Coastal Impressions
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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. -
Name These Glacial Features 1.) 1
Name these Glacial Features 1.) 1.)____________________________________ 2.) 2.) ___________________________________ 3.) 3.)_____________________________________ 4.) 4.) ____________________________________ Name these types of Glaciers 5.) 5.)___________________________________________ 6.) 6.) __________________________________________ 7.) 7.) __________________________________________ 8.) 8.) __________________________________________ True or False 9.) __________ The terminus marks the farthest extent of a glacier. 10.) _________ An arête is a bow or amphitheater shape in a glacier. 11.) _________CO2 levels are higher during glacial episodes. 12.) _________ Methane Hydrate breaks down into H20. 13.) _________ Glaciers exist on every continent. 14.) _________ The Great Lakes were created by glaciation. 15.) _________ Calving is a process that creates icebergs. 16.) ________ Glacier National Park is in Alaska 17.) ________ Alaska has 100 glaciers. 18.) ________ 75% of the world’s glaciers are retreating. 19.) ________ A glacier can move forward and retreat at the same time. 20.) ________ Ogives are alternating wave crests and valleys that appear as dark and light bands of ice on glacier surfaces. 21.) ________ A drumlin field east of Rochester, New York is estimated to contain about 100 drumlins. Short Answer 22.) Give a general definition of the milankovitch cycles. _________________________________________________________________________________ _________________________________________________________________________________ _________________________________________________________________________________ -
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. -
The Alaska Boundary Dispute
University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at ucpress@ ucalgary.ca Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specificwork without breaching the artist’s copyright. -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
VGP) Version 2/5/2009
Vessel General Permit (VGP) Version 2/5/2009 United States Environmental Protection Agency (EPA) National Pollutant Discharge Elimination System (NPDES) VESSEL GENERAL PERMIT FOR DISCHARGES INCIDENTAL TO THE NORMAL OPERATION OF VESSELS (VGP) AUTHORIZATION TO DISCHARGE UNDER THE NATIONAL POLLUTANT DISCHARGE ELIMINATION SYSTEM In compliance with the provisions of the Clean Water Act (CWA), as amended (33 U.S.C. 1251 et seq.), any owner or operator of a vessel being operated in a capacity as a means of transportation who: • Is eligible for permit coverage under Part 1.2; • If required by Part 1.5.1, submits a complete and accurate Notice of Intent (NOI) is authorized to discharge in accordance with the requirements of this permit. General effluent limits for all eligible vessels are given in Part 2. Further vessel class or type specific requirements are given in Part 5 for select vessels and apply in addition to any general effluent limits in Part 2. Specific requirements that apply in individual States and Indian Country Lands are found in Part 6. Definitions of permit-specific terms used in this permit are provided in Appendix A. This permit becomes effective on December 19, 2008 for all jurisdictions except Alaska and Hawaii. This permit and the authorization to discharge expire at midnight, December 19, 2013 i Vessel General Permit (VGP) Version 2/5/2009 Signed and issued this 18th day of December, 2008 William K. Honker, Acting Director Robert W. Varney, Water Quality Protection Division, EPA Region Regional Administrator, EPA Region 1 6 Signed and issued this 18th day of December, 2008 Signed and issued this 18th day of December, Barbara A. -
Part III-2 Longshore Sediment Transport
Chapter 2 EM 1110-2-1100 LONGSHORE SEDIMENT TRANSPORT (Part III) 30 April 2002 Table of Contents Page III-2-1. Introduction ............................................................ III-2-1 a. Overview ............................................................. III-2-1 b. Scope of chapter ....................................................... III-2-1 III-2-2. Longshore Sediment Transport Processes ............................... III-2-1 a. Definitions ............................................................ III-2-1 b. Modes of sediment transport .............................................. III-2-3 c. Field identification of longshore sediment transport ........................... III-2-3 (1) Experimental measurement ............................................ III-2-3 (2) Qualitative indicators of longshore transport magnitude and direction ......................................................... III-2-5 (3) Quantitative indicators of longshore transport magnitude ..................... III-2-6 (4) Longshore sediment transport estimations in the United States ................. III-2-7 III-2-3. Predicting Potential Longshore Sediment Transport ...................... III-2-7 a. Energy flux method .................................................... III-2-10 (1) Historical background ............................................... III-2-10 (2) Description ........................................................ III-2-10 (3) Variation of K with median grain size................................... III-2-13 (4) Variation of K with -
Tide Simplified by Phil Clegg Sea Kayaking Anglesey
Tide Simplified By Phil Clegg Sea Kayaking Anglesey Tide is one of those areas that the more you learn about it, the more you realise you don’t know. As sea kayakers, and not necessarily scientists, we don’t have to know every detail but a simplified understanding can help us to understand and predict what we might expect to see when we are out on the water. In this article we look at the areas of tide you need to know about without having to look it up in a book. Causes of tides To understand tide is convenient to imagine the earth with an envelope of water all around it, spinning once every 24 hours on its north-south axis with the moon on a line parallel to the equator. Moon Gravity A B Earth Ocean C The tides are primarily caused by the gravitational attraction of the moon. Simplifying a bit, at point A the gravitational pull is the strongest causing a high tide, point B experiences a medium pull towards the moon, while point C has the weakest pull causing a second high tide. Because the earth spins once every 24 hours, at any location on its surface there are two high tides and two low tides a day. There are approximately six hours between high tide and low tide. One way of predicting the approximate time of high tide is to add 50 minutes to the high tide of the previous day. The sun has a similar but weaker gravitational effect on the tides. On average this is about 40 percent of that of the moon. -
Hubbard Glacier
National Park Service Park News U.S. Department of the Interior Hubbard Glacier Hubbard Glacier Fact Sheet --The Hubbard Glacier is North America’s largest tidewater glacier. It is 76 miles long, 7 miles wide, and 600 feet tall at its terminal face (350 feet exposed above the waterline and 250 feet below the waterline). --The Hubbard Glacier starts at Mt. Logan (19850 ft) in the Yukon Territory. Mt. Logan is the 2nd tallest mountain on the North American continent. --The Hubbard Glacier is currently advanc- ing (last 100 years), while most Alaskan glaciers are retreating (95%). This is not in contradiction with current global tempera- ture increases. The Hubbard Glacier will advance during times of warming climate and retreat in time of colder climates. The The Hubbard Glacier (right) and the Turner Glacier looking from Russell Fjord. current rate of advance is approximately 80 feet per year. 700 years ago – advanced to fill the entire pressure applied from the snow accumulat- --The glacier’s rate of overall forward ve- Yakutat Bay ing above. locity is much higher, but the advance is due its calving. Why do glaciers advance and retreat? --Once the ice becomes more than 150 feet thick the ice can behave plastically, and --The ice you see at the terminal face is ap- --Glaciers will always try to reach a balance start to flow under the influence of gravity. proximately 450 years old and is over 2000 between the amount of ice they gain to feet thick at some locations. the amount of ice they lose (equilibrium). -
Aerial Rapid Assessment of Hurricane Damages to Northern Gulf Coastal Habitats
8786 ReportScience Title and the Storms: the USGS Response to the Hurricanes of 2005 Chapter Five: Landscape5 Changes The hurricanes of 2005 greatly changed the landscape of the Gulf Coast. The following articles document the initial damage assessment from coastal Alabama to Texas; the change of 217 mi2 of coastal Louisiana to water after Katrina and Rita; estuarine damage to barrier islands of the central Gulf Coast, especially Dauphin Island, Ala., and the Chandeleur Islands, La.; erosion of beaches of western Louisiana after Rita; and the damages and loss of floodplain forest of the Pearl River Basin. Aerial Rapid Assessment of Hurricane Damages to Northern Gulf Coastal Habitats By Thomas C. Michot, Christopher J. Wells, and Paul C. Chadwick Hurricane Katrina made landfall in southeast Louisiana on August 29, 2005, and Hurricane Rita made landfall in southwest Louisiana on September 24, 2005. Scientists from the U.S. Geological Survey (USGS) flew aerial surveys to assess damages to natural resources and to lands owned and managed by the U.S. Department of the Interior and other agencies. Flights were made on eight dates from August Introduction 27 through October 4, including one pre-Katrina, three post-Katrina, The USGS National Wetlands and four post-Rita surveys. The Research Center (NWRC) has a geographic area surveyed history of conducting aerial rapid- extended from Galveston, response surveys to assess Tex., to Gulf Shores, hurricane damages along the Ala., and from the Gulf coastal areas of the Gulf of of Mexico shoreline Mexico and Caribbean inland 5–75 mi Sea. Posthurricane (8–121 km). -
Public Law 96-487 (ANILCA)
APPENDlX - ANILCA 587 94 STAT. 2418 PUBLIC LAW 96-487-DEC. 2, 1980 16 usc 1132 (2) Andreafsky Wilderness of approximately one million note. three hundred thousand acres as generally depicted on a map entitled "Yukon Delta National Wildlife Refuge" dated April 1980; 16 usc 1132 {3) Arctic Wildlife Refuge Wilderness of approximately note. eight million acres as generally depicted on a map entitled "ArcticNational Wildlife Refuge" dated August 1980; (4) 16 usc 1132 Becharof Wilderness of approximately four hundred note. thousand acres as generally depicted on a map entitled "BecharofNational Wildlife Refuge" dated July 1980; 16 usc 1132 (5) Innoko Wilderness of approximately one million two note. hundred and forty thousand acres as generally depicted on a map entitled "Innoko National Wildlife Refuge", dated October 1978; 16 usc 1132 (6} Izembek Wilderness of approximately three hundred note. thousand acres as �enerally depicted on a map entitied 16 usc 1132 "Izembek Wilderness , dated October 1978; note. (7) Kenai Wilderness of approximately one million three hundred and fifty thousand acres as generaJly depicted on a map entitled "KenaiNational Wildlife Refuge", dated October 16 usc 1132 1978; note. (8) Koyukuk Wilderness of approximately four hundred thousand acres as generally depicted on a map entitled "KoxukukNational Wildlife Refuge", dated July 1980; 16 usc 1132 (9) Nunivak Wilderness of approximately six hundred note. thousand acres as generally depicted on a map entitled "Yukon DeltaNational Wildlife Refuge", dated July 1980; 16 usc 1132 {10} Togiak Wilderness of approximately two million two note. hundred and seventy thousand acres as generally depicted on a map entitled "Togiak National Wildlife Refuge", dated July 16 usc 1132 1980; note. -
WATER ENVIRONMENT A3d.1 INTRODUCTION
Offshore Energy SEA APPENDIX 3d - WATER ENVIRONMENT A3d.1 INTRODUCTION A number of aspects of the water environment are reviewed below in a UK context, and for individual Regional Seas: • The major water masses and residual circulation patterns in UK seas • Density stratification (influenced principally by temperature and salinity) and frontal zones between different water masses – these represent potentially important areas for biological productivity • Tidal flows • Overall patterns of temperature and salinity • Wave climate • Ambient noise Recent assessments of changes in hydrographic conditions are summarised, based mainly on reports by DEFRA (2004a, b) and MCCIP (2007). Overall, significant anomalies and changes have been noted in sea surface temperature (SST), thermal stratification, circulation patterns, wave climate, pH and sea level – many appear to be correlated to atmospheric climate variability as described by the North Atlantic Oscillation (NAO). Larger- scale trends and process changes have also been noted in the North Atlantic (e.g. in the strength of the Gulf Stream and Atlantic Heat Conveyor (more properly characterised as the Meridional Overturning Circulation (MOC), or the Atlantic Thermohaline circulation (THC) e.g. Trumper 2005), Northern Hemisphere (Weijerman et al. 2005) and globally (IPCC 2007a). There are varying degrees of confidence in the interpretation of observed data and prediction of future trends. Finally, the specific environmental issue of eutrophication is summarised. This is an area of concern in specific geographical areas, notably the southern North Sea and various coastal and estuarine locations. A3d.2 UK CONTEXT The history of broadscale studies of North Sea circulation and hydrographic patterns (e.g. temperature and salinity distribution) was briefly reviewed in SEA 2.