Guide to Fishing and Diving New Jersey Reefs
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Coastal Flood Defences - Groynes
Coastal Flood Defences - Groynes Coastal flood defences are key to protecting our coasts against flooding, which is when normally dry, low lying flat land is inundated by sea water. Hard engineering methods are forms of coastal flood defences which mitigate the risk of flooding and coastal erosion and the consequential effects. Hard Engineering Hard engineering methods are often used as a temporary measure to protect against coastal flooding as they are costly and only last for a relatively short amount of time before they require maintenance. However, they are very effective at protecting the coastline in the short-term as they are immediately effective as opposed to some longer term soft engineering methods. But they are often intrusive and can cause issues elsewhere at other areas along the coastline. Groynes are low lying wood or concrete structures which are situated out to sea from the shore. They are designed to trap sediment, dissipate wave energy and restrict the transfer of sediment away from the beach through long shore drift. Longshore drift is caused when prevailing winds blow waves across the shore at an angle which carries sediment along the beach.Groynes prevent this process and therefore, slow the process of erosion at the shore. They can also be permeable or impermeable, permeable groynes allow some sediment to pass through and some longshore drift to take place. However, impermeable groynes are solid and prevent the transfer of any sediment. Advantages and Disadvantages +Groynes are easy to construct. +They have long term durability and are low maintenance. +They reduce the need for the beach to be maintained through beach nourishment and the recycling of sand. -
A Quick Guide to Southeast Florida's Coral Reefs
A Quick Guide to Southeast Florida’s Coral Reefs DAVID GILLIAM NATIONAL CORAL REEF INSTITUTE NOVA SOUTHEASTERN UNIVERSITY Spring 2013 Prepared by the Land-based Sources of Pollution Technical Advisory Committee (TAC) of the Southeast Florida Coral Reef Initiative (SEFCRI) BRIAN WALKER NATIONAL CORAL REEF INSTITUTE, NOVA SOUTHEASTERN Southeast Florida’s coral-rich communities are more valuable than UNIVERSITY the Spanish treasures that sank nearby. Like the lost treasures, these amazing reefs lie just a few hundred yards off the shores of Martin, Palm Beach, Broward and Miami-Dade Counties where more than one-third of Florida’s 19 million residents live. Fishing, diving, and boating help attract millions of visitors to southeast Florida each year (30 million in 2008/2009). Reef-related expen- ditures generate $5.7 billion annually in income and sales, and support more than 61,000 local jobs. Such immense recreational activity, coupled with the pressures of coastal development, inland agriculture, and robust cruise and commercial shipping industries, threaten the very survival of our reefs. With your help, reefs will be protected from local stresses and future generations will be able to enjoy their beauty and economic benefits. Coral reefs are highly diverse and productive, yet surprisingly fragile, ecosystems. They are built by living creatures that require clean, clear seawater to settle, mature and reproduce. Reefs provide safe havens for spectacular forms of marine life. Unfortunately, reefs are vulnerable to impacts on scales ranging from local and regional to global. Global threats to reefs have increased along with expanding ART SEITZ human populations and industrialization. Now, warming seawater temperatures and changing ocean chemistry from carbon dioxide emitted by the burning of fossil fuels and deforestation are also starting to imperil corals. -
Brighton Beach Groynes
CASE STUDY: BRIGHTON BEACH GROYNES BRIGHTON, SOUTH AUSTRALIA FEBRUARY 2017 CLIENT: CITY OF HOLDFAST BAY Adelaide’s beaches are affected by a common phenomenon called ELCOROCK® longshore drift - the flow of water, in one direction, along a beach occurring as a result of winds and currents. In Adelaide longshore drift flows from south to north and it frequently erodes beaches The ELCOROCK system consists of sand- over time, particularly during storm events when tides are high and filled geotextile containers built to form sea is rough. a stabilising, defensive barrier against coastal erosion. Without sand replenishment, the southern end of Adelaide’s beaches will slowly erode and undermine existing infrastructure at The robustness and stability of Elcorock the sea/land interface. The objective of Elcorock sand container geotextile containers provide a solutions groynes, laid perpendicular to the beach, is to capture some of for other marine structures such as groynes and breakwaters. These the natural sand as well as dredged sand, that moves along the structures extend out into the wave zone coast. Over time, this process builds up the beach, particularly and provide marina and beach protection, between the groynes which results in the protection of the existing sand movement control and river training. infrastructure. The size of the container can easily be Geofabrics met with the city of Holdfast Bay in the early stages of selected based on the wave climate and the project to discuss the product, durability and previous projects other conditions ensuring stability under with a similar application. Due to recent weather events, the beach the most extreme conditions. -
Basic Concepts in Oceanography
Chapter 1 XA0101461 BASIC CONCEPTS IN OCEANOGRAPHY L.F. SMALL College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, United States of America Abstract Basic concepts in oceanography include major wind patterns that drive ocean currents, and the effects that the earth's rotation, positions of land masses, and temperature and salinity have on oceanic circulation and hence global distribution of radioactivity. Special attention is given to coastal and near-coastal processes such as upwelling, tidal effects, and small-scale processes, as radionuclide distributions are currently most associated with coastal regions. 1.1. INTRODUCTION Introductory information on ocean currents, on ocean and coastal processes, and on major systems that drive the ocean currents are important to an understanding of the temporal and spatial distributions of radionuclides in the world ocean. 1.2. GLOBAL PROCESSES 1.2.1 Global Wind Patterns and Ocean Currents The wind systems that drive aerosols and atmospheric radioactivity around the globe eventually deposit a lot of those materials in the oceans or in rivers. The winds also are largely responsible for driving the surface circulation of the world ocean, and thus help redistribute materials over the ocean's surface. The major wind systems are the Trade Winds in equatorial latitudes, and the Westerly Wind Systems that drive circulation in the north and south temperate and sub-polar regions (Fig. 1). It is no surprise that major circulations of surface currents have basically the same patterns as the winds that drive them (Fig. 2). Note that the Trade Wind System drives an Equatorial Current-Countercurrent system, for example. -
Armed Sloop Welcome Crew Training Manual
HMAS WELCOME ARMED SLOOP WELCOME CREW TRAINING MANUAL Discovery Center ~ Great Lakes 13268 S. West Bayshore Drive Traverse City, Michigan 49684 231-946-2647 [email protected] (c) Maritime Heritage Alliance 2011 1 1770's WELCOME History of the 1770's British Armed Sloop, WELCOME About mid 1700’s John Askin came over from Ireland to fight for the British in the American Colonies during the French and Indian War (in Europe known as the Seven Years War). When the war ended he had an opportunity to go back to Ireland, but stayed here and set up his own business. He and a partner formed a trading company that eventually went bankrupt and Askin spent over 10 years paying off his debt. He then formed a new company called the Southwest Fur Trading Company; his territory was from Montreal on the east to Minnesota on the west including all of the Northern Great Lakes. He had three boats built: Welcome, Felicity and Archange. Welcome is believed to be the first vessel he had constructed for his fur trade. Felicity and Archange were named after his daughter and wife. The origin of Welcome’s name is not known. He had two wives, a European wife in Detroit and an Indian wife up in the Straits. His wife in Detroit knew about the Indian wife and had accepted this and in turn she also made sure that all the children of his Indian wife received schooling. Felicity married a man by the name of Brush (Brush Street in Detroit is named after him). -
The 46Th Annual
the 46th Annual 2018 TO BENEFIT NANTUCKET COMMUNITY SAILING PROUD TO SPONSOR MURRAY’S TOGGERY SHOP 62 MAIN STREET | 800-368-3134 2 STRAIGHT WHARF | 508-325-9600 1-800-892-4982 2018 elcome to the 15th Nantucket Race Week and the 46th Opera House Cup Regatta brought to you by Nantucket WCommunity Sailing, the Nantucket Yacht Club and the Great Harbor Yacht Club. We are happy to have you with us for an unparalleled week of competitive sailing for all ages and abilities, complemented by a full schedule of awards ceremonies and social events. We look forward to sharing the beauty of Nantucket and her waters with you. Thank you for coming! This program celebrates the winners and participants from last year’s Nantucket Race Week and the Opera House Cup Regatta and gives you everything you need to know about this year’s racing and social events. We are excited to welcome all sailors in the Nantucket community to join us for our inaugural Harbor Rendezvous on Sunday, August 12th. We are also pleased to welcome all our competitors, including young Opti and 420 racers; lasers, Hobies and kite boarders; the local one design fleets; the IOD Celebrity Invitational guest tacticians and amateur teams; and the big boat regatta competitors ranging from Alerions and Wianno Seniors to schooners and majestic classic yachts. Don’t forget that you can go aboard and admire some of these beautiful classics up close, when they will be on display to the public for the 5th Classic Yacht Exhibition on Saturday, August 18th. -
A Numerical Study of the Long- and Short-Term Temperature Variability and Thermal Circulation in the North Sea
JANUARY 2003 LUYTEN ET AL. 37 A Numerical Study of the Long- and Short-Term Temperature Variability and Thermal Circulation in the North Sea PATRICK J. LUYTEN Management Unit of the Mathematical Models, Brussels, Belgium JOHN E. JONES AND ROGER PROCTOR Proudman Oceanographic Laboratory, Bidston, United Kingdom (Manuscript received 3 January 2001, in ®nal form 4 April 2002) ABSTRACT A three-dimensional numerical study is presented of the seasonal, semimonthly, and tidal-inertial cycles of temperature and density-driven circulation within the North Sea. The simulations are conducted using realistic forcing data and are compared with the 1989 data of the North Sea Project. Sensitivity experiments are performed to test the physical and numerical impact of the heat ¯ux parameterizations, turbulence scheme, and advective transport. Parameterizations of the surface ¯uxes with the Monin±Obukhov similarity theory provide a relaxation mechanism and can partially explain the previously obtained overestimate of the depth mean temperatures in summer. Temperature strati®cation and thermocline depth are reasonably predicted using a variant of the Mellor±Yamada turbulence closure with limiting conditions for turbulence variables. The results question the common view to adopt a tuned background scheme for internal wave mixing. Two mechanisms are discussed that describe the feedback of the turbulence scheme on the surface forcing and the baroclinic circulation, generated at the tidal mixing fronts. First, an increased vertical mixing increases the depth mean temperature in summer through the surface heat ¯ux, with a restoring mechanism acting during autumn. Second, the magnitude and horizontal shear of the density ¯ow are reduced in response to a higher mixing rate. -
I. I NOV20 2017
or UNITED STATES DEPARTMENT OF COMMERCE / National Oceanic and Atmospheric Administration * i. I NATIONAL MARINE FISHERIES SERVICE Southeast Regional Office 4rES O LQi 3U Ie1U SOU St. Petersburg, Florida 33701-5505 http://sero.nmfs.noaa.gov F/SER3 1: NMB SER-2015- 17616 NOV20 2017 Mr. Donald W. Kinard Chief, Regulatory Division U.S. Army Corps of Engineers P.O. Box 4970 Jacksonville, Florida 32232-0019 Ref.: U.S. Army Corps of Engineers Jacksonville District’s Programmatic Biological Opinion (JAXBO) Dear Mr. Kinard: Enclosed is the National Marine Fisheries Service’s (NMFS’s) Programmatic Biological Opinion (Opinion) based on our review of the impacts associated with the U.S. Army Corps of Engineers (USACE’s) Jacksonville District’s authorization of 10 categories of minor in-water activities within Florida and the U.S. Caribbean (Puerto Rico and the U.S. Virgin Islands). The Opinion analyzes the effects from 10 categories of minor in-water activities occurring in Florida and the U.S. Caribbean on sea turtles (loggerhead, leatherback, Kemp’s ridley, hawksbill, and green); smalitooth sawfish; Nassau grouper; scalloped hammerhead shark, Johnson’s seagrass; sturgeon (Gulf, shortnose, and Atlantic); corals (elkhom, staghorn, boulder star, mountainous star, lobed star, rough cactus, and pillar); whales (North Atlantic right whale, sei, blue, fin, and sperm); and designated critical habitat for Johnson’s seagrass; smalltooth sawfish; sturgeon (Gulf and Atlantic); sea turtles (green, hawksbill, leatherback, loggerhead); North Atlantic right whale; and elkhorn and staghorn corals in accordance with Section 7 of the Endangered Species Act. We also analyzed effects on the proposed Bryde’s whale. -
A Numerical Assessment of Artificial Reef Pass Wave-Induced Currents As a Renewable Energy Source
Journal of Marine Science and Engineering Article A Numerical Assessment of Artificial Reef Pass Wave-Induced Currents as a Renewable Energy Source Damien Sous 1,2 1 Mediterranean Institute of Oceanography (MIO), Aix Marseille Université, CNRS, IRD, Université de Toulon, 13288 La Garde, France; [email protected]; Tel.: +33-(0)4-9114-2109 2 Univ Pau & Pays Adour/E2S UPPA, Chaire HPC-Waves, Laboratoire des Sciences de l’Ingénieur Appliquées à la Méchanique et au Génie Electrique - Fédération IPRA, EA4581, 64600 Anglet, France Received: 21 July 2019; Accepted: 19 August 2019; Published: 22 August 2019 Abstract: The present study aims to estimate the potential of artificial reef pass as a renewable source of energy. The overall idea is to mimic the functioning of natural reef–lagoon systems in which the cross-reef pressure gradient induced by wave breaking is able to drive an outward flow through the pass. The objective is to estimate the feasibility of a positive energy breakwater, combining the usual wave-sheltering function of immersed breakwater together with the production of renewable energy by turbines. A series of numerical simulations is performed using a depth-averaged model to understand the effects of each geometrical reef parameter on the reef–lagoon hydrodynamics. A synthetic wave and tide climate is then imposed to estimate the potential power production. An annual production between 50 and 70 MWh is estimated. Keywords: artificial reef; positive energy breakwater; numerical simulation; turbines 1. Introduction Low-lying nearshore areas host a significant and increasing population. Under the combined actions of sea level rise [1], modified storm patterns [2], and increasing urbanization, these regions will face growing risks of submersion, inundation, and erosion [3–6]. -
Mapping Current and Future Priorities
Mapping Current and Future Priorities for Coral Restoration and Adaptation Programs International Coral Reef Initiative (ICRI) Ad Hoc Committee on Reef Restoration 2019 Interim Report This report was prepared by James Cook University, funded by the Australian Institute for Marine Science on behalf of the ICRI Secretariat nations Australia, Indonesia and Monaco. Suggested Citation: McLeod IM, Newlands M, Hein M, Boström-Einarsson L, Banaszak A, Grimsditch G, Mohammed A, Mead D, Pioch S, Thornton H, Shaver E, Souter D, Staub F. (2019). Mapping Current and Future Priorities for Coral Restoration and Adaptation Programs: International Coral Reef Initiative Ad Hoc Committee on Reef Restoration 2019 Interim Report. 44 pages. Available at icriforum.org Acknowledgements The ICRI ad hoc committee on reef restoration are thanked and acknowledged for their support and collaboration throughout the process as are The International Coral Reef Initiative (ICRI) Secretariat, Australian Institute of Marine Science (AIMS) and TropWATER, James Cook University. The committee held monthly meetings in the second half of 2019 to review the draft methodology for the analysis and subsequently to review the drafts of the report summarising the results. Professor Karen Hussey and several members of the ad hoc committee provided expert peer review. Research support was provided by Melusine Martin and Alysha Wincen. Advisory Committee (ICRI Ad hoc committee on reef restoration) Ahmed Mohamed (UN Environment), Anastazia Banaszak (International Coral Reef Society), -
Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
World Ocean Thermocline Weakening and Isothermal Layer Warming
applied sciences Article World Ocean Thermocline Weakening and Isothermal Layer Warming Peter C. Chu * and Chenwu Fan Naval Ocean Analysis and Prediction Laboratory, Department of Oceanography, Naval Postgraduate School, Monterey, CA 93943, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-831-656-3688 Received: 30 September 2020; Accepted: 13 November 2020; Published: 19 November 2020 Abstract: This paper identifies world thermocline weakening and provides an improved estimate of upper ocean warming through replacement of the upper layer with the fixed depth range by the isothermal layer, because the upper ocean isothermal layer (as a whole) exchanges heat with the atmosphere and the deep layer. Thermocline gradient, heat flux across the air–ocean interface, and horizontal heat advection determine the heat stored in the isothermal layer. Among the three processes, the effect of the thermocline gradient clearly shows up when we use the isothermal layer heat content, but it is otherwise when we use the heat content with the fixed depth ranges such as 0–300 m, 0–400 m, 0–700 m, 0–750 m, and 0–2000 m. A strong thermocline gradient exhibits the downward heat transfer from the isothermal layer (non-polar regions), makes the isothermal layer thin, and causes less heat to be stored in it. On the other hand, a weak thermocline gradient makes the isothermal layer thick, and causes more heat to be stored in it. In addition, the uncertainty in estimating upper ocean heat content and warming trends using uncertain fixed depth ranges (0–300 m, 0–400 m, 0–700 m, 0–750 m, or 0–2000 m) will be eliminated by using the isothermal layer.