Academic literature on the topic 'Beach erosion'

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Journal articles on the topic "Beach erosion"

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Takeda, Ichirou, and Tsuguo Sunamura. "Conditions for beach erosion on a barred beach." Zeitschrift für Geomorphologie 36, no. 4 (December 29, 1992): 453–64. http://dx.doi.org/10.1127/zfg/36/1992/453.

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TSUCHIYA, Yoshito. "Beach erosion control." Doboku Gakkai Ronbunshu, no. 387 (1987): 11–23. http://dx.doi.org/10.2208/jscej.1987.387_11.

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Morris, Victor F. "Florida Beach Erosion." Weatherwise 43, no. 1 (February 1990): 12–13. http://dx.doi.org/10.1080/00431672.1990.9927101.

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Kim, Hyun Dong, Shin-ichi Aoki, Nobuhisa Kobayashi, and Susumu Onaka. "THE EFFECTIVE METHOD OF BEACH NOURISHMENT PLACEMENT." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 66. http://dx.doi.org/10.9753/icce.v36.sediment.66.

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When erosion occurs, sandy beach cannot maintain the sufficient sand width and the foreshore slope becomes steeper by the frequent erosion effect. As a result, the beach is trapped in a vicious circle of becoming vulnerable by the incident waves. In order to repair or protect the erosive beach, beach nourishment can be used as a countermeasure while minimizing the environmental impacts. However, beach nourishment is not a permanent solution and requires periodic renourishment after several years. To alleviate such problem, minimizing the period of renourishment must be an economical alternative. In that respect, selecting the optimum grain size of the sand for the beach nourishment is very important. Generally, larger grain sized sand is more resistant to the erosion, thus extending the period of renourishment. In addition to selecting the optimum grain size of the sand nourishment, determining the durability as well as maintaining the familiarity of the users of the native sand should be considered.
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Lemke, Laura, and Jon K. Miller. "Role of Storm Erosion Potential and Beach Morphology in Controlling Dune Erosion." Journal of Marine Science and Engineering 9, no. 12 (December 14, 2021): 1428. http://dx.doi.org/10.3390/jmse9121428.

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Coastal erosion is controlled by two sets of factors, one related to storm intensity and the other related to a location’s vulnerability. This study investigated the role of each set in controlling dune erosion based on data compiled for eighteen historical events in New Jersey. Here, storm intensity was characterized by the Storm Erosion Index (SEI) and Peak Erosion Intensity (PEI), factors used to describe a storm’s cumulative erosion potential and maximum erosive power, respectively. In this study, a direct relationship between these parameters, beach morphology characteristics, and expected dune response was established through a classification tree ensemble. Of the seven input parameters, PEI was the most important, indicating that peak storm conditions with time scales on the order of hours were the most critical in predicting dune impacts. Results suggested that PEI, alone, was successful in distinguishing between storms most likely to result in no impacts (PEI < 69) and those likely to result in some (PEI > 102), regardless of beach condition. For intensities in between, where no consistent behavior was observed, beach conditions must be considered. Because of the propensity for beach conditions to change over short spatial scales, it is important to predict impacts on a local scale. This study established a model with the computational effectiveness to provide such predictions.
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Pao, Chun-Hung, Takaaki Uda, Yu-Hsiang Lin, and Jia-Lin Julie Chen. "BEACH EROSION ON GOLDEN BEACH IN SOUTH TAIWAN." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 46. http://dx.doi.org/10.9753/icce.v36.sediment.46.

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Golden Beach in Taiwan is a sandy beach attracting many beachgoers because of its wide sandy beach and beautiful sunset. In recent years, this beach has been eroded. The cause of the beach erosion is considered to be due to the wave-sheltering effect of the Anping Harbor breakwaters constructed 4 km north of the beach. Now the restoration of sandy beach is underway by the construction of groins as well as beach nourishment using sand procured from the downcoast deposition area. This study aims to investigate the cause of the beach erosion of this beach to work out the effective measures against beach erosion.
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Elliott, Dabney O. "THE BEACH EROSION BOARD." Coastal Engineering Proceedings 1, no. 1 (May 12, 2010): 12. http://dx.doi.org/10.9753/icce.v1.12.

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The purpose of this paper is to describe the methods by which, and the extent to which the Federal Government participates with local agencies in the control of beach erosion. The Beach Erosion Board of the Corps of Engineers is the instrumentality through which this participation is affected. However, before describing this Board, it is necessary to sketch very briefly the background of the beach erosion problem as viewed from the national standpoint. The necessity for the control of beach erosion by one means or another has no doubt been recognized from the beginning of the practice of coastal engineering in the United States. The early technical records of the Corps of Engineers contain numerous references to the mutual effects which navigation structures and the adjacent shorelines exert upon each other. As an example, chosen at random, I may mention the construction in 1874 of twelve stone groins along the shore of the State of Connecticut between Welshs Point and Indian River, and of a stone jetty at the mouth of that river in the following year, to stabilize the shoreline and to prevent the movement of sand into the navigation channel of that river.
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Brunel, Cédric, and François Sabatier. "Provence pocket beach erosion." Méditerranée, no. 108 (January 1, 2007): 77–82. http://dx.doi.org/10.4000/mediterranee.175.

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Kobayashi, Nobuhisa, and Hooyoung Jung. "Beach Erosion and Recovery." Journal of Waterway, Port, Coastal, and Ocean Engineering 138, no. 6 (November 2012): 473–83. http://dx.doi.org/10.1061/(asce)ww.1943-5460.0000147.

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Onaka, S., T. Uda, T. San-Nami, K. Miyagawa, and T. Mori. "Coastal conditions and long-term topographic changes of Tanjung Benoa Beach on Bali Island, Indonesia." IOP Conference Series: Earth and Environmental Science 1343, no. 1 (May 1, 2024): 012041. http://dx.doi.org/10.1088/1755-1315/1343/1/012041.

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Abstract Tanjung Benoa Beach on Bali Island, a globally recognized coastal resort with well-developed coral reefs, is experiencing beach erosion. This study aimed to formulate measures against the beach erosion, with a quantitative analysis of the coastal mechanisms through field observations, aerial photographs, satellite images and bathymetric data. The results indicate that the beach erosion on Tanjung Benoa Beach has occurred over time due to the longshore sediment transport, although the rate reduced by a construction of a groin. Additionally, the eroded area can be considered as a closure system of sediment transport between two groins at both ends, where accumulation and erosion of sand occur simultaneously. Based on these results, sand back pass was proposed, and its implementation plan was examined through numerical calculations for three-dimensional beach topographic changes. The numerical calculation compared a case of beach nourishment alone to adding four groins, suggesting that beach nourishment without groins is more effective for achieving the target beach width, maintenance plan efficiency and the high demand for beach uses on Tanjung Benoa Beach. This plan represents one of the few instances of sand back pass in Indonesia and promotes sustainable solutions to beach erosion, balancing beach utilization and conservation.
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Dissertations / Theses on the topic "Beach erosion"

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Olsen, Michael James. "Methodology for assessing coastal change using terrestrial laser scanning." Diss., [La Jolla] : University of California, San Diego, 2009. http://nsgl.gso.uri.edu/casg/casgy09005.pdf.

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Thesis (Ph. D.)--University of California, San Diego, 2009.
Title from first page of PDF file (viewed July 14, 2009). Available via ProQuest Digital Dissertations. Vita. Includes bibliographical references (p. 258-267).
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Bear, Alison Louise. "Erosion and Sedimentation Processes at Northern Waihi Beach." The University of Waikato, 2009. http://hdl.handle.net/10289/2783.

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The northern sector of Waihi Beach is an example of chronic erosive tendency. The sediment deficit along the area of beach fronting the seawall means that there is often no beach at high tide. This existing situation, and the various remedial options suggested, has created an emotive issue for beach residents. Accordingly, the current study was undertaken to identify and evaluate the fundamental coastal processes impacting upon the erosion at northern Waihi Beach. Methods used to investigate this problem included: beach profiling and shallow water hydrographic surveying; mapping of sediments and the distribution of bedforms on the inner shelf using side-scan sonar, identification of nearshore sediment transport pathways from sediment textural analyses; collection and analysis of nearshore wave and current data; and numerical modelling of wave refraction and sediment transport processes. A side-scan sonar survey, ground-truthed by surficial sediment analyses and underwater video and diver observations, indicated that the shallow inshore zone is characterised by a relatively featureless seabed dominated by fine sands. Large shore-normal sand ridges (η=0.4-2.5 m, λ=300-1400), with crests oriented northeast to southwest were identified between 15-30 m water depth offshore northern Waihi Beach. These very pronounced features consist of coarse megarippled (η≈0.12 m, λ≈1 m) sediment. Sediment textural analyses revealed that offshore sediments vary from fine to coarse sand, showing a seaward-coarsening progression. Beach sediments consist of predominantly fine sands, with a slight inferred fining in grain size that occurs towards the northern end of the beach. This is possibly a result of lower wave energy when subject to swell and sea waves from the north, due to sheltering in the lee of Rapitiotio Point. 80 days of wave and current data were collected offshore northern Waihi Beach, during two separate deployments in Nov/Dec 2007 and May/June 2008. The summer deployment was characterised by waves from a northeast-east origin (Hs=1.09m; Ts=7.13s). Similar conditions were exhibited during the winter deployment (Hs=0.95m; Ts=6.79s). Observed relationships between wind direction and near-bed current direction, combined with calculated sediment entrainment rates, enabled predictions of the frequency of shoreward sediment transport by bottom currents to be made. Onshore currents, associated with winds from the southwest, prevailed during the deployment period. However, observed current velocities alone were generally incapable of inducing sediment motion. Analysis suggests that wave properties are likely to govern the frequency of sediment transport in the nearshore, as their presence is required to lift sediment into suspension for dispersal by ambient background currents. Onshore movement of sediment was estimated to be ~11,800 m3/year or 2.6 m3/m. Monochromatic wave statistics measured during the field study were used to calibrate a numerical wave refraction model. The wave refraction influence of Mayor Island was found to be the major feature influencing the distribution of wave energy along the shoreline, which is likely to contribute to localised accelerated beach erosion and dune setback. Wave energy focusing at northern Waihi Beach is maximised by swell waves, resulting in greater wave heights along eroding sectors of the beach. Potential sediment transport rates were investigated. Results suggest the littoral drift direction was bi-directional at northern Waihi Beach, although net littoral drift was southeasterly during the study period. An estimated net loss of 46,200 m3/year or 10.3 m3/m was predicted for northern Waihi Beach during the present study. Longer-term drift patterns were examined using a five year record of wave data collected offshore Pukehina by Environment Bay or Plenty from 2003-2008. Similar patterns but with lower magnitudes of sediment transport were obtained, with net annual drift rates estimated to range from 1,300-58,000 m3/year. A conceptual model of nearshore sediment dynamics is proposed for Waihi Beach to identify the major factors contributing to long-term erosion in the northern sector. Approximately 115,000 m3 of sediment was estimated to be moving within the defined northern Waihi Beach littoral cell during the study period. The derived sediment budget produced a net deficit of sediment of approximately 36,000 m3/year or -8 m3/year during the year commencing November 2007. The net southeasterly littoral drift was determined the major contributor to the net erosion rate during the study period, with alongshore transport rates exceeding available supply to the beach from diabathic movement of sediment onshore. Several aspects of the erosion problem at northern Waihi Beach are recommended to be researched further to identify what coastal management options are required.
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Yeung, Hoi-yan Esther. "Beach erosion and recovery on the beaches of southeast Hong Kong Island, Hong Kong SAR, China." Click to view the E-thesis via HKUTO, 2009. http://sunzi.lib.hku.hk/hkuto/record/B42904559.

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Mason, Susan Jane. "Beach development, sediment budget and coastal erosion at Holderness." Thesis, University of Sheffield, 1985. http://etheses.whiterose.ac.uk/1811/.

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Complex relationships exist among offshore conditions, beach sediment transport and morphology, and till cliff erosion. Modelled and measured sediment transport rates established for the Holderness coast are similar to those on comparable coasts elsewhere. The direction of sediment drift depends on wave approach, and determining sediment transport rates, cliff composition and cliff retreat rates allows a sediment budget to be prepared. The beach response predicted by the sediment budget was confirmed by field observations, with budget surpluses and deficits coinciding with full and depleted beach profiles respectively. The area of deficit in the north of the study area was associated with the reduced sheltering effect of Flamborough Head on sediment drift. At most profiles, especially those with a sediment deficit, high energy waves may remove the sand veneer completely, leaving the till platform exposed. These bare till patches which elsewhere have been called ords and have been regarded as unique, were thought, in the present study,to represent a normal beach response to limited sediment supply and prevailing offshore conditions. Beach evolution was also modelled formally, the range of beach profiles exhibited on the Holderness coast being grouped into a number of distinct types, and evolution among them described and predicted by a first-order Markov model. This can be refined to provide different models for "winter" and "summer". Different modal types occur at different locations, and certain types of transitions between classes can be associated with particular ranges of wave conditions. Beach Development, Sediment Budget and Coastal Erosion at Holderness Susan J. Mason. Till cliff retreat at Holderness is extremely variable, both spatially and temporally, being influenced by beach level, energy conditions, cliff moisture content and the actions of man. The sediment transport rates, cliff retreat data, sediment budget and beach behaviour model are all essential elements of a research programme currently being undertaken to find a cheap method of protecting this coast.
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Gonzales, Jack Joseph. "Comparing UAV and Pole Photogrammetry for Monitoring Beach Erosion." Thesis, Virginia Tech, 2021. http://hdl.handle.net/10919/104997.

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Sandy beaches are vulnerable to extreme erosion during large storms, as well as gradual erosion processes over months and years. Without monitoring and adaptation strategies, erosion can put people, homes, and other infrastructure at risk. To effectively manage beach resources and respond to erosion hazards, coastal managers must have a reliable means of surveying the beach to monitor erosion and accretion. These elevation surveys typically incorporate traditional ground-based surveying methods or lidar surveys flown from large, fixed-wing aircraft. While both strategies are effective, advancements in photogrammetric technology offers a new solution for topographic surveying: Structure from Motion (SfM). Using a set of overlapping aerial photographs, the SfM workflow can generate accurate topographic surveys, and promises to provide a fast, inexpensive, and reliable method for routine beach surveying. Unmanned aerial vehicles (UAVs) are often successfully employed for SfM surveys but can be limited by poor weather ad government regulations, which can make flying difficult or impossible. To circumvent these limitations, a digital camera can be attached to a tall pole on a mobile platform to obtain aerial imagery, avoiding the restrictions of UAV flight. This thesis compares these two techniques of image acquisition for routine beach monitoring. Three surveys were conducted at monthly intervals on a beach on the central South Carolina coast, using both UAV and pole photogrammetry. While both methods use the same software and photogrammetric workflow, the UAV produced better results with far fewer processing artifacts compared to pole photogrammetry.
Master of Science
Beach environments are vulnerable to extreme erosion, especially in the face of sea level rise and large storms like hurricanes. Monitoring erosion is a crucial part of a coastal management strategy, to mitigate risk to coastal hazards like extreme erosion, storm surge, and flooding. Erosion monitoring usually involves repeated elevation surveys to determine how much sand is being lost from the beach, and where that sand is being eroded away. Within the past decade, Structure from Motion (SfM) photogrammetry, the process of deriving ground elevation maps from multiple overlapping aerial photographs, has become a common technique for repeated elevation surveys. Unmanned aerial vehicles (UAVs) are often used to gather aerial imagery for SfM elevation surveys but are limited by poor weather conditions and government flight regulations, both of which can prohibit flight. However, similar aerial photographs can be taken with a camera mounted atop a tall pole, which can be used in wider range of weather conditions and without government regulations, providing an alternative when UAV flight is not an option. This study compares these two platforms for routine beach erosion monitoring surveys, evaluating them based on performance, cost, and feasibility. The UAV system is found to be fast, affordable, and effective, while the pole photogrammetry system is heavily affected by the slow speed of surveying and processing errors that make it unusable without significant improvement.
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Foster, Duncan James. "The Morphodynamics of Motunau Beach and Management Implications." Thesis, University of Canterbury. Geography, 2010. http://hdl.handle.net/10092/4170.

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Motunau Beach is situated upon a small coastal promontory which is approximately 3 km in length. Around this promontory a complex of coastal processes are interacting. In the past there has been concern for people s property due to eroding sandstone cliffs. In response to the erosion hazard piecemeal structural solutions have been sought; however, due to their short longevity have proved inadequate. Based on regular shoreline profiling and observations in conjunction with a broad international literature base, the processes of wave refraction, cliff erosion, river mouth dynamics, and sand beach adjustment have been discussed. Sediment transport pathways have been inferred based upon the natural and human processes around the promontory and the morphological response since the 1950s. To analyse the coastal processes and morphological change at Motunau Beach a combination of qualitative and quantitative research methods have been used. The field study period of three months, July to September 2009, has focussed on the shortduration and high-frequency processes of change and nested within a broader context of coastal change since the 1950s. Initial results suggest that between the years 1950 to 1968 there was a loss of beach width on Sandy Bay of approximately 25 m. This was then followed by an increased rate of cliff erosion during the 1980s. Analysis of historical hindcast wave data since 1979 suggests the wave climate at Motunau is not distinctive from the rest of the east coast; however, the processes of wave refraction within the nearshore create a turbulent and dynamic nearshore wave environment which has implications on shoreline morphology. Results from this study indicate that nearshore sediment supplies are being exhausted by a increasing wave height of approximately 4 mm yr-1 since 1979. The turbulent wave environment of the nearshore zone at Motunau Beach is encouraging the offshore transfer of nearshore sediment supplies to a depth beyond the reworking of waves during swell condition. This has obvious implications for the long-term shoreline morphology at Motunau and shoreline protection from highintensity low frequency wave events.
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Buck, Mitchell Arthur. "Experiments and numerical model for berm and dune erosion." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 190 p, 2008. http://proquest.umi.com/pqdweb?did=1456291111&sid=6&Fmt=2&clientId=8331&RQT=309&VName=PQD.

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Whitcombe, Leslie John. "Sediment transport processes, with particular reference to Hayling Island." Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.294696.

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Schmied, Lauren. "Cross shore sediment transport and beach profile change." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 297 p, 2006. http://proquest.umi.com/pqdweb?did=1203570311&sid=4&Fmt=2&clientId=8331&RQT=309&VName=PQD.

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Figlus, Jens. "Seasonal and yearly profile changes of Delaware beaches." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 198 p, 2007. http://proquest.umi.com/pqdlink?did=1253510781&Fmt=7&clientId=79356&RQT=309&VName=PQD.

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Books on the topic "Beach erosion"

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Chrzastowski, Michael. Illinois pilot erosion-rate data study. Champaign, Ill: Illinois State Geological Survey, 1993.

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Agustina, Heni. Pedoman pengendalian kerusakan di wilayah pesisir akibat gelombang laut. Jakarta: Deputi Bidang Peningkatan Konservasi Sumberdaya Alam dan Pengendalian Kerusakan Lingkungan, Kementerian Negara Lingkungan Hidup, 2008.

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Geological Survey (U.S.), ed. West-Central Florida coast: Limited sand resources for eroding beaches. [St. Petersburg, FL]: U.S. Dept. of Interior, U.S. Geological Survey, 1997.

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Gentilini, Giorgio. Litoralis: Un contributo allo studio delle cause dell'erosione del litorale pisano : con varie notizie storiche sui fiumi Arno e Serchio. Ospedaletto: Edizioni Offset grafica, 2001.

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Riggs, Stanley R. Shoreline erosion in North Carolina. Raleigh, NC]: North Carolina Sea Grant, North Carolina State University, 2001.

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Vries, J. S. M. van Thiel de. Dune erosion during storm surges. Amsterdam: IOS Press, 2009.

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Cambers, Gillian. Sandy coast monitoring: The Dominica example (1987-1992). [Paris]: Unesco, 1994.

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Chrzastowski, Michael. Inventory of federal and state historical maps, charts, and vertical aerial photographs applicable to erosion-rate studies along the Illinois coast of Lake Michigan. Champaign, Ill: Illinois State Geological Survey, 1993.

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Rogers, Spencer M. Managing erosion on estuarine shorelines. Raleigh, NC]: North Carolina Sea Grant, North Carolina State University, 2001.

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United States. Office of the Assistant Secretary of the Army (Civil Works). Shoreline erosion and storm damages at Lake Worth Inlet, Palm Beach Harbor, Florida: Communication frrom the Acting Assistant Secretary (Civil Works), the Department of the Army, transmitting a report on a project for mitigation of shoreline erosion and storm damages caused by existing federal navigation improvements at Lake Worth Inlet, Palm Beach Harbor, Florida, pursuant to Pub. L. 104-303, sec. 101(b)(8). Washington: U.S. G.P.O., 1997.

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Book chapters on the topic "Beach erosion"

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Anthony, Edward J. "Beach Erosion." In Encyclopedia of Earth Sciences Series, 234–46. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_33.

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Anthony, Edward J. "Beach Erosion." In Encyclopedia of Earth Sciences Series, 1–13. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-48657-4_33-2.

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Hayes, Miles O., Eric Bird, Brian Greenwood, Karl F. Nordstrom, Robin Davidson-Arnott, Per Bruun, Edward J. Anthony, et al. "Beach Erosion." In Encyclopedia of Coastal Science, 140–45. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_33.

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Bird, Eric, and Nick Lewis. "Causes of Beach Erosion." In Beach Renourishment, 7–28. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09728-2_2.

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Bird, Eric, and Nick Lewis. "Responses to Beach Erosion." In Beach Renourishment, 29–39. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09728-2_3.

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Dean, R. G., T. L. Walton, J. D. Rosati, and L. Absalonsen. "Beach Erosion: Causes and Stabilization." In Coastal Hazards, 319–65. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5234-4_13.

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Montero, Guillermo García, and José L. Juanes Martí. "Beach erosion and mitigation: The case of Varadero Beach, Cuba." In Small Islands: Marine Science and Sustainable Development, 238–49. Washington, D. C.: American Geophysical Union, 1996. http://dx.doi.org/10.1029/ce051p0238.

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Ghersi, Adriana. "Capo Mele: a story-telling experimental beach in Laigueglia (sv)." In Proceedings e report, 242–49. Florence: Firenze University Press, 2020. http://dx.doi.org/10.36253/978-88-5518-147-1.24.

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The transformation of the coastal landscape assumes a significant importance, as far as global changes and erosion risks are concerned. The experience at Capo Mele to stage a new approach to the beach, managed by a smart private agent, allows more readings and new possible strategic actions. The initiative promotes the beach area as an active museum, to test and monitor new mechanisms for the use, protection and narration of landscape values, in the various aspects of adaptability, socio-cultural development and enhancement of the potential of the beach as a treasure chest of biodiversity.
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Pagán, José Ignacio, Isabel López, Luis Aragonés, and Antonio J. Tenza-Abril. "Experiences with beach nourishments on the coast of Alicante, Spain." In Proceedings e report, 441–50. Florence: Firenze University Press, 2020. http://dx.doi.org/10.36253/978-88-5518-147-1.44.

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The historical evolution of sandy beaches on the coast of Alicante (Spain) has been analysed from aerial images from 1956 to 2019. The beach nourishments carried out in the 1990s to avoid coastal damages and to improve the touristic offer were studied. Shoreline evolution and beach surface has been obtained using GIS. The change of the sediment composition, from gravel to sand, due to the fills has caused a relevant imbalance. Beach nourishments failed its main aim of avoiding the shoreline erosion, causing environmental damages to the nearby Posidonia oceanica meadows.
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Pikelj, Kristina, Petra Godec, and Blanka Cvetko Tešović. "Sedimentological consequences of Posidonia Oceanica banquette removal: Sakarun beach case study (Dugi otok, Croatia)." In Ninth International Symposium “Monitoring of Mediterranean Coastal Areas: Problems and Measurement Techniques”, 83–92. Florence: Firenze University Press, 2022. http://dx.doi.org/10.36253/979-12-215-0030-1.08.

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Removal of Posidonia oceanica banquettes from Sakarun beach (Dugi otok Island, Croatia) was a common practice to increase recreational use during the summer tourist season. The sandy part of the beach showed gradual erosion and has partially disappeared. Geological and geomorphological were conducted over nine-month period to investigate the relationship between the banquette removal and sediment loss. The results indicate that the continuous removal of sediment-laden posidonia banquette may cause a deficit in the beach sediment budget, the effects of which may not become apparent until several-year delay.
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Conference papers on the topic "Beach erosion"

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Ahrens, John P., and Edward B. Hands. "Parameterizing Beach Erosion/Accretion Conditions." In 26th International Conference on Coastal Engineering. Reston, VA: American Society of Civil Engineers, 1999. http://dx.doi.org/10.1061/9780784404119.179.

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Hayashi, Ralph M. "Beachwalls for Beach Erosion Protection." In 20th International Conference on Coastal Engineering. New York, NY: American Society of Civil Engineers, 1987. http://dx.doi.org/10.1061/9780872626003.140.

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Syamsudin, Abdul R., Yoshito Tsuchiya, and Takao Yamashita. "Beach Erosion in Kuta Beach, Bali and Its Stabilization." In 24th International Conference on Coastal Engineering. New York, NY: American Society of Civil Engineers, 1995. http://dx.doi.org/10.1061/9780784400890.195.

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Martínez, Jesús, Ricardo Alvarez, and Ignacio Alonso. "Storm Erosion on a Sandy Beach." In 22nd International Conference on Coastal Engineering. New York, NY: American Society of Civil Engineers, 1991. http://dx.doi.org/10.1061/9780872627765.198.

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Young, William, Siva Kesevan, and Yuwei Chang. "Post-Hurricane Sandy Beach Erosion Protection." In 14th Triennial International Conference. Reston, VA: American Society of Civil Engineers, 2016. http://dx.doi.org/10.1061/9780784479902.044.

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Leatherman, Stephen P. "Beach Erosion Studies on Tropical Islands." In First International Symposium on Carbonate Sand Beaches. Reston, VA: American Society of Civil Engineers, 2002. http://dx.doi.org/10.1061/40640(305)18.

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AZORAKOS, GEORGIOS, KASPER KÆRGAARD, JOSHUA A. SIMMONS, and KRISTEN D. SPLINTER. "BEACH DUNE EROSION, OBSERVATION AND MODELLING." In International Conference on Coastal Sediments 2019. WORLD SCIENTIFIC, 2019. http://dx.doi.org/10.1142/9789811204487_0104.

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SAN-NAMI, TOSHIRO, TAKAAKI UDA, KOU FURUIKE, and YUKIYOSHI HOSHIGAMI. "BEACH EROSION OF SOUTH KUJUKURI BEACH TRIGGERED BY COMPOUND ANTHROPOGENIC FACTORS." In Proceedings of the 5th International Conference on APAC 2009. World Scientific Publishing Company, 2009. http://dx.doi.org/10.1142/9789814287951_0170.

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Uda, Takaaki. "K1. BEACH EROSION ARISING FROM ANTHROPOGENIC FACTORS." In Coastal Dynamics 2009 - Impacts of Human Activities on Dynamic Coastal Processes. WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789814282475_0001.

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Takemura, Junichi, Yoichi Nakagawa, and Masanori Kawano. "BEACH EROSION CONTROL ON NIIGATA WEST COAST." In Proceedings of the 6th International Conference. WORLD SCIENTIFIC, 2013. http://dx.doi.org/10.1142/9789814412216_0145.

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Reports on the topic "Beach erosion"

1

Wise, Randall A., and S. J. Smith. Numerical Modeling of Storm-Induced Beach Erosion,. Fort Belvoir, VA: Defense Technical Information Center, March 1996. http://dx.doi.org/10.21236/ada308848.

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Smith, S. J., Mark B. Gravens, and Jane M. Smith. Monmouth Beach, New Jersey: Beach-Fill Hot Spot" Erosion Evaluation. Report 1. Physical Processes Analysis.". Fort Belvoir, VA: Defense Technical Information Center, August 1999. http://dx.doi.org/10.21236/ada367919.

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Smith, S. J., Gregory L. Williams, and Nicholas C. Kraus. Monmouth Beach, New Jersey: Beach-Fill Hot Spot" Erosion Evaluation. Report 2. Functional Design of Shore-Protection Alternatives for Beach-Fill Longevity.". Fort Belvoir, VA: Defense Technical Information Center, July 1999. http://dx.doi.org/10.21236/ada366974.

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Morang, Andrew, and Jeffrey Melton. Beach Erosion and Sediment Processes Study, North East Marina, Erie County, Pennsylvania. Fort Belvoir, VA: Defense Technical Information Center, June 2001. http://dx.doi.org/10.21236/ada396033.

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Hart, Kate, Jodi Lejeune, Rebecca Beavers, Sam Whitin, Christopher Overcash, Monique LaFrance Bartley, and Suzie Boltz. National Park Service beach nourishment guidance (second edition). National Park Service, May 2023. http://dx.doi.org/10.36967/2299256.

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Abstract:
Sandy coastal areas (including coastal dunes, beaches, and submerged intertidal and nearshore areas) are naturally dynamic ecosystems. These areas experience accretion, erosion, dune and island migration, overwash, and other processes as sediments are transported by the wind, waves, tides, and currents. If these natural physical processes are disrupted, the beach ecosystem may transform, become unstable, or disappear completely over time. Human development of coastal areas, sea level rise, and increasing frequency and intensity of coastal storms are examples of coastal change that interfere with sediment transport and therefore threaten the stability of coastal ecosystems. Beach nourishment is a nature-based engineering strategy that artificially delivers sand (a size of sediment) to a coastal ecosystem to lessen the disruption of sediment supply. Generally, beach nourishment is intended to mitigate erosion, protect infrastructure and buildings, and/or to restore habitat. The National Park Service (NPS) has produced an updated guidance manual that provides a consistent approach to beach nourishment based on sound coastal science and engineering. The goal of this updated guidance is to provide information on this method to protect and preserve the beaches and associated resources of the National Park System.
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Johnson, Bradley D. Lake Michigan: Prediction of Sand Beach and Dune Erosion for Flood Hazard Assessment. Fort Belvoir, VA: Defense Technical Information Center, August 2012. http://dx.doi.org/10.21236/ada571220.

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Wahl, Ronald E., John F. Peters, Kris McNamara, and Ira Brotman. Analysis of Reinforced Revetment Slope of Sargent Beach Erosion Protection Project on the Gulf Intracoastal Waterway. Fort Belvoir, VA: Defense Technical Information Center, March 1997. http://dx.doi.org/10.21236/ada325067.

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Martin, Thomas R., and J. B. Smith. Analysis of the Performance of the Prefabricated Erosion Prevention (P.E.P.) Reef System, Town of Palm Beach, Florida. Fort Belvoir, VA: Defense Technical Information Center, March 1997. http://dx.doi.org/10.21236/ada591267.

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Li, Honghai, Grace Maze, Kevin Conner, and John Hazelton. Sediment transport modeling at Stono Inlet and adjacent beaches, South Carolina. Engineer Research and Development Center (U.S.), December 2021. http://dx.doi.org/10.21079/11681/42501.

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This report documents a numerical modeling investigation for dredged material from nearshore borrow areas and placed on Folly Beach adjacent to Stono Inlet, South Carolina. Historical and newly collected wave and hydrodynamic data around the inlet were assembled and analyzed. The datasets were used to calibrate and validate a coastal wave, hydrodynamic and sediment transport model, the Coastal Modeling System. Sediment transport and morphology changes within and around the immediate vicinity of the Stono Inlet estuarine system, including sand borrow areas and nearshore Folly Beach area, were evaluated. Results of model simulations show that sand removal in the borrow areas increases material backfilling, which is more significant in the nearshore than the offshore borrow areas. In the nearshore Folly Beach area, the dominant flow and sediment transport directions are from the northeast to the southwest. Net sediment gain occurs in the central and southwest sections while net sediment loss occurs in the northeast section of Folly Island. A storm and a 1-year simulation developed for the study produce a similar pattern of morphology changes, and erosion and deposition around the borrow areas and the nearshore Folly Beach area.
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CORPS OF ENGINEERS WALTHAM MA NEW ENGLAND DIV. Reconnaissance Report, Local Study Cost Sharing Agreement, Shore Protection And Erosion Control Project; Nantasket Beach Shore Protection Study Hull, Massachusetts. Fort Belvoir, VA: Defense Technical Information Center, August 1993. http://dx.doi.org/10.21236/ada336748.

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