WAVE MECHANICS FOR OCEAN ENGINEERING
|
|
- Karen Burns
- 5 years ago
- Views:
Transcription
1 Elsevier Oceanography Series, 64 WAVE MECHANICS FOR OCEAN ENGINEERING P. Boccotti Faculty of Engineering University of Reggio-Calabria Feo di Vito Reggio-Calabria Italy 2000 ELSEVIER Amsterdam - Lausanne - New York - Oxford - Shannon - Singapore - Tokyo
2 XIX LIST OF CONTENTS Chapter 1 Periodic wave pattern: the approach of differential calculus The irrotational flow, the continuity equation, the Bernoulli equation The differential equations of an irrotational flow with a free surface Introduction to wave mechanics Stokes' theory to the first order Analysis of the linear dispersion rule The flow field Stokes' theory to the second order Non-linearity effects Wave-current interaction. Part I: velocity potential and wavelength Preliminary remarks on three dimensional waves Wave reflection Wave diffraction References Chapter 2 Periodic wave pattern: the control volume approach The linear momentum equation for a control volume The energy equation for a control volume Radiation stress, mean energy flux, mean wave energy per unit surface Formulae for radiation stress and mean energy flux of progressive waves The problem of the control volume extending from deep to shallow water Practical consequences of the control volume problem A current associated with the wave motion Wave refraction for an arbitrary configuration of the seabed The group celerity Wave-current interaction. Part II: shoaling and set-down References
3 XX List of contents Chapter 3 Wave effects on coasts The control volume from the breaker line to the beach The run-up The longshore transport The analytical approach to the problem of beach planform evolution Problem of beach planform evolution: the case of contour lines parallel up to deep water Problem of beach planform evolution: the case of contour lines parallel only within a certain distance from the shoreline Planform evolution of a natural shoreline Stability of a nourished beach Planform evolution of beach nourishment projects A useful simplification Beach planform evolution caused by structures References Chapter 4 Wind generated waves: basic concepts The sea state The theory of the sea states Some basic relations in the theory of the sea states How to obtain the input data of the theory A mathematical form of the wind wave spectrum Possibility of testing small scale models in sea or lakes Inferring the nature of waves from the bandwidth References Chapter 5 Analysis of the sea states: the time domain Why the surface displacement represents a stationary Gaussian process Joint probability of surface displacements Rice's problem Rice's logic Corollaries of Rice's problem Solved and still unsolved problems The period of a very high wave and the wave height probability under general bandwidth assumptions Experimental verification
4 List of contents XXI Characteristic wave heights The maximum expected wave height in a sea state of given duration References Chapter 6 The wave climate The function H s (t) The probability of the significant wave height The probability of the significant wave height for a given direction of wave advance Probabilities of the significant wave height for a few areas of the globe The maximum expected wave height in a storm with a given history The concept of "equivalent triangular storm" Storm durations References Chapter 7 Design waves and risk analysis The return period of a sea storm where the significant wave height exceeds a fixed threshold The significant wave height and its persistence vs the return period The encounter probability The chain: lifetime, encounter probability => return period => significant wave height Coastal structures: the design sea state The return period of a wave with a height exceeding a fixed threshold The return period of a sea storm containing at least one wave higher than a fixed threshold Offshore structures: the design wave Calculations for different wave directions Corollary of risk analysis: a general relation between the confidence interval and the sampling rate References Chapter 8 Analysis of the sea states in the space-time The concept of homogeneous wave field The wave field in the open sea
5 XXII List of contents References The directional spectrum Shoaling and refraction of the wind-generated waves Reflection of the wind-generated waves Diffraction of the wind-generated waves Long-crested random waves: the link between periodic waves and windgenerated waves Direct proportion between the maximum expected wave height and the diffraction coefficient Space-time covariances Chapter 9 The theory of quasi-determinism A sufficient condition for occurrence of a wave of given height very large A necessary condition for occurrence of a wave of given height very large The water surface on space-time, if a wave of given height very large occurs at a fixed point The velocity potential if a wave of given height very large occurs at a fixed point Theory's generality and consistency with Stokes' theory Formal proof of the necessary condition. Part I: symbols and assumptions Formal proof of the necessary condition. Part II: core of the proof Formal proof of the necessary condition. Part III: the central inequality Formal proof of the necessary condition. Part IV: conclusion Corollary: the closed solution for the wave height distribution Chapter 10 Uses and consequences of the quasi-determinism theory The first way to employ the theory A three dimensional wave group The waves are higher on the time domain than on the space domain! Effects of water depth and of spectrum shape on the wave group Shoaling and refraction of the wave group Explanation of the first big difference between sea waves and periodic waves Explanation of the second big difference between sea waves and periodic waves The second way to employ the theory The "genetic code" of the sea waves The determinism arises from within the random waves References
6 List of contents XXIII Chapter 11 Analysis of the wave forces on offshore structures 11.1 Wave forces on gravity offshore platforms 11.2 Local perturbation of the flow field at an offshore structure 11.3 Wave forces on submerged tunnels 11.4 The diffraction coefficients of the forces 11.5 Wave forces on space frame structures 11.6 The long-structure problem 392 References Chapter 12 Calculation of the wave forces on offshore structures Calculation of the wave forces on a, gravity offshore platform Calculation of the wave forces on a space frame structure Design of a submerged tunnel. I: calculation of the wave forces Design of a submerged tunnel. II: the effect of currents Design of a submerged tunnel. Ill: the risk of resonance Chapter 13 Stability analysis of coastal structures Wave pressure on a wall Forces on a vertical breakwater Design of vertical breakwaters Further verifications of the vertical breakwaters The Japanese practice The problem of the rubble mound breakwaters References Chapter 14 Topics calling for an overall overview of offshore and coastal engineering ' A comparison between tsunami and wind waves from the open sea to the coast Small scale models Wave measurements References
7 XXIV List of contents Appendix A Appendix to chapters 6 and 7: use of wave hindcast and wave measurements from satellites 463 A.I Long term wave statistics from satellite data 464 A.2 Wave hindcast 470 A.3 Trend in the wave climate and its effects on engineering 473 References Appendix B Appendix to chapters 9 and 10: the wave group of the maximum expected crest elevation, and the wave group of the maximum expected crest-to-trough height B.I B.2 B.3 The first version of the quasi-determinism theory Corollaries of the first version The relationship between the two versions of the theory References
INTRODUCTION TO COASTAL ENGINEERING AND MANAGEMENT
Advanced Series on Ocean Engineering Volume 16 INTRODUCTION TO COASTAL ENGINEERING AND MANAGEMENT J. William Kamphuis Queen's University, Canada World Scientific Singapore New Jersey London Hong Kong Contents
More informationWaves. G. Cowles. General Physical Oceanography MAR 555. School for Marine Sciences and Technology Umass-Dartmouth
Waves G. Cowles General Physical Oceanography MAR 555 School for Marine Sciences and Technology Umass-Dartmouth Waves Sound Waves Light Waves Surface Waves Radio Waves Tidal Waves Instrument Strings How
More informationOECS Regional Engineering Workshop September 29 October 3, 2014
B E A C H E S. M A R I N A S. D E S I G N. C O N S T R U C T I O N. OECS Regional Engineering Workshop September 29 October 3, 2014 Coastal Erosion and Sea Defense: Introduction to Coastal Dynamics David
More informationIMPACTS OF COASTAL PROTECTION STRATEGIES ON THE COASTS OF CRETE: NUMERICAL EXPERIMENTS
IMPACTS OF COASTAL PROTECTION STRATEGIES ON THE COASTS OF CRETE: NUMERICAL EXPERIMENTS Tsanis, I.K., Saied, U.M., Valavanis V. Department of Environmental Engineering, Technical University of Crete, Chania,
More informationThe inner shelf is a friction-dominated realm where surface and bottom boundary layers overlap.
Wave Hydrodynamics. Beach Terminology The inner shelf is a friction-dominated realm where surface and bottom boundary layers overlap. (From Nitrouer, C.A. and Wright, L.D., Rev. Geophys., 32, 85, 1994.
More informationAdvanced Series on Ocean Engineering - Volume 14 COASTAL STABILIZATION. Richard Silvester John R C Hsu. \v? World Scientific
Advanced Series on Ocean Engineering - Volume 14 COASTAL STABILIZATION Richard Silvester John R C Hsu \v? World Scientific Contents PREFACE xv 1 INTRODUCTION 1 /. / Coastal Environment 2 J.2 State of Beach
More informationOCEAN WAVES NAME. I. Introduction
NAME OCEAN WAVES I. Introduction The physical definition of a wave is a disturbance that transmits energy from one place to another. In the open ocean waves are formed when wis blowing across the water
More informationAiry Wave Theory 1: Wave Length and Celerity
Airy Wave Theory 1: Wave Length and Celerity Wave Theories Mathematical relationships to describe: (1) the wave form, (2) the water motion (throughout the fluid column) and pressure in waves, and (3) how
More informationCoastal & Marine Environment. Chapter. Wave Transformation. Mazen Abualtayef Assistant Prof., IUG, Palestine
Coastal & Marine Wave Transformation Mazen Abualtayef Assistant Prof., IUG, Palestine Wave Transformation Wave transformation describes what happens to waves as they travel from deep into shallow water
More informationChapter. The Dynamic Ocean
Chapter The Dynamic Ocean An ocean current is the mass of ocean water that flows from one place to another. 16.1 The Composition of Seawater Surface Circulation Surface Currents Surface currents are movements
More informationpage - Laboratory Exercise #5 Shoreline Processes
page - Laboratory Exercise #5 Shoreline Processes Section A Shoreline Processes: Overview of Waves The ocean s surface is influenced by three types of motion (waves, tides and surface currents). Shorelines
More informationShoreline Evolution Due to Oblique Waves in Presence of Submerged Breakwaters. Nima Zakeri (Corresponding Author), Mojtaba Tajziehchi
Shoreline Evolution Due to Oblique Waves in Presence of Submerged Breakwaters Nima Zakeri (Corresponding Author), Mojtaba Tajziehchi Department of Civil Engineering, Faculty of Engineering, University
More informationChapter 10 Waves. wave energy NOT the water particles moves across the surface of the sea. wave form moves and with it, energy is transmitted
Capillary Waves, Wind Waves, Chapter 10 Waves Anatomy of a Wave more like a real wave Tsunamis, Internal waves big waves huge waves rogue waves small waves more like a sine wave Wave direction Wave wave
More informationOceans - Laboratory 12
Oceans - Laboratory 12 (Name) How do ocean waves form? All waves are disturbances of a fluid medium through which energy is moved (Davis, 1997). Ocean waves travel on the interface between oceans and the
More informationChapter 10 Lecture Outline. The Restless Oceans
Chapter 10 Lecture Outline The Restless Oceans Focus Question 10.1 How does the Coriolis effect influence ocean currents? The Ocean s Surface Circulation Ocean currents Masses of water that flow from one
More informationChapter 8 Wave climate and energy dissipation near Santa Cruz Island, California
Chapter 8 Wave climate and energy dissipation near Santa Cruz Island, California NATHAN BURLEY A* AND ROBYN SUDDETH B A CIVIL & ENVIRONMENTAL ENGINEERING B GRADUATE GROUP IN HYDROLOGIC SCIENCES UNIVERSITY
More informationName Class Date. Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used.
Assessment Chapter Test B The Movement of Ocean Water USING KEY TERMS Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used.
More informationNumerical modeling of refraction and diffraction
Numerical modeling of refraction and diffraction L. Balas, A. inan Civil Engineering Department, Gazi University, Turkey Abstract A numerical model which simulates the propagation of waves over a complex
More informationThe NOEL, Natural Ocean Engineering Laboratory, of Reggio Calabria (Italy)
July 2011 NOEL, Lungomare Falcomatà, Rada delle Mura Greche, Reggio Calabria The NOEL, Natural Ocean Engineering Laboratory, of Reggio Calabria (Italy) Felice Arena Professor of Ocean Engineering Mediterranea
More informationWaves. Types of Waves. Parts of a wave. Insert wind_wave.wmv. Shark attack
Waves Recall: Waves = transmitted energy What causes waves? Wind gravity Earthquakes We will talk about all of these, but first Insert wind_wave.wmv Shark attack Types of Waves Body waves transmit energy
More informationWhat is a wave? Even here the wave more or less keeps it s shape and travelled at a constant speed. YouTube. mexicanwave.mov
Waves What is a wave? Waves transmit a disturbance / energy from one part of a material to another. The energy is transmitted without substantial movement of the material. Waves occur in lots of places,
More informationUndertow - Zonation of Flow in Broken Wave Bores
Lecture 22 Nearshore Circulation Undertow - Zonation of Flow in Broken Wave Bores In the wave breaking process, the landward transfer of water, associated with bore and surface roller decay within the
More informationMODELLING OF WATER FLOW ON SMALL VESSEL S DECK
Monika Warmowska, Jan Jankowski, Polski Rejestr Statków S.A., al. gen. Józefa Hallera 126, Poland, Gdańsk, 80-416 MODELLING OF WATER FLOW ON SMALL VESSEL S DECK Summary Green water moving on deck of small
More informationDeep-water orbital waves
What happens when waves approach shore? Deep-water orbital waves Fig. 9.16, p. 211 Wave motion is influenced by water depth and shape of the shoreline wave buildup zone surf zone beach Wave base deepwater
More informationWaves. harmonic wave wave equation one dimensional wave equation principle of wave fronts plane waves law of reflection
Waves Vocabulary mechanical wave pulse continuous periodic wave amplitude wavelength period frequency wave velocity phase transverse wave longitudinal wave intensity displacement wave number phase velocity
More informationEl Niño Southern Oscillation. Pressure systems over Darwin Australia and Tahiti Oscillate Typically occurs every 4-7 years
El Niño Southern Oscillation Pressure systems over Darwin Australia and Tahiti Oscillate Typically occurs every 4-7 years 1 2 What is it? Normal Conditions... What is it? During El Niño. 3 Local Effects
More informationLecture 21: Potpourri
Lecture 21: Potpourri Lecturer: H. Segur. Write-up: Ali Mashayek and Hélène Scolan June 26, 2009 1 Introduction In this last lecture of the 2009 GFD series, a collection of topics is presented including:
More informationReading Material. Inshore oceanography, Anikouchine and Sternberg The World Ocean, Prentice-Hall
Reading Material Inshore oceanography, Anikouchine and Sternberg The World Ocean, Prentice-Hall BEACH PROCESSES AND COASTAL ENVIRONMENTS COASTAL FEATURES Cross section Map view Terminology for Coastal
More informationTsunami generation, propagation, and devastation. John Fenton
Tsunami generation, propagation, and devastation John Fenton Tsunami Tsunami is a Japanese term that means "harbour wave". It is used worldwide to describe a large sea wave generated by sea-floor disturbance.
More informationLecture Outlines PowerPoint. Chapter 15 Earth Science, 12e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 15 Earth Science, 12e Tarbuck/Lutgens 2009 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More informationUndertow - Zonation of Flow in Broken Wave Bores
Nearshore Circulation Undertow and Rip Cells Undertow - Zonation of Flow in Broken Wave Bores In the wave breaking process, the landward transfer of water, associated with bore and surface roller decay
More informationMAR 110 LECTURE #15 Wave Hazards
1 MAR 110 LECTURE #15 Wave Hazards Rogue Wave Hazard Rogue waves are very large open ocean waves of sometimes can range in height from 60 ft (20m) to120 feet (40m) and thus a significant hazard to large
More information/50. Physical Geology Shorelines
Physical Geology Shorelines Multiple Guess: (You know the drill 2 points each) 1. The path of movement of a water particle in a wave at sea is 1. circular 2. horizontal 3. vertical 4. elliptical 5. none
More informationPRINCIPLES OF FLUID FLOW AND SURFACE WAVES RIVERS, ESTUARIES, SEAS AND OCEANS. Leo C. van Rijn
PRINCIPLES OF FLUID FLOW AND SURFACE WAVES IN RIVERS, ESTUARIES, SEAS AND OCEANS (Edition 2011) Leo C. van Rijn Physical Geography Other publications: Principles of Sediment Transport in Rivers, Estuaries
More informationGarrett McNamara, Portugal, 30 Jan What is a wave?
Waves Garrett McNamara, Portugal, 30 Jan 2013 What is a wave? Waves transmit a disturbance / energy from one part of a material to another. The energy is transmitted without substantial movement of the
More informationWIND SPEED LENGTH OF TIME WIND BLOWS (Duration) DISTANCE OVER WHICH IT BLOWS (Fetch)
WAVES Up and down movement of ocean surface Transportation of energy across the water over vast distances If not stopped by anything, waves can travel entire oceans Size and speed depend upon: WIND SPEED
More informationCROSS-SHORE SEDIMENT PROCESSES
The University of the West Indies Organization of American States PROFESSIONAL DEVELOPMENT PROGRAMME: COASTAL INFRASTRUCTURE DESIGN, CONSTRUCTION AND MAINTENANCE A COURSE IN COASTAL DEFENSE SYSTEMS I CHAPTER
More informationSalmon: Introduction to ocean waves
10 Breakers, bores and longshore currents There is lots more to say about linear, shallow-water waves, but now we want to say something about the more general, nonlinear case. To keep the math as simple
More informationPhysics Mechanics
1 Physics 170 - Mechanics Lecture 33 Waves Wave notion 2 A wave pulse is a disturbance that propagates through a medium. It transfers energy without transferring matter; the energy is a combination of
More informationCHAPTER 14 VIBRATIONS & WAVES
Physics Approximate Timeline Students are expected to keep up with class work when absent. CHAPTER 14 VIBRATIONS & WAVES Day Plans for the day Assignments for the day 1 Section 14.1 Periodic Motion o Definitions
More informationShorelines Earth - Chapter 20 Stan Hatfield Southwestern Illinois College
Shorelines Earth - Chapter 20 Stan Hatfield Southwestern Illinois College The Shoreline A Dynamic Interface The shoreline is a dynamic interface (common boundary) among air, land, and the ocean. The shoreline
More informationCVEN Computer Applications in Engineering and Construction. Programming Assignment #4 Analysis of Wave Data Using Root-Finding Methods
CVEN 30-501 Computer Applications in Engineering and Construction Programming Assignment #4 Analysis of Wave Data Using Root-Finding Methods Date distributed: 9/30/016 Date due: 10/14/016 at 3:00 PM (electronic
More informationChapter 11. Beach Fill and Soft Engineering Structures
Chapter 11 Beach Fill and Soft Engineering Structures Solutions to Coastal Erosion Soft Structures Hard Structures Retreat No such thing as low cost coastal protection Beach Nourishment Beach Filling Beach
More informationArtificial headlands for coastal restoration
Artificial headlands for coastal restoration J. S. Mani Professor, Department of Ocean Engineering, Indian Institute of Technology Madras, Chennai 636, India Abstract Construction of a satellite harbour
More informationSUPERGEN Wind Wind Energy Technology Rogue Waves and their effects on Offshore Wind Foundations
SUPERGEN Wind Wind Energy Technology Rogue Waves and their effects on Offshore Wind Foundations Jamie Luxmoore PhD student, Lancaster University SUPERGEN Wind II - 7 th training seminar 3 rd - 4 th September
More informationTechnical Brief - Wave Uprush Analysis Island Harbour Club, Gananoque, Ontario
Technical Brief - Wave Uprush Analysis RIGGS ENGINEERING LTD. 1240 Commissioners Road West Suite 205 London, Ontario N6K 1C7 October 31, 2014 Table of Contents Section Page Table of Contents... i List
More informationWAVE AND CURRENT HYDRODINAMICS STUDY AT BATANG AIR DINGIN RIVER MOUTHPADANG, INDONESIA
International Journal of Civil Engineering and Technology (IJCIET) Volume 9, Issue 11, November 2018, pp. 2054 2062, Article ID: IJCIET_09_11_202 Available online at http://www.iaeme.com/ijciet/issues.asp?jtype=ijciet&vtype=9&itype=11
More informationENERGY OF WAVES ch.1 PRACTICE TEST
ENERGY OF WAVES ch.1 PRACTICE TEST Multiple Choice Identify the choice that best completes the statement or answers the question. 1. If a wave is traveling at a certain speed and its frequency is doubled,
More informationCharacteristics of Waves
Chapter 15 Characteristics of Waves Waves disturbances that carry energy through matter or space Waves transfer energy. The energy being transferred may spread out as waves travel. Characteristics of Waves
More informationOcean Waves. Capillary. Gravity. Wind generated. Tides Tsunamis Seiches
Ocean Waves Capillary Wind generated Gravity Tides Tsunamis Seiches Capillary waves are driven by the surface tension produced by electrically polarized water molecule San Pedro Lighthouse Waves are alternate
More informationAn experimental study of internal wave generation through evanescent regions
An experimental study of internal wave generation through evanescent regions Allison Lee, Julie Crockett Department of Mechanical Engineering Brigham Young University Abstract Internal waves are a complex
More informationMAR 110 LECTURE #20 Storm-Generated Waves & Rogue Waves
MAR 110 LECTURE #20 Storm-Generated Waves & Rogue Waves Wave Principles Review Figure 20.1 Wave Principles (ABOVE) A simple ocean surface wave is a sea level distortion that repeats itself over a distance
More informationAbstract. 1 Introduction
A computational method for calculatingthe instantaneous restoring coefficients for a ship moving in waves N. El-Simillawy College of Engineering and Technology, Arab Academyfor Science and Technology,
More informationA Little Math. Wave speed = wave length/wave period C= L/T. Relationship of Wave Length to Depth of Wave Motion
Ocean Waves 1 2 1 A Little Math Wave speed = wave length/wave period C= L/T 3 Relationship of Wave Length to Depth of Wave Motion 4 2 Motion of Water as Wave Passes Water in the crest of the wave move
More informationWave Propagation and Shoaling
Wave Propagation and Shoaling Focus on movement and natural alteration of the characteristics of waves as they travel from the source region toward shore Waves moving from deep to intermediate/shallow
More informationChapter 11 Tides. A tidal bore is formed when a tide arrives to an enclosed river mouth. This is a forced wave that breaks.
Chapter 11 Tides A tidal bore is formed when a tide arrives to an enclosed river mouth. This is a forced wave that breaks. Tidal range can be very large Tide - rhythmic oscillation of the ocean surface
More informationBILLY BISHOP TORONTO CITY AIRPORT PRELIMINARY RUNWAY DESIGN COASTAL ENGINEERING STUDY
Bâtiment Infrastructures municipales Transport Industriel Énergie Environnement BILLY BISHOP TORONTO CITY AIRPORT PRELIMINARY RUNWAY DESIGN COASTAL ENGINEERING STUDY N. Guillemette 1, C. Glodowski 1, P.
More informationPREDICTION OF BEACH CHANGES AROUND ARTIFICIAL REEF USING BG MODEL
PREDICTION OF BEACH CHANGES AROUND ARTIFICIAL REEF USING BG MODEL Hiroaki Fujiwara 1, Takaaki Uda 2, Toshiaki Onishi 1, Shiho Miyahara 3 and Masumi Serizawa 3 On the Kaike coast, one of the twelve detached
More informationThe construction of Deepwater Navigation Channel (DNC) in the Bystry arm of the Danube Delta has started in The whole project provides the
Annex 45 Numerical Studies of Waves, Currents and Sediment Transport at the Marine Part of Deepwater Navigation Channel through the Bystry Arm of the Danube Delta and Model Verification based on Laboratory
More informationChapter - Oceans and Coasts
Chapter - Oceans and Coasts Discussion: What do oceans contribute to the environment of Earth? How do Earth s major systems relate to the oceans? Oceans and Coasts Oceans are important - Thermal regulation
More informationMONITORING SEDIMENT TRANSPORT PROCESSES AT MANAVGAT RIVER MOUTH, ANTALYA TURKEY
COPEDEC VI, 2003 in Colombo, Sri Lanka MONITORING SEDIMENT TRANSPORT PROCESSES AT MANAVGAT RIVER MOUTH, ANTALYA TURKEY Isikhan GULER 1, Aysen ERGIN 2, Ahmet Cevdet YALCINER 3 ABSTRACT Manavgat River, where
More informationMODELING OF CLIMATE CHANGE IMPACTS ON COASTAL STRUCTURES - CONTRIBUTION TO THEIR RE-DESIGN
Proceedings of the 14 th International Conference on Environmental Science and Technology Rhodes, Greece, 3-5 September 2015 MODELING OF CLIMATE CHANGE IMPACTS ON COASTAL STRUCTURES - CONTRIBUTION TO THEIR
More information4/20/17. #30 - Coastlines - General Principles Coastlines - Overview
Writing Assignment Due one week from today by 11:59 pm See main class web pages for detailed instructions Essays will be submitted in Illinois Compass (instructions later) Pick one: Earthquakes, tsunamis,
More informationWhat are Waves? Earthquake. Waving flags. Vocal Cords Vibrate
Waves Ch. 10 What are Waves? All waves are movement of energy through a medium (air, rock, water) Series of vibrations or undulations in a medium Wave types: ocean, sound, light, seismic Vocal Cords Vibrate
More informationDUXBURY WAVE MODELING STUDY
DUXBURY WAVE MODELING STUDY 2008 Status Report Duncan M. FitzGerald Peter S. Rosen Boston University Northeaster University Boston, MA 02215 Boston, MA 02115 Submitted to: DUXBURY BEACH RESERVATION November
More informationOCEANOGRAPHY STUDY GUIDE
OCEANOGRAPHY STUDY GUIDE Chapter 2 Section 1 1. Most abundant salt in ocean. Sodium chloride; NaCl 2. Amount of Earth covered by Water 71% 3. Four oceans: What are they? Atlantic, Pacific, Arctic, Indian
More informationSPH applied to coastal engineering problems
2 nd Iberian Workshop Ourense, 3 rd and 4 th December 2015 SPH applied to coastal engineering problems (validating the SPH concept) ALTOMARE, CRESPO, DOMINGUEZ, SUZUKI http://www.flandershydraulicsresearch.be/
More informationDETRMINATION OF A PLUNGER TYPE WAVE MAKER CHARACTERISTICE IN A TOWING TANK
The 9 th International Conference on Coasts, Ports and Marine Structures (ICOPMAS 2010) 29 Nov.-1 Dec. 2010 (Tehran) DETRMINATION OF A PLUNGER TYPE WAVE MAKER CHARACTERISTICE IN A TOWING TANK sayed mohammad
More informationWave Load Pattern Definition
COMPUTERS AND STRUCTURES, INC., AUGUST 2010 AUTOMATIC WAVE LOADS TECHNICAL NOTE DEFINING WAVE LOADS This section describes how to define automatic wave loads. The automatic wave load is a special type
More informationMeasurement and simulation of the flow field around a triangular lattice meteorological mast
Measurement and simulation of the flow field around a triangular lattice meteorological mast Matthew Stickland 1, Thomas Scanlon 1, Sylvie Fabre 1, Andrew Oldroyd 2 and Detlef Kindler 3 1. Department of
More informationSection 1 Types of Waves
CHAPTER OUTLINE Section 1 Types of Waves Key Idea questions > What does a wave carry? > How are waves generated? > What is the difference between a transverse wave and a longitudinal wave? > How do the
More informationTechnical Brief - Wave Uprush Analysis 129 South Street, Gananoque
Technical Brief - Wave Uprush Analysis 129 South Street, Gananoque RIGGS ENGINEERING LTD. 1240 Commissioners Road West Suite 205 London, Ontario N6K 1C7 June 12, 2013 Table of Contents Section Page Table
More informationCOASTAL ENVIRONMENTS. 454 lecture 12
COASTAL ENVIRONMENTS Repeated movement of sediment & water constructs a beach profile reflecting the balance between average daily or seasonal wave forces and resistance of landmass to wave action Coasts
More informationGravity waves in stable atmospheric boundary layers
Gravity waves in stable atmospheric boundary layers Carmen J. Nappo CJN Research Meteorology Knoxville, Tennessee 37919, USA Abstract Gravity waves permeate the stable atmospheric planetary boundary layer,
More informationDetermination Of Nearshore Wave Conditions And Bathymetry From X-Band Radar Systems
Determination Of Nearshore Wave Conditions And Bathymetry From X-Band Radar Systems Okey G. Nwogu Dept. of Naval Architecture and Marine Engineering University of Michigan Ann Arbor, MI 489 phone: (734)
More informationSensitivity of storm waves in Montevideo (Uruguay) to a hypothetical climate change
Vol. 9: 81-85,1997 1 CLIMATE RESEARCH Clim Res I Published December 29 Sensitivity of storm waves in Montevideo (Uruguay) to a hypothetical climate change Eugenio Lorenzo*, Luis Teixeira Instituto de Mecanica
More informationMetocean criteria for fatigue assessment. Rafael V. Schiller 5th COPEDI Seminar, Oct 8th 2014.
Metocean criteria for fatigue assessment Rafael V. Schiller 5th COPEDI Seminar, Oct 8th 2014. Metocean requirements along the lifecycle of a project Metocean criteria for fatigue Analysis techniques and
More information2. Water levels and wave conditions. 2.1 Introduction
18 2. Water levels and wave conditions 2.1 Introduction This Overtopping Manual has a focus on the aspects of wave run-up and wave overtopping only. It is not a design manual, giving the whole design process
More informationTesting TELEMAC-2D suitability for tsunami propagation from source to near shore
Testing TELEMAC-2D suitability for tsunami propagation from source to near shore Alan Cooper, Giovanni Cuomo, Sébastien Bourban, Michael Turnbull, David Roscoe HR Wallingford Ltd, Howbery Park, Wallingford,
More informationDetermination of Nearshore Wave Conditions and Bathymetry from X-Band Radar Systems
Determination of Nearshore Wave Conditions and Bathymetry from X-Band Radar Systems Okey G. Nwogu Dept. of Naval Architecture and Marine Engineering University of Michigan Ann Arbor, MI 48109 Phone: (734)
More informationSea State Analysis. Topics. Module 7 Sea State Analysis 2/22/2016. CE A676 Coastal Engineering Orson P. Smith, PE, Ph.D.
Sea State Analysis Module 7 Orson P. Smith, PE, Ph.D. Professor Emeritus Module 7 Sea State Analysis Topics Wave height distribution Wave energy spectra Wind wave generation Directional spectra Hindcasting
More informationNumerical simulation of linear wave propagation, wave-induced circulation, sediment transport and beach evolution
Numerical simulation of linear wave propagation, wave-induced circulation, sediment transport and beach evolution Theofanis V. Karambas Aristotle University of Thessaloniki, Department of Civil Engineering,
More informationOceans and Coasts. Chapter 18
Oceans and Coasts Chapter 18 Exploring the oceans The ocean floor Sediments thicken and the age of the seafloor increases from ridge to shore The continental shelf off the northeast United States Constituent
More informationSection 1: Types of Waves
Waves Section 1 Section 1: Types of Waves Preview Key Ideas Bellringer What Is a Wave? Vibrations and Waves Transverse and Longitudinal Waves Surface Waves Waves Section 1 Key Ideas What does a wave carry?
More informationA.J.C. Crespo, J.M. Domínguez, C. Altomare, A. Barreiro, M. Gómez-Gesteira
A.J.C. Crespo, J.M. Domínguez, C. Altomare, A. Barreiro, M. Gómez-Gesteira OUTLINE Oscillating Water Column - What OWC is? - Numerical modelling of OWC SPH functionalities - Wave generation (1 st order
More information( max)o Wind Waves 10 Short Swell (large wave steepness) 25 Long Swell (small wave steepness) 75
CEPi-I-18 REvKn, 3188 IRREGULAR WAVE DIFFRACTION BY GODA'S KETHOD PURPOSE : To provide a simplified method for determining random wave diffraction coefficients for a semi-infinite breakwater. GENERAL :
More informationChapter 16 Waves and Sound
Chapter 16 WAVES AND SOUND PREVIEW A wave is a disturbance which causes a transfer of energy. Mechanical waves need a medium in which to travel, but electromagnetic waves do not. Waves can be transverse
More informationGeneral Coastal Notes + Landforms! 1
General Coastal Notes + Landforms! 1 Types of Coastlines: Type Description Primary Coast which is essentially in the same condition when sea level stabilized Coastline after the last ice age, younger.
More informationAppendix E Cat Island Borrow Area Analysis
Appendix E Cat Island Borrow Area Analysis ERDC/CHL Letter Report 1 Cat Island Borrow Area Analysis Multiple borrow area configurations were considered for Cat Island restoration. Borrow area CI1 is located
More informationWaves Part II. non-dispersive (C g =C)
Waves Part II Previously we discussed Surface Gravity Waves Deep Water Waves Shallow Water Waves C g T 2 C g h dispersive (C g =C/2) Definitions: phase speed C= /T= /k non-dispersive (C g =C) group speed
More informationWAVE RUNUP ON COMPOSITE-SLOPE AND CONCAVE BEACHES ABSTRACT
CHAPTER 168 WAVE RUNUP ON COMPOSITE-SLOPE AND CONCAVE BEACHES R. H. Mayer 1 and D. L. Kriebel 1 ABSTRACT Laboratory experiments were carried out for regular and irregular wave runup over non-uniform beach
More informationComputational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy
Computational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy 1 OUTLINE Overview of Oil Spill & its Impact Technical Challenges for Modeling Review
More informationWave Motion. interference destructive interferecne constructive interference in phase. out of phase standing wave antinodes resonant frequencies
Wave Motion Vocabulary mechanical waves pulse continuous periodic wave amplitude period wavelength period wave velocity phase transverse wave longitudinal wave intensity displacement amplitude phase velocity
More informationSURFACE CURRENTS AND TIDES
NAME SURFACE CURRENTS AND TIDES I. Origin of surface currents Surface currents arise due to the interaction of the prevailing wis a the ocean surface. Hence the surface wi pattern (Figure 1) plays a key
More informationAiry Wave Theory 2: Wave Orbitals and Energy. Compilation of Airy Equations
Airy Wave Theory 2: Wave Orbitals and Energy Compilation of Airy Equations 1 Orbital Motion of Water Particles Airy Wave Theory also predicts water particle orbital path trajectories. Orbital path divided
More informationNTHMP - Mapping & Modeling Benchmarking Workshop: Tsunami Currents
NTHMP - Mapping & Modeling Benchmarking Workshop: Tsunami Currents Ahmet Cevdet Yalçıner, Andrey Zaytsev, Utku Kanoğlu Deniz Velioglu, Gozde Guney Dogan, Rozita Kian, Naeimeh Shaghrivand, Betul Aytore
More informationIMO REVISION OF THE INTACT STABILITY CODE. Proposal of methodology of direct assessment for stability under dead ship condition. Submitted by Japan
INTERNATIONAL MARITIME ORGANIZATION E IMO SUB-COMMITTEE ON STABILITY AND LOAD LINES AND ON FISHING VESSELS SAFETY 49th session Agenda item 5 SLF 49/5/5 19 May 2006 Original: ENGLISH REVISION OF THE INTACT
More informationRogue Wave Statistics and Dynamics Using Large-Scale Direct Simulations
Rogue Wave Statistics and Dynamics Using Large-Scale Direct Simulations Dick K.P. Yue Center for Ocean Engineering Department of Mechanical Engineering Massachusetts Institute of Technology Cambridge,
More informationCheck out Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.
Name: Mr. Willis Conceptual Physics: Date: Unit VII Mechanical Waves & Sound Need extra help? Check out http://www.bayhicoach.com Unit VII Study Guide Multiple Choice Identify the letter of the choice
More informationSEDIMENT BUDGET OF LIDO OF PELLESTRINA (VENICE) Written by Marcello Di Risio Under the supervision of Giorgio Bellotti and Leopoldo Franco
SEDIMENT BUDGET OF LIDO OF PELLESTRINA (VENICE) Written by Marcello Di Risio Under the supervision of Giorgio Bellotti and Leopoldo Franco Table of contents: 1. Introduction...3 2. Protection structures
More information