Canadian Engineer Creates Biggest Explosions in the World
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Statistical Models of Cloud-Turbulence Interactions
Statistical Models of Cloud-Turbulence Interactions by Christopher A. M. Jeffery M.Sc, University of British Columbia, 1996 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Doctor of Philosophy in THE FACULTY OF GRADUATE STUDIES (Department of Earth and Ocean Sciences) We accept this thesis as conforming to the required standard The University of British Columbia September 2001 © Christopher A. M. Jeffery, 2001 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department The University of British Columbia Vancouver, Canada DE-6 (2/88) Abstract The application of statistical turbulence theory to the study of atmospheric clouds has a long history that traces back to the pioneering work of L. F. Richardson in the 1920s. At a phenomenological level, both atmospheric clouds and turbulence are now well understood, but analytic theories with the power to predict as well as explain are still lacking. This deficiency is notable because the prediction of statistical cloud change in response to anthropogenic forcing is a preeminent scientific challenge in atmospheric science. In this dissertation, I apply the statistical rigor of new developments in passive scalar theory to problems in cloud physics at small scales (9(10 cm), where a white- in-time or (^-correlated closure is asymptotically exact, and at large scales 0(100 km) where a statistical approach towards unresolved cloud variability is essential. -
Tidal Currents – Capt. Geoff the Waters
Tidal Currents – Capt. Geoff The waters around Campbell River are among the most beautiful in the world. There are hundreds of miles of sheltered channels surrounded by majestic mountain views. There is fishing, diving, whale, bear and other wildlife watching; as well as beachcombing opportunities almost everywhere. However this same geography creates special challenges. Where the channels are constricted, the currents are among the strongest in the world. Where even moderate currents occur in semi-open waters, small wind driven waves can be changed into steep, dangerous breaking seas. But with knowledge these dangers can be avoided and even turned to advantage. --------- Introduction to currents For people on the water, in this area of narrow channels, tidal currents can be as important or even more important as tide height. In constricted areas such as Seymour Narrows, currents can reach almost 16 knots (almost 30kph). And it is not just the current strength that is the problem when transiting. As the shoreline and bottom are often not smooth or straight, water gushing through these narrow passages creates cross currents, eddies, whirlpools and upwellings that can throw even a larger vessel around quite violently. What can cause confusion when planning your voyage, is that the time of high or low water (when the water level stops rising or falling) can be several hours different from "slack" water (when the horizontal motion ceases). And the time of both high/low water and slack water changes as you move up or down the channels. For me, the way to make sense of it, is to think of a long ditch running into a pond at one end. -
Assessing the Site Potential for Underwater Turbines in Tidal Channels Using Numerical Modeling and Advanced Ocean Current Measurements
Assessing the Site Potential for Underwater Turbines in Tidal Channels Using Numerical Modeling and Advanced Ocean Current Measurements David B. Fissel, Jianhua Jiang, Rick Birch, Jan Buermans and David Lemon ASL Environmental Sciences Inc., 1986 Mills Rd., Sidney, BC, V8L 5Y3, Canada, Phone Number (250) 656-0177, [email protected] Abstract -A combination of advanced ocean current profiling level differences exist between two sides of the dam with the measurements and high resolution 3D numerical models was maximum heads up to 1.5 m during spring tides and 0.8 m used to assess site potential for underwater turbines in tidal during neap tides. The difference in water levels on either channels of the inland waters off the coast of British Columbia, side of the dam has the potential for significant renewable Canada. The measurements involved the use of ADCP transects energy through installation of underwater turbines for through potential sites. Due to the very strong tidal currents of up to 10 knots or more, special procedures are required to generating electrical power. Numerical modeling simulations generate accurate and reliable maps of the very strong ocean of the currents and water levels were conducted, including the currents. The three-dimensional, coastal circulation model present conditions for model calibration and verification, COCIRM was used to map these detailed flows under different possible future conditions in which the dam is completely scenarios and assess the potential at various sites for operation removed and the Pass is restored to its original configuration, of underwater turbines after validated using available water and possible future conditions in which the dam is partially elevation and ocean current data. -
1 Applications of 3D Coastal Circulation Numerical Model In
Applications of 3D Coastal Circulation Numerical Model in Assessing Potential locations of Installing Underwater Turbines1 Jianhua Jiang2, David B. Fissel1 Abstract The three-dimensional, coastal circulation numerical model COCIRM-SED was recently adapted and optimized to simulate and predict the flows in southern Discovery Passage and Canoe Pass, BC, Canada. These model results provided reliable, detailed flow information for use in assessing potential locations of installing and operating underwater tidal current turbines. In the application of modeling flows in southern Discovery Passage, the model involved tidal forcing with 69 constituents at open boundaries as well as the effects of the Campbell River freshwater input and the Coriolis. Detailed hourly model flows for typical neap and spring tides were extracted for use in the site assessment of potential locations for tidal current turbines. In the other application of modeling flows in Canoe Pass, the model was used to predict the water flows and water levels through Canoe Pass if the dam in Canoe Pass, which has been in place since the 1940’s, were completely removed and replaced by a passage of 40 m wide between Quadra and Maude Islands. In both studies, the model went through extensive calibration and verification processes using available measurements of water levels and ocean currents at various sites in the modeling areas. It was demonstrated that the 3D model has very good capabilities for simulating water level and currents in both model areas under different conditions. Introduction Electricity generation using underwater turbines in areas of strong tidal currents can provide a very dependable and predictable source of clean and renewable energy, often with minimal and/or mitigatible impact on the natural environment. -
High Resolution 3-D Finite-Volume Coastal Ocean Modeling in Lower Campbell River and Discovery Passage, British Columbia, Canada
J. Mar. Sci. Eng. 2014, 2, 209-225; doi:10.3390/jmse2010209 OPEN ACCESS Journal of Marine Science and Engineering ISSN 2077-1312 www.mdpi.com/journal/jmse Article High Resolution 3-D Finite-Volume Coastal Ocean Modeling in Lower Campbell River and Discovery Passage, British Columbia, Canada Yuehua Lin * and David B. Fissel ASL Environmental Sciences Inc., #1-6703 Rajpur Place, Victoria, British Columbia, V8M 1Z5, Canada; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-250-656-0177 (ext. 146); Fax: +1-250-656-2162. Received: 10 December 2013; in revised form: 1 February 2014 / Accepted: 19 February 2014 / Published: 19 March 2014 Abstract: The 3-D unstructured-grid, Finite-Volume Coastal Ocean Model (FVCOM) was used to simulate the flows in Discovery Passage including the adjoining Lower Campbell River, British Columbia, Canada. Challenges in the studies include the strong tidal currents (e.g., up to 7.8 m/s in Seymour Narrows) and tailrace discharges, small-scale topographic features and steep bottom slopes, and stratification affected by the Campbell River freshwater discharges. Two applications of high resolution 3-D FVCOM modeling were conducted. One is for the Lower Campbell River extending upstream as far as the John Hart Hydroelectric dam. The horizontal resolution varies from 0.27 m to 32 m in the unstructured triangular mesh to resolve the tailrace flow. The bottom elevation decreases ~14 m within the distance of ~1.4 km along the river. This pioneering FVCOM river modeling demonstrated a very good performance in simulating the river flow structures. -
Final Interim Version of the Seymour Narrows Guidelines Section 1
Final interim version of the Seymour Narrows Guidelines Section 1. Fishing vessel recommendations Proposed changes Comments 1) The 2003 Advisory from Canadian Coast Guard should be adopted as a solution with the following suggested additions: a. All vessels over 24m in length should participate in the Vessel Traffic System. b. Concentrations of cruise ships can be expected from April to October in the Seymour Narrows area during slack water periods. c. At times north bound commercial traffic will use Race Passage. 2) All vessels should monitor the VTS operating channel for the area. A copy of the Amended 2003 Advisory is attached as Appendix 1. 1 | P a g e Section 2. Tugs and tow recommendations Proposed changes Comments 1) The 2003 Advisory from Canadian Coast Guard should be adopted as a solution. 2) All vessels should monitor the operational VTS channel for the area. 3) All tugs should provide MCTS with an ETA for Maude Island. 4) The Pacific Pilotage Authority will provide both US and Canadian tug operators with a detailed schedule of cruise vessel passages planned for Seymour Narrows, prior to the beginning of each cruise season and posted on the Pilotage Authority website. The schedule will be kept up to date as required. 5) Tugs should take note of the order of passage arranged by the pilots of the cruise ship. 6) Tug operators should fully consider the rules of the road as well as the intentions of the cruise vessels and then broadcast intentions for their passage on the VTS channel. 2 | P a g e Section 3. -
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. -
Ripple Rock Estates 1127921 BC Ltd
Strathcona REGIONAL DISTRICT STAFF REPORT DATE: February 5, 2021 FILE: 0540-04 Board TO: Chair and Directors Regional District Board FROM: Dave Leitch Chief Administrative Officer RE: CITY OF CAMPBELL RIVER DEVELOPMENT PROPOSAL (RIPPLE ROCK ESTATES) PURPOSE To consider further information concerning the proposed Ripple Rock Estates development that was previously referred to the Regional District by the City of Campbell River. POLICY ANALYSIS At its June 10, 2020 meeting the Board considered the attached report and passed the following resolution: Adams/Kerr: SRD 437/20 THAT the City of Campbell River be advised that the SRD supports in principal the proposal pending advice received from the Ministry of Transportation and Infrastructure regarding the primary access route, a subsequent traffic impact study is submitted and the development receives preliminary senior government approval for the proposed community sanitary sewer and water systems. EXECUTIVE SUMMARY Since the Board last considered the proposal for a 34.4 hectare (85.0 acre) 193 lot residential resort community known as Ripple Rock Estates the bylaw has received first and second readings and was the subject of a public hearing conducted on January 25, 2021. Information related to the Board's June 10, 2020 resolution was provided through an email from City staff on January 26, 2021 in which the SRD was advised that the Ministry of Environment and Climate Change Strategy has 'received in a form and manner acceptable to the director' the wastewater treatment and discharge proposal, a subsequent traffic impact study was submitted and MoTI requires the construction of a deceleration/right turn lane for the northbound right turn vehicles. -
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. -
M2 Tidal Dissipation Around Vancouver Island: an Inverse Approach
ARTICLE IN PRESS Continental Shelf Research 24 (2004) 2167–2185 www.elsevier.com/locate/csr M2 tidal dissipation around Vancouver Island: an inverse approach M.G.G. ForemanÃ, G. Sutherland, P.F. Cummins Department of Fisheries and Oceans, Institute of Ocean Sciences, P.O. Box 6000, Sidney, BC, Canada V8L 4B2 Available online 11 September 2004 Abstract A representer approach is used to assimilate M2 tide gauge harmonics into a high-resolution two-dimensional finite element model of Puget Sound and the waters surrounding Vancouver Island. A preliminary model solution which employs a conventional drag coefficient for quadratic bottom friction is shown to produce elevation amplitudes and phases that differ significantly from the harmonics computed from an analysis of tide gauge observations. The assimilation procedure not only rectifies this problem but also shows that this better fit implies significant momentum equation residuals in regions where strong turbulent mixing and internal tide generation are known to occur. Thus, the assimilation identifies regions where dissipation beyond conventional bottom friction is required. Computed dissipation rates arising from these residuals reveal the largest energy sinks to be in the Gulf and San Juan Islands, Juan de Fuca Strait, and the channels off northeast Vancouver Island. Crown Copyright r 2004 Published by Elsevier Ltd. All rights reserved. Keywords: Tides; Modelling; Assimilation; Representers 1. Introduction (Crean et al., 1988; Stronach, 1991; Foreman et al., 1995 (henceforth F95); Foreman and Thomson, This paper describes the assimilation of M2 tide 1997; Cummins et al., 2000) and a circulation gauge harmonics into a high-resolution, two- model covering approximately the same domain dimensional (2D), tidal model of Puget Sound has been developed to study the buoyancy flows and the waters surrounding Vancouver Island (Masson and Cummins, 2000), this is the first (Fig. -
Ripple Rock Trail
Ripple Rock Trail Ripple Rock Trail This trail was designed for hikers and is not Ripple Rock Trail suitable for those on horseback, mountain bike, motorcycle, ATV or four wheel drive. Quadra Island Please help make this hiking experience Menzies Creek enjoyable for everyone. 1" W 24' 1 o 125 Seymour 50o 08' 14" N Narrows Sayward 56 km Vancouver Island Menzies Maud Bay Ripple Rock Island Explosion Location Nymphe Cove 19 BC Wilfred Point MAP LEGEND Stephenson N Point PARKING Campbell River 16 km PICNIC TABLE W E VIEWPOINT TRAIL S BRIDGE endy Ravai 0 250 500 750 1000 19 HIGHWAY Scale in metres BC Photo - W Difficulty: Easy to moderate Please report all forest fires. Phone toll-free: 1 800 663 5555 Hiking Length: 8.0 km (round trip) Time: 2.5 - 3.0 hours (round trip) For More Information Recreation Sites and Trails Branch Access: The Ripple Rock Trail head is located just off Email: [email protected] highway 19 approximately 16 km north of Campbell River. Ph: 250 286-9300 There is a turn off from the highway to a parking lot, www.sitesandtrailsBC.ca which is visible from the highway. Please lock vehicles and store valuables out of site. Picnic Areas: There are three picnic areas located on the trail, one at the beach, one at the first lookout and Menzies Bay as seen from second viewpoint one near the last viewpoint. In April of 1995, the old wooden towers supporting the power lines across Seymour Narrows were replaced by taller, steel Ripple Rock Trail towers. -
Illdal ACTION in BRITISH COLUMBIA HEATERS
illDAL ACTION IN BRITISH COLUMBIA HEATERS 535T CAFt- CHARLES WARREN C^fES ngnrnnBi ym TIDAL ACTION IN 1 BRITISH COLUMBIA WATERS ' By CAPT CHARLES WARREN CATES • • NORTH VANCOUVER CANADA 1952 COPYRIGHT 1952 II 1 This little book which sets out to be the story of the massive, eternal tides is really the story of four men. Authored by one man, Capt. Charles Cates, it was, in the truest sense of the word, inspired also by his father Charles Henry Cates, and his brothers John and James. You will draw much knowledge and pleasure from this book. The information is authentic. Let me tell you why. The three brothers grew, up ^with the tides of British Columbia. The Cates familyjis part of the waterfront here. Old Charles Henry, a beloved figure, was towboating round here before the boys were born,—in 1886. His first "tug" was a twin-screw scow, named Spratt's Ark. What an unbelievable story was her career! He went on from strength to strength, and so the boys as they came along grew up with the tugboating drama. John, Charles, James Cates . shipmaster^ the world over know them, have turned to them for advice and help. You might well do the same by studying this book which contains the knowledge not of one man alone/ but' of four. The information is authentic also because all three brothers are certified master mariners, with a lifelong experience of the movements of the great waters around this coast. But the little book also contains good stories of life on this coast.