Technical Report No. 142
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Gary's Charts
Gary’s Garage Sale - Chart List Chart Number Chart Name Area Scale Condition Price 3410 Sooke Inlet West Coast Vancouver Island 1:20 000 Good $ 10.00 3415 Victoria Harbour East Coast Vancouver Island 1:6 000 Poor Free 3441 Haro Strait, Boundary Pass and Sattelite Channel East Vancouver Island 1:40 000 Fair/Poor $ 2.50 3441 Haro Strait, Boundary Pass and Sattelite Channel East Vancouver Island 1:40 000 Fair $ 5.00 3441 Haro Strait, Boundary Pass and Sattelite Channel East Coast Vancouver Island 1:40 000 Poor Free 3442 North Pender Island to Thetis Island East Vancouver Island 1:40 000 Fair/Poor $ 2.50 3442 North Pender Island to Thetis Island East Vancouver Island 1:40 000 Fair $ 5.00 3443 Thetis Island to Nanaimo East Vancouver Island 1:40 000 Fair $ 5.00 3459 Nanoose Harbour East Vancouver Island 1:15 000 Fair $ 5.00 3463 Strait of Georgia East Coast Vancouver Island 1:40 000 Fair/Poor $ 7.50 3537 Okisollo Channel East Coast Vancouver Island 1:20 000 Good $ 10.00 3537 Okisollo Channel East Coast Vancouver Island 1:20 000 Fair $ 5.00 3538 Desolation Sound & Sutil Channel East Vancouver Island 1:40 000 Fair/Poor $ 2.50 3539 Discovery Passage East Coast Vancouver Island 1:40 000 Poor Free 3541 Approaches to Toba Inlet East Vancouver Island 1:40 000 Fair $ 5.00 3545 Johnstone Strait - Port Neville to Robson Bight East Coast Vancouver Island 1:40 000 Good $ 10.00 3546 Broughton Strait East Coast Vancouver Island 1:40 000 Fair $ 5.00 3549 Queen Charlotte Strait East Vancouver Island 1:40 000 Excellent $ 15.00 3549 Queen Charlotte Strait East -
Ecosystem Status and Trends Report for the Strait of Georgia Ecozone
C S A S S C C S Canadian Science Advisory Secretariat Secrétariat canadien de consultation scientifique Research Document 2010/010 Document de recherche 2010/010 Ecosystem Status and Trends Report Rapport de l’état des écosystèmes et for the Strait of Georgia Ecozone des tendances pour l’écozone du détroit de Georgie Sophia C. Johannessen and Bruce McCarter Fisheries and Oceans Canada, Institute of Ocean Sciences 9860 W. Saanich Rd. P.O. Box 6000, Sidney, B.C. V8L 4B2 This series documents the scientific basis for the La présente série documente les fondements evaluation of aquatic resources and ecosystems scientifiques des évaluations des ressources et in Canada. As such, it addresses the issues of des écosystèmes aquatiques du Canada. Elle the day in the time frames required and the traite des problèmes courants selon les documents it contains are not intended as échéanciers dictés. Les documents qu’elle definitive statements on the subjects addressed contient ne doivent pas être considérés comme but rather as progress reports on ongoing des énoncés définitifs sur les sujets traités, mais investigations. plutôt comme des rapports d’étape sur les études en cours. Research documents are produced in the official Les documents de recherche sont publiés dans language in which they are provided to the la langue officielle utilisée dans le manuscrit Secretariat. envoyé au Secrétariat. This document is available on the Internet at: Ce document est disponible sur l’Internet à: http://www.dfo-mpo.gc.ca/csas/ ISSN 1499-3848 (Printed / Imprimé) ISSN 1919-5044 (Online / En ligne) © Her Majesty the Queen in Right of Canada, 2010 © Sa Majesté la Reine du Chef du Canada, 2010 TABLE OF CONTENTS Highlights 1 Drivers of change 2 Status and trends indicators 2 1. -
DISCOVERY PASSAGE SCHOOL CLOSU RE CONSULTATION PROCESS Late Submissions
DISCOVERY PASSAGE SCHOOL CLOSU RE CONSULTATION PROCESS Late Submissions CONSULTATION INDEX DATE DESCRIPTION 03-05-2016 Claire Metcalfe 03-01-2016 Curtis and Amanda Smith i Lee-Ann Kruse From: Claire Metcalfe <[email protected]> Sent: March-OS-16 9:09 AM To: facilities plan; Susan Wilson; Ted Foster; Richard Franklin; Daryl Hagen; John Kerr; Gail Kirschner; Joyce McMann Cc: [email protected]; [email protected]; [email protected] Subject Fwd: SD72 School Closures Trolly kids All of the students in our district are standing on the train tracks and there is an out of control trolly headed for them all. Do we toss a few in the way (the elementary school kids who will also be tossed again when it comes to rebuilding the high school) to prevent them from all being hurt? Or do we ask no one to budge and see who survives? This is a morality question that has been presented to the trustees before, and I believe at a very appropriate time. Lers do something different. Pick an answer that isn't already proposed. I propose that we ask them to all step away from the tracks and let the train (Christy Clark) go along on it's merry way. I know the solution is not that simple. There has to be another way of building new schools in our district and supporting our childrens education other than following the paths that other districts are, just because it is what we are supposed to. Our district staff and trustees are smart, creative leaders of our community, and I would like for them to come up with another way to go about this. -
Spring Bloom in the Central Strait of Georgia: Interactions of River Discharge, Winds and Grazing
MARINE ECOLOGY PROGRESS SERIES Vol. 138: 255-263, 1996 Published July 25 Mar Ecol Prog Ser I l Spring bloom in the central Strait of Georgia: interactions of river discharge, winds and grazing Kedong yinl,*,Paul J. Harrisonl, Robert H. Goldblattl, Richard J. Beamish2 'Department of Oceanography, University of British Columbia, Vancouver, British Columbia, Canada V6T 124 'pacific Biological Station, Department of Fisheries and Oceans, Nanaimo, British Columbia, Canada V9R 5K6 ABSTRACT: A 3 wk cruise was conducted to investigate how the dynamics of nutrients and plankton biomass and production are coupled with the Fraser River discharge and a wind event in the Strait of Georgia estuary (B.C.,Canada). The spring bloom was underway in late March and early Apnl, 1991. in the Strait of Georgia estuary. The magnitude of the bloom was greater near the river mouth, indicat- ing an earher onset of the spring bloom there. A week-long wind event (wind speed >4 m S-') occurred during April 3-10 The spring bloom was interrupted, with phytoplankton biomass and production being reduced and No3 in the surface mixing layer increasing at the end of the wind event. Five days after the lvind event (on April 15),NO3 concentrations were lower than they had been at the end of the wind event, Indicating a utilization of NO3 during April 10-14. However, the utilized NO3 did not show up in phytoplankton blomass and production, which were lower than they had been at the end (April 9) of the wind event. During the next 4 d, April 15-18, phytoplankton biomass and production gradu- ally increased, and No3 concentrations in the water column decreased slowly, indicating a slow re- covery of the spring bloom Zooplankton data indicated that grazing pressure had prevented rapid accumulation of phytoplankton biomass and rapid utilization of NO3 after the wind event and during these 4 d. -
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. -
Burrard Inlet Underwater Noise Study
Vancouver Fraser Port Authorit Burrard Inlet underwater noise study: 2020 final report ECHO Program study summary This study was undertaken for the Vancouver Fraser Port Authority-led Enhancing Cetacean Habitat and Observation (ECHO) Program and project partner Tsleil-Waututh Nation with financial support from Transport Canada to learn more about underwater noise and cetacean presence in Burrard Inlet. Building upon the 2019 monitoring project in Burrard Inlet, this project set out to monitor underwater noise and the presence of cetaceans (whales, dolphins and porpoise) in Burrard Inlet, a marine mammal habitat and a key waterway for commercial shipping, port-related activities, and passenger transportation. This document summarizes the project question and describes the methods, key findings, and conclusions. What questions was the study trying to answer? The second year of the Burrard Inlet underwater noise study sought to evaluate longer-term trends in total ambient noise and marine mammal presence, while building upon the results from 2019. Who conducted the project? SMRU Consulting North America (SMRU) was awarded the contract for the 2019 monitoring program, and was retained by Vancouver Fraser Port Authority to continue monitoring though 2020 at fewer sampling locations. What methods were used? Bottom-mounted SoundTrap hydrophone recorders were deployed in two locations in the inner and outer harbour: one at Burrard Inlet East near the Tsleil-Waututh Nation reserve lands and Burnaby petroleum terminals, and one in English Bay between anchorages 1 and 3. Acoustic data were collected over approximately one year between February 2020 and February 2021. The figure below shows the approximate locations of the hydrophone deployments. -
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. -
A Nitrogen Budget for the Strait of Georgia, British Columbia, with Emphasis on Particulate Nitrogen and Dissolved Inorganic Nitrogen
Biogeosciences, 10, 7179–7194, 2013 Open Access www.biogeosciences.net/10/7179/2013/ doi:10.5194/bg-10-7179-2013 Biogeosciences © Author(s) 2013. CC Attribution 3.0 License. A nitrogen budget for the Strait of Georgia, British Columbia, with emphasis on particulate nitrogen and dissolved inorganic nitrogen J. N. Sutton1,2, S. C. Johannessen1, and R. W. Macdonald1 1Institute of Ocean Sciences, Fisheries and Oceans Canada, 9860 West Saanich Road, P.O. Box 6000, Sidney, British Columbia, V8L 4B2, Canada 2Department of Earth and Planetary Science, University of California, Berkeley, California, 94720, USA Correspondence to: J. N. Sutton ([email protected]) Received: 6 March 2013 – Published in Biogeosciences Discuss.: 23 April 2013 Revised: 29 September 2013 – Accepted: 10 October 2013 – Published: 12 November 2013 Abstract. Balanced budgets for dissolved inorganic N (DIN) 1 Introduction and particulate N (PN) were constructed for the Strait of Georgia (SoG), a semi-enclosed coastal sea off the west coast of British Columbia, Canada. The dominant control on the The nitrogen (N) cycle is a crucial underpinning of marine N budget is the advection of DIN into and out of the SoG biological productivity (Gruber and Galloway, 2008). Dur- via Haro Strait. The annual influx of DIN by advection from ing the past 150 yr, the global N cycle has been dramati- the Pacific Ocean is 29 990 (±19 500) Mmol yr−1. The DIN cally changed by human activities that have loaded reactive N flux advected out of the SoG is 24 300 (±15 500) Mmol yr−1. into ecosystems in amounts that rival natural sources (Rabal- Most of the DIN that enters the SoG (∼ 23 400 Mmol yr−1) ais, 2002; Galloway et al., 2004). -
MARINE BIRD SURVEYS in QC STRAIT-Final
MARINE BIRD SURVEYS IN QUEEN CHARLOTTE STRAIT AND ADJACENT CHANNELS, AUGUST-SEPTEMBER 2020 December 2020 2 MARINE BIRD SURVEYS IN QUEEN CHARLOTTE STRAIT AND ADJACENT CHANNELS, AUGUST-SEPTEMBER 2020 Anthony Gaston, Mark Maftei, Sonya Pastran, Ken Wright, Graham Sorenson, Iwan Lewylle Cite as: Gaston AJ, M Maftei, S Pastran, K Wright, G Sorenson and I Lewylle. 2020. MARINE BIRD SURVEYS IN QUEEN CHARLOTTE STRAIT AND ADJACENT CHANNELS, AUGUST-SEPTEMBER 2020. Raincoast Education Society, Tofino, BC. 3 1084 Pacific Rim Highway, Tofino, BC (https://raincoasteducation.org/) 4 CONTENTS Introduction 7 Methods Field methods 10 Analysis 13 Results Distribution by zones 16 Total numbers of birds present 17 Timing of arrival/migration Sea ducks 18 Phalaropes 18 Auks 20 Gulls 20 Loons 21 Grebes 22 Petrels 23 Cormorants 23 Comparison with other studies 24 Marine Mammals 26 Discussion Total numbers of birds 28 Timing of arrival/migration 29 Summary 29 Acknowledgements 31 References 32 Appendices 35 5 6 INTRODUCTION Queen Charlotte Strait, a funnel-shaped passage extending ESE from the open waters of Queen Charlotte Sound, separates northern Vancouver Island from the mainland of British Columbia. It is connected, via Johnstone Strait, Discovery Passage and associated channels, with the more or less enclosed waters of the Salish Sea (Figure 1). Anecdotal information from eBird lists suggests that this area supports a high diversity of marine birds in winter and during the periods of northward and southward migration (https://ebird.org/canada/ accessed 7 November 2020; hereafter “eBird”). In addition, this area is important for marine mammals, being used regularly by the Northern Resident Orca stock, and by Humpback and Minke Whales, Dall’s and Harbour Porpoises and Pacific White-sided Dolphins, and supporting several permanent haul-outs of Steller’s Sea Lions (Ford 2014). -
Psc Draft1 Bc
138°W 136°W 134°W 132°W 130°W 128°W 126°W 124°W 122°W 120°W 118°W N ° 2 6 N ° 2 DR A F T To navigate to PSC Domain 6 1/26/07 maps, click on the legend or on the label on the map. Domain 3: British Columbia R N ° k 0 6 e PSC Region N s ° l Y ukon T 0 e 6 A rritory COBC - Coastal British Columbia Briti sh Columbia FRTH - Fraser R - Thompson R GST - Georgia Strait . JNST - Johnstone Strait R ku NASK - Nass R - Skeena R Ta N QCI - Queen Charlotte Islands ° 8 5 TRAN N TRAN - Transboundary Rivers in Canada ° 8 r 5 ive R WCVI - Western Vancouver Island e in r !. City/Town ik t e v S i Major River R t u k Scale = 1:6,750,000 Is P Miles N ° 0 30 60 120 180 January 2007 6 A B 5 N ° r 6 i 5 C t i s . A h R Alaska l I b C s e F s o a NASK r l N t u a r m I e v S i C tu b R a i rt a N a ° Prince Rupert en!. R 4 ke 5 !. S Terrace iv N e ° r 4 O F 5 !. ras er C H Prince George R e iv c e QCI a r t E e . r R S ate t kw r lac Quesnel A a B !. it D e an R. N C F N COBC h FRTH ° i r 2 lc a 5 o N s ti ° e n !. -
Western Canada Explorer Featuring Vancouver, Victoria and Whistler
Antioch Seniors AND TravelCenter Travel & Tours presents... 9 DAY HOLIDAY Western Canada Explorer featuring Vancouver, Victoria and Whistler July 24 - August 1, 2020 Tour Dates: Western Canada Explorer Unforgettable experiences await 9 Days • 15 Meals in Canada’s Golden Triangle featuring mountain gondolas, a First Nations cultural experience, a regional Foodie Tour and an incredible wildlife cruise. TOUR HIGHLIGHTS 4 15 Meals (8 breakfasts, 3 lunches and 4 dinners) 4 Round trip airport transfers 4 Spend 3 nights in cosmopolitan Vancouver 4 Take a panoramic tour of Vancouver to see its downtown core, spectacular North Shore and beautiful Stanley Park and visit Capilano Suspension Bridge 4 Travel the scenic “Sea to Sky Highway” to and enjoy the PEAK 2 PEAK experience, a 1.88-mile long gondola ride between Blackcomb and Whistler Mountains 4 Travel by BC Ferry to Vancouver Island and visit world-famous Butchart Gardens 4 Included city tour of Victoria with its delightful English flavor, red double-decker buses and Tudor-style buildings Cross the Capilano Suspension Bridge and enjoy views of the spectacular rainforest 4 Visit Victorian-era Craigdarroch Castle and take the walking Victoria Food Tour, a delicious culinary experience 4 Enjoy a First Nations Cultural Experience at the I-Hos Gallery DAY 1 – Arrive in Beautiful British Columbia featuring a weaving workshop and included lunch with traditional Welcome to Canada’s rugged Northwest in Vancouver and transfer Bannock bread to your hotel. Meet your Tour Manager in the hotel lobby at 6:00 4 Spend 2 nights at the illustrious Painter’s Lodge, located on the p.m. -
Relationship of Variable Oceanographic Factors to Migration and Survival of Fraser River Salmon
RELATIONSHIP OF VARIABLE OCEANOGRAPHIC FACTORS TO MIGRATION AND SURVIVAL OF FRASER RIVER SALMON 1. A. ROYAL International Pacific Salmon Fisheries Commission and J. P. TULLY Fisheries Research Board of Canada INTRODUCTION north through Queen Charlotte and Johnstone Straits. In 1957 it was noted that a larger share of Management of the various Fraser River salmon the population approached Vancouver Island from fisheries requires an intimate knowledge of the abund- the north, a larger percentage (approximately 16 ance and movements of salmon runs, which is drawn per cent) diverted through Queen Charlotte Strait largely from a detailed study of commercial catches. and it was also noted that the fish were slightly de- Abnormalities in abundance, in routes of migration layed, and migrated over a longer period of time. or times of occurrence, unless forecasted, may negate the beneficial effect of fishing regulations formulated In 1958, the sockeye run of approximately 19,000,- in advance of the fishing season. A flexible method of 000 fish failed to appear off the west coast of Van- regulatory adjustment during the course of fishing couver Island in its usual initial landfall and arrived may help rectify the adverse effects of vagaries in the northerly of Vancouver Island in the Queen Char- salmon population but it cannot be accepted as a lotte Sound area. The fish then moved in a southerly substitute for advance knowledge and planning. direction with an estimated thirty-five to forty per cent of the total population entering Queen Char- lotte Strait, thus approaching the Fraser River, from OCEANOGRAPHIC FACTORS AFFECTING the north instead of the usual route through the Juan SOCKEYE SALMON MIGRATIONS IN de Fuca Strait.