Shedding Light on Our Estuary & Our Economy
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Coastal Erosion - Orrin H
COASTAL ZONES AND ESTUARIES – Coastal Erosion - Orrin H. Pilkey, William J. Neal, David M. Bush COASTAL EROSION Orrin H. Pilkey Program for the Study of Developed Shorelines, Division of Earth and Ocean Sciences, Duke University, Durham, NC, U.S.A. William J. Neal Department of Geology, Grand Valley State University, Allendale, MI, USA. David M. Bush Department of Geosciences, State University of West Georgia, Carrollton, GA, USA. Keywords: erosion, shoreline retreat, sea level rise, barrier islands, beach, coastal management, shoreline armoring, seawalls, sand supply Contents 1. Introduction 2. Causes of Erosion 2.1. Sea Level Rise 2.2. Sand Supply 2.3. Shoreline Engineering 2.4. Wave Energy and Storm Frequency 3. "Special" Cases 4. Solutions to Coastal Erosion 5. The Future Glossary Bibliography Biographical Sketches Summary Almost all of the world’s shorelines are retreating in a landward direction—a process called shoreline erosion. Sea level rise and the reduction of sand supply to the shoreline by damming of rivers, armoring of shorelines and the dredging of navigation channels are among the major causes of shoreline retreat. As sea levels continue to rise, sometimesUNESCO enhanced by subsidence caused – byEOLSS oil and water extraction, global erosion rates should increase in coming decades. Three response alternatives are available to "solve" the erosionSAMPLE problem. These are cons tructionCHAPTERS of seawalls and other engineering structures, beach nourishment and relocation or abandonment of buildings. No matter what path is chosen, response to the erosion problem is costly. 1. Introduction Coastal erosion is a major problem for developed shorelines everywhere in the world. Such erosion is regarded as a coastal hazard and is a common focus of local and national coastal management. -
Biogeography of the Blue Crab Fishery, Barataria Estuary, Louisiana. Eugene Jaworski Louisiana State University and Agricultural & Mechanical College
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1971 Biogeography of the Blue Crab Fishery, Barataria Estuary, Louisiana. Eugene Jaworski Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Jaworski, Eugene, "Biogeography of the Blue Crab Fishery, Barataria Estuary, Louisiana." (1971). LSU Historical Dissertations and Theses. 1929. https://digitalcommons.lsu.edu/gradschool_disstheses/1929 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. 71-20,601 JAWORSKI, Eugene, 1941- BIOGEOGRAPHY OF THE BLUE CRAB FISHERY, BARATARIA ESTUARY, LOUISIANA. The Louisiana State University and Agricultural and Mechanical College, Ph.D., 1971 Ecology University Microfilms, A XEROX Company, Ann Arbor, Michigan THIS DISSERTATION HAS BEEN MICROFILMED EXACTLY AS RECEIVED BIOGEOGRAPHY OF THE BLUE CRAB FISHERY, BARATARIA ESTUARY, LOUISIANA A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography and Anthropology by Eugene Jaworski B.S., University of Wisconsin, Madison, 1966 January, 1971 ACKNOWLEDGMENT Sincere gratitude Is extended to Dr. William G. Mclntire, chairman of the dissertation committee, whose guidance and understanding made the project possible. Special thanks go to Dr. Jack R. Van Lopik, for arranging financial support through Louisiana State University's Sea Grant Program. -
Coastal Land Loss and Wktlanb Restoration
COASTAL LAND LOSS AND WKTLANB RESTORATION tSI R. E. Turner estuaryare causallyrelated to the landlosses this sealevel ri se,climate change~, soil type,geomorphic century." I then comparethe strengthof this frameworkand age, subsidence or tnanagement. hypothesisto someof theother hypothesized causes of land loss on this coast, There are laboratoryand Four Hypotheses small-scale field trials that support various hypotheses,It seemsto me thatthe mostreliable Four hypothesesabout the causes of indirect interpretationsare basedon what happensin the wetlandlosses in BaratariaBay will be addressed field, andnot on the resultsof computermodels, here adapted from Turner 1997!: laboratorystudies or conceptualdiagrams. H l. i ct n ences of The test results discussed herein are derived t !tin oil banks v d solelyfrom data derived at a landscapescale. The 'ori of 1 loss sin h data set is restricted to a discussion of the Barataria watershed. This watershed is a significant H2. componentof theLouisiana coastal zorie 14,000 lv ha!and there are a varietyof habitatdata available i tl on it. Its easternboundary is the MississippiRiver from whichoccasional overflowing waters are v n.vi hypothesizedto deliver enoughsediinents and on 1 v tno I freshwaterto significantlyinfluence the balanceof rit f i land lossor gain in the receivingwatershed, and whosere-introduction would restore the estuary's wetlands. Improvingour understandingof the H4. w rin si ecologicalprocesses operating in this watershed h ' ' of mightassist in the managementof others. The effect of geologicalsubsidence and sea DIrect and Indirect Causes of Wetland Loss level rise are not included in this list because both factorshave remained relatively stablethis century Wetlandloss is essentiallythe same as land loss when the land-loss rates rose and fell, Local on thiscoast Baurnann and Turner 1990!. -
Mississippi River Delta Basinn
2009 MMiissssiissssiippppii RRiivveerr DDeellttaa BBaassiinn Characterization Report Louisiana State Reservoir Priority and Development Program BASIN CHARACTERIZATION REPORT FOR THE MISSISSIPPI RIVER DELTA BASIN The Louisiana Department of Transportation and Development (DOTD) is responsible for reviewing and prioritizing proposed reservoir projects for which State of Louisiana (State) funding is being sought, and then recommending projects to the State Legislature. To support reservoir project review, prioritization, and recommendation efforts, DOTD has prepared characterization reports of water resources conditions in each of the nine principal surface water Report Topics Page basins in the State. These characterization reports provide an overview of water uses, Basin Overview ...................................2 needs, and concerns, and can be used by applicants for State funding, and by State Land Use and Legal Entities ...................4 agencies as they evaluate the applications. The basin characterization reports also Physiographic and Climatic contain extensive references that interested parties can use to find more information Information ........................................5 from Federal, State, and local agencies or other sources. The reports represent a Water Use .........................................6 “snapshot” of conditions in early 2009 (or when the references cited in the reports Surface Water ....................................9 were published). Groundwater ....................................13 Flooding ..........................................16 -
Coastal Processes Study at Ocean Beach, San Francisco, CA: Summary of Data Collection 2004-2006
Coastal Processes Study at Ocean Beach, San Francisco, CA: Summary of Data Collection 2004-2006 By Patrick L. Barnard, Jodi Eshleman, Li Erikson and Daniel M. Hanes Open-File Report 2007–1217 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2007 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Barnard, P.L.., Eshleman, J., Erikson, L., and Hanes, D.M., 2007, Coastal processes study at Ocean Beach, San Francisco, CA; summary of data collection 2004-2006: U. S. Geological Survey Open-File Report 2007- 1217, 171 p. [http://pubs.usgs.gov/of/2007/1217/]. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Executive Summary of Major Findings..................................................................................................................................1 Chapter 2 - Beach Topographic Mapping..............................................................................................................1 -
COASTAL LAND LOSS in FLORIDA Ralph R
COASTAL LAND LOSS IN FLORIDA Ralph R. Clark1 Abstract Florida has approximately 593 miles of shoreline fronting on the Atlantic Ocean and Straits of Florida and approximate ly 673 miles of shoreline fronting on the Gulf of Mexico with an additional 5,000 miles of bay and estuary shoreline (U.S. Army Corps of Engineers, 1971). Of a statewide total of 818.9 miles of open coast sandy beaches, 337.2 miles or 41.2 percent of the beaches are identified as erosion problem areas. These erosion problem areas include those beaches with a high erosion rate or recent significant erosion conditions, those beaches with a moderate or low erosion rate, but with a narrow width fronting a highly developed area, and those restored beaches with an active maintenance nourishment pro gram. Of these erosion problem areas, 217.8 miles or 26.6 percent of the statewide beach length, are areas of critical erosion, that is, segments of the shoreline where substantial development or recreation interests are threatened by the erosion processes. On a shorewide basis the Atlantic Ocean beaches of Florida typically have historical erosion rates of between 0 and -3 feet per year, while the Gulf of Mexico beaches typically have historical erosion rates of between 0 and -2 feet per year. Many of the problem areas have shoreline erosion rates in the magnitude of between -3 and -5 feet per year. The most extreme erosion rates are occurring along the southern portion of St. Joseph Peninsula at Cape San Bias where the annual shoreline recession exceeds -20 feet. -
Managing the Anthropocene Marine Transgression to the Year 2100 and Beyond in the State of Florida U.S.A
Climatic Change (2015) 128:85–98 DOI 10.1007/s10584-014-1301-2 Managing the Anthropocene marine transgression to the year 2100 and beyond in the State of Florida U.S.A. Randall W. Parkinson & Peter W. Harlem & John F. Meeder Received: 21 February 2014 /Accepted: 25 November 2014 /Published online: 10 December 2014 # Springer Science+Business Media Dordrecht 2014 Abstract We simulate the vulnerability of all 35 Florida coastal counties to the ongoing Anthropocene marine transgression using a bathtub model unconstrained by the artificial end date of year 2100. Our projections are based upon the association between rising sea level and atmospheric temperature; a 2.3 m rise per each 1 °C increase (Levermann et al., Proc Natl Acad Sci 10.1073/pnas.1219414110, 2013). Results are organized into seven regions based upon an assessment of hypsographic and geologic attributes. Each represents an area of common vulnerability characterized in this study as high (10 to 29 % average land loss), higher (15 to 77 % average land loss), and highest (43 to 95 % average land loss). This regional approach is designed to facilitate the implementation of effective adaptation activities by providing a logical basis for establishing or re-enforcing collaboration based upon a common threat and the utility of shared technical and financial resources. The benefits of a regional perspective in formulating an actionable response to climate change have already been demonstrated in south Florida. It is our intent to facilitate regional adaptation activities in other parts of the state and adjacent southern and southeastern seaboard. 1 Introduction The State of Florida is especially vulnerable to climate change and concomitant sea level rise. -
NATURAL DEFENSES in ACTION HARNESSING NATURE to PROTECT OUR COMMUNITIES Copyright © 2016 National Wildlife Federation
NATURAL DEFENSES IN ACTION HARNESSING NATURE TO PROTECT OUR COMMUNITIES Copyright © 2016 National Wildlife Federation Suggested citation: Small-Lorenz, S.L., B. A. Stein, K. Schrass, D.N. Holstein, and A.V. Mehta. 2016. Natural Defenses in Action: Harnessing Nature to Protect Our Communities. Washington, DC: National Wildlife Federation. Natural Defenses in Action is available online at: www.nwf.org/nature-in-action Cover photo: Oystercatchers, Jamaica Bay, New York City. Photo: Don Riepe/ALS National Wildlife Federation 1990 K Street NW Washington, DC 20006 www.nwf.org NATURAL DEFENSES IN ACTION HARNESSING NATURE TO PROTECT OUR COMMUNITIES Stacy L. Small-Lorenz, Bruce A. Stein, Karl Schrass, D. Nicole Holstein, and Avalon V. Mehta Dunes, Stone Harbor, NJ. Photo: Stacy Small-Lorenz/NWF NATURAL DEFENSES IN ACTION | ii CONTENTS CONTENTS ...................................................................................... iii EXECUTIVE SUMMARY ..................................................................... 1 NATURAL DEFENSES IN ACTION ........................................................ 2 Mounting Risks, Increasing Losses ....................................................................................... 2 Using Nature to Better Protect Communities ............................................................................ 3 What Are Natural Defenses? ............................................................................................. 4 HIGHLIGHTING WHAT WORKS: PROFILES OF RESILIENCE ALLIES ......... 7 Discouraging -
Relationship Between Growth Faults, Subsidence, and Land Loss: an Example from Cameron Parish, Southwestern Louisiana, USA
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/340069701 Relationship between Growth Faults, Subsidence, and Land Loss: An Example from Cameron Parish, Southwestern Louisiana, USA Article in Journal of Coastal Research · March 2020 DOI: 10.2112/JCOASTRES-D-19-00108.1 CITATION READS 1 257 1 author: Raphael Gottardi University of Louisiana at Lafayette 41 PUBLICATIONS 136 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Basin Analysis View project All content following this page was uploaded by Raphael Gottardi on 23 March 2020. The user has requested enhancement of the downloaded file. Journal of Coastal Research 00 0 000–000 Coconut Creek, Florida Month 0000 Relationship between Growth Faults, Subsidence, and Land Loss: An Example from Cameron Parish, Southwestern Louisiana, USA Matthew O’Leary and Raphael Gottardi* School of Geosciences University of Louisiana at Lafayette Lafayette, LA 70504, U.S.A. ABSTRACT O’Leary, M. and Gottardi, R., 0000. Relationship between growth faults, subsidence, and land loss: An example from Cameron Parish, Southwestern Louisiana, USA. Journal of Coastal Research, 00(0), 000–000. Coconut Creek (Florida), ISSN 0749-0208. This study investigates the relationship between faulting, subsidence, and land loss in coastal Louisiana. A methodology that integrates three-dimensional (3D) seismic data, well logs, high-resolution topographic mapping (LIDAR), and historical aerial photography is successfully developed to identify fault-related geomorphic changes in southwestern Louisiana’s Chenier Plain. Analysis of a 3D seismic survey and well logs reveals the presence of 10 normal faults that form an east-west graben in the middle of the study area. -
Download File
Hazard Mitigation Technical Assistance Program Contract No. EMW-2000-CO-0247 Task Order 415 Hurricane Katrina Rapid Response Wind Water Line (WWL) Data Collection – Louisiana FEMA-1603-DR-LA Final Report June 9, 2006 Submitted to: Federal Emergency Management Agency Region IV Atlanta, GA Prepared by: URS Group, Inc. 200 Orchard Ridge Drive Suite 101 Gaithersburg, MD 20878 FOR PUBLIC RELEASE HMTAP Task Order 415 June 9, 2006 Table of Contents Abbreviations and Acronyms------------------------------------------------------------------------------- iii Glossary of Terms -------------------------------------------------------------------------------------------- iv Background------------------------------------------------------------------------------------------------------1 Overview of Impacts in Louisiana--------------------------------------------------------------------------3 Purpose---------------------------------------------------------------------------------------------------------11 Methodology---------------------------------------------------------------------------------------------------15 Findings and Observations --------------------------------------------------------------------------------25 Conclusion -----------------------------------------------------------------------------------------------------31 List of Figures Figure 1: Hurricane Katrina Storm Track-----------------------------------------------------------------1 Figure 2: FEMA-1603-DR-LA Disaster Declaration ---------------------------------------------------5 -
Mercury Bioaccumulation in Estuarine Food Webs
Ecological Applications, 22(2), 2012, pp. 606–623 Ó 2012 by the Ecological Society of America Mercury bioaccumulation in estuarine food webs 1,2,4 3 BRIAN FRY AND MATTHEW M. CHUMCHAL 1Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, Louisiana 70803 USA 2Australian Rivers Institute, Griffith University, Nathan Campus, Kessels Road, Queensland 4121 Australia 3Biology Department, Texas Christian University, Fort Worth, Texas 76129 USA Abstract. We tested for unintended mercury contamination problems associated with estuarine floodplain restoration projects of the Louisiana coastal zone, USA. Barataria Bay and Breton Sound are two neighboring deltaic estuaries that were isolated by levees from the Mississippi River about 100 years ago. These estuaries recently have been reconnected to the nutrient-rich Mississippi River, starting major river diversion (input) flows in 1991 for Breton Sound and in 2004 for Barataria Bay. We collected .2100 fish over five years from 20 stations in these estuaries to test two hypotheses about Hg bioaccumulation: (H1) Background Hg bioaccumulation in fish would be highest in low-salinity upper reaches of estuaries, and (H2) recent river inputs to these upper estuarine areas would increase Hg bioaccumulation in fish food webs. For H1, we surveyed fish Hg concentrations at several stations along a salinity gradient in Barataria Bay in 2003–2004, a time when this estuary lacked strong river inputs. Results showed that average Hg concentrations in fish communities were lowest (150 ng/g dry mass) in higher salinity areas and ;2.43 higher (350 ng/g) in low-salinity oligohaline and freshwater upper reaches of the estuary. -
Final Determination of the U.S
FINAL DETERMINATION OF THE U.S. ENVIRONMENTAL PROTECTION AGENCY'S ASSISTANT ADMINISTRATOR FOR EXTERNAL AFFAIRS CONCERNING THE BAYOU AUX CARPES SITE IN JEFFERSON PARISH, LOUISIANA PURSUANT TO SECTION 404(C) OF THE CLEAN WATER ACT TABLE OF CONTENTS Page I. Introduction 11. Background and History 3 A. The project B. Litigation C. 404(c) proceedings 111. Description of the Site 9 IV. Ecological Values Associated With Site 11 A. Contribution to Barataria Bay Estuary B. Fishery values C. Wildlife values D. Water Retention and Pol 1ution Fi1 teri ng Values E . Recreat ion Val ues F . Concl usion V. Unacceptable Adverse Impacts 15 A. Impacts to Shell fish Beds & Fishery Areas B. Impacts to Wildlife Values C. Impacts to Water Retention & Pollution Filtering Values 0. Impacts to Recreation E. Impacts to the Barataria Unit of the Jean Lafitte National Historical Park F. Cumulative Impacts VI. A Discussion of the Report Prepared by Steimle and Associates, 2 0 Inc. on Behalf of the Property Owners VII. Restriction on the Use of the Bayou Aux Carpes Site for - Specification as a Disposal Site I. Introduction Under Section 404(c) of the Clean Water Act (CWA, 33 U.S.C. 1251 et seq), the Administrator of the Environme~tal Protectior! Agency (EPA) is authFized to prohibit the specification (including withdrawal of specification) of any defined area as a disposal site, and he is authorized to deny or restrict the use of any defined area for specification (including the withdrawal of speci- fication) as a disposal site, whenever he determines, after notice and oppor- tunity for publ ic hearing, that the discharge of dredged or fill materials into such area will have an unacceptable adverse effect on municipal water supplies, shellfish beds and fishery areas (including spawning and breediny areas), wildlife, or recreational areas.