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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. -
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. -
A1d Water Environment
Offshore Energy SEA 3: Appendix 1 Environmental Baseline Appendix 1D: Water Environment A1d.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 • Density stratification (influenced principally by temperature and salinity) and frontal zones between different water masses • Tidal flows • Tidal range • Overall patterns of temperature and salinity • Wave climate • Internal waves • Water Framework Directive ecological status of coastal and estuarine water bodies • Eutrophication • Ambient noise Recent assessments of changes in hydrographic conditions are summarised, based mainly on reports by Defra (2010a, b) and MCCIP (2013) but incorporating a range of other grey and peer reviewed literature sources. 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), northern hemisphere and globally. There are varying degrees of confidence in the interpretation of observed data and prediction of future trends. A1d.2 UK context There have been a number of information gathering and assessment initiatives which provide significant information on the current state of the UK and neighbouring seas, and the activities which affect them. These include both UK wide overview programmes and longer term specific monitoring and measuring studies. -
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. -
Phuket City Bang Wad Dam Freedom Bay King Rama Mai Phai Cape IMAGE Asia IX Park
63 A3 See listing page 72 PHUKETPHUKET ISLAND Where to Eat in Phuket Sarasin Bridge Thepka ssatri Rd. Mai Khao Beach Tha Maphrao Bay Phuket International Airport Blue Canyon Sirinart Kung Bay National Park Nai Yang Beach Mission Hill . d 16 R i r 15 t a s Sai Cape Helipad s a Yang Cape k p e h T 13 Nai Thon 22 Kho Phra Teaw Beach National Park 10 Po Bay Bang Pae Waterfall Layan Ao Po Cape Thalang Tonsai Koh Kala Waterfall Phuket Layan Beach Airpark Bang Rong T h 6 Bay 17 e p k a s Paklok s a t ri Bang Tao Beach R 4 d Heroines' . Monument Son Cape Cherngtalay 6 2 8 Yamu Cape Rd. Surin Beach Srisoonthorn Tha Ruea Bay Tha Ruea Sing Cape Kamala Beach Koh Keaw . d R 2 i Kathu Waterfall r Koh Maphrao t a s Loch Palm By Pass Rd s a k p e Sapam h Kathu 4 T Tourise Police Kalim Beach Phra Baramee Rd. Tesco Lotus Index Patong Beach View Point Phuket Country Club Big C Jungceylon Central Festival Homeworks Koh Sire Phuket City Bang Wad Dam Freedom Bay King Rama Mai Phai Cape IMAGE asia IX Park est W ad Vichit o Phap Pla Cape Relax Bay R Saphan hin ofa st a Ea h d C a o R Phuket Bay fa Koh Kui o a h Wat Chalong C Karon Beach Nam Bo Cape P Koh Taphao Noi a View Point t a k HomePro Village Ao Chalong Koh Taphao Yai Rd Ao Makham Koh Pu . -
Studies of Marine Mammals in Welsh High Tidal Waters
Assessment of Risk to Marine Mammals from Underwater Marine Renewable Devices in Welsh waters Phase 2 - Studies of Marine Mammals in Welsh High Tidal Waters On Behalf of Welsh Assembly Government Date: 28th March 2011 Our Ref: JER3688 RPS Conrad House Beaufort Square Chepstow Monmouthshire NP16 5EP Tel: (0)1291 621 821 Fax: (0)1291 627 827 Email: [email protected] This document is Printed on FSC certified, 100% post-consumer recycled paper, bleached using an elemental chlorine- free process. JER3688 Welsh Assembly Government Planning & Development th 28 March 2011 IMS J 0014v0 Studies of Marine Mammals in Welsh High Tidal Waters Quality Management Prepared by: Jonathan Gordon (Ecologic UK Ltd.) Prepared by: Dave Thompson (SMRU) Prepared by: Russell Leaper (University of Aberdeen) Prepared by: Douglas Gillespie (SMRU) Prepared by: Chris Pierpoint (Eurydice) Prepared by: Susannah Calderan Prepared by: Jamie Macaulay (Ecologic UK Ltd.) Prepared by: Thomas Gordon (Vanishing Point) Authorised by: Nicola Simpson Date: 28th March 2011 Revision: 5 Project Number: JER3688 Document Reference: JER3688R110408JG Phase 2 - Studies of Marine Mammals in Welsh High Tidal Energy Waters v5.doc Document File Path: O:\JER3688 - Marine renewable Strategy for Wales\STAGE 2\Project File\Task 1&2 Marine Mammals Collision Risk\JER3688R110408JG Phase 2 - Studies of Marine Mammals in Welsh High Tidal Energy Waters v5.doc JER3688 Welsh Assembly Government Planning & Development i 28th March 2011 Studies of Marine Mammals in Welsh High Tidal Waters DISCLAIMER The -
Multi-Criteria Assessment of Wave and Tidal Power Along the Atlantic Coast of the Southeastern Usa
MULTI-CRITERIA ASSESSMENT OF WAVE AND TIDAL POWER ALONG THE ATLANTIC COAST OF THE SOUTHEASTERN USA A Dissertation Presented to The Academic Faculty by Zafer Defne In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the School of Civil and Environmental Engineering Georgia Institute of Technology May 2010 MULTI-CRITERIA ASSESSMENT OF WAVE AND TIDAL POWER ALONG THE ATLANTIC COAST OF THE SOUTHEASTERN USA Approved by: Dr. Kevin Haas, Committee Chair Dr. Emanuele Di Lorenzo School of Civil and Environmental School of Earth and Atmospheric Sciences Engineering Georgia Institute of Technology Georgia Institute of Technology Dr. Dirk Schaefer Dr. Hermann Fritz, Committee Co-Chair School of Mechanical Engineering School of Civil and Environmental Georgia Institute of Technology Engineering Georgia Institute of Technology Date Approved: January 5, 2010 Dr. Paul Work School of Civil and Environmental Engineering Georgia Institute of Technology ACKNOWLEDGMENTS I would like to express my immense gratitude to my advisors Dr. Kevin Haas and Dr. Hermann Fritz for giving me the opportunity to do this research, and for their guidance throughout the entire study. Their invaluable comments are much appreciated. I am deeply thankful to Dr. Haas for his contributions in developing the fundamentals of this study and for his patience during our long discussions. I would like to extend my thanks to Dr. Paul Work, Dr. Emanuele Di Lorenzo and Dr. Dirk Schaefer for serving as the committee members. Their time, effort, and comments are greatly appreciated. A special thanks goes to Dr. John Warner for helping me with my questions on ROMS modeling and my colleague Dr. -
Tidal Theory
TIDAL THEORY 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 dinghy sailors) 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. Causes of Tide To understand tide it 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 C Ocean 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. The main importance of the sun is the effect of either reinforcing the moon’s force or reducing it depending on their positions relative to each other. -
Additions to the Italian Annotated Bibliography on Bluefin Tuna (Thunnus Thynnus, Linnaeus, 1758) and Comprehensive Overview
SCRS/2020/057 Collect. Vol. Sci. Pap. ICCAT, 77(2): 226-274 (2020) ADDITIONS TO THE ITALIAN ANNOTATED BIBLIOGRAPHY ON BLUEFIN TUNA (THUNNUS THYNNUS, LINNAEUS, 1758) AND COMPREHENSIVE OVERVIEW Antonio Di Natale1 SUMMARY After the very first attempt to list together the many papers published so far on bluefin tuna (Thunnus thynnus) by Italian scientists, concerning the biology of this species, the fisheries and many other scientific and cultural issues, it was necessary to prepare an addition to the annotated bibliography published in 2019. Therefore, the present paper provides 351 additional papers, all annotated with specific key words, which brings the available papers on this species up to 2100, all duly annotated. This paper also provides an overview of the papers published over the centuries and decades, the main authors and the score of the main topics and themes included in the papers. This updated bibliography was set together to serve the scientists and to help them in finding some rare references that might be useful for their work. RÉSUMÉ Après la première tentative d’établir une liste des nombreux articles publiés à ce jour sur le thon rouge (Thunnus thynnus) par des scientifiques italiens, concernant la biologie de cette espèce, la pêche et bien d'autres questions scientifiques et culturelles, un complément à la bibliographie annotée publiée en 2019 s’est avéré nécessaire. Par conséquent, le présent document fournit 351 articles supplémentaires, tous annotés avec des mots clés spécifiques, ce qui porte à 2100 le nombre d'articles disponibles sur cette espèce, tous dûment annotés. Ce document fournit également un aperçu des articles publiés au cours des siècles et des décennies, les principaux auteurs et la note des principaux sujets et thèmes inclus dans ceux-ci. -
Coastal Impressions
CoastalA Photographic Journey Impressions along Alaska’s Gulf Coast i Exhibit compiled by Susan Saupe, Mandy Lindeberg, and Dr. G. Carl Schoch Photographs selected by Mandy Lindeberg and Susan Saupe Photo editing and printing by Mandy Lindeberg Photo annotations by Dr. G. Carl Schoch Booklet prepared by Susan Saupe with design services by Fathom Graphics, Anchorage Photo mounting and laminating by Digital Blueprint, Anchorage Digital Maps for Exhibit and Booklet prepared by GRS, Anchorage January 2012 Second Printing November 2012 Exhibit sponsored by Cook Inlet RCAC and developed in partnership with NMFS AFSC Auke Bay Laboratories, and Alaska ShoreZone Program. ii Acknowledgements This exhibit would not exist without the vision of Dr. John Harper of Coastal and Ocean Resources, Inc. (CORI), whose role in the development and continued refinement of ShoreZone has directly led to habitat data and imagery acquisition for every inch of coastline between Oregon and the Alaska Peninsula. Equally important, Mary Morris of Archipelago Marine Research, Inc. (ARCHI) developed the biological component to ShoreZone, participated in many of the Alaskan surveys, and leads the biological habitat mapping efforts. CORI and ARCHI have provided experienced team members for aerial survey navigation, imaging, geomorphic and biological narration, and habitat mapping, each of whom contributed significantly to the overall success of the program. We gratefully acknowledge the support of organizations working in partnership for the Alaska ShoreZone effort, including over 40 local, state, and federal agencies and organizations. A full list of partners can be seen at www.shorezone.org. Several organizations stand out as being the earliest or staunchest supporters of a comprehensive Alaskan ShoreZone program. -
Seascape Character Assessment Report
Seascape Character Assessment for the South West Inshore and Offshore marine plan areas MMO 1134: Seascape Character Assessment for the South West Inshore and Offshore marine plan areas September 2018 Report prepared by: Land Use Consultants (LUC) Project funded by: European Maritime Fisheries Fund (ENG1595) and the Department for Environment, Food and Rural Affairs Version Author Note 0.1 Sally First draft desk-based report completed May 2016 Marshall Maria Grant 1.0 Sally Updated draft final report following stakeholder Marshall/ consultation, August 2018 Kate Ahern 1.1 Chris MMO Comments Graham, David Hutchinson 2.0 Kate Ahern Final Report, September 2018 2.1 Chris Independent QA Sweeting © Marine Management Organisation 2018 You may use and re-use the information featured on this website (not including logos) free of charge in any format or medium, under the terms of the Open Government Licence. Visit www.nationalarchives.gov.uk/doc/open-government- licence/ to view the licence or write to: Information Policy Team The National Archives Kew London TW9 4DU Email: [email protected] Information about this publication and further copies are available from: Marine Management Organisation Lancaster House Hampshire Court Newcastle upon Tyne NE4 7YH Tel: 0300 123 1032 Email: [email protected] Website: www.gov.uk/mmo Disclaimer This report contributes to the Marine Management Organisation (MMO) evidence base which is a resource developed through a large range of research activity and methods carried out by both MMO and external experts. The opinions expressed in this report do not necessarily reflect the views of MMO nor are they intended to indicate how MMO will act on a given set of facts or signify any preference for one research activity or method over another. -
Location Guidance.Pdf
PART 2: REGIONAL LOCATIONAL GUIDANCE FOR MARINE ENERGY 101 SECTION 1: INTRODUCTION TO REGIONAL LOCATIONAL GUIDANCE FOR MARINE ENERGY FOCUS OF THE REGIONAL LOCATIONAL GUIDANCE (RLG) FOR MARINE 100m. It is recognised that depths greater than 60m may be a current ENERGY economic/practical limit for seabed tidal devices, but deeper deployments may be viable. Wave devices are capable of significantly greater water depth deployment The Regional Locational Guidance (RLG) for Marine energy (wave and tidal due to the use of moorings. stream energy) has been prepared in support of the MSP Framework and the rapid increase in interest in the development of wave and tidal energy within the Tidal devices operating in water depths of less than 30m may be feasible in areas Pentland Firth. where vessel movements may be excluded or where development of the device results in a very low height requirement. The aims of the RLG are twofold: Bathymetry information has been obtained from UKHO admiralty chart data 1. Provide guidance to marine renewable energy developers on potential (Seazone). Given the age and limited sounding information used to form these areas of opportunity for future development and to highlight likely requirements for charts, it is likely that there are areas where the actual bathymetry may vary surveys, monitoring or interactions with existing uses that may be issues for significantly from that currently recorded. development. Tidal current information has been based on a hydrodynamic model operated by 2. Progress the marine spatial planning process in a way which enables Metoc based on a 200m rectilinear grid. The model is adequate for identifying the stakeholders and decision makers to respond to the rapid increase in interest in main resource areas but may be too coarse for the inter-island areas with narrow marine renewable energy developments whilst enabling ‘issues’ relating to other channels and poorly resolved bathymetry data.