An Evaluation of Design Factors and Performance of Groynes
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Management of Coastal Erosion by Creating Large-Scale and Small-Scale Sediment Cells
COASTAL EROSION CONTROL BASED ON THE CONCEPT OF SEDIMENT CELLS by L. C. van Rijn, www.leovanrijn-sediment.com, March 2013 1. Introduction Nearly all coastal states have to deal with the problem of coastal erosion. Coastal erosion and accretion has always existed and these processes have contributed to the shaping of the present coastlines. However, coastal erosion now is largely intensified due to human activities. Presently, the total coastal area (including houses and buildings) lost in Europe due to marine erosion is estimated to be about 15 km2 per year. The annual cost of mitigation measures is estimated to be about 3 billion euros per year (EUROSION Study, European Commission, 2004), which is not acceptable. Although engineering projects are aimed at solving the erosion problems, it has long been known that these projects can also contribute to creating problems at other nearby locations (side effects). Dramatic examples of side effects are presented by Douglas et al. (The amount of sand removed from America’s beaches by engineering works, Coastal Sediments, 2003), who state that about 1 billion m3 (109 m3) of sand are removed from the beaches of America by engineering works during the past century. The EUROSION study (2004) recommends to deal with coastal erosion by restoring the overall sediment balance on the scale of coastal cells, which are defined as coastal compartments containing the complete cycle of erosion, deposition, sediment sources and sinks and the transport paths involved. Each cell should have sufficient sediment reservoirs (sources of sediment) in the form of buffer zones between the land and the sea and sediment stocks in the nearshore and offshore coastal zones to compensate by natural or artificial processes (nourishment) for sea level rise effects and human-induced erosional effects leading to an overall favourable sediment status. -
1 the Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration
1 The Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration 2 of Soft Cliff Coastlines 3 4 Sally Brown1*, Max Barton1, Robert J Nicholls1 5 6 1. Faculty of Engineering and the Environment, University of Southampton, 7 University Road, Highfield, Southampton, UK. S017 1BJ. 8 9 * Sally Brown ([email protected], Telephone: +44(0)2380 594796). 10 11 Abstract: Building defences, such as groynes, on eroding soft cliff coastlines alters the 12 sediment budget, changing the shoreline configuration adjacent to defences. On the 13 down-drift side, the coastline is set-back. This is often believed to be caused by increased 14 erosion via the ‘terminal groyne effect’, resulting in rapid land loss. This paper examines 15 whether the terminal groyne effect always occurs down-drift post defence construction 16 (i.e. whether or not the retreat rate increases down-drift) through case study analysis. 17 18 Nine cases were analysed at Holderness and Christchurch Bay, England. Seven out of 19 nine sites experienced an increase in down-drift retreat rates. For the two remaining sites, 20 retreat rates remained constant after construction, probably as a sediment deficit already 21 existed prior to construction or as sediment movement was restricted further down-drift. 22 For these two sites, a set-back still evolved, leading to the erroneous perception that a 23 terminal groyne effect had developed. Additionally, seven of the nine sites developed a 24 set back up-drift of the initial groyne, leading to the defended sections of coast acting as 1 25 a hard headland, inhabiting long-shore drift. -
Guidance for Flood Risk Analysis and Mapping
Guidance for Flood Risk Analysis and Mapping Coastal Notations, Acronyms, and Glossary of Terms May 2016 Requirements for the Federal Emergency Management Agency (FEMA) Risk Mapping, Assessment, and Planning (Risk MAP) Program are specified separately by statute, regulation, or FEMA policy (primarily the Standards for Flood Risk Analysis and Mapping). This document provides guidance to support the requirements and recommends approaches for effective and efficient implementation. Alternate approaches that comply with all requirements are acceptable. For more information, please visit the FEMA Guidelines and Standards for Flood Risk Analysis and Mapping webpage (www.fema.gov/guidelines-and-standards-flood-risk-analysis-and- mapping). Copies of the Standards for Flood Risk Analysis and Mapping policy, related guidance, technical references, and other information about the guidelines and standards development process are all available here. You can also search directly by document title at www.fema.gov/library. Coastal Notation, Acronyms, and Glossary of Terms May 2016 Guidance Document 66 Page i Document History Affected Section or Date Description Subsection Initial version of new transformed guidance. The content was derived from the Guidelines and Specifications for Flood Hazard Mapping Partners, Procedure Memoranda, First Publication May 2016 and/or Operating Guidance documents. It has been reorganized and is being published separately from the standards. Coastal Notation, Acronyms, and Glossary of Terms May 2016 Guidance Document 66 -
ENVIRONMENT in COASTAL ENGINEERING: DEFINITIONS and EXAMPLES** Cyril Galvin, M. ASCE* ABSTRACT in Current Usage, Environmental A
ENVIRONMENT IN COASTAL ENGINEERING: DEFINITIONS AND EXAMPLES** Cyril Galvin, M. ASCE* ABSTRACT In current usage, environmental aspects of coastal engineering design include aspects of ecology and aesthe- tics, as well as environment. In practice, the aspect of environment is a limited one, considering man's surround- ings, with the works of man left out. The increased consid- eration of environmental aspects over the past 15 years has brought real benefits to the coastal engineering profession, as well as obvious problems. One problem is a mythology of coastal processes that has become widely accepted. Priori- ties in coastal engineering design remain a structure that will last a useful lifetime and perform its intended func- tion without creating new problems. After satisfying these fundamental requirements, the structure should minimize ecological change, and fit pleasingly in its setting. INTRODUCTION Design and THE Environment. A coastal structure must remain standing when hit by the most severe waves, currents, and winds that can reasonably be expected during its intended lifetime. Waves, currents, and winds are basic elements of the physical environment. In this structural sense, good coastal engineering is always sensitive to the environment. But the designer who creates a structure that doesn't fall down has not necessarily solved a coastal problem. The structure must also perform a function, without creating significant new problems. it must reduce beach erosion, prevent flooding, maintain a channel, provide a quiet anchorage, convey liquids across the shore, or serve other functions. There are groins standing out at sea after the beach has eroded away; jetties exist that enclose a deposit of sand rather than a navigable waterway; some seawalls are regularly overtopped by moderate seas; water intakes are silted in. -
Coastal Risk Assessment for Ebeye
Coastal Risk Assesment for Ebeye Technical report | Coastal Risk Assessment for Ebeye Technical report Alessio Giardino Kees Nederhoff Matthijs Gawehn Ellen Quataert Alex Capel 1230829-001 © Deltares, 2017, B De tores Title Coastal Risk Assessment for Ebeye Client Project Reference Pages The World Bank 1230829-001 1230829-00 1-ZKS-OOO1 142 Keywords Coastal hazards, coastal risks, extreme waves, storm surges, coastal erosion, typhoons, tsunami's, engineering solutions, small islands, low-elevation islands, coral reefs Summary The Republic of the Marshall Islands consists of an atoll archipelago located in the central Pacific, stretching approximately 1,130 km north to south and 1,300 km east to west. The archipelago consists of 29 atolls and 5 reef platforms arranged in a double chain of islands. The atolls and reef platforms are host to approximately 1,225 reef islands, which are characterised as low-lying with a mean elevation of 2 m above mean sea leveL Many of the islands are inhabited, though over 74% of the 53,000 population (2011 census) is concentrated on the atolls of Majuro and Kwajalein The limited land size of these islands and the low-lying topographic elevation makes these islands prone to natural hazards and climate change. As generally observed, small islands have low adaptive capacity, and the adaptation costs are high relative to the gross domestic product (GDP). The focus of this study is on the two islands of Ebeye and Majuro, respectively located on the Ralik Island Chain and the Ratak Island Chain, which host the two largest population centres of the archipelago. -
Mathematical Model of Groynes on Shingle Beaches
HR Wallingford Mathematical Model of Groynes on Shingle Beaches A H Brampton BSc PhD D G Goldberg BA Report SR 276 November 1991 Address:Hydraulics Research Ltd, wallingford,oxfordshire oxl0 gBA,United Kingdom. Telephone:0491 35381 Intemarional + 44 49135381 relex: g4gsszHRSwALG. Facstunile:049132233Intemarional + M 49132233 Registeredin EngtandNo. 1622174 This report describes an investigation carried out by HR Wallingford under contract CSA 1437, 'rMathematical- Model of Groynes on Shingle Beaches", funded by the Ministry of Agri-culture, Fisheries and Food. The departmental nominated. officer for this contract was Mr A J Allison. The company's nominated. project officer was Dr S W Huntington. This report is published on behalf of the Ministry of Agriculture, Fisheries and Food, but the opinions e>rpressed are not necessarily those of the Ministry. @ Crown Copyright 1991 Published by permission of the Controller of Her Majesty's Stationery Office Mathematical model of groSmes on shingle beaches A H Brampton BSc PhD D G Goldberg BA Report SR 276 November 1991 ABSTRACT This report describes the development of a mathematical model of a shingle beach with gro5mes. The development of the beach plan shape is calculated given infornation on its initial position and information on wave conditions just offshore. Different groyne profiles and spacings can be specified, so that alternative gro5me systems can be investigated. Ttre model includes a method for dealing with varying water levels as the result of tidal rise and fall. CONTENTS Page 1. INTRODUCTION I 2. SCOPEOF THE UODEL 3 2.t Model resolution and input conditions 3 2.2 Sediment transport mechanisms 6 2.3 Vertical distribution of sediment transport q 2.4 Wave transformation modelling L0 3. -
Shoreline Stabilisation
Section 5 SHORELINE STABILISATION 5.1 Overview of Options Options for handling beach erosion along the western segment of Shelley Beach include: • Do Nothing – which implies letting nature take its course; • Beach Nourishment – place or pump sand on the beach to restore a beach; • Wave Dissipating Seawall – construct a wave dissipating seawall in front of or in lieu of the vertical wall so that wave energy is absorbed and complete protection is provided to the boatsheds and bathing boxes behind the wall for a 50 year planning period; • Groyne – construct a groyne, somewhere to the east of Campbells Road to prevent sand from the western part of Shelley Beach being lost to the eastern part of Shelley Beach; • Offshore Breakwater – construct a breakwater parallel to the shoreline and seaward of the existing jetties to dissipate wave energy before it reaches the beach; and • Combinations of the above. 5.2 Do Nothing There is no reason to believe that the erosion process that has occurred over at least the last 50 years, at the western end of Shelley Beach, will diminish. If the water depth over the nearshore bank has deepened, as it appears visually from aerial photographs, the wave heights and erosive forces may in fact increase. Therefore “Do Nothing” implies that erosion will continue, more structures will be threatened and ultimately damaged, and the timber vertical wall become undermined and fail, exposing the structures behind the wall to wave forces. The cliffs behind the wall will be subjected to wave forces and will be undermined if they are not founded on solid rock. -
Functional Design of Coastal Structures
FUNCTIONALFUNCTIONAL DESIGNDESIGN OFOF David R. Basco, Ph.D, P.E. Director, The Coastal Engineering Center Old Dominion University,Norfolk, Virginia USA 23529 [email protected] DESIGNDESIGN OFOF COASTALCOASTAL STRUCTURESSTRUCTURES •• FunctionFunction ofof structurestructure •• StructuralStructural integrityintegrity •• PhysicalPhysical environmentenvironment •• ConstructionConstruction methodsmethods •• OperationOperation andand maintenancemaintenance OUTLINEOUTLINE •• PlanPlan formform layoutlayout - headland breakwaters - nearshore breakwaters - groin fields • WaveWave runuprunup andand overtopping*overtopping* - breakwaters and revetments (seawalls, beaches not covered here) •• WaveWave reflectionsreflections (materials(materials includedincluded inin notes)notes) * materials from ASCE, Coastal Engineering Short Course, CEM Preview, April 2001 SHORESHORE PARALLELPARALLEL BREAKWATERS:BREAKWATERS: HEADLANDHEADLAND TYPETYPE Design Rules, Hardaway et al. 1991 • Use sand fill to create tombolo for constriction from land • Set berm elevation so tombolo always present at high tide • Set Yg/Lg =• 1.65 for stable shaped beach • Set Ls/Lg = 1 • Always combine with new beach fill • See CEM 2001 V-3 for details KEYKEY VARIABLESVARIABLES FORFOR NEARSHORENEARSHORE BREAKWATERBREAKWATER DESIGNDESIGN Dally and Pope, 1986 Definitions: Y = breakwater distance from nourished shoreline Ls = length of breakwater Lg = gap distance d = water depth at breakwater (MWL) ds = water depth• at breakwater (MWL) •Tombolo formation: Ls/Y = 1.5 to 2 single = 1.5 system •Salient formation: Ls/ = 0.5 to 0.67 = 0.125 long systems (a) (b) Process Parameter Description 1. Bypassing Dg/Hb Depth at groin tip/breaking wave height 2. Permeability • Over-passing Zg (y) Groin elevation across profile, tidal range • Through-passing P(y) Grain permeability across shore • Shore-passing Zb/R Berm elevation/runup elevation 3. Longshore transport Qn/Qg Net rate/gross rate Property Comment 1. Wave angle and wave height Accepted. -
Environmentally Friendly Coastal Protection the ECOPRO Project Abstract
Environmentally Friendly Coastal Protection The ECOPRO Project Brendan Dollard1 Abstract In the battle to preserve land against the ravages of the sea man has created many inappropriate protection structures on the coast. Often the coastline which is being protected is, inherently, in dis-equilibrium with nature. When combined with the increased recreational usage of the coastal zone, the rise in sea level and the increased incidence of storms, accelerated erosion rates are often the result. The Environmentally Friendly Coastal Protection project, or ECOPRO for short, developed a coastal erosion assessment method for the non-specialist. It devised a system for optimising erosion monitoring and developed a guide to select of an appropriate coastal protection response. The project results are contained in the ECOPRO Code of Practice. This 320-page guide explains the steps involved in assessing and monitoring coastal erosion problems, planning protective actions and evaluating their environmental impact. Prepared by the Offshore & Coastal Engineering Unit of Enterprise Ireland, it is the result of four years of work which was supported under the EU LIFE Programme and drew on expertise from Ireland, Northern Ireland and Denmark. This paper presents details of the project and the development of the Code. 1. Introduction In recent years it has become accepted that the coastline is a valuable natural resource which needs careful and sensitive management. This is especially so in the case of small island countries where the coastal zone has a direct and major influence on the economic welfare of the country. Coastal erosion has always been seen as one of the main threats to this resource and for centuries man has been fighting what was perceived as the ravages of the sea. -
The Case-Study of Fongafale, Atool of Funafuti
Shoreline of human-impacted coralline atolls: need for a concerted management. The case-study of Fongafale, atoll of Funafuti, Tuvalu Caroline Rufin The atoll of Funafuti (Tuvalu archipelago) is located in the South Pacific Ocean at latitude 8.31° South and longitude 179.13° East (Figure 1). According to its morphology, Fongafale island (atoll of Funafuti) can be split into three distinct geographical areas, i.e. the northern, central and southern parts. The present study deals with the central part, which results from the deposition of sediments from the two other areas following North and South longshore drifts. Marshall •• Islands, 1o·N Kiribati! . ~ ~· ... ' ... .. ·. ~ Samoa .. o_. •• Vanuatu b •! ; . b\ Fiji ,::::1 . ~ 0 Tonga .. ' '· : .... 2o·s New .. ~.'•. ' •• Caledon~. • • • 100· 110· 180' 170' 160"W Source : from Mclean et Hosking. 1991 Figure 1 Localisation of Tuvalu within the Pacific Bassin. 436 Coral reefs in the Pacifie: Status and monitoring, Resources and management Through the example of Fongafale island, the present study is aimed at thinking about the manage ment of low coralline islands confronted with erosion problems most often in relation with excessive coastal planning. This thought will be developed in terms of global geography while taking into account ail the environmental conditions. Our purpose will be not to demonstrate which of the two factors, Man or Nature, is the more disturb ing. However, from the analysis of our data set it is clear that the contribution of the former is greater than that of the latter. We will first draw a schedule of Fongafale lagoon shoreline from aerial pictures and topographical readings; it will be essential to understand the environmental problems which this atoll is submitted to. -
EIA for the Proposed Coastal Protection and Beach Nourishment at Madifushi Island, Meemu Atoll
EIA for the Proposed Coastal Protection and Beach Nourishment at Madifushi Island, Meemu Atoll Madifushi Island; Photo by: Water Solutions Pvt Ltd Proposed by: Maldives Inflight Caterings Pte Ltd Prepared by: Ahmed Jameel (EIA P07/2007) and Mohamed Umar (EIA P02/2019) For Water Solutions Pvt. Ltd., Maldives March 2021 EIA for the Proposed Coastal Protection and Beach Nourishment at Madifushi, Meemu Atoll Blank Page Prepared by Water Solutions Pvt. Ltd, March 2021 Page 2 EIA for the Proposed Coastal Protection and Beach Nourishment, Meemu Atoll 1 Table of contents EIA for the Proposed Coastal Protection and Beach Nourishment at Madifushi Island, Meemu Atoll .............................................................................................................................. 1 1 Table of contents ...................................................................................................... 3 2 List of Figures and Tables ........................................................................................ 8 3 Declaration of the consultants ................................................................................ 10 4 Proponents Commitment and Declaration ............................................................. 11 5 Non-Technical Summary ....................................................................................... 16 6 Introduction ............................................................................................................ 18 Structure of the EIA .......................................................................................... -
Engineering for Climate: Coastal Engineering Methods for Resilient Atoll Nations in Productive Oceans
Engineering for Climate Coastal Engineering Methods for Resilient Atoll Nations in Productive Oceans Presented to Asian Development Bank (ADB), Maldives By: Michael J.H. Foley, Ph.D., P.E. August 28, 2019 Welcome to Our Future Climate 10/8/19 2 Beach & Shoreline Erosion Mitigation Protecting Against Sea Level Rise Nature-Based Designs to Restore Eroded Shorelines & Enhance Coastal Resilience • Engineering • Design • Ecosystems • Technology 3 Land Subsidence Drivers of Coastal Erosion Rainfall Betio Runoff Currents Wave Runup Bairiki Rising Sea Levels 4 Sea Level Rise Increases Shoreline Wave Heights and Flooding Beach Reef Crest Reef Flat Forereef Sea Level Rise Bad for Atoll Islands Reef Crest Reef Flat Lagoon Forereef Mitigation of Erosion Hazards Adaptation Managed Retreat 10/8/19 7 Mitigation of Shoreline Erosion Armored Slopes Vertical Walls 10/8/19 8 Beaches Natural Erosion Protection 10/8/19 9 Mitigation of Beach & Shoreline Erosion Sand Nourishment Vegetated Coastal Berm Before After 10/8/19 10 Beach Stabilization Groins Breakwaters 10/8/19 11 Design by Nature – Beach Stabilization 10/8/19 12 Crescent Beaches Natural Biomimicry Crescent Engineered Beach Lagoon Crescent Beach Natural Lagoon Source: Google Earth Waves Move Sand Long-Shore Sediment Transport Cross-Shore Sediment Transport Source: Google Earth Source: Google Earth Wave Reef Interactions - Refraction Swell Deep Submerged Reef Water Channel Rotated Wave Crest Submerged Reef Waves Slow, Rotate and Converge Swell Wave Energy Diverted Source: Google Earth Source: Google