A1d Water Environment
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Time and Tides in the Gulf of Maine a Dockside Dialogue Between Two Old Friends
1 Time and Tides in the Gulf of Maine A dockside dialogue between two old friends by David A. Brooks It's impossible to visit Maine's coast and not notice the tides. The twice-daily rise and fall of sea level never fails to impress, especially downeast, toward the Canadian border, where the tidal range can exceed twenty feet. Proceeding northeastward into the Bay of Fundy, the range grows steadily larger, until at the head of the bay, "moon" tides of greater than fifty feet can leave ships wallowing in the mud, awaiting the water's return. My dockside companion, nodding impatiently, interrupts: Yes, yes, but why is this so? Why are the tides so large along the Maine coast, and why does the tidal range increase so dramatically northeastward? Well, my friend, before we address these important questions, we should review some basic facts about the tides. Here, let me sketch a few things that will remind you about our place in the sky. A quiet rumble, as if a dark cloud had suddenly passed overhead. Didn’t expect a physics lesson on this beautiful day. 2 The only physics needed, my friend, you learned as a child, so not to worry. The sketch is a top view, looking down on the earth’s north pole. You see the moon in its monthly orbit, moving in the same direction as the earth’s rotation. And while this is going on, the earth and moon together orbit the distant sun once a year, in about twelve months, right? Got it skippah. -
Moons Phases and Tides
Moon’s Phases and Tides Moon Phases Half of the Moon is always lit up by the sun. As the Moon orbits the Earth, we see different parts of the lighted area. From Earth, the lit portion we see of the moon waxes (grows) and wanes (shrinks). The revolution of the Moon around the Earth makes the Moon look as if it is changing shape in the sky The Moon passes through four major shapes during a cycle that repeats itself every 29.5 days. The phases always follow one another in the same order: New moon Waxing Crescent First quarter Waxing Gibbous Full moon Waning Gibbous Third (last) Quarter Waning Crescent • IF LIT FROM THE RIGHT, IT IS WAXING OR GROWING • IF DARKENING FROM THE RIGHT, IT IS WANING (SHRINKING) Tides • The Moon's gravitational pull on the Earth cause the seas and oceans to rise and fall in an endless cycle of low and high tides. • Much of the Earth's shoreline life depends on the tides. – Crabs, starfish, mussels, barnacles, etc. – Tides caused by the Moon • The Earth's tides are caused by the gravitational pull of the Moon. • The Earth bulges slightly both toward and away from the Moon. -As the Earth rotates daily, the bulges move across the Earth. • The moon pulls strongly on the water on the side of Earth closest to the moon, causing the water to bulge. • It also pulls less strongly on Earth and on the water on the far side of Earth, which results in tides. What causes tides? • Tides are the rise and fall of ocean water. -
Tsunami, Seiches, and Tides Key Ideas Seiches
Tsunami, Seiches, And Tides Key Ideas l The wavelengths of tsunami, seiches and tides are so great that they always behave as shallow-water waves. l Because wave speed is proportional to wavelength, these waves move rapidly through the water. l A seiche is a pendulum-like rocking of water in a basin. l Tsunami are caused by displacement of water by forces that cause earthquakes, by landslides, by eruptions or by asteroid impacts. l Tides are caused by the gravitational attraction of the sun and the moon, by inertia, and by basin resonance. 1 Seiches What are the characteristics of a seiche? Water rocking back and forth at a specific resonant frequency in a confined area is a seiche. Seiches are also called standing waves. The node is the position in a standing wave where water moves sideways, but does not rise or fall. 2 1 Seiches A seiche in Lake Geneva. The blue line represents the hypothetical whole wave of which the seiche is a part. 3 Tsunami and Seismic Sea Waves Tsunami are long-wavelength, shallow-water, progressive waves caused by the rapid displacement of ocean water. Tsunami generated by the vertical movement of earth along faults are seismic sea waves. What else can generate tsunami? llandslides licebergs falling from glaciers lvolcanic eruptions lother direct displacements of the water surface 4 2 Tsunami and Seismic Sea Waves A tsunami, which occurred in 1946, was generated by a rupture along a submerged fault. The tsunami traveled at speeds of 212 meters per second. 5 Tsunami Speed How can the speed of a tsunami be calculated? Remember, because tsunami have extremely long wavelengths, they always behave as shallow water waves. -
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. -
How a Tide Clock Works.Pub
Conventional time clocks have a 12 hour cycle, with 1 hand for hours, another for minutes. Tide clocks have a single hand, and a cycle of 12 hours 25 minutes, coinciding to an average time of about 6 hours 12 minutes between high and low tides. High tide is indicated when the hand is at the ‘12 o’clock’ position, low tide is indicated with the hand at the ‘6 o’clock’ position. A tide clock is not indicating 6 or 12 o’clock of course. It is merely a convenient reference point on the dial, showing us when our local tide is high or low. 12 is marked as High, 6 is marked as Low. However, the hour markings on the dial between the High and Low tide points do show us the number of hours since the last high or low tide, and the hours before the next high or low tide. A tide clock which has been initially set correctly will continue to display tide predictions quite accurately, requiring resetting only at intervals of about 4 months, depending upon the location. A brief explanation of how the tidal cycle works The Moon is the major cause of the tides. The ‘lunar day’ (the time it takes for the Moon to re-appear at the same place in the sky) is 24 hours and 50 minutes. New Zealand, and many other places in the world, have 2 high tides and 2 low tides each day. These are called semi-diurnal tides. Some areas of the world (eg Freemantle in Australia), have only one tide cycle per day, known as diurnal tides. -
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. -
II. Causes of Tides III. Tidal Variations IV. Lunar Day and Frequency of Tides V
Tides I. What are Tides? II. Causes of Tides III. Tidal Variations IV. Lunar Day and Frequency of Tides V. Monitoring Tides Wikimedia FoxyOrange [CC BY-SA 3.0 Tides are not explicitly included in the NGSS PerFormance Expectations. From the NGSS Framework (M.S. Space Science): “There is a strong emphasis on a systems approach, using models oF the solar system to explain astronomical and other observations oF the cyclic patterns oF eclipses, tides, and seasons.” From the NGSS Crosscutting Concepts: Observed patterns in nature guide organization and classiFication and prompt questions about relationships and causes underlying them. For Elementary School: • Similarities and diFFerences in patterns can be used to sort, classiFy, communicate and analyze simple rates oF change For natural phenomena and designed products. • Patterns oF change can be used to make predictions • Patterns can be used as evidence to support an explanation. For Middle School: • Graphs, charts, and images can be used to identiFy patterns in data. • Patterns can be used to identiFy cause-and-eFFect relationships. The topic oF tides have an important connection to global change since spring tides and king tides are causing coastal Flooding as sea level has been rising. I. What are Tides? Tides are one oF the most reliable phenomena on Earth - they occur on a regular and predictable cycle. Along with death and taxes, tides are a certainty oF liFe. Tides are apparent changes in local sea level that are the result of long-period waves that move through the oceans. Photos oF low and high tide on the coast oF the Bay oF Fundy in Canada. -
WATER ENVIRONMENT A3d.1 INTRODUCTION
Offshore Energy SEA APPENDIX 3d - WATER ENVIRONMENT A3d.1 INTRODUCTION A number of aspects of the water environment are reviewed below in a UK context, and for individual Regional Seas: • The major water masses and residual circulation patterns in UK seas • Density stratification (influenced principally by temperature and salinity) and frontal zones between different water masses – these represent potentially important areas for biological productivity • Tidal flows • Overall patterns of temperature and salinity • Wave climate • Ambient noise Recent assessments of changes in hydrographic conditions are summarised, based mainly on reports by DEFRA (2004a, b) and MCCIP (2007). Overall, significant anomalies and changes have been noted in sea surface temperature (SST), thermal stratification, circulation patterns, wave climate, pH and sea level – many appear to be correlated to atmospheric climate variability as described by the North Atlantic Oscillation (NAO). Larger- scale trends and process changes have also been noted in the North Atlantic (e.g. in the strength of the Gulf Stream and Atlantic Heat Conveyor (more properly characterised as the Meridional Overturning Circulation (MOC), or the Atlantic Thermohaline circulation (THC) e.g. Trumper 2005), Northern Hemisphere (Weijerman et al. 2005) and globally (IPCC 2007a). There are varying degrees of confidence in the interpretation of observed data and prediction of future trends. Finally, the specific environmental issue of eutrophication is summarised. This is an area of concern in specific geographical areas, notably the southern North Sea and various coastal and estuarine locations. A3d.2 UK CONTEXT The history of broadscale studies of North Sea circulation and hydrographic patterns (e.g. temperature and salinity distribution) was briefly reviewed in SEA 2. -
Tide Clock Print Ver Instructions.Pub
THANK YOU FOR PURCHASING THIS TIDE CLOCK An ‘AA’ size battery is required for operation. Insert into the holder on the rear of the movement A high quality battery will last longer and is also much less likely to leak corrosive fluid. Never leave a discharged battery in the clock. Properly cared for, this clock should provide years of service SETTING YOUR CLOCK Conventional time clocks have a 12 hour cycle. Tide clocks have a cycle of 12 hours 25 minutes. This coincides to an average time of about 6 hours 12 minutes between high and low tides. For the reasons outlined in more detail below, and to attain the best accuracy, it is recommended to first set the clock on a day when your local high tide coincides with a full Moon. Obtain a local tide table and calendar showing phases of the Moon from the links page of our website, www.cruisingelectronics.co.nz or your local newspaper, a Nautical Almanac or similar. On the day of a full Moon, use the small adjusting wheel on the rear of the clock movement to adjust the clock hand to the high tide position at your exact local time of high tide. Set in this way, the clock will exhibit a minimum error throughout the month, usually less than 30 minutes DO NOT adjust your tide clock for daylight saving time Please read below for a more detailed description of the tides and their influences. A brief explanation of how the Tidal cycle works The Moon is the major cause of the tides. -
Merging Velocity Measurements and Modeling to Improve Understanding of Tidal Stream Resource in Alderney Race
Merging velocity measurements and modeling to improve understanding of tidal stream resource in Alderney Race. Maxime Thiébaut, Alexei Sentchev, Pascal Bailly Du Bois To cite this version: Maxime Thiébaut, Alexei Sentchev, Pascal Bailly Du Bois. Merging velocity measurements and modeling to improve understanding of tidal stream resource in Alderney Race.. Energy, Elsevier, 2019, 178, pp.460-470. 10.1016/j.energy.2019.04.171. hal-02336285 HAL Id: hal-02336285 https://hal.archives-ouvertes.fr/hal-02336285 Submitted on 28 Oct 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License Merging velocity measurements and modeling to improve understanding of tidal stream resource in Alderney Race Maxime Thiébaut1,2 , Alexei Sentchev*1 and Pascal Bailly du Bois3 (1) Univ. Littoral Côte d’Opale, Univ. Lille, CNRS, UMR 8187, LOG, Laboratoire d’Océanologie et de Géosciences, Wimereux, France (2) France Énergies Marines, Technopôle Brest-Iroise, Batîment Cap Océan, 525 Avenue de Rochon, Plouzané, France (3) IRSN/DEI/SECRE/LRC, Institut de Radioprotection et de Sûreté Nucléaire, Direction de l Environnement et de l Intervention, Laboratoire de Radioécologie de Cherbourg Octeville, France (*) Corresponding author: [email protected] Phone : +33 3 21 99 64 17 Fax : + 33 3 21 99 64 01 Abstract Tidal circulation and tidal stream resource in Aldemey Race (Raz Blanchard) were assessed by using a towed acoustic Doppler current profiler (ADCP) system and tidal modeling. -
Physical and Dynamical Oceanography of Liverpool Bay
Ocean Dynamics (2011) 61:1421–1439 DOI 10.1007/s10236-011-0431-6 Physical and dynamical oceanography of Liverpool Bay Jeffrey A. Polton · Matthew Robert Palmer · Michael John Howarth Received: 2 December 2010 / Accepted: 28 April 2011 / Published online: 31 May 2011 © Springer-Verlag 2011 Abstract The UK National Oceanography Centre has eastward erosion of the plume during spring tides is maintained an observatory in Liverpool Bay since identified as a potentially important freshwater mixing August 2002. Over 8 years of observational measure- mechanism. Novel climatological maps of temperature, ments are used in conjunction with regional ocean salinity and density from the CTD surveys are pre- modelling data to describe the physical and dynam- sented and used to validate numerical simulations. The ical oceanography of Liverpool Bay and to validate model is found to be sensitive to the freshwater forcing the regional model, POLCOMS. Tidal dynamics and rates, temperature and salinities. The existing CTD plume buoyancy govern the fate of the fresh water survey grid is shown to not extend sufficiently near the as it enters the sea, as well as the fate of its sedi- coast to capture the near coastal and vertically mixed ment, contaminants and nutrient loads. In this con- component the plume. Instead the survey grid captures text, an overview and summary of Liverpool Bay tidal the westward spreading, shallow and transient, portion dynamics are presented. Freshwater forcing statistics of the plume. This transient plume feature is shown in are presented showing that on average the bay re- both the long-term averaged model and observational ceives 233 m3 s−1. -
TIDAL RANGE POWER a Future Reliable Renewable Energy Resource Introduction
1 TIDAL RANGE POWER A future reliable renewable energy resource Introduction The British Hydropower Association [BHA] is the only trade membership organisation dedicated to representing the best interests of the UK hydropower community. Hydropower, or water power, is one of the most reliable, predictable and least environmentally 2 intrusive of all the renewable energy technologies and the BHA strives to ensure that the full potential and associated economic and community benefits are fully realised. The BHA continues to promote and support the development of tidal range power projects as it provides predictable and secure generation capacity. Current research into a number of tidal range technologies and offshore hydropower is proceeding at a number of sites around the UK. Need for renewable energy > 3 The target for the country is to have net-zero carbon emissions by 2050. This is a real challenge as no currently renewable resources are available all the time - the sun not shining at night and the wind not always blowing. However the UK, with the second highest tides in the world, has good tidal range resources which have not yet been developed. 4 The time of high water varies around the coast, so it should be possible to stagger generation and provide reliable, predictable, and almost continuous power. > The proposed Swansea Bay tidal lagoon wall. The length of 854 London buses parked in a row. Explanation Tidal range power utilises the difference The tidal range system is different to tidal in head between the sea and a basin. stream which generates energy solely by 5 The basin is usually formed by a barrage the flow of tidal water through a turbine/ of tidal range across an estuary or bay or by a lagoon generator in a high tidal velocity location, power > wall.