Rip Current Generation, Flow Characteristics and Implications for Beach Safety in South Florida
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Rip Current Observations Via Marine Radar
Rip Current Observations via Marine Radar Merrick C. Haller, M.ASCE1; David Honegger2; and Patricio A. Catalan3 Abstract: New remote sensing observations that demonstrate the presence of rip current plumes in X-band radar images are presented. The observations collected on the Outer Banks (Duck, North Carolina) show a regular sequence of low-tide, low-energy, morphologically driven rip currents over a 10-day period. The remote sensing data were corroborated by in situ current measurements that showed depth-averaged rip current velocities were 20e40 cm=s whereas significant wave heights were Hs 5 0:5e1 m. Somewhat surprisingly, these low-energy rips have a surface signature that sometimes extends several surf zone widths from shore and persists for periods of several hours, which is in contrast with recent rip current observations obtained with Lagrangian drifters. These remote sensing observations provide a more synoptic picture of the rip current flow field and allow the identification of several rip events that were not captured by the in situ sensors and times of alongshore deflection of the rip flow outside the surf zone. These data also contain a rip outbreak event where four separate rips were imaged over a 1-km stretch of coast. For potential comparisons of the rip current signature across other radar platforms, an example of a simply calibrated radar image is also given. Finally, in situ observations of the vertical structure of the rip current flow are given, and a threshold offshore wind stress (.0:02 m=s2)isfoundto preclude the rip current imaging. DOI: 10.1061/(ASCE)WW.1943-5460.0000229. -
Safe Boating Through the St. Lucie Inlet
Information: Florida Fish & Wildlife Commission 850-488-4676 SAFE BOATING US Coast Guard - Ft. Pierce 772-461-7606 THROUGH THE ST. LUCIE INLET US Coast Guard Auxiliary 772-465-8128 US Army Corps of Engineers 772-221-3349 St. Lucie Inlet Coastal 772-225-2300 Weather Station HERE ARE SOME THINGS TO REMEMBER: • Listen to the most recent weather forecast for the times you plan to go out AND come back in the inlet. • Look in the Tide Tables or local newspapers for the times St. Lucie Inlet of predicted high and low tides for the day you plan to go out. Remember the outgoing (ebb) tital current at low Newcomers tide is the worst time to make a passage through the St. Lucie Inlet. If you are a boater new to this area, it is highly • Safe boating practices are even more important in inlets. recommended that you make your first passage of Check your boat before you head out. Life preservers the St. Lucie Inlet as an observer. An experienced should be worn when going through inlets. boater with local knowledge at the helm can point • Expect the unexpected. Watch the clouds to anticipate out various hazards and conditions to avoid. This is severe weather such as thunderstorms. Be on the lookout for shifting shoals and changing channels. especially important if you have no prior experience • Engine failure is common in small boats in rough seas. with any ocean inlets. The extra roughness agitates gasoline and settled dirt or water in the fuel system, which can cause engine failure Notes on Navigation at Night at a crtical time. -
Beach Safety in Atypical Rip Current Systems: Testing Traditional Beach Safety Messages in Non-Traditional Settings
Beach safety in atypical rip current systems: testing traditional beach safety messages in non-traditional settings Benjamin Robert Van Leeuwen A thesis in fulfilment of the requirements for the degree of Master of Science School of Biological, Earth and Environmental Science (BEES) Faculty of Science Supervisors: Associate Professor Robert Brander, School of Biological, Earth and Environmental Sciences, UNSW Australia, Sydney, NSW, 2052, Australia Professor Ian Turner, Water Research Laboratory, School of Civil and Environmental Engineering, UNSW Australia, Manly Vale, NSW, 2093, Australia July 2015 PLEASE TYPE THE UNIVERSITY OF NEW SOUTH WALES Thesis/Dissertation Sheet Surname or Family name: Van Leeuwen First name: Benjamin Other name/s: Robert Abbreviation for degree as given in the University calendar: MSc School: School of Biological, Earth and Environmental Sciences Faculty: Science Title: Beach safety in atypical rip current systems: testing traditional beach safety messages in non-traditional settings Abstract 350 words maximum: (PLEASE TYPE) As a major coastal process and hazard, rip currents are a topic of considerable interest from both a scientific and safety perspective. Collaborations between these two areas are a recent development, yet a scientific basis for safety information is crucial to better understanding how to avoid and mitigate the hazard presented by rip currents. One such area is the field of swimmer escape strategies. Contemporary safety advice is divided on the relative merits of a ‘Stay Afloat’ versus ‘Swim Parallel’ strategy, yet conceptual understanding of both these strategies is largely based on an idealised model of rip current morphology and flow dynamics where channels are incised in shore-connected bars. -
1 the Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration
1 The Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration 2 of Soft Cliff Coastlines 3 4 Sally Brown1*, Max Barton1, Robert J Nicholls1 5 6 1. Faculty of Engineering and the Environment, University of Southampton, 7 University Road, Highfield, Southampton, UK. S017 1BJ. 8 9 * Sally Brown ([email protected], Telephone: +44(0)2380 594796). 10 11 Abstract: Building defences, such as groynes, on eroding soft cliff coastlines alters the 12 sediment budget, changing the shoreline configuration adjacent to defences. On the 13 down-drift side, the coastline is set-back. This is often believed to be caused by increased 14 erosion via the ‘terminal groyne effect’, resulting in rapid land loss. This paper examines 15 whether the terminal groyne effect always occurs down-drift post defence construction 16 (i.e. whether or not the retreat rate increases down-drift) through case study analysis. 17 18 Nine cases were analysed at Holderness and Christchurch Bay, England. Seven out of 19 nine sites experienced an increase in down-drift retreat rates. For the two remaining sites, 20 retreat rates remained constant after construction, probably as a sediment deficit already 21 existed prior to construction or as sediment movement was restricted further down-drift. 22 For these two sites, a set-back still evolved, leading to the erroneous perception that a 23 terminal groyne effect had developed. Additionally, seven of the nine sites developed a 24 set back up-drift of the initial groyne, leading to the defended sections of coast acting as 1 25 a hard headland, inhabiting long-shore drift. -
A Nonlinear Relationship Between Marsh Size and Sediment Trapping Capacity Compromises Salt Marshes’ Stability Carmine Donatelli1*, Xiaohe Zhang2*, Neil K
https://doi.org/10.1130/G47131.1 Manuscript received 22 October 2019 Revised manuscript received 9 March 2020 Manuscript accepted 26 April 2020 © 2020 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 10 June 2020 A nonlinear relationship between marsh size and sediment trapping capacity compromises salt marshes’ stability Carmine Donatelli1*, Xiaohe Zhang2*, Neil K. Ganju3, Alfredo L. Aretxabaleta3, Sergio Fagherazzi2† and Nicoletta Leonardi1† 1 Department of Geography and Planning, School of Environmental Sciences, Faculty of Science and Engineering, University of Liverpool, Roxby Building, Chatham Street, Liverpool L69 7ZT, UK 2 Department of Earth Sciences, Boston University, 675 Commonwealth Avenue, Boston, Massachusetts 02215, USA 3 Woods Hole Coastal and Marine Science Center, U.S. Geological Survey, Woods Hole, Massachusetts 02543, USA ABSTRACT tidal flats to keep pace with sea-level rise (Mari- Global assessments predict the impact of sea-level rise on salt marshes with present-day otti and Fagherazzi, 2010). levels of sediment supply from rivers and the coastal ocean. However, these assessments do Regional effects are crucial when evaluating not consider that variations in marsh extent and the related reconfiguration of intertidal area coastal interventions under the management of affect local sediment dynamics, ultimately controlling the fate of the marshes themselves. multiple agencies. Though many studies have We conducted a meta-analysis of six bays along the United States East Coast to show that focused on local marsh dynamics, less atten- a reduction in the current salt marsh area decreases the sediment availability in estuarine tion has been paid to how changes in marsh systems through changes in regional-scale hydrodynamics. -
What Are Rip Currents? Types of Rips Are Rips Dangerous
What are Rip Currents? Rips are strong, narrow currents that flow from the shoreline seaward past the breaking waves. They exist as a way of getting water carried to the beach by breaking waves back out to sea and are usually confined to deeper channels between shallow sand bars. The bigger the waves, the stronger the rip. Think of them as "rivers of the sea". Types of Rips • Low energy rips are the most common and occur when waves are smaller or haven't changed in a while. They are usually fixed in place and sit in channels between sand bars and don't move much. • High energy or flash rips are bigger and occur when waves have increased suddenly, or during a storm. They tend to move around a bit and flow faster. • Headland and fixed rips are often permanent and occur next to headlands and structures such as groynes and jetties. Low Energy Rip High Energy Rip Are Rips Dangerous? Rips are only dangerous if you don't understand what they are and you are not a good swimmer. They can carry you more than 100 m offshore in less than a minute and are the major cause of surf drownings and rescues in Australia. However, surfers use rips to their advantage to help them swim out through the surf quickly. Page1of2 © 2007 Dr R Brander continued Spotting a Rip Since rips often sit in deeper channels between shallow sand bars, always spend 5-10 minutes looking at the surf zone for consistent darker and "calmer" areas of water that extend offshore between the breaking waves. -
Identification of Rip Current Hazards Using Fluorescent Dye and Unmanned Aerial Vehicle (A Case Study of Drini Beach, Gunungkidul, Indonesia)
https://doi.org/10.5194/nhess-2021-221 Preprint. Discussion started: 23 August 2021 c Author(s) 2021. CC BY 4.0 License. Identification of Rip Current Hazards Using Fluorescent Dye And Unmanned Aerial Vehicle (A Case Study Of Drini Beach, Gunungkidul, Indonesia) 5 1Hendy Fatchurohman1, Alfiatun Nur Khasanah1, Ahmad Cahyadi2 1Department of Earth Science, Vocational College, Universitas Gadjah Mada. Sekip Utara Jalan Kaliurang, Bulaksumur, Yogyakarta, Indonesia, 55281 2Department of Environmental Geography, Faculty of Geography, Universitas Gadjah Mada. Sekip Utara Jalan Kaliurang, 10 Bulaksumur, Yogyakarta, Indonesia, 55281 Correspondence to: Hendy Fatchurohman ([email protected]) Abstract. Coastal tourism is a leading sector substantially contributing to the regional income of Gunungkidul Regency, 15 Indonesia. However, with more tourists visiting the beach, more lives are threatened by coastal hazards. Rip currents are a channel of powerful, narrow, fast-moving water that can carry floating objects away from the shore, presenting one of the most common coastal hazards to swimmers. Unfortunately, most tourists are unaware of rip currents and their threats and how to avoid them. This study was designed to identify the types and dimensions of rip current in one of the regency’s tourist attractions, Drini Beach. For this purpose, an environmentally friendly fluorescent dye, Uranine, was injected from the 20 shoreline, then the velocity and direction of its movements were observed from aerial video footage captured with a drone. Results showed stationary rip currents with a narrow channel, called a channel rip, with the mean dimensions: 250 m from the shoreline to the head and 10.25 m in width. -
Rip Current Generation and Management Implications in South Florida
MOJ Ecology & Environmental Sciences Research Article Open Access Rip current generation and management implications in south Florida Abstract Volume 3 Issue 3 - 2018 Miami Beach is one of the most dangerous beaches for rip current drownings in the Stephen B Leatherman United States. There are three principal wave generators that result in rip currents: Department of Earth & Environment, Florida International onshore winds associated with high pressure cells, swell waves produced by offshore University, USA nor’easters, and tropical storms. A logistic regression analysis showed a correlation between rip currents, wave height and month of the year even under low wave energy Correspondence: Stephen B Leatherman, Department of conditions at Miami area beaches. Most rips were found to occur during 15–20 knot Earth & Environment, Florida International University, 11200 onshore winds with 0.6–0.9m significant wave height. Eleven social, physical and SW 8th Street, Florida Miami, Florida 33199, USA, Tel 1305- safety factors make Miami Beach a rip current hotspot and pose a major coastal 3482-00, Email [email protected] management challenge. Received: November 16, 2017 | Published: May 31, 2018 Keywords: rip current forecasting, rip current drowning, rip current hot spots, safety factors, beaches Introduction generated by 0.6 to 1.2 m waves during fair–weather conditions, which seem like perfect beach days, making these rips deceptively dangerous South Florida is a tourism destination that is well known for its to bathers. Another type of rip generator is nor’easters offshore the beaches. Miami Beach is one of the ten most famous beaches in the mid–Atlantic and Northeast coast, which produce large swells (Figure 1 world and boasts of tens of millions of visitors each year. -
Street Names - in Alphabetical Order
Street Names - In Alphabetical Order District / MC-ID NO. Street Name Location County Area Aalto Place Sumter - Unit 692 (Villa San Antonio) 1 Sumter County Abaco Path Sumter - Unit 197 9 Sumter County Abana Path Sumter - Unit 206 9 Sumter County Abasco Court Sumter - Unit 821 (Mangrove Villas) 8 Sumter County Abbeville Loop Sumter - Unit 80 5 Sumter County Abbey Way Sumter - Unit 164 8 Sumter County Abdella Way Sumter - Unit 180 9 Sumter County Abdella Way Sumter - Unit 181 9 Sumter County Abel Place Sumter - Unit 195 10 Sumter County Aber Lane Sumter - Unit 967 (Ventura Villas) 10 Sumter County SE 84TH Abercorn Court Marion - Unit 45 4 Marion County Abercrombie Way Sumter - Unit 98 5 Sumter County Aberdeen Run Sumter - Unit 139 7 Sumter County Abernethy Place Sumter - Unit 99 5 Sumter County Abner Street Sumter - Unit 130 6 Sumter County Abney Avenue VOF - Unit 8 12 Sumter County Abordale Lane Sumter - Unit 158 8 Sumter County Acorn Court Sumter - Unit 146 7 Sumter County Acosta Court Sumter - Unit 601 (Villa De Leon) 2 Sumter County Adair Lane Sumter - Unit 818 (Jacaranda Villas) 8 Sumter County Adams Lane Sumter - Unit 105 6 Sumter County Adamsville Avenue VOF - Unit 13 12 Sumter County Addison Avenue Sumter - Unit 37 3 Sumter County Adeline Way Sumter - Unit 713 (Hillcrest Villas) 7 Sumter County Adelphi Avenue Sumter - Unit 151 8 Sumter County Adler Court Sumter - Unit 134 7 Sumter County Adriana Way Sumter - Unit 711 (Adriana Villas) 7 Sumter County Adrienne Way Sumter - Unit 176 9 Sumter County Adrienne Way Sumter - Unit 949 (Megan -
Reef Rip Current Generated by Tide and Wave During Summer Season: Field Observation Conducted in Yoshiwara Coast, Ishigakijima, Okinawa, Japan
Proceedings of the 11th International Coral Reef Symposium, Ft. Lauderdale, Florida, 7-11 July 2008 Session number 15 Reef Rip Current Generated by Tide and Wave during Summer Season: Field Observation Conducted in Yoshiwara Coast, Ishigakijima, Okinawa, Japan M.P. de Leon1, R. Nishi2, F. Kumasaka3, T. Takaesu4, R. Kitamura5, A. Otani6 1) Graduate School of Science and Engineering, Kagoshima University, 1-21-40 Korimoto, Kagoshima, Japan 2) Faculty of Fisheries, Kagoshima University, 4-50-20 Shimoarata, Kagoshima, Japan 3) Japan Hydrographic Association, Tsukiji, Tokyo, Japan 4) Marine Information Science, 11th Japan Coast Guard, Naha, Okinawa, Japan 5) Department of Ocean Civil Engineering, Kagoshima University, 1-21-40 Korimoto, Kagoshima, Japan 6) IO Technic, 2-28-19 Minami, Tsukushino, Machida, Tokyo, Japan Abstract. In 2004 and 2005, five drowning accidents in Ishigakijima, Okinawa were documented by Japan Coast Guard and were found to be caused by a strong offshore current commonly known as “reef current”. This type of current has been identified to be responsible in generating the circulation of water and transportation of sediment in coral reefs. In this paper, however, high-speed offshore current in coral reefs is specifically referred to as “reef rip current”. Considering that the generation mechanism of reef rip current is not revealed yet, the researchers conducted a hydrodynamic study in Yoshiwara Coast, Ishigakijima, Okinawa in two phases (normal and storm conditions) during summer season to determine the location and time of occurrence of the strong offshore current that will significantly address safe utilization of coral reef and carbonate beach thereby reducing drowning accidents. -
Earth's Atmosphere
Earth & Space Science Packet April 20th- May 1st, 2020 Griffin & King This packet contains: 1. Worksheets for Ocean Floor, Ocean Water and Ocean Life, Earth’s Atmosphere 2. All About Waves Article 3. Atmospheric Density Lab What needs to be turned in for a GRADE? ● Worksheets with questions answered (Ocean Floor and Ocean Water/Life is April 20-24; Atmosphere is April 27-May 1) Optional/Enrichment included: ● Labs ● Science Articles If these are completed, we would LOVE for you to share: Send us pictures on remind/email, or tag @TheBurgScience and #Team DCS on Twitter EARTH & SPACE SCIENCE GRIFFIN & KING THE OCEAN FLOOR ___ THE VAST WORLD OCEAN ● Nearly 70 percent of Earth’s surface is covered by the global ocean. ● Oceanography is a science that draws on the methods and knowledge of geology, chemistry, physics, and biology to study all aspects of the world ocean. ● The world ocean can be divided into four main ocean basins- the Pacific Ocean, the Atlantic Ocean, the Indian Ocean, and the Arctic Ocean. ● The topography of the ocean floor is as diverse as that of continents. ● Bathymetry (bathos=depth, metry=measurement) is the measurement of ocean depths and the charting of the shape or topography of the ocean floor. ● Today’s technology- particular sonar, satellites, and submersibles- allows scientists to study the ocean floor in a more efficient and precise manner than ever before. ● Sonar is an acronym for sound navigation and ranging. Sonar calculates ocean depth by recording the time it takes sound waves to reach the ocean floor and return. -
Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds
Appendix 5.4, Page 1 Appendix 5.4 Marine and Coastline Habitats Featured Species-associated Intertidal Habitats: Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds A swath of intertidal habitat occurs wherever the ocean meets the shore. At 44,000 miles, Alaska’s shoreline is more than double the shoreline for the entire Lower 48 states (ACMP 2005). This extensive shoreline creates an impressive abundance and diversity of habitats. Five physical factors predominantly control the distribution and abundance of biota in the intertidal zone: wave energy, bottom type (substrate), tidal exposure, temperature, and most important, salinity (Dethier and Schoch 2000; Ricketts and Calvin 1968). The distribution of many commercially important fishes and crustaceans with particular salinity regimes has led to the description of “salinity zones,” which can be used as a basis for mapping these resources (Bulger et al. 1993; Christensen et al. 1997). A new methodology called SCALE (Shoreline Classification and Landscape Extrapolation) has the ability to separate the roles of sediment type, salinity, wave action, and other factors controlling estuarine community distribution and abundance. This section of Alaska’s CWCS focuses on 3 main types of intertidal habitat: rocky intertidal, mudflats and beaches, and eelgrass beds. Tidal marshes, which are also intertidal habitats, are discussed in the Wetlands section, Appendix 5.3, of the CWCS. Rocky intertidal habitats can be categorized into 3 main types: (1) exposed, rocky shores composed of steeply dipping, vertical bedrock that experience high-to- moderate wave energy; (2) exposed, wave-cut platforms consisting of wave-cut or low-lying bedrock that experience high-to-moderate wave energy; and (3) sheltered, rocky shores composed of vertical rock walls, bedrock outcrops, wide rock platforms, and boulder-strewn ledges and usually found along sheltered bays or along the inside of bays and coves.