Perigean Spring Tide in Loughborough Inlet, 1792
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Flood Mitigation and Sea Level Rise Adaptation for Kiawah Island: a Report
Flood Mitigation and Sea Level Rise Adaptation for Kiawah Island: A Report Story and photographs by Jack Kotz unny day or nuisance flooding is a relatively new term for most of us. As we described in the Winter/Spring 2018 issue of Naturally Kiawah, it refers to temporary flooding of low-lying areas in the absence of any precipitation or storm impacts, usually occurring during new or full moons. The higher than usual tides during these lunar periods are called “spring Stides.” Several times a year, when the new or full moon is closest to the Earth (at its perigee), the gravitational force is even greater. This causes a “king tide” or a “perigean spring tide” that often results in nuisance flooding. 16 The problem for Charleston and other coastal cities, as annual flooding. He estimates that in the next 50 years flooding well as Kiawah Island, is that the number of nuisance floods will be experienced by 15 percent of the buildings in the area. is increasing. In the 1970s there were only about two days On Kiawah, we experienced 16–20 inches of rainfall over a each year with nuisance floods in Charleston, whereas in 2015 four-day period in the 2015 rain event, and at least 42 percent Charleston had 38 days of tidal flooding, and in 2016 there of the land area of the Island was flooded. During Hurricane were 50 days of flooding. It is predicted there could be as Matthew in 2016, the storm tide was 3.5 feet above MHHW many as 180 days of flooding per year in the 2040s. -
British Columbia Regional Guide Cat
National Marine Weather Guide British Columbia Regional Guide Cat. No. En56-240/3-2015E-PDF 978-1-100-25953-6 Terms of Usage Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: • Exercise due diligence in ensuring the accuracy of the materials reproduced; • Indicate both the complete title of the materials reproduced, as well as the author organization; and • Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1-800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Disclaimer: Her Majesty is not responsible for the accuracy or completeness of the information contained in the reproduced material. Her Majesty shall at all times be indemnified and held harmless against any and all claims whatsoever arising out of negligence or other fault in the use of the information contained in this publication or product. Photo credits Cover Left: Chris Gibbons Cover Center: Chris Gibbons Cover Right: Ed Goski Page I: Ed Goski Page II: top left - Chris Gibbons, top right - Matt MacDonald, bottom - André Besson Page VI: Chris Gibbons Page 1: Chris Gibbons Page 5: Lisa West Page 8: Matt MacDonald Page 13: André Besson Page 15: Chris Gibbons Page 42: Lisa West Page 49: Chris Gibbons Page 119: Lisa West Page 138: Matt MacDonald Page 142: Matt MacDonald Acknowledgments Without the works of Owen Lange, this chapter would not have been possible. -
Basics of Tide & Tide Forecasting
Basics of tide & tide forecasting K. Srinivas Ocean State Forecast Lab (ISG) INCOIS, Hyderabad E-mail: [email protected] Phone: 040-23886057 040-23895017 Time and TIDE wait for none !!! Tides are an important physical forcing on the ocean particularly the coastal and estuarine seas ! Tide is the periodic rise and fall of a body of water due to gravitational interactions between the sun, moon and Earth Different positions of the sun and moon create two different types of tides: spring tides and neap tides Residual force is the difference between the gravitational force and centrifugal force They are very important for a proper understanding of : physics, chemistry, biology and geology of the coastal and estuarine waters The same location in the High Tide Low Tide Bay of Fundy at low and high tide. The maximum tidal range is approximately 17m The tidal range is the vertical difference between the low tide and the succeeding high tide. High Tide April 20, 2001 Low Tide September 30, 2002 Tidal extremes - The Bay of Fundy Vegetation is green, and water ranges from dark blue (deeper water) to light purple (shallow water) Tides at Halls Harbour on Nova Scotia's Bay of Fundy. This is a time lapse of the tidal rise and fall over a period of six and a half hours. There are two high tides every 25 hours. Presence of tide The most obvious indication of the presence of tide at any location (coastal or deep sea) is a characteristic, sinusoidal oscillation in the water level/ pressure records, containing either two main cycles per day (semidiurnal tides), one cycle per day (diurnal tides), or a combination of the two (mixed tides). -
Development of an Updated Coastal Marine Area Boundary for the Auckland Region
Development of an updated Coastal Marine Area boundary for the Auckland Region Prepared for Auckland Council July 2012 Authors/Contributors : Scott Stephens Sanjay Wadhwa For any information regarding this report please contact: Scott Stephens Coastal Scientist Coastal and Estuarine Processes +64-7-856 7026 [email protected] National Institute of Water & Atmospheric Research Ltd Gate 10, Silverdale Road Hillcrest, Hamilton 3216 PO Box 11115, Hillcrest Hamilton 3251 New Zealand Phone +64-7-856 7026 Fax +64-7-856 0151 NIWA Client Report No: HAM2012-111 Report date: July 2012 NIWA Project: ARC13233 © All rights reserved. This publication may not be reproduced or copied in any form without the permission of the copyright owner(s). Such permission is only to be given in accordance with the terms of the client’s contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Whilst NIWA has used all reasonable endeavours to ensure that the information contained in this document is accurate, NIWA does not give any express or implied warranty as to the completeness of the information contained herein, or that it will be suitable for any purpose(s) other than those specifically contemplated during the Project or agreed by NIWA and the Client. Contents Executive summary .......................................................................................................................7 1 Introduction ........................................................................................................................9 -
Rockfish Conservation Areas
ROCKFISH CONSERVATION AREAS Protecting British Columbia’s Rockfish Yelloweye rockfish Quillback rockfish Copper rockfish China rockfish Tiger rockfish (Sebastes ruberrimus) (Sebastes maliger) (Sebastes caurinus) (Sebastes nebulosus) (Sebastes nigrocinctus) Inshore rockfish identification Yelloweye rockfish (Sebastes ruberrimus) are pink to orangey red in colour with bright yellow eyes. Juvenile fish are a darker red with two white stripes along the sides. These stripes fade as the fish grows and large fish may have one or no white stripe along the lateral line. There are two prominent ridges on the top of the head. Fins may be fringed in black. Found in steep rocky reef and boulder habitats from 50 m to 550 m in depth but most common in 150 m (82 fa) depths. Maximum length up to 91 cm (36 in). Quillback rockfish (Sebastes maliger) are dark brownish black, mottled with orangey yellow. The lower anterior portion of the body is speckled brown. Dorsal fin spines are very high and moderately notched. The body is deep. Found in rocky habitats from the subtidal to 275 m in depth but most common between 50 m and 100 m (55 fa) in depth. Maximum length up to 61 cm (24 in). Copper rockfish (Sebastes caurinus) are brown to copper in colour with pink or yellow blotches. A white stripe runs along the lateral line on the anterior two thirds of the body. Two dark, sometimes yellow, bars radiate from the eye. Found in kelp beds and rock to gravel habitats from the subtidal to 180 m in depth but most common in water less than 40 m (22 fa). -
What Is High Tide Flooding?
https://oceanservice.noaa.gov/facts/high-tide-flooding.html%20 Examples of why Highway 80 going out to Tybee Islands floods and low-lying areas throughout Savannah where the coastal waters connect with elevations near 6 NAVD 1988. National Ocean ServiceNational Oceanic and Atmospheric AdministrationU.S. Department of Commerce SearchSearch National Ocean Service • HOMEHome 1. Facts 2. What is high tide flooding? What is high tide flooding? High tide flooding—flooding that leads to public inconveniences such as road closures — is increasingly common as coastal sea levels rise. High tide flooding events have increased around the U.S., but especially off the East Coast. To down load the image click on: | Download PDF As relative sea level increases, it no longer takes a strong storm or a hurricane to cause coastal flooding. Flooding now occurs with high tides in many locations due to climate- related sea level rise, land subsidence, and the loss of natural barriers. High tide flooding — which causes such public inconveniences as frequent road closures, overwhelmed storm drains and compromised infrastructure — has increased in the U.S. on average by about 50 percent since 20 years ago and 100 percent since 30 years ago. The effects of rising sea levels along most of the continental U.S. coastline are expected to become more noticeable and much more severe in the coming decades, likely more so than any other climate-change related factor. Any acceleration in sea level rise that is https://oceanservice.noaa.gov/facts/high-tide-flooding.html%20 predicted to occur this century will further intensify high tide flooding impacts over time, and will further reduce the time between flood events. -
INTERNAL DOCUMENT Tide, Surge and Still Water Levels at Chesil Beach. Graham Alcock. Institute of Oceanographic Sciences Bidston
INTERNAL DOCUMENT 2/0 Tide, Surge and Still Water Levels at Chesil Beach. Graham Alcock. Institute of Oceanographic Sciences Bidston Observatory Birkenhead. June 1984. [This document should not be cited in a published bibliography, and is supplied for the use of the recipient only]. INSTITUTE OF \ OCEANOGRAPHIC SCIENCES ''loi INSTITUTE OF OCEANOGRAPHIC SCIENCES Wormley, Godalming, Surrey GU8 5UB (042-879-4141) (Director: Dr. A. S. Laughton) Bidston Observatory, Crossway, Birkenhead, Taunton, Mersey side L43 7RA Somerset TA1 2DW (051-653-8633) (0823-86211) (Assistant Director: Dr. D. E. Cartwright) (Assistant Director: M.J. Tucker) \ Tide, Surge and Still Water Levels at Chesil Beach. Graham A1cock. Institute of Oceanographic Sciences Bidston Observatory Birkenhead. June 1984. Internal Document No. 210. "This information or advice is given in good faith and is believed to be correct, but no responsibility can be accepted by the Natural Environment Research Council for any consequential loss or damage arising from any use that is made of it." 1. Introduction C.H. Dobbie (CHD) are acting as Consulting Engineers on a project concerning shore processes and protection at Chesil Beach, in conjunction with the Department of Civil Engineering at Imperial College, Hydraulics Research Ltd., Wessex Water Authority and Ministry of Agriculture, Fisheries and Food. CHD need to supply HRS with estimates of still water level (i.e. tide + surge) during the flood events of 13 December 1978, 13 February 1979» 20 December 1983s and 26 January 1984. lOS were commissioned by CHD to provide and prepare a pressure gauge for deployment off of Chesil Beach, to process and analyse the record to yield tide and surge statistics, and to hindcast levels for the flood events. -
Tide 1 Tides Are the Rise and Fall of Sea Levels Caused by the Combined
Tide 1 Tide The Bay of Fundy at Hall's Harbour, The Bay of Fundy at Hall's Harbour, Nova Scotia during high tide Nova Scotia during low tide Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun and the rotation of the Earth. Most places in the ocean usually experience two high tides and two low tides each day (semidiurnal tide), but some locations experience only one high and one low tide each day (diurnal tide). The times and amplitude of the tides at the coast are influenced by the alignment of the Sun and Moon, by the pattern of tides in the deep ocean (see figure 4) and by the shape of the coastline and near-shore bathymetry.[1] [2] [3] Most coastal areas experience two high and two low tides per day. The gravitational effect of the Moon on the surface of the Earth is the same when it is directly overhead as when it is directly underfoot. The Moon orbits the Earth in the same direction the Earth rotates on its axis, so it takes slightly more than a day—about 24 hours and 50 minutes—for the Moon to return to the same location in the sky. During this time, it has passed overhead once and underfoot once, so in many places the period of strongest tidal forcing is 12 hours and 25 minutes. The high tides do not necessarily occur when the Moon is overhead or underfoot, but the period of the forcing still determines the time between high tides. -
Scale Site SS Region SS District Site Name SS Location Phone
Scale SS SS Site Region District Site Name SS Location Phone 001 RCB DQU MISC SITES SIFR 01B RWC DQC ABFAM TEMP SITE SAME AS 1BB 2505574201 1001 ROM DPG BKB CEDAR Road past 4G3 on the old Lamming Ce 2505690096 1002 ROM DPG JOHN DUNCAN RESIDENCE 7750 Lower Mud river Road. 1003 RWC DCR PROBYN LOG LTD. Located at WFP Menzies#1 Scale Site 1004 RWC DCR MATCHLEE LTD PARTNERSHIP Tsowwin River estuary Tahsis Inlet 2502872120 1005 RSK DND TOMPKINS POST AND RAIL Across the street from old corwood 1006 RWC DNI CANADIAN OVERSEAS FOG CREEK - North side of King Isla 6046820425 1007 RKB DSE DYNAMIC WOOD PRODUCTS 1839 Brilliant Road Castlegar BC 2503653669 1008 RWC DCR ROBERT (ANDY) ANDERSEN Mobile Scale Site for use in marine 1009 ROM DPG DUNKLEY- LEASE OF SITE 411 BEAR LAKE Winton Bear lake site- Current Leas 2509984421 101 RWC DNI WESTERN FOREST PRODUCTS INC. MAHATTA RIVER (Quatsino Sound) - Lo 2502863767 1010 RWC DCR WESTERN FOREST PRODUCTS INC. STAFFORD Stafford Lake , end of Loughborough 2502863767 1011 RWC DSI LADYSMITH WFP VIRTUAL WEIGH SCALE Latitude 48 59' 57.79"N 2507204200 1012 RWC DNI BELLA COOLA RESOURCE SOCIETY (Bella Coola Community Forest) VIRT 2509822515 1013 RWC DSI L AND Y CUTTING EDGE MILL The old Duncan Valley Timber site o 2507151678 1014 RWC DNI INTERNATIONAL FOREST PRODUCTS LTD Sandal Bay - Water Scale. 2 out of 2502861881 1015 RWC DCR BRUCE EDWARD REYNOLDS Mobile Scale Site for use in marine 1016 RWC DSI MUD BAY COASTLAND VIRTUAL W/S Ladysmith virtual site 2507541962 1017 RWC DSI MUD BAY COASTLAND VIRTUAL W/S Coastland Virtual Weigh Scale at Mu 2507541962 1018 RTO DOS NORTH ENDERBY TIMBER Malakwa Scales 2508389668 1019 RWC DSI HAULBACK MILLYARD GALIANO 200 Haulback Road, DL 14 Galiano Is 102 RWC DNI PORT MCNEILL PORT MCNEILL 2502863767 1020 RWC DSI KURUCZ ROVING Roving, Port Alberni area 1021 RWC DNI INTERNATIONAL FOREST PRODUCTS LTD-DEAN 1 Dean Channel Heli Water Scale. -
Chapter 12. Johnstone Strait Region
Chapter 12. Johnstone Strait Region The complex system of waterways that extends sea- environment. Experience has demonstrated, for example, ward from the northern end of the Strat of Georgia that the channels ofthe Johnstone Strait region form a key provides access to some of the most spectacular scenery on link in the migration route of Pacific salmon. Indicative of the British Columbia coast. Snow-capped mountain this importance is the fact that fypically 10-20% of Eraser peaks, cascading waterfalls, steep-sided channels, and sur- River sockeye salmon that return to the coast every 4 yr ging tidal narrows contribute to a stark ruggedness (Fig. enter the river via Johnstone Strait rather than Juan de 12.1).Settlements are few and far between, but wildlife is Fuca Strait. In certain years of the 4yr cyde, this ‘‘hver- abundant, and it is not uncommon to see a pod of killer sion” of salmon through the northern passages is close to whales or a school of porpoises movin easily through the half the returning run. In 1978, for example, approx- cMy waters. The large numbers ofkiller whales that imately 57% of the run chose this route rather than Juan frequently gather in Robson Bight, at the western end of de Fuca Strait, and in 1980 there was a record diversion of Johnstone Suait, create an impressive sight, unequalled in 70%. few areas of the coast. Because the three main channels carry most of the water that flows between the Pacific Ocean and the north- em end of the Strait of Georgia, they further influence the physical oceanographic structure of the inside passage and adjoining fiords. -
Coastal Resilience Forum 2/12/2020 Notes
Coastal Resilience Forum 2/12/2020 Notes Dr. Cheryl Hapke, USF College of Marine Science A Unified Approach to Mapping Florida’s Coastal Waters: Process and Applications • Dr. Cheryl Hapke, Research Professor at the University of South Florida, College of Maine Science and coordinator of the Florida Coastal Mapping Program (FCMaP), will present on the data inventory, gap analysis, and statewide prioritization accomplished over the past 2 years by the program. FCMaP is a Federal-State partnership working to provide modern, uniform, high resolution seafloor data for all of Florida’s coastal waters in the next decade. Applications of the data include improving storm surge forecasts and coastal hazard assessments that are integral to sea level rise adaptation planning. Cheryl announced that the Coastal Mapping Summit will be held March 31, 2020 in St. Petersburg at FWRI. Registration ends February 25. https://www.eventbrite.com/e/fcmap-2020-florida-coastal-mapping-summit-tickets-90958245561 • The story map for the Florida Coastal Mapping Program can be found at arcg.is/1Of0OT0 • FCMaP has aligned their sea level rise adaptation planning guidance with the Florida Adaptation Planning Guidebook. Paul Fanelli, NOAA NOAA’s Inundation Dashboard • Paul Fanelli, Lead Oceanographer with the Data Monitoring and Assessment Team, at NOAA’s Center for Operational Oceanographic Products and Services will present the new National Ocean Service (NOS) Coastal Inundation Dashboard web mapping tool. This application pulls together historical flooding information at NOS long-term water level stations along with real-time water level data, which can be used to monitor coastal inundation with causes ranging from high tide flooding to storm surge resulting from tropical cyclones. -
Oceanography of the British Columbia Coast
CANADIAN SPECIAL PUBLICATION OF FISHERIES AND AQUATIC SCIENCES 56 DFO - L bra y / MPO B bliothèque Oceanography RI II I 111 II I I II 12038889 of the British Columbia Coast Cover photograph West Coast Moresby Island by Dr. Pat McLaren, Pacific Geoscience Centre, Sidney, B.C. CANADIAN SPECIAL PUBLICATION OF FISHERIES AND AQUATIC SCIENCES 56 Oceanography of the British Columbia Coast RICHARD E. THOMSON Department of Fisheries and Oceans Ocean Physics Division Institute of Ocean Sciences Sidney, British Columbia DEPARTMENT OF FISHERIES AND OCEANS Ottawa 1981 ©Minister of Supply and Services Canada 1981 Available from authorized bookstore agents and other bookstores, or you may send your prepaid order to the Canadian Government Publishing Centre Supply and Service Canada, Hull, Que. K1A 0S9 Make cheques or money orders payable in Canadian funds to the Receiver General for Canada A deposit copy of this publication is also available for reference in public librairies across Canada Canada: $19.95 Catalog No. FS41-31/56E ISBN 0-660-10978-6 Other countries:$23.95 ISSN 0706-6481 Prices subject to change without notice Printed in Canada Thorn Press Ltd. Correct citation for this publication: THOMSON, R. E. 1981. Oceanography of the British Columbia coast. Can. Spec. Publ. Fish. Aquat. Sci. 56: 291 p. for Justine and Karen Contents FOREWORD BACKGROUND INFORMATION Introduction Acknowledgments xi Abstract/Résumé xii PART I HISTORY AND NATURE OF THE COAST Chapter 5. Upwelling: Bringing Cold Water to the Surface Chapter 1. Historical Setting Causes of Upwelling 79 Origin of the Oceans 1 Localized Effects 82 Drifting Continents 2 Climate 83 Evolution of the Coast 6 Fishing Grounds 83 Early Exploration 9 El Nifio 83 Chapter 2.