Tidal Currents River Currents Gravity Pulls Water from Higher Elevation to Lower Elevations

Total Page:16

File Type:pdf, Size:1020Kb

Tidal Currents River Currents Gravity Pulls Water from Higher Elevation to Lower Elevations Ocean Skills Workshops Welcome! We’ll get started at 6:30pm I. Navigation - April 14-15 II. Tides, Currents & Waves - April 21-22 III. Trip-Planning - April 28-29 Tides Why do tides matter to kayakers? Bay of Fundy, Nova Scotia Neap Tide vs. Spring Tide Neap = Smallest tide cycles (lowest highs and highest lows) Spring = Biggest tide cycles (highest highs and lowest lows) Tides are highest on the new and the full moon phases when the gravitational forces of the sun and the moon work together. Tides are lowest on the half moon phases when the gravitational pull of the moon and the sun work against each other. Gravitational Force Inertia Centrifical Force Proximity Tidal Cycles Diurnal Semi-Diurnal (Maine) Mixed Semi-Diurnal: Two highs and two lows A “tidal day” is 24.8 hours. There are 12.4 hours between one high tide and the next. Tidal Prediction - Resources and how to Use them Tide Stations in Southern Maine Tide charts and other data from each of these stations can be found on NOAA’s website. The link is on our course webpage. Maine Harbors Tide Chart The Rule of Twelfths A rule of thumb for predicting the height of the tide. The Rule of Twelfths Graphic: eOceanic Tidal Range Casco Bay’s mean tidal range = 9 feet Source: Researchgate.com Intertidal Zone Four Zones: ● Splash Zone. ● Upper Littoral Zone ● Mid-Littoral Zone ● Lower Littoral Zone Exercise #1: Assess Tides for a trip around Mackworth Island You are launching from the East End Beach at 9AM on May 31, 2021. ● Can you paddle around Mackworth Island? ● At noon how much can you expect the water level to have risen since the last low tide? Use the rule of twelfths. May Tide Chart, Portland Harbor Currents Offshore banks affect the flow of currents entering the Gulf of Maine Types of Currents Ocean Currents River Currents Rip Currents Tidal Currents River Currents Gravity pulls water from higher elevation to lower elevations. Near river mouths these currents interact with various ocean currents Rip Currents Strong, localized current of water moving directly away from the shore, cutting through breaking waves like a river running out to sea Source: Live Science Rip Currents Source: Live Science Tidal Currents Blue Hill Falls Photo:Andy Gagne When are tidal currents Fastest/slowest? Between high and low tide the water accelerates to reach maximum speed (max flood or max ebb) then slows until it changes direction (slack water). Geographic Features Casco Bay has that Affect Currents many features that ● Shallows constrict tidal flow, ● Surf causing ● Headlands faster ● Cliffs currents ● River mouths ● Ledges ● Bathymetry Lower Hell Gate Large volumes of water flowing through a narrow channel creates tidal rapid. SouthWest of Fort Gorges in Portland Harbor Currents from Fore River and eastern harbor combine to create turbulent waters Currents: Friend or Foe? Old Sow Whirlpool in Eastport Current Symbols on Charts These symbols are rarely found on charts that sea kayakers use in Maine, but are more common and useful in other regions. Flood tide stream with mean spring rate Ebb tide stream with mean spring rate Circumnavigating Manhattan Island, NYC Via the East River, Harlem River and Hudson River Exercise #2: Assessing Tides & Currents on a plotted course You are paddling the course you plotted from Mere Point to Whaleboat Island on May 26, launching at 10:30AM. 1. How will the water level change throughout your trip due to tides? 2. How will the currents be flowing throughout your trip? (Estimate direction & speed) 3. Where do you expect the strongest currents? Answers 1. The water will be rising for the first hour, then falling until 5:32pm. 2. The large tidal range, caused by a full moon, will create especially strong currents. You’ll be paddling against a mild flood current during the first hour, then very little current during slack tide, then an ebb current will peak at around 2:30pm. 3. The current is likely to be strong in the narrow channel between Whaleboat I. and Harpswell. Waves What are waves? Energy moving through water Words to Describe Waves lumpy, steep, choppy, frothy, standing, haystack, rooster tail, breakers, rollers, rebounding, refracting, glassy, towering, messy, spilling, collapsing.... Waves: Friend or Foe? Types of Waves: Ocean Swell Caused by an often distant gale or seismic disturbance. Only encountered in areas exposed to vast open waters. Types of Waves: WInd Waves (Chop) Caused by wind moving over water. Can be encountered on any body of water. You’re unlikely to encounter swell when paddling with land between you and the open ocean Today’s Marine Forecast for Casco Bay E WINDS 5 TO 10 KT, BECOMING SE EARLY THIS AFTERNOON, THEN BECOMING S 10 TO 20 KT WITH GUSTS UP TO 30 KT LATE. SEAS 1 TO 2 FT. Would a kayaker on Casco Bay encounter significant waves today? Types of Waves: Breaking Waves When the wave height becomes 1.3 times the water depth, the crest falls, forming a breaker Three main types of Breakers Spilling: Gently sloped beach. Breaks far from shore Plunging: Moderate sloped beach. Surging: Steeply sloped beach. Breaks close to shore. Where are you likely to find Breaking waves? ● Exposed rocks ● Shallow areas ● Beaches ● Sandbars Types of Waves: Refracting Waves Clapotis When waves moving in different directions encounter each other. Wave length – distance between crests or troughs. Wave height – distance from base to the crest. Wave period – Time for peaks to pass a point. Fetch The distance the wind has traveled over open water More Fetch = Bigger Waves In a westerly wind there is fetch of about .5 ½ Mile miles where the star is positioned In a northeasterly wind there is essentially no fetch where the star is positioned In southeasterly winds the fetch could be up to 4 miles where the star is positioned! Expect big waves if winds are strong. .
Recommended publications
  • Tidal Hydrodynamic Response to Sea Level Rise and Coastal Geomorphology in the Northern Gulf of Mexico
    University of Central Florida STARS Electronic Theses and Dissertations, 2004-2019 2015 Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico Davina Passeri University of Central Florida Part of the Civil Engineering Commons Find similar works at: https://stars.library.ucf.edu/etd University of Central Florida Libraries http://library.ucf.edu This Doctoral Dissertation (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Electronic Theses and Dissertations, 2004-2019 by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Passeri, Davina, "Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico" (2015). Electronic Theses and Dissertations, 2004-2019. 1429. https://stars.library.ucf.edu/etd/1429 TIDAL HYDRODYNAMIC RESPONSE TO SEA LEVEL RISE AND COASTAL GEOMORPHOLOGY IN THE NORTHERN GULF OF MEXICO by DAVINA LISA PASSERI B.S. University of Notre Dame, 2010 A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Civil, Environmental, and Construction Engineering in the College of Engineering and Computer Science at the University of Central Florida Orlando, Florida Spring Term 2015 Major Professor: Scott C. Hagen © 2015 Davina Lisa Passeri ii ABSTRACT Sea level rise (SLR) has the potential to affect coastal environments in a multitude of ways, including submergence, increased flooding, and increased shoreline erosion. Low-lying coastal environments such as the Northern Gulf of Mexico (NGOM) are particularly vulnerable to the effects of SLR, which may have serious consequences for coastal communities as well as ecologically and economically significant estuaries.
    [Show full text]
  • Appendix S6 Benthic Habitat Mapping of the Darwin Region
    Technical Appendix S6 Ichthys Gas Field Development Project: benthic habitat mapping of the Darwin region—methods of data collection, collation and map production Ichthys Gas Field Development Project: Benthic Habitat Mapping of the Darwin Region— Methods of data collection, collation and map production Rev 0 | 30 March 2011 INPEX Document No. C036-AH-REP-0121 Phone: +61 408 857 056 E-mail: [email protected] Address: 8/260 West Coast Highway Scarborough, WA Web: www.geooceans.com Table of Contents 1. Introduction.............................................................................5 2. Data collection methods ........................................................6 2.1. Towed video survey ................................................................................... 6 2.1.1. Field sampling ............................................................................................ 6 2.1.2. Video transects .......................................................................................... 6 2.1.3. Towed video system .................................................................................. 6 2.1.4. Video data analysis and habitat classification............................................ 7 2.1.5. Quality assurance and quality control ........................................................ 9 2.1.6. Bathymetry ................................................................................................. 9 2.1.7. Depth correction for tide..........................................................................
    [Show full text]
  • Ahead of the Wave
    sciencenewsf o rkids.o rg http://www.sciencenewsforkids.org/2013/02/scientists-are-working-to-predict-and-tame-the-tsunamis-that-can-threaten-some- coastal-communities/ Ahead of the wave By Stephen Ornes / February 13, 2013 Bump a glass and any water inside might slop over the side. Splash in the bathtub and waves slosh. Toss a rock into a pond and ripples move outward in expanding rings. In each case, the water moves in waves. Those waves carry energy. And the more energy that gets added to a watery environment, the more powerf ul the waves may become. Now imagine an undersea earthquake and the tremendous amount of energy it can transf er to the ocean. That is because the movement of the Earth’s crust can shif t huge volumes of water, unleashing a parade of great and powerf ul waves. The water races away at speeds up to 800 kilometers (500 miles) per hour, or as f ast as a jet plane. Eventually those waves reach shallow Wate r p o urs asho re as a tsunami strike s the e ast co ast o f Jap an o n March 11, 2011. Cre d it: Mainichi Shimb un/Re ute rs water. They slow down and swell, sometimes as high as a 10-story building. When the waves eventually crash onto land, they can swamp hundreds of kilometers (miles) of shoreline. They may snap trees like twigs, collapse of f ice buildings and sweep away cars. Among nature’s most powerf ul f orces of destruction, these waves are called tsunamis (tzu NAAM eez).
    [Show full text]
  • Documenting Inuit Knowledge of Coastal Oceanography in Nunatsiavut
    Respecting ontology: Documenting Inuit knowledge of coastal oceanography in Nunatsiavut By Breanna Bishop Submitted in partial fulfillment of the requirements for the degree of Master of Marine Management at Dalhousie University Halifax, Nova Scotia December 2019 © Breanna Bishop, 2019 Table of Contents List of Tables and Figures ............................................................................................................ iv Abstract ............................................................................................................................................ v Acknowledgements ........................................................................................................................ vi Chapter 1: Introduction ............................................................................................................... 1 1.1 Management Problem ...................................................................................................................... 4 1.1.1 Research aim and objectives ........................................................................................................................ 5 Chapter 2: Context ....................................................................................................................... 7 2.1 Oceanographic context for Nunatsiavut ......................................................................................... 7 2.3 Inuit knowledge in Nunatsiavut decision making .........................................................................
    [Show full text]
  • Tide Simplified by Phil Clegg Sea Kayaking Anglesey
    Tide Simplified By Phil Clegg Sea Kayaking Anglesey Tide is one of those areas that the more you learn about it, the more you realise you don’t know. As sea kayakers, and not necessarily scientists, we don’t have to know every detail but a simplified understanding can help us to understand and predict what we might expect to see when we are out on the water. In this article we look at the areas of tide you need to know about without having to look it up in a book. Causes of tides To understand tide is convenient to imagine the earth with an envelope of water all around it, spinning once every 24 hours on its north-south axis with the moon on a line parallel to the equator. Moon Gravity A B Earth Ocean C The tides are primarily caused by the gravitational attraction of the moon. Simplifying a bit, at point A the gravitational pull is the strongest causing a high tide, point B experiences a medium pull towards the moon, while point C has the weakest pull causing a second high tide. Because the earth spins once every 24 hours, at any location on its surface there are two high tides and two low tides a day. There are approximately six hours between high tide and low tide. One way of predicting the approximate time of high tide is to add 50 minutes to the high tide of the previous day. The sun has a similar but weaker gravitational effect on the tides. On average this is about 40 percent of that of the moon.
    [Show full text]
  • Chapter 5 Water Levels and Flow
    253 CHAPTER 5 WATER LEVELS AND FLOW 1. INTRODUCTION The purpose of this chapter is to provide the hydrographer and technical reader the fundamental information required to understand and apply water levels, derived water level products and datums, and water currents to carry out field operations in support of hydrographic surveying and mapping activities. The hydrographer is concerned not only with the elevation of the sea surface, which is affected significantly by tides, but also with the elevation of lake and river surfaces, where tidal phenomena may have little effect. The term ‘tide’ is traditionally accepted and widely used by hydrographers in connection with the instrumentation used to measure the elevation of the water surface, though the term ‘water level’ would be more technically correct. The term ‘current’ similarly is accepted in many areas in connection with tidal currents; however water currents are greatly affected by much more than the tide producing forces. The term ‘flow’ is often used instead of currents. Tidal forces play such a significant role in completing most hydrographic surveys that tide producing forces and fundamental tidal variations are only described in general with appropriate technical references in this chapter. It is important for the hydrographer to understand why tide, water level and water current characteristics vary both over time and spatially so that they are taken fully into account for survey planning and operations which will lead to successful production of accurate surveys and charts. Because procedures and approaches to measuring and applying water levels, tides and currents vary depending upon the country, this chapter covers general principles using documented examples as appropriate for illustration.
    [Show full text]
  • SPH Based Shallow Water Simulation
    Workshop on Virtual Reality Interaction and Physical Simulation VRIPHYS (2011) J. Bender, K. Erleben, and E. Galin (Editors) SPH Based Shallow Water Simulation Barbara Solenthaler1 Peter Bucher1 Nuttapong Chentanez2 Matthias Müller2 Markus Gross1 1ETH Zurich 2NVIDIA PhysX Research Abstract We present an efficient method that uses particles to solve the 2D shallow water equations. These equations describe the dynamics of a body of water represented by a height field. Instead of storing the surface heights using uniform grid cells, we discretize the fluid with 2D SPH particles and compute the height according to the density at each particle location. The particle discretization offers the benefits that it simplifies the use of sparsely filled domains and arbitrary boundary geometry. Our solver can handle terrain slopes and supports two-way coupling of the particle-based height field with rigid objects. An improved surface definition is presented that reduces visible bumps related to the underlying particle representation. It furthermore smoothes areas with separating particles to achieve better rendering results. Both the physics and the rendering are implemented on modern GPUs resulting in interactive performances in all our presented examples. Categories and Subject Descriptors (according to ACM CCS): I.3.5 [Computer Graphics]: Computational Geometry and Object Modeling—Physically Based Modeling; I.3.7 [Computer Graphics]: Three-Dimensional Graphics and Realism—Animation and Virtual Reality 1. Introduction in height field methods as well as in full 3D simulations. The grid discretization allows for efficient simulations, but Physically-based simulations have become an important el- handling irregular domain boundaries that are not aligned ement of real-time applications like computer games.
    [Show full text]
  • Casco Bay Weekly : 8 June 1989
    Portland Public Library Portland Public Library Digital Commons Casco Bay Weekly (1989) Casco Bay Weekly 6-8-1989 Casco Bay Weekly : 8 June 1989 Follow this and additional works at: http://digitalcommons.portlandlibrary.com/cbw_1989 Recommended Citation "Casco Bay Weekly : 8 June 1989" (1989). Casco Bay Weekly (1989). 23. http://digitalcommons.portlandlibrary.com/cbw_1989/23 This Newspaper is brought to you for free and open access by the Casco Bay Weekly at Portland Public Library Digital Commons. It has been accepted for inclusion in Casco Bay Weekly (1989) by an authorized administrator of Portland Public Library Digital Commons. For more information, please contact [email protected]. JUNE 8, 1989 FREE The Maine Island Trail STORY by Wayne Curtis PHOTOS by Tonee Harbert fanfare, Casco Bay has become the starting begins in the protected point of the Maine Island Trail, a 32S-mile LaUer day Eskimos are paddling up waterway that winds up the coast to Ma­ waters of Casco Bay- Casco Bay in roto-molded polyethylene chias. Billed as a watery Appaiachian Trail, and Kevlar boats loaded with point-and­ it permits kayakers and other small-boat but unprepared boaters click cameras and freeze-dried food. On owners to island-hop along the shaggy Portland's Commercial Street, their fringe of northeasternmost United States, arrive quickly at the center brightly colored, narrow kayaks rest atop much the way A.T. hikers can traverse the foreign cars like mobile missiles in search East Coast's mountain spine. of a stormy debate over ?f a launch pad. Some fear that the Maine Island Trail wilderness access.
    [Show full text]
  • Waves and Structures
    WAVES AND STRUCTURES By Dr M C Deo Professor of Civil Engineering Indian Institute of Technology Bombay Powai, Mumbai 400 076 Contact: [email protected]; (+91) 22 2572 2377 (Please refer as follows, if you use any part of this book: Deo M C (2013): Waves and Structures, http://www.civil.iitb.ac.in/~mcdeo/waves.html) (Suggestions to improve/modify contents are welcome) 1 Content Chapter 1: Introduction 4 Chapter 2: Wave Theories 18 Chapter 3: Random Waves 47 Chapter 4: Wave Propagation 80 Chapter 5: Numerical Modeling of Waves 110 Chapter 6: Design Water Depth 115 Chapter 7: Wave Forces on Shore-Based Structures 132 Chapter 8: Wave Force On Small Diameter Members 150 Chapter 9: Maximum Wave Force on the Entire Structure 173 Chapter 10: Wave Forces on Large Diameter Members 187 Chapter 11: Spectral and Statistical Analysis of Wave Forces 209 Chapter 12: Wave Run Up 221 Chapter 13: Pipeline Hydrodynamics 234 Chapter 14: Statics of Floating Bodies 241 Chapter 15: Vibrations 268 Chapter 16: Motions of Freely Floating Bodies 283 Chapter 17: Motion Response of Compliant Structures 315 2 Notations 338 References 342 3 CHAPTER 1 INTRODUCTION 1.1 Introduction The knowledge of magnitude and behavior of ocean waves at site is an essential prerequisite for almost all activities in the ocean including planning, design, construction and operation related to harbor, coastal and structures. The waves of major concern to a harbor engineer are generated by the action of wind. The wind creates a disturbance in the sea which is restored to its calm equilibrium position by the action of gravity and hence resulting waves are called wind generated gravity waves.
    [Show full text]
  • Maine Guide Training
    Maine Guide Training 2021 History of Maine Guides ● First hired guides in Maine were Abenaki people who led European explorers, military officials, traders, priests and lumbermen. ● Guiding industry emerged in late 1900s as people in more urban and industrialized regions sought wilderness for recreation ● Cornelia “Fly Rod” Crosby was first guide licensed in 1897; 1700 others were licensed that year. Maine’s Legal Definition of “Guide” Any person who receives any form of remuneration for his services in accompanying or assisting any person in the fields, forests or on the waters or ice within the jurisdiction of the State while hunting, fishing, trapping, boating, snowmobiling or camping at a primitive camping area. Sea Kayaking Guide Specialization Guides can lead paddlesports trips on the State's territorial seas and tributaries of the State up to the head of tide and out to the three mile limit. This classification includes overnight camping trips in conjunction with those sea-kayaking and paddlesports. Testing Process 1. Criminal Background Check 2. Oral Examination ■ Chart and compass work ■ Catastrophic scenario 3. Written Examination (minimum score of 70 to pass) What Maine Sea Kayak Guides CAn Do ● Lead commercial sea kayaking and SUP trips on Maine’s coastal waters ● Lead overnight camping trips associated with these trips (new as of 2005) ● Lead trips with up to 12 people per guide What Sea Kayak Guides CAN’T Do ● Lead paddling trips on inland waters (by kayak, canoe, SUP or raft) ● Take clients fishing or hunting ● Lead trips that require another type of guide license What are the qualities that you most appreciated in guides you’ve encountered? ● Wilderness Guide Association’s Definition of a Guide A trained and experienced professional with a high level of nature awareness.
    [Show full text]
  • Nearshore Current Pattern and Rip Current Occurrence at Jungmun Beach, Jeju by Numerical Computation 1. Introduction
    한국항해항만학회지 제41권 제2호 J. Navig. Port Res. Vol. 41, No. 2 : 55-62, April 2017 (ISSN:1598-5725(Print)/ISSN:2093-8470(Online)) DOI : http://dx.doi.org/10.5394/KINPR.2017.41.2.55 Nearshore Current Pattern and Rip Current Occurrence at Jungmun Beach, Jeju by Numerical Computation Seung-Hyun An*․†Nam-Hyeong Kim *Coastal, Harbor and Disaster Prevention Research Institute, Sekwang Engineering Consultants Co., LTD. †Department of Civil Engineering, J eju National University, Jeju 63243, Korea Abstract : A nearshore current or a wave-induced current is an important phenomenon in a nearshore zone, which is composed of longshore, cross-shore, and rip currents. The nearshore current is closely related to the occurrence of coastal accidents by beachgoers. A considerable number of coastal accidents by beachgoers involving the rip current have been reported at Jungmun Beach. However, in studies and observations of the nearshore current of Jungmun Beach, understanding of the rip current pattern remains unclear. In this study, a scientific approach is taken to understand the nearshore current and the rip current patterns at Jungmun Beach by numerical computation for year of 2015. From results of numerical computation, the occurrence and spatial characteristics of the rip current, and the similarities between the rip current and incident wave conditions are analyzed. The primary results of this study reveal that the rip currents are frequently generated at Jungmun Beach, especially in the western parts of the beach, and that the rip currents often occur with a wave breaking height of around 0.5 ~ 0.7 m, a wave period of around 6 ~ 8 seconds, and a breaking angle of around 0 ~ 15 degrees.
    [Show full text]
  • Dan-Tipp-Corryvreckan.Pdf
    Corryvreckan The name ‘Corryvreckan’ probably derives from two words ‘Coire’ which in Irish means cauldron and ‘Breccán’ or ‘Breacan’, which is taken to be a proper noun i.e. the name of an individual called Breccán. Although this has also been translated as ‘speckled’ from the adjective brecc ‘spotted, speckled’ etc. combined with the suffix of place – an. There is an Old Irish text known as Cormac’s Glossary written by the then King and Bishop of Cashel, Cormac mac Cuilennáin who died in the year 908. The text is written in the form of Dictionary combined with an encyclopaedia. In it are various attempts at providing explanations, meanings and the significances of various words. At entry 323 it provides probably the fullest description of the Coire Breccáin of the early Irish material, a great whirlpool which is between Ireland and Scotland to the north, in the meeting of various seas, viz., the sea which encompasses Ireland at the north-west, and the sea which encompasses Scotland at the north-east, and the sea to the south between Ireland and Scotland. They whirl around like moulding compasses, each of them taking the place of the other, like the paddles… of a millwheel, until they are sucked into the depths so that the cauldron remains with its mouth wide open; and it would suck even the whole of Ireland into its yawning gullet. It vomits iterum {again & again} that draught up, so that its thunderous eructation and its bursting and its roaring are heard among the clouds, like the steam boiling of a caldron of fire.i This form of description was known in Irish as a Dindshenchas (pronounced dunn- hanakus) tale.
    [Show full text]