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Coastal and Delta Flood Management
INTEGRATED FLOOD MANAGEMENT TOOLS SERIES COASTAL AND DELTA FLOOD MANAGEMENT ISSUE 17 MAY 2013 The Associated Programme on Flood Management (APFM) is a joint initiative of the World Meteorological Organization (WMO) and the Global Water Partnership (GWP). It promotes the concept of Integrated Flood Management (IFM) as a new approach to flood management. The programme is financially supported by the governments of Japan, Switzerland and Germany. www.apfm.info The World Meteorological Organization is a Specialized Agency of the United Nations and represents the UN-System’s authoritative voice on weather, climate and water. It co-ordinates the meteorological and hydrological services of 189 countries and territories. www.wmo.int The Global Water Partnership is an international network open to all organizations involved in water resources management. It was created in 1996 to foster Integrated Water Resources Management (IWRM). www.gwp.org Integrated Flood Management Tools Series No.17 © World Meteorological Organization, 2013 Cover photo: Westkapelle, Netherlands To the reader This publication is part of the “Flood Management Tools Series” being compiled by the Associated Programme on Flood Management. The “Coastal and Delta Flood Management” Tool is based on available literature, and draws findings from relevant works wherever possible. This Tool addresses the needs of practitioners and allows them to easily access relevant guidance materials. The Tool is considered as a resource guide/material for practitioners and not an academic paper. References used are mostly available on the Internet and hyperlinks are provided in the References section. This Tool is a “living document” and will be updated based on sharing of experiences with its readers. -
Geography for the IB DIPLOMA
OXFORD IB STUDY GUIDES Garrett Nagle Briony Cooke Geography FOR THE IB DIPLOMA 2nd edition OPTION A FRESHWATER – DRAINAGE BASINS 1 DRAINAGE BASIN HYDROLOGY AND GEOMORPHOLOGY The drainage basin DEFINITIONS Evaporation is the physical process by which a liquid becomes a gas. It is a function of: The drainage basin is an area that is drained by a river • vapour pressure and its tributaries. Drainage basins have inputs, stores, • air temperature processes and outputs. The inputs and outputs cross the • wind boundary of the drainage basin, hence the drainage basin • rock surface, for example, bare soils and rocks have is an open system. The main input is precipitation, which is high rates of evaporation compared with surfaces regulated by various means of storage. The outputs include which have a protective tilth where rates are low. evaporation and transpiration. Flows include infiltration, throughflow, overland flow and base flow, and stores Transpiration is the loss of water from vegetation. include vegetation, soil, aquifers and the cryosphere (snow Evapotranspiration is the combined loss of water and ice). from vegetation and water surfaces to the atmosphere. Drainage basin hydrology Potential evapotranspiration is the rate of water loss from an area if there were no shortage of water. PRECIPITATION Channel Interception precipitation 1. VEGETATION FLOWS Stemflow & throughfall Infiltration is the process by which water sinks into the Overland flow 2. SURFACE STORAGE 5. CHANNEL ground. Infiltration capacity refers to the amount of Floods moisture that a soil can hold. By contrast, the infiltration Capilliary Infiltration rise rate refers to the speed with which water can enter the Interflow 3. -
Hooper Beach Dune Erosion Assessment Report
Hoopers Beach Robe Dune Erosion Assessment Report Quality Information Document Draft Report Ref 2018-06 Date 17-10-18 Prepared by D Bowers Reviewed by D Bowers Revision History Revision Authorised Revision Details Date Name/Position Signature A 20-7-18 Draft report D Bowers/ Managing Director B 24-8-18 Draft Report D Bowers/ Managing Director C 17-10-18 Final Report D Bowers/ Managing Director 2 2018-06 Disclaimer The outcomes and findings of this report have in part been informed by information supplied by the client or third parties. Civil & Environmental Solutions Pty Ltd has not attempted to verify the accuracy of such client or third party information and shall be not be liable for any loss resulting from the client or any third parties’ reliance on that information. 3 2018-06 Table of Contents Quality Information 2 Revision History 2 Disclaimer 3 1. Background 5 2. Assessment Methodology 6 Site Inspection & Site Observations 7 Discussions with Key Stakeholders 14 Client 14 DEW 15 Coastal Processes 15 Reference Document Review 15 Wind Patterns 16 Waves 18 5.3.1 Swell Waves 18 5.3.2 Wind waves 18 Sea levels including storm surge and sea level rise 20 5.4.1 Existing Climatic Conditions 20 5.4.2 Future Climatic Conditions 21 2050 Projections 21 2100 Projections 22 Erosion 22 5.5.1 Coastal Erosion and Recession 22 Short-term Storm Erosion 24 5.5.2 Long Term Recession 24 5.5.3 Recession due to Sea Level Rise (future climate) 27 5.5.4 Total estimated coastal recession 28 5.5.5 Causes of Current Accelerated Dune Erosion 29 Coastal Hazards Risk Assessment 29 Coastal Hazards 29 6.1.1 Current Hazards & Risks (0-10 years) 29 6.1.2 Future Hazards & Risk (Beyond 10 years) 29 6.1.3 Likelihood Consequence & Risk Rating 30 Potential Management Options 30 Short Term Management Options 31 Long Term Management Options 31 7.2.1 Soft Engineering Options 31 7.2.2 Hard Engineering Options 32 Development Plan Provisions 35 Conclusions 36 Recommendations 38 Appendix A 39 4 2018-06 1. -
Geomorphological Evolution of Phlegrean Volcanic Islands Near Naples, Southern Italy1
Berlin .Stuttgart Geomorphological evolution of Phlegrean volcanic islands near Naples, southern Italy1 by G.AIELLO, D.BARRA, T.DE PIPPO, C.DONADIO, and C.PETROSINO with 9 figures and 5 tables Summary. Using volcanological, morphological, palaeoecological and geoarchaeological data we reconstructed the complex evolution of the island volcanic system of Procida-Vivara, situated west of Naples betweenthe lsland of lschia and the PhlegreanFields, far the last 75 ky. Late Pleistocenemorphological evolution was chiefly controlled by a seriesof pyroclas tic eruptions that resulted in at least eight volcanic edifices, mainly under water. Probably the eruptive centresshifted progressively clockwise until about 18 ky BP when volcanic develop ment on the islands ceased. The presenceof stretches of marine terraces and traces of wave cut notches, both be low and abovè'current sea levels, the finding of exposed infralittoral rnicrofossils, and the identification of three palaeo-surfacesburied by palaeosoilsindicates at least three differen tial uplift phases.These phases interacted with postglacial eustaticfIuctuations, and were sep arated by at least two periods of generai stability in vertical movements. A final phase of ground stability, characterisedby the deposition of Phlegrean and lschia pyroclastics, start ed in the middle Holocene. Finally, fIattened surfacesand a sandy tombolo developedup to the present-day. Recent archaeological surveys and soil-borings at Procida confirm the presence of a lagoon followed by marshland at the back of a sandy tombolo that were formed after the last uplift between the Graeco-Roman periodandthe15di_16dicentury. These areaswere gradu ally filled with marine and continental sedimentsup to the 20di century. ' Finally, our investigation showed that the volcanic sector of Procida-Vivara in the late Pleistocene-Holocenewas affected by vertical displacementswhich were independent of and less marked than the concurrent movement in the adjacent sectors of lschia and of the Phle grean Fields. -
St George's Academy Geography OCR B
St George’s Academy Geography OCR B REVISION BOOKLET – Distinctive Landscapes Name: _______________________ Class teacher: _____________Tutor Group ______ PERSONAL LEARNING CHECKLIST The first thing to do whenever you start revising is to find out what you know and what you aren’t as confident on. Complete the table below by shading or ticking the correct ranking for your confidence level. 1 = Not confident at all 4 = Really confident and I can prove it! Distinctive Landscapes 1 2 3 4 1. What are the key words? 2. What is a distinctive landscape? 3. What are the upland and lowland landscapes like in the UK? 4. How does geology influence the landscape of the UK? 5. How does climate influence the landscape of the UK? 6. How does human activity influence the landscape of the UK? 7. What are the geomorphic processes that affect the UK landscape? 8. What coastal landforms are caused by erosion? 9. What coastal landforms are caused by deposition? 10. What is coastal management? 11. Coastal Case Study – Hunstanton – Norfolk Coastline 12. What is a river basin? 13. What features are found along a river’s long profile? 14. River Case Study – River Tees Once you have this grid completed you will have a good idea of where you will want to focus your revision. The following booklet will help you in all areas but you will want to focus more on the areas where you are less confident in your extra revision slots Task 1 – What are the Key Words? Abrasion Aquifer Arch Attrition Backwash Bay Beach Beach nourishment Biological weathering Abrasion Aquifer -
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. -
Characterisation and Prediction of Large-Scale, Long-Term Change of Coastal Geomorphological Behaviours: Final Science Report
Characterisation and prediction of large-scale, long-term change of coastal geomorphological behaviours: Final science report Science Report: SC060074/SR1 Product code: SCHO0809BQVL-E-P The Environment Agency is the leading public body protecting and improving the environment in England and Wales. It’s our job to make sure that air, land and water are looked after by everyone in today’s society, so that tomorrow’s generations inherit a cleaner, healthier world. Our work includes tackling flooding and pollution incidents, reducing industry’s impacts on the environment, cleaning up rivers, coastal waters and contaminated land, and improving wildlife habitats. This report is the result of research commissioned by the Environment Agency’s Science Department and funded by the joint Environment Agency/Defra Flood and Coastal Erosion Risk Management Research and Development Programme. Published by: Author(s): Environment Agency, Rio House, Waterside Drive, Richard Whitehouse, Peter Balson, Noel Beech, Alan Aztec West, Almondsbury, Bristol, BS32 4UD Brampton, Simon Blott, Helene Burningham, Nick Tel: 01454 624400 Fax: 01454 624409 Cooper, Jon French, Gregor Guthrie, Susan Hanson, www.environment-agency.gov.uk Robert Nicholls, Stephen Pearson, Kenneth Pye, Kate Rossington, James Sutherland, Mike Walkden ISBN: 978-1-84911-090-7 Dissemination Status: © Environment Agency – August 2009 Publicly available Released to all regions All rights reserved. This document may be reproduced with prior permission of the Environment Agency. Keywords: Coastal geomorphology, processes, systems, The views and statements expressed in this report are management, consultation those of the author alone. The views or statements expressed in this publication do not necessarily Research Contractor: represent the views of the Environment Agency and the HR Wallingford Ltd, Howbery Park, Wallingford, Oxon, Environment Agency cannot accept any responsibility for OX10 8BA, 01491 835381 such views or statements. -
AN INTERNSHIP with the US GEOLOGICAL SURVEY by Justin
ABSTRACT NAMES AND GEOGRAPHIC FEATURES: AN INTERNSHIP WITH THE U.S. GEOLOGICAL SURVEY by Justin Arthur Bedocs Place names are vital to orienting ourselves in the world. In ancient times, people must have had names for places like hunting grounds or berry groves. This act of naming roughly delineates geographic features which can be revisited and described to others, affixing an added cultural meaning to that place. Place naming has since come a long way. Official place names for the United States and its territories are managed by the United States Geological Survey (USGS), National Geospatial Technical Operations Center (NGTOC). This report details my experience working in the Geographic Names Unit. As a Pathways Career Intern, my main duties were to manage the Geographic Names Information System (GNIS), a database containing official place names for features outlined on federal topographic maps. Most of the work involved duplicate names; an issue where there are two name records for one feature, often indicating that one record is a copy and should be deleted. Sometimes the two records were not copies, and the correct locations were identified by visually analyzing historic and recent maps. The coordinates were then updated respectively in the GNIS. I gained valuable experience reading topographic maps, identifying features and managing a large database of geographic names. NAMES AND GEOGRAPHIC FEATURES: AN INTERNSHIP WITH THE U.S. GEOLOGICAL SURVEY An Internship Report Submitted to the Faculty of Miami University in partial fulfillment of the requirements for the degree of Master of Environmental Science by Justin Arthur Bedocs Miami University Oxford, Ohio 2016 Advisor: Robbyn Abbitt, MS Reader: Suzanne Zazycki, JD Reader: Mark Allen Peterson, PhD ©2016 Justin Arthur Bedocs This internship report titled NAMES AND GEOGRAPHIC FEATURES: AN INTERNSHIP WITH THE U.S. -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
Year 11 Units of Work - GEOGRAPHY Year 11 Autumn 1 Autumn 2 Spring 1 Spring 2 Summer 1 Summer 2
Year 11 Units of Work - GEOGRAPHY Year 11 Autumn 1 Autumn 2 Spring 1 Spring 2 Summer 1 Summer 2 Unit of Work Topic 3 Topic 3 Topic 6 Topic 6 Revision Revision Distinctive Landscapes Distinctive Landscapes Dynamic Development Dynamic Development Paper 1 Paper 1 Paper 2 Paper 2 + GCSE Exams + GCSE Exams Curriculum Map Landscapes Year 11 Autumn Mock Exam week Measuring development Year 11Spring Mock Exam week In class revision with particular focus on In class revision with particular focus on (Links to OCR B What is a landscape (natural and built) Topics 3,4,5,7 and human fieldwork practice What is meant by development? Paper 3 practice linked to topics 4,6,8 Paper 1. Paper 2 and 3. 9-1 GCSE) UK Landscapes (upland, lowland and glacial) – paper What is meant by uneven development? distribution and characteristics How can countries be classified by Use revision booklets, green revision guides Use revision booklets, green revision guides River Landscapes development?(AC’s, EDC’s, LIDC’s) CASE STUDY of a LIDC – Zambia and other strategies such as quick quizzes, and other strategies such as quick quizzes, AO1 Coastal Landscapes What geomorphic processes shape river Global distribution of AC’s, EDC’s, LIDC’s Location and background case study mind-maps, flash cards, case study mind-maps, flash cards, Geographical What geomorphic processes shape coastal landscapes? (Erosion, weathering, mass Economic, social, environmental and Current level of development knowledge organisers and use of past papers knowledge organisers and use of past Knowledge landscapes? (Types of erosion, weathering, movement, transportation and deposition) combined measures of development. -
Copyright Pearson Education Iii
Contents Introduction v The natural environment (Section A) Chapter 1: River environments 1 Chapter 2: Coastal environments 11 Chapter 3: Hazardous environments 21 People and their environments (Section B) Chapter 4: Economic activity and energy 31 Chapter 5: Ecosystems and rural environments 41 Chapter 6: Urban environments 50 Global issues (Section D) Chapter 7: Fragile environments 60 Chapter 8: Globalisation and migration 71 Chapter 9: Development and human welfare 81 Contents Preparing for the exam 91 Glossary Sample 95 Index 99 Copyright Pearson Education iii Geog_Rev_Guide-5thProof.indb 3 22/01/2013 13:29 Chapter 2: Coastal environments The coast as a system The coast is an open system. For example, sediment comes into the system (input) from a river delta. Waves transport the sediment or it is stored in beaches or sand dunes. Sediment may be lost to the coastal system if it moves into the open sea (output). Coastal processes are divided into marine processes (waves) and sub-aerial processes (weathering and mass movement). Waves and erosion and deposition Constructive waves Destructive waves weak tall waves with short swash long wavelength strong swash shallow wavelength gradient steep gradient waves waves h sh as wa ackw ack d) ak b g b de we ron ero st ach beach built up by (be deposition of material brought up in wash (Section A) Figure 2.1 Constructive and destructive waves Constructive waves build the beach by deposition. Destructive waves erode the beach. Their backwash Their swash is stronger than their backwash so they is stronger than their swash, so they drag material carry material up the beach and deposit it there. -
Dicionarioct.Pdf
McGraw-Hill Dictionary of Earth Science Second Edition McGraw-Hill New York Chicago San Francisco Lisbon London Madrid Mexico City Milan New Delhi San Juan Seoul Singapore Sydney Toronto Copyright © 2003 by The McGraw-Hill Companies, Inc. All rights reserved. Manufactured in the United States of America. Except as permitted under the United States Copyright Act of 1976, no part of this publication may be repro- duced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written permission of the publisher. 0-07-141798-2 The material in this eBook also appears in the print version of this title: 0-07-141045-7 All trademarks are trademarks of their respective owners. Rather than put a trademark symbol after every occurrence of a trademarked name, we use names in an editorial fashion only, and to the benefit of the trademark owner, with no intention of infringement of the trademark. Where such designations appear in this book, they have been printed with initial caps. McGraw-Hill eBooks are available at special quantity discounts to use as premiums and sales promotions, or for use in corporate training programs. For more information, please contact George Hoare, Special Sales, at [email protected] or (212) 904-4069. TERMS OF USE This is a copyrighted work and The McGraw-Hill Companies, Inc. (“McGraw- Hill”) and its licensors reserve all rights in and to the work. Use of this work is subject to these terms. Except as permitted under the Copyright Act of 1976 and the right to store and retrieve one copy of the work, you may not decom- pile, disassemble, reverse engineer, reproduce, modify, create derivative works based upon, transmit, distribute, disseminate, sell, publish or sublicense the work or any part of it without McGraw-Hill’s prior consent.