Breakwater Design
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Pulse-To-Pulse Coherent Doppler Measurements of Waves and Turbulence
1580 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 16 Pulse-to-Pulse Coherent Doppler Measurements of Waves and Turbulence FABRICE VERON AND W. K ENDALL MELVILLE Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California (Manuscript received 7 August 1997, in ®nal form 12 September 1998) ABSTRACT This paper presents laboratory and ®eld testing of a pulse-to-pulse coherent acoustic Doppler pro®ler for the measurement of turbulence in the ocean. In the laboratory, velocities and wavenumber spectra collected from Doppler and digital particle image velocimeter measurements compare very well. Turbulent velocities are obtained by identifying and ®ltering out deep water gravity waves in Fourier space and inverting the result. Spectra of the velocity pro®les then reveal the presence of an inertial subrange in the turbulence generated by unsteady breaking waves. In the ®eld, comparison of the pro®ler velocity records with a single-point current measurement is satisfactory. Again wavenumber spectra are directly measured and exhibit an approximate 25/3 slope. It is concluded that the instrument is capable of directly resolving the wavenumber spectral levels in the inertial subrange under breaking waves, and therefore is capable of measuring dissipation and other turbulence parameters in the upper mixed layer or surface-wave zone. 1. Introduction ence on the measurement technique. For example, pro- ®ling instruments have been very successful in mea- The surface-wave zone or upper surface mixed layer suring microstructure at greater depth (Oakey and Elliot of the ocean has received considerable attention in re- 1982; Gregg et al. 1993), but unless the turnaround time cent years. -
Felixstowe Central and South
Management Responsibilities SCDC: Fel 19.1 to Fel 19.3 SCDC Assets: Fel 19.1 Reinforced concrete block revetment with groynes, rock armour revetment in front of concrete wall, two fishtail breakwaters Fel 19.2 Concrete seawall with rock groynes, concrete splash wall, mass concrete seawall with promenade, timber groynes with concrete cladding Fel 19.3 Mass concrete sea wall with promenade, timber groynes with concrete cladding EA: Fel 19.4 to Fel 20.1 (with flood wall responsibility in SCDC frontages) EA Assets: Fel 19.2 / 19.3 Secondary flood wall Fel 19.4 Manor Terrace sea wall, concrete block-work revetment with toe piling, Landguard Common sea wall with concrete apron SMP Information Area vulnerable to flood risk: Approx. 7,017,000m² No. of properties vulnerable to flooding: 1071 Area vulnerable to erosion: Approx. 640,000m² (2105 prediction – no defences) No. of properties vulnerable to erosion: 111 Vulnerable infrastructure / assets: Felixstowe Leisure Centre, Bartlet Hospital, Felixstowe Docks, Martello Tower, Landguard caravan park, Harwich Harbour Ferry, Landguard Common, Landguard Fort, Orwell Estuary, Stour Estuary SMP Objectives To improve Felixstowe as a viable commercial centre and tourist destination in a sustainable manner; To protect the port of Felixstowe and provide opportunities for its development; To develop and maintain the Blue Flag beach; To maintain flood protection to residential properties; To maintain a high standard of ongoing defence to the area; To maintain existing facilities essential in supporting ongoing regeneration; To integrate maintenance of coastal defence, while promoting sustainable development of the hinterland; To maintain the historical heritage of the frontage; To maintain biological and geological features of Landguard Common SSSI in a favourable condition. -
URBAN COASTAL FLOOD MITIGATION STRATEGIES for the CITY of HOBOKEN & JERSEY CITY, NEW JERSEY by Eleni Athanasopoulou
©[2017] Eleni Athanasopoulou ALL RIGHTS RESERVED URBAN COASTAL FLOOD MITIGATION STRATEGIES FOR THE CITY OF HOBOKEN & JERSEY CITY, NEW JERSEY By Eleni Athanasopoulou A dissertation submitted to the Graduate School- New Brunswick Rutgers, The State University of New Jersey In partial fulfillment of requirements For the degree of Doctor of Philosophy Graduate Program in Civil and Environmental Engineering Written under the direction of Dr. Qizhong Guo And approved by New Jersey, New Brunswick January 2017 ABSTRACT OF THE DISSERTATION URBAN COASTAL FLOOD MITIGATION STRATEGIES FOR THE CITY OF HOBOKEN & JERSEY CITY, NEW JERSEY by ELENI ATHANASOPOULOU Dissertation Director: Dr. Qizhong Guo Coastal cities are undeniably vulnerable to climate change. Coastal storms combining with sea level rise have increased the risk of flooding and storm surge damage in coastal communities. The communities of the City of Hoboken and Jersey City are low-lying areas along the Hudson River waterfront and the Newark Bay/Hackensack River with little or no relief. Flooding in these areas is a result of intense precipitation and runoff, tides and/or storm surges, or a combination of all of them. During Super-storm Sandy these communities experienced severe flooding and flood-related damage as a result of the storm surge. ii Following the damage that was created on these communities by flooding from Sandy, this research was initiated in order to develop comprehensive strategies to make Hoboken and Jersey City more resilient to flooding. Commonly used flood measures like storage, surge barrier, conveyance, diversion, pumping, rainfall interception, etc. are examined, and the research is focused on their different combination to address different levels of flood risk at different scales. -
Fire Island—Historical Background
Chapter 1 Fire Island—Historical Background Brief Overview of Fire Island History Fire Island has been the location for a wide variety of historical events integral to the development of the Long Island region and the nation. Much of Fire Island’s history remains shrouded in mystery and fable, including the precise date at which the barrier beach island was formed and the origin of the name “Fire Island.” What documentation does exist, however, tells an interesting tale of Fire Island’s progression from “Shells to Hotels,” a phrase coined by one author to describe the island’s evo- lution from an Indian hotbed of wampum production to a major summer resort in the twentieth century.1 Throughout its history Fire Island has contributed to some of the nation’s most important historical episodes, including the development of the whaling industry, piracy, the slave trade, and rumrunning. More recently Fire Island, home to the Fire Island National Seashore, exemplifies the late twentieth-century’s interest in preserving natural resources and making them available for public use. The Name. It is generally believed that Fire Island received its name from the inlet that cuts through the barrier and connects the Great South Bay to the ocean. The name Fire Island Inlet is seen on maps dating from the nineteenth century before it was attributed to the barrier island. On September 15, 1789, Henry Smith of Boston sold a piece of property to several Brookhaven residents through a deed that stated the property ran from “the Head of Long Cove to Huntting -
The Influence of Groynes of the River Oder on Larval Assemblages Of
Hydrobiologia (2018) 819:177–195 https://doi.org/10.1007/s10750-018-3636-6 PRIMARY RESEARCH PAPER Human impact on large rivers: the influence of groynes of the River Oder on larval assemblages of caddisflies (Trichoptera) Edyta Buczyn´ska . Agnieszka Szlauer-Łukaszewska . Stanisław Czachorowski . Paweł Buczyn´ski Received: 17 June 2017 / Revised: 28 April 2018 / Accepted: 30 April 2018 / Published online: 9 May 2018 Ó The Author(s) 2018 Abstract The influence of groynes in large rivers on assemblages. The distribution of Trichoptera was caddisflies has been poorly studied in the literature. governed inter alia by the plant cover and the amount Therefore, we carried out an investigation on the of detritus, and consequently, the food resources. 420-km stretch of the River Oder equipped with Oxygen, nitrates, phosphates and electrolytic conduc- groynes. At 29 stations, we caught caddisflies in four tivity were important as well. Groynes have had habitats: current sites, groyne fields, riverine control positive effects for caddisflies—not only those in the sites without groynes and in the river’s oxbows. We river itself, but also those in its valley. They can found that groyne construction increased species therefore be of significance in river restoration richness, diversity, evenness, and altered the structure (although originally they served other purposes), of functional groups into more diversified and sus- especially with respect to the radically transformed tainable ones compared to the control sites. The ecosystems of large rivers. groyne field fauna is similar to that of natural lentic habitats, but its composition is largely governed by the Keywords Trichoptera Á Species assemblages Á presence of potential colonists in the nearby oxbows. -
Coastal and Ocean Engineering
May 18, 2020 Coastal and Ocean Engineering John Fenton Institute of Hydraulic Engineering and Water Resources Management Vienna University of Technology, Karlsplatz 13/222, 1040 Vienna, Austria URL: http://johndfenton.com/ URL: mailto:[email protected] Abstract This course introduces maritime engineering, encompassing coastal and ocean engineering. It con- centrates on providing an understanding of the many processes at work when the tides, storms and waves interact with the natural and human environments. The course will be a mixture of descrip- tion and theory – it is hoped that by understanding the theory that the practicewillbemadeallthe easier. There is nothing quite so practical as a good theory. Table of Contents References ....................... 2 1. Introduction ..................... 6 1.1 Physical properties of seawater ............. 6 2. Introduction to Oceanography ............... 7 2.1 Ocean currents .................. 7 2.2 El Niño, La Niña, and the Southern Oscillation ........10 2.3 Indian Ocean Dipole ................12 2.4 Continental shelf flow ................13 3. Tides .......................15 3.1 Introduction ...................15 3.2 Tide generating forces and equilibrium theory ........15 3.3 Dynamic model of tides ...............17 3.4 Harmonic analysis and prediction of tides ..........19 4. Surface gravity waves ..................21 4.1 The equations of fluid mechanics ............21 4.2 Boundary conditions ................28 4.3 The general problem of wave motion ...........29 4.4 Linear wave theory .................30 4.5 Shoaling, refraction and breaking ............44 4.6 Diffraction ...................50 4.7 Nonlinear wave theories ...............51 1 Coastal and Ocean Engineering John Fenton 5. The calculation of forces on ocean structures ...........54 5.1 Structural element much smaller than wavelength – drag and inertia forces .....................54 5.2 Structural element comparable with wavelength – diffraction forces ..56 6. -
Geochronology and Geomorphology of the Jones
Geomorphology 321 (2018) 87–102 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Geochronology and geomorphology of the Jones Point glacial landform in Lower Hudson Valley (New York): Insight into deglaciation processes since the Last Glacial Maximum Yuri Gorokhovich a,⁎, Michelle Nelson b, Timothy Eaton c, Jessica Wolk-Stanley a, Gautam Sen a a Lehman College, City University of New York (CUNY), Department of Earth, Environmental, and Geospatial Sciences, Gillet Hall 315, 250 Bedford Park Blvd. West, Bronx, NY 10468, USA b USU Luminescence Lab, Department of Geology, Utah State University, USA c Queens College, School of Earth and Environmental Science, City University of New York, USA article info abstract Article history: The glacial deposits at Jones Point, located on the western side of the lower Hudson River, New York, were Received 16 May 2018 investigated with geologic, geophysical, remote sensing and optically stimulated luminescence (OSL) dating Received in revised form 8 August 2018 methods to build an interpretation of landform origin, formation and timing. OSL dates on eight samples of quartz Accepted 8 August 2018 sand, seven single-aliquot, and one single-grain of quartz yield an age range of 14–27 ka for the proglacial and Available online 14 August 2018 glaciofluvial deposits at Jones Point. Optical age results suggest that Jones Point deposits largely predate the glacial Lake Albany drainage erosional flood episode in the Hudson River Valley ca. 15–13 ka. Based on this Keywords: fi Glaciofluvial sedimentary data, we conclude that this major erosional event mostly removed valley ll deposits, leaving elevated terraces Landform evolution during deglaciation at the end of the Last Glacial Maximum (LGM). -
COWI World-Wide
COWI has over 7,000 employees COWI World-wide JANUARY 17, 2013 2 PANYNJ FLOOD BARRIER Ben C. Gerwick, Inc. › Internationally renowned engineering consulting firm HQ in Oakland, CA › History of creative solutions that minimize risk, cost, and time › Focused on constructability, serviceability, maintenance, and durability of structures in waterways and marine sites › Conceptual design, cost estimates planning, permitting, final design and construction support › Documentation & quality control › Decades of experience with government design criteria to streamline the approval and permitting process › Work is exemplified by New Orleans IHNC Floodgates, Braddock Dam, Olmsted Dam, and Chickamauga Lock. IHNC Swing Gate Tow 3 Select projects Experience › IHNC Lake Borgne Barrier (Design/ Constr. Supt.) › Montezuma Slough Salinity Barrier (Concept. Des./ Constr. Eng.) › Braddock Dam (Design/ Constr. Supt.) › Chickamauga Lock (Design/ Constr. Eng.) › Olmsted Lock and Dam (Design/ Constr. Eng.) › Venice Storm Surge Barrier (Conceptual Des.) › Yeong-Am Lift Gate (Conceptual Des.) 4 Venice Storm Surge Barrier Compressed air is used to raise gates during a storm. Gerwick performed detailed constructability review for this project. 5 Montezuma Slough Salinity Barrier Complex Radial gate structure for Salinity Barrier in the California Delta. Offsite prefabrication & float-in. 6 Chickamauga Lock Cofferdam, Chattanooga, TN 7 Olmsted Dam Construction Photos › Over 4,000-ton Elements have Been Placed with 1-Inch Accuracy in Six Degrees of Freedom JANUARY 17, 2013 8 PANYNJ FLOOD BARRIER Braddock Dam – Dam Segment Tow to Site Float-in of dam elements allows for minimal construction time, saving money and time 9 Braddock Dam, Pittsburgh, PA – Graving Site Two-Level Graving Dock for Float-in Shell 10 IHNC Hurricane Protection Project New Orleans, Louisiana Sector Gate (150') & • Gerwick is the Lead Designer Swing Gate (150') for the $1.3-billion design-build contract for the USACE Hurricane Protection Office. -
North-Coast of Texel: a Comparison Between Reality and Prediction
North-Coast of Texel: A Comparison between Reality and Prediction Rob Steijn1 Dano Roelvink2 Jan Ribberink4 Jan van Overeem1 Abstract For an efficient protection of the north coast of the Dutch Waddensea island Texel, a long dam was constructed in 1995. The position of this dam is on the southern swash platform of the ebb tidal delta of the Eijerlandse Gat: the tidal inlet between the two Waddensea islands Texel and Vlieland. The long dam changed the hydro-morpho- logical conditions in this tidal inlet. The changes in the inlet's morphology have been monitored through regular bathymetry surveys. This paper describes some of the most remarkable changes that occurred in the inlet after the construction of the long dam. The impact of the long dam on the inlet's morphology and the adjacent shoreline stability has been examined with the use of a medium-term morphodynamic model. From a comparison between the observed and predicted morphological changes it followed that the model was able to simulate the large scale morphological response of the inlet system. However, on a smaller scale there were still important discrepan- cies between the observations and the predictions. Introduction The Dutch Government decided in 1990 to maintain the coastline at its 1990-position by means of artificial sand nourishments. However, at certain coastal sections, where nourishments appear to be less effective, alternative coastal protection methods could be considered. The north-coast of Texel (Figure 1) appeared to be such a coastal section. Over a distance of some 6 km, the north-coast of Texel has lost in the last decades on average about 0.5 million m3 sand per year. -
Technology Fact Sheet Seawall and Revetment Technologyi
Technology Fact Sheet Seawall and revetment technologyi 1) Introduction In every coastal area and beach in Indonesia, integrated coastal management will be applied. This is a process of coastal natural resource management and environmental services that integrate the activities of government, business and society covering horizontal and vertical planning, preserving land and marine ecosystems, application of science and management, so that this resource management will improve and be sustainable for the surrounding community welfare. Lack of understanding of coastal dynamics will lead the efforts to harness the economic potential even bring up new problems such as erosion and abrasion as well as accretion. Besides, the incidence of sea level rise and tropical storms will also lead to coastal erosion. Various efforts to solve the problems through the development of Seawall and revetment have been and some are being done by government, business and the society. Because the incidence of abrasion and erosion of beaches are scattered throughout Indonesia, the location that has a significant impact will be followed up in advance. Development of Seawall and revetment is one of the appropriate adapt technology in dealing with further damage of coastal and beaches. A) Feasibility of technology and operational necessities Seawall and revetment are structures that were built on coastline as a barrier of the mainland on one side and waters on the other. The function of this structure is to protect and keep the coastline from waves and to hold the soil behind the seawall. The seawall is expected to cease erosion process. On the north coast of Java, many cities are experiencing abrasion and erosion resulting from a decrease of land and sea-level rise. -
Appendix G. Flood Hazard Management Risk Areas
APPENDIX G. FLOOD HAZARD MANAGEMENT RISK AREAS This appendix contains a complete listing of the flooding and erosion related risk areas identified by the River and Floodplain Management Program staff during the preparation of the 2006 King County Flood Hazard Management Plan. The approach to identifying and characterizing these risk areas varied from river to river and was influenced by both the characteristics of each river, and by the professional judgment of the team compiling this information. This risk identification was the first step in the development of project and program proposals contained in Appendices E and F of this Plan. These project and program recommendation are cross referenced in the last columns of this table. In many cases the magnitude of these risks described is not well understood but will be further evaluated through future technical studies and risk assessments. South Fork Skykomish River, Miller River, Maloney Creek, Tye River and Anthracite Creek (WRIA 7) In DS US Bank Flood or Channel Migration Risk Action Proposed Project RM RM Plan? 6.4 19.9 L, R South Fork Skykomish River Channel Migration Zone Y South Fork Skykomish Channel Migration Zone: Study and Map: Channel migration is a type of flood Conduct South Fork Skykomish River Channel Migration hazard. King County maps channel migration zones to Zone Study and Mapping. (Skykomish River, identify the extent of this flood hazard and regulate land use Unincorporated) in the affected areas. Historical and recent evidence indicates that this part of the South Fork Skykomish River is subject to channel migration. A South Fork Skykomish River channel migration zone study and map will be completed under this project for use by the King County Department of Development and Environmental Services in land use regulation within King County. -
Marine Environment Quality Assessment of the Skagerrak - Kattegat
Journal ol Sea Research 35 (1-3):1-8 (1996) MARINE ENVIRONMENT QUALITY ASSESSMENT OF THE SKAGERRAK - KATTEGAT RUTGER ROSENBERG1, INGEVRN CATO2, LARS FÖRLIN3, KJELL GRIP4 ANd JOHAN RODHEs 1Göteborg university, Kristineberg Marine Research Station, 5-450 34 Fiskebäckskil, Sweden 2Geological Survey of Sweden, Box 670, 5-751 28 Llppsala, Sweden 3cöteborg university, Department of Zoophysiology, Medicinaregatan 18, S-413 90 Göteborg, Sweden aSwedish Environment Protection Agency, S-106 48 Stockholm, Sweden ,Göteborg lJniversity, Department of Oceanography, Earth Science Centre, 5413 81 Göteborg, Sweden ABSTRACT This quality assessment of the Skagerrak-Kattegat is mainly based on recent results obtained within the framework ol the Swedish multidisciplinaiy research projekt 'Large'scale environmental effects and ecological processes in the Skagerrak-Kattegat'completed with relevant data from other research publications. The results show that the North Sea has a significant impact on the marine ecosystem in the Skagerrak and the northern Kattegat. Among environmental changes recently documented for some of these areas are: increased nutrient concentrations, increased occurrence of fast-growing fila- mentous algae in coastal areas affecting nursery and feeding conditions lor fish, declining bottom water oxygen concentrations with negative effects on benthic fauna, and sediment toxicity to inverte brates also causing physiological responses in fish. lt is concluded that, due to eutrophication and toxic substances, large-scale environmental changes and effects occur in the Skagerrak-Kattegat area. Key words: eutrophication, contaminants, nutrients, oxygen concentrations, toxicity, benthos, fish l.INTRODUCTION direction. This water constitutes the bulk of the water in the Skagerrak. A weaker inflow from the southern The Kattegat and the Skagerrak (Fig.