Report: Impacts of Sand Removal from and Placement in Coastal Barrier
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F!13Il-.-.; A:: It: Identification of Littoral Cells
Journal of Coastal Research 381-400 Fort Lauderdale, Florida Spring 1995 Littoral Cell Definition and Budgets for Central Southern England Malcolm J. Bray, David J. Carter and Janet M. Hooke Department of Geography University of Portsmouth Portsmouth, POI 3HE, England ABSTRACT . BRAY, M.J.; CARTER, D.J., and HOOKE, J.M., 1995. Littoral cell definition and budgets for central southern England. Journal of Coastal Research, 11(2),381-400. Fort Lauderdale (Florida), ISSN 0749 ,tllllllll,.e 0208. Differentiation of natural process units is promoted as a means of better understanding the interconnected . ~ ~ - nature of coastal systems at various scales. This paper presents a new holistic methodology for the f!13Il-.-.; a:: it: identification of littoral cells. Testing is undertaken through application to an extensive region of central ... bJLt southern England. Diverse sources of information are compiled to map 8. detailed series of local sediment circulations both at the shoreline and in the offshore zone. Cells and sub-cells are subsequently defined by thorough examination of the continuity of sediment transport pathways and by identification of boundaries where there are discontinuities. Important distinctions are made between the nature and stability of different boundaries and a classification of types is devised. Application of sediment budget analysis to major process units helps to clarify the regional significance of different sediment sources, stores and sinks. Within the study area, it is shown that sediments circulate from distinct eroding cliff sources to well defined sinks. Natural beaches are transient and dependent upon the continued functioning of supply pathways from cliff sources. Relict cells with residual circulations are identified as a consequence of interference. -
Stability Domains in Barrier Island Dune Systems J
Ecological Complexity 2 (2005) 410–430 http://www.elsevier.com/locate/ecocom Stability domains in barrier island dune systems J. Anthony Stallins * Department of Geography, Florida State University, Room 323 Bellamy Bldg. Tallahassee, FL 32306, USA Received 1 February 2005; received in revised form 12 April 2005; accepted 25 April 2005 Available online 17 October 2005 Abstract Early ecological descriptions of barrier island dune landscapes recognized the importance of biogeomorphic feedbacks and thresholds. However, these dynamics have not been formally linked to complexity theory. In this article, I develop models of dune landscape phase states, or stability domains, based on a synthesis of these prior studies and statistical analyses. Data for these analyses were obtained from compositional and topographic sampling along Sapelo Island, Georgia and South Core Banks, North Carolina. These undeveloped barrier islands are at opposite ends of a regional meteorological gradient in storm- forced overwash disturbance along the southeastern US Atlantic coast. The topography and plant functional group abundances on each island were supportive of earlier studies noting the propensity for distinct self-organizing biogeomorphic feedbacks to emerge along barrier coasts. On South Core Banks, where storm forcings of overwash are more frequent, the recovery processes initiated by burial-tolerant species may reduce topographic resistance to overwash exposure and contagion. On Sapelo Island, a greater abundance of dune-building and burial-intolerant swale species may confer a higher topographic roughness and more resistance to overwash exposure and contagion. Conceptually, the biogeomorphic modifications of overwash forcings on each island perpetuate the habitat conditions and dominant dune plant species in a weak positive feedback. -
Stochastic Dynamics of Barrier Island Elevation
Stochastic dynamics of barrier island elevation Orencio Duran´ Vinenta,1 , Benjamin E. Schafferb, and Ignacio Rodriguez-Iturbea,1 aDepartment of Ocean Engineering, Texas A&M University, College Station, TX 77843-3136; and bDepartment of Civil and Environmental Engineering, Princeton University, Princeton, NJ 08540 Contributed by Ignacio Rodriguez-Iturbe, November 11, 2020 (sent for review June 29, 2020; reviewed by Carlo Camporeale and A. Brad Murray) Barrier islands are ubiquitous coastal features that create low- a marked Poisson process with exponentially distributed marks. energy environments where salt marshes, oyster reefs, and man- The mark of a HWE is defined as the maximum water level groves can develop and survive external stresses. Barrier systems above the beach during the duration of the event and charac- also protect interior coastal communities from storm surges and terizes its size and intensity. This result opens the way for a wave-driven erosion. These functions depend on the existence of probabilistic model of the temporal evolution of the barrier/dune a slowly migrating, vertically stable barrier, a condition tied to elevation, along the lines of the stochastic model of soil moisture the frequency of storm-driven overwashes and thus barrier ele- dynamics (4). The knowledge of the transient probability dis- vation during the storm impact. The balance between erosional tribution function of barrier elevation allows the calculation of and accretional processes behind barrier dynamics is stochastic in after-storm recovery times, overwash probability and frequency, nature and cannot be properly understood with traditional con- and the average overwash transport rate driving the landward tinuous models. Here we develop a master equation describing migration of barriers. -
Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches Tiffany Roberts University of South Florida, [email protected]
University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School January 2012 Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches Tiffany Roberts University of South Florida, [email protected] Follow this and additional works at: http://scholarcommons.usf.edu/etd Part of the American Studies Commons, Geology Commons, and the Geomorphology Commons Scholar Commons Citation Roberts, Tiffany, "Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches" (2012). Graduate Theses and Dissertations. http://scholarcommons.usf.edu/etd/4216 This Dissertation is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches by Tiffany M. Roberts A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Geology College of Arts and Sciences University of South Florida Major Professor: Ping Wang, Ph.D. Bogdan P. Onac, Ph.D. Nathaniel Plant, Ph.D. Jack A. Puleo, Ph.D. Julie D. Rosati, Ph.D. Date of Approval: July 12, 2012 Keywords: barrier island beaches, beach morphodynamics, beach nourishment, longshore sediment transport, cross-shore sediment transport. Copyright © 2012, Tiffany M. Roberts Dedication To my eternally supportive mother, Darlene, my brother and sister, Trey and Amber, my aunt Pat, and the friends who have been by my side through every challenge and triumph. -
Barrier Island Migration Sea Level Rise and the Future
Barrier Island Migration stable location and absence of historic inlets in this area suggest that barrier migration may not be a These barrier islands retreated or migrated north- continuous process over timescales of a thousand ward as the ocean continued rising. There is some years or less. Further to the east, the barriers are debate about how the barriers actually moved. more mobile and one can find evidence of barrier Some research suggests that the barriers slowly island rollover processes such as old flood shoals drowned in place and then “jumped” or “skipped” in the bay that were associated with inlets that have landward to a new position coinciding with the new opened and closed naturally over the last several position of the shoreline. More recent studies indi- hundred years. cate the islands move in a more continuous process where sand is transported across the island from the ocean to the bay, allowing the island to migrate Sea Level Rise and the Future landward. There are three primary ways that sand can be transported across a barrier island: inlet Along the New York coast, sea level is not only ris- formation, overwash processes and eolian (or wind) ing, the land is also slowly sinking, or subsiding due transport. On Long Island’s south shore, the inlets to geologic processes. The rise in the water level in are actually far more important than either over- relation to the land surface due to the sinking of the washes or the wind in terms of moving sand land- land and the raising of the sea is known as relative ward and driving barrier migration. -
Field Guide for Oil Spill Response in Arctic Waters
FIELD GUIDE FOR OIL SPILL RESPONSE IN ARCTIC WATERS (SECOND EDITION, 2017) ISBN 978-82-93600-29-9 (digital, PDF) © Arctic Council Secretariat, 2017 This report is licensed under the Creative Commons Attribu- tion-NonCommercial 4.0 International License. To view a copy of the license visit http://creativecommons.org/licenses/y-nc/4.0 Suggested citation EPPR, 2017, Field Guide for Oil Spill Response in Arctic Waters (Second Edition, 2017). 443 pp. The revised second edition was funded by the Oil Spill Recovery Institute, Prince William Sound Science Center in Cordova, Alaska, as a project of EPPR. Authors E.H. Owens, Owens Coastal Consultants L.B. Solsberg, Counterspil Research Inc. D.F. Dickins, DF Dickins Associates, LLC This EPPR project was led by the United States, with contribu- tions for Arctic States, Permanent Participants, and Arctic Council Working Groups. Published by Arctic Council Secretariat This report is available as an electronic document from the Arctic Council’s open access repository: https://oaarchive.arctic-council. org/handle/11374/2100 Cover image © Xxsalguodxx – stock.adobe.com Inside cover painting “Arctic” by Christopher Walker Field Guide for Oil Spill Response in Arctic Waters (Second Edition, 2017) DISCLAIMER Nothing in the Guide shall be understood as prejudicing the legal position that any Arctic country may have regarding the determi- nation of its maritime boundaries or the legal status of any waters. Regardless of suggested response strategies and procedures shown in this Guide, it is expected that individual -
Types and Causes of Beach Erosion Anomaly Areas in the U.S. East Coast Barrier Island System: Stabilized Tidal Inlets
Middle States Geographer, 2007, 40:158-170 TYPES AND CAUSES OF BEACH EROSION ANOMALY AREAS IN THE U.S. EAST COAST BARRIER ISLAND SYSTEM: STABILIZED TIDAL INLETS Francis A. Galgano Jr. Department of Geography and the Environment Villanova University 800 Lancaster Avenue Villanova, Pennsylvania 19085 ABSTRACT: Contemporary research suggests that most U.S. beaches are eroding, and this has become an important political and economic issue because beachfront development is increasingly at risk. In fact, the Heinz Center and Federal Emergency Management Agency (FEMA) estimate that over the next 60 years, beach erosion may claim one out of four homes within 150 meters of the U.S. shoreline. This is significant because approximately 350,000 structures are located with 150 meters of the shoreline in the lower 48 states, not including densely populated coastal cities such as New York and Miami. Along the East Coast, most beaches are eroding at 1 to 1.5 meters per year. However, beach erosion is especially problematic along so-called beach erosion anomaly areas (EAAs) where erosion rates can be as much as five times the rate along adjacent beaches. Identifying and understanding these places is important because property values along U.S. East Coast barrier islands are estimated to be in the trillions of dollars, and the resultant beach erosion may also destroy irreplaceable habitat. There are a number of factors⎯natural and anthropogenic⎯that cause beaches to erode at anomalous rates. This paper will focus on the barrier island system of the U.S. East Coast, classify beach EAAs, and examine beach erosion down drift from stabilized tidal inlets because they are perhaps the most spatially extensive and destructive EAAs. -
Understanding Our Coastal Environment
Preface The South Carolina Beachfront Management Act In the Beginning The Coastal Zone Management Act of 1977 was enacted to protect our coastal resources from unwise development. This legislation served the beaches well during its first decade, but as South Carolina became a more popular tourist destination, it became apparent that the portion of the Act that dealt with beaches was inadequate. As development crept seaward, seawalls and rock revetments proliferated, damaging the public’s beach. In many areas there was no beach left at high tide. In some areas, there was no beach at low tide, either. In 1988 and again in 1990, South Carolina’s legislators took action and amended and strengthened the Coastal Zone Management Act. The resulting Beachfront Management Act protects South Carolina’s sandy shores by increasing the state’s jurisdiction and encouraging development to move landward. South Carolina’s Beachfront Jurisdiction To find the boundaries of this jurisdiction, staff from the Office of Ocean and Coastal Resource Management must first locate the baseline, which is the crest of the primary oceanfront sand dune. Where there are no dunes, the agency uses scientific methods to determine where the natural dune would lie if natural or man-made occurrences had not interfered with nature’s dune building process. The setback line is the most landward boundary and is measured from the baseline. To find the depth of the setback line, the beach’s average annual erosion rate for the past forty years is calculated and multiplied by forty. For example, if the erosion rate is one foot per year, the results will be a setback line that stretches forty feet from the baseline. -
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. -
Fluvial Sediment Management
Climate Change Adaptation Technologies for Water A practitioner’s guide to adaptation technologies for increased water sector resilience WATER ADAPTATION TECHNOLOGY BRIEF Fluvial sediment management Challenge: Sea level rise Adaptation response: Accommodation and management Description Fluvial sediment management is the holistic management of sediment supply from rivers to the coast, taking the full range of human activities at the river basin level into account. Sediment transported by rivers makes up 95% of the sediment entering the ocean, with an annual discharge of 15-20 billion tonnes (Syvitski et al. 2003; Milliman and Mei-e 1995). Human activities can both increase and reduce this sediment supply. However, the general reduction of fluvial sediment supply, particularly due to sediment trapping by dams, is a major global challenge. Many of the world's rivers have experienced a dramatic decrease in sediment supply over the past few decades (Walling 2006). Consequently, downstream coastal areas often suffer major sediment deficits, with associated erosion, inundation and flooding. Implementation There is no standard approach for fluvial sediment management, but a clear understanding of factors affecting coastal sediment supply for a river basin is a key prerequisite. In some cases, the decline of larger coastal areas due to decreasing fluvial sediment supply and geological sediment compaction is much more significant than global sea level rise, hence fluvial sediment management awareness is of vital importance (Milliman and Mei-e 1995). Coastal areas suffering from river management decisions that are difficult to reverse may need to focus on management measures such as hard-engineering structures and beach nourishment. However, fluvial sediment management should be considered in all new management decisions made at the river basin level to get a holistic view of the entire river basin and downstream coastline. -
BARRIER ISLAND STATUS REPORT Fiscal Year 2020 Annual Plan
BARRIER ISLAND STATUS REPORT Fiscal Year 2020 Annual Plan In compliance with Act 297 of the 2006 Regular Legislative Session, the Coastal Protection and Restoration Authority (CPRA) provides this barrier island status report as part of the Annual Plan document, which will be submitted to each member of the Louisiana Legislature. The current Barrier Island Status report is available electronically at the CPRA website. Please visit www.coastal.LA.gov to download and review the full report. A summary of the report is provided below. CONSTRUCTED PROJECTS The coastlines of the modern Mississippi River delta plain are bordered by numerous barrier islands from Raccoon Island in the west to Hewes Point in the northern Chandeleur Islands (Figure 1). These barrier islands could be grouped to represent fragmented remnants of distal extremities of several major delta lobes and headlands: to identify these barrier islands with their respective delta lobes they have been grouped from west to east as the Early Lafourche Delta System, Late Lafourche Delta System, Modern Delta System, and the St. Bernard Delta System. The back- barrier lagoons are connected to the Gulf of Mexico by approximately 25 tidal inlets which separate these barrier islands from each other and allow the exchange of diurnal tides. Figure 1: Location of barrier islands belonging to Early Lafourche, Late Lafourche, Modern, and St. Bernard barrier island systems in Louisiana The restoration of Louisiana’s barrier islands and barrier island systems has been a priority for a number of restoration programs over the past several decades and over 40 barrier island projects have been constructed to date (including 13 in the Early Lafourche Delta System, 18 in the Late Lafourche Delta System, 9 in the Modern Delta System, and 2 in the St. -
Chapter One the North Carolina Coast
11 Chapter One The North Carolina Coast 12 THE ECOLOGY Visitors to the North Carolina coast might well think that barrier islands and their beaches are the heart of the coastal area. They are, after all, the center of activity for thousands of people every summer day. An aerial photograph of the coast tells a different story, though: the islands appear to be only a slender, slightly bowed, ribbon in the midst of an enormous sea. Water domi- nates the image, an image that is the key to understand- ing North Carolina’s coastal ecosystem. The Atlantic Ocean, too wide for all of it to fit into the frame of the photograph, has an equal amount of influence in shaping the lands, waters, plants and animals of the coastal area. Wind, waves, and tides – all affected by (and affecting) the huge body of water – are constantly at work, shaping the size and location of barrier islands and inlets, determining what types of plants will grow where. For example, just wind-borne salt significantly affects how maritime trees, and thus the shape of entire forests, develop. Climate, which the ocean affects through the temperature of water currents, in turn influences the types of plants and animals found along the coast. The rising and falling of tides affect not only the types of organisms found on a beach and the specific places where they can survive, but the types of species found behind the barrier islands, in the sounds, as well. 13 THE ECOLOGY This leads to the other half of that watery photograph - the estuarine system.