

Nowadays, renewable energy is a topic widely discussed in scientific community. Specifically wave energy attracts attention because it has a high energy potential distributed throughout the planet. Oscillating Water Column (OWC) wave energy converter is one of the most studied devices that have promising perspectives to be installed commercially. This study aims investigating the influence of chamber sizes and turbine characteristics dimensions of an OWC device located at the southern Brazilian coast is carried out. Numerical simulations for incident waves with period T = 7 s and 10 s and height H = 1.5 m, by using the FLUENT® model, based on the finite volume method (VFM) are carried out. Efficiencies for different chamber sizes and Wells turbine characteristic relations (kt) in each incident wave are determined. The highest efficiencies were obtained by a chamber with 5 x 5 m and kt = 530 Pa.s/m³ in the case of an incident wave with T = 7s (52%), and 30 x 30 m and kt = 15 Pa.s/m³ at T = 10s (65%).

Port terminals downtimes lead to large economic losses and largely affect the port

This paper describes the physical model, experimental setup and tests performed to study the motions and forces of a ship moored to the pier A at the Leixões oil terminal, following the breakwater

HIDRALERTA is a forecast, early warning and risk assessment system for port and coastal areas that uses measurements and estimates of sea-waves and water levels to evaluate overtopping/flooding events. The calculation of the mean overtopping discharge over a maritime structure is performed through artificial neural network-based tools and/or empirical formulae. The system is developed in open source software, mainly using the Python language. This paper presents the application of HIDRALERTA system to reproduce the hurricane Lorenzo conditions and impacts at Lajes das Flores port on October 2nd 2019, the most affected port in Azores. This hurricane was regarded as the strongest storm to hit Azores in 20 years. The system predicted the expected results for the hurricane wave characteristics, as well as overtopping discharge volumes. Further validation still need to be improved with the collaboration of the local authorities and the use of historical data.

Numerical models are useful tools to predict the effects of storms in coastal areas. The objective of this work was to simulate the effects of storms in São Pedro de Moel beach by using XBeach. The nearshore sea state was obtained by propagating offshore conditions using the SWAN model. The XBeach model was divided into two setups to analyse overtopping events and coastal evolution. Sensibility tests, calibration, and validation, using information from different storms, were performed for the different setups. The results from the overtopping simulation were compared against results from an empirical formula. The comparison showed lower values obtained with the empirical formula. The coastal evolution run point out to the necessity of having better field data before and after storms to improve the model setting and accuracy.

The assessment of damage evolution in scale model tests of rubble-mound breakwaters can be achieved by comparing eroded depths and volumes between consecutive surveys. This paper focuses on damage evolution of a model of a rubble-mound breakwater and on the novelty of the non-intrusive survey methodologies such as laser scanning and Time of Flight (ToF) techniques, based on point clouds, enabling the extraction of profiles and the calculation of eroded depths and eroded volumes. The final objective of this work is to evaluate the applicability of the estimation the number of displaced armour units, using a non-dimensional damage parameter based on the calculated eroded volume.The paper will also describe the experiments conducted under the RODBreak, a project sponsored by the HYDRALAB+ Transnational Access Program, in which a stretch of a rubble-mound breakwater was built at the wave-current basin of the Leibniz University Hannover (LUH) to assess the structure behavior. Four scan surveys were conducted using a Faro Focus 3D laser scan, as well as a ToF sensor. Those surveys were carried out before and after two test series, in order to evaluate the eroded volume and profile evolution.

Neste trabalho é efetuada a validação do protótipo To-SEAlert para o porto da Ericeira. Para a validação dos resultados do modelo SWAN foram utilizados os dados de duas boias situadas ao largo da Nazaré e para a validação das previsões do sistema de cálculo do grau de risco foram simuladas as depressões Elsa e Fabien (ocorridas em dezembro de 2019) e que foram responsáveis por fortes danos na cabeça do molhe do porto da Ericeira. Verificou-se uma boa concordância entre os dados das boias e os resultados do modelo SWAN, tendo no entanto o modelo reproduzido melhor a direção média e a altura significativa do que o período de pico. Relativamente aos valores de galgamento, os resultados obtidos na simulação das depressões Elsa e Fabien estiveram em concordância com os valores referidos na literatura como causadores de danos nas estruturas.

This work aims to determine the exploitable wave energy resource at six potential sites, located in the Azores, Madeira and Sines breakwater city harbours. For that purpose, the thirdgeneration wave model SWAN is used to estimate the sea-wave conditions over the last 40 years. Boundary conditions of the sea states and wind fields are provided by the climate reanalysis datasets (ERA5). Using those results as inputs to the SWAN model, the sea-states were propagated shoreward, in order to estimate and analyse the wave climate conditions in the regions of interest. By combining the average energy flux per unit-length of wave front and the probability of occurrence of each sea state, the average exploitable annual energy per unit length of wave crest can be computed. The variability of this energy flux is described, since it is of fundamental importance for the efficiency of the Wave Energy Converters (WEC).

Former investigations on wave run-up and overtopping of (impermeable and permeable) coastal structures aimed at quantifying the influence of oblique waves on mean overtopping discharge, water layer thickness and velocities by developing empirical formulas of a reduction factor for wave obliquity,

In 2017, the RODBreak experiment was conducted. The experiment aimed at characterizing wave run-up, overtopping and damage in rubble-mound breakwaters. The reason for these experiments was the huge impact that climate can have on maritime structures, particularly in rubble mound breakwaters. In fact, the forecast sea level rise associated with more frequent and severe storms will have consequences either on the increase of wave runup, wave overtopping or on damage on existent structures since they were not design for those extreme values. However, for those climate change scenarios, little is known about the actual failure probability of such structures.Within this framework, a stretch of a rubble-mound breakwater was built in a wave basin. Under extreme wave conditions, with different incident wave angles (from 40° to 90°), a total of 49 tests were performed. Each test had different testing parameters, such as significant wave height (Hs), peak period (Tp) and wave direction. Also, for each test, different types of measurements were considered. Incident sea waves were measured with 3 arrays of 6 acoustic wave probes each as well as with isolated acoustic wave probes and 5 Acoustic Doppler Velocimeters (ADV

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