DOCSLIB.ORG

The Resilience of the City of Kelowna: Exploring Mitigation Before, During and After the Okanagan Mountain Park Fire

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Resilience of the City of Kelowna: Exploring Mitigation Before, During and After the Okanagan Mountain Park Fire Institute for Catastrophic Institut de Prévention Loss Reduction des Sinistres Catastrophiques Building resilient communities Construction de resilient communities The resilience of the City of Kelowna: Exploring mitigation before, during and after the Okanagan Mountain Park Fire By Dan Sandink January 2009 The resilience of the City of Kelowna: Exploring mitigation before, during and after the Okanagan Mountain Park Fire By Dan Sandink Institute for Catastrophic Loss Reduction January 2009 ICLR research paper series – number 45 Published by Institute for Catastrophic Loss Reduction 20 Richmond Street East, Suite 210 Toronto, Ontario, Canada M5C 2R9 This material may be copied for purposes related to the document as long as the author and copyright holder are recognized. The opinions expressed in this paper are those of the author and not necessarily those of the Institute for Catastrophic Loss Reduction. Cover photos: (large) Lars Karstad, (small) Shutterstock. ISBN: 978-0-9811792-0-9 Copyright©2008 Institute for Catastrophic Loss Reduction ICLR’s mission is to reduce the loss of life and property caused by severe weather and earthquakes through the identification and support of sustained actions that improve society’s capacity to adapt to, anticipate, mitigate, withstand and recover from natural disasters. ICLR is achieving its mission through the development and implementation of its programs Open for Business™, to increase the disaster resilience of small businesses, Designed… for safer living, which increases the disaster resilience of homes, and RSVP cities, to increase the disaster resilience of communities. Table of contents Executive summary . .i 1. Introduction . .1 2. Context . .3 2.1 Wildfires in Canada . 3 2.1.1 Wildfire damages . 4 2.2 Wildland-Urban interface risk . 6 2.2.1 Wildland-Urban interface fire hazard management . 6 2.3 Resilience . 9 2.3.1 Vulnerability to natural hazards . 12 2.3.2 Resilience to natural hazards: Disaster mitigation . 15 2.3.21 Pre- and post-disaster mitigation . 16 2.3.2.1.1 Pre-disaster mitigation . 16 2.3.2.1.2 Post-disaster mitigation . 17 2.4 Disaster mitigation at the local level . 21 2.4.1 Disaster mitigation assistance at the provincial level in British Columbia . 22 2.4.1.1 Mitigation in provincial acts and regulations . 23 2.4.2 Local level mitigation assistance at the federal level . 24 2.4.2.1 Joint Emergency Preparedness Program . 25 2.4.2.2 Federal disaster financial assistance arrangements . 25 2.4.2.3 NDMS and revised DFAA . 26 2.4.3 Barriers to resilience and mitigation at the municipal level . 27 2.4.3.1 Liability as a barrier . 30 2.5 Insurance . 31 3. Methods . .34 3.1 Data gathering . 34 3.2 Case study . 34 3.2.1 2003 fires in British Columbia and the Kelowna area . 35 3.2.1.1 The Okanagan Mountain Park Fire . 36 3.2.1.1.1 Post wildfire hazards . 39 3.2.1.1.2 The B.A. Blackwell & Associates report . 39 3.2.1.1.3 Mitigation strategies . 44 Table of contents (continued) 4. Results and discussion . .45 4.1 OMPF impacts on the Corporation of the City of Kelowna . 46 4.2 Wildfire risk mitigation and private-property owners . 47 4.3 Alteration of physical development to reduce vulnerability . 49 4.4 Learning from other communities . 50 4.5 Assessing WUI fire hazard areas . 51 4.6 Communications . 52 4.7 Fire Guard . 54 4.8 Disaster Recovery Centres . 54 4.9 Insurance and recovery resource management . 55 4.9.1 Insurance coverage . 55 4.9.2 Recovery resource management . 56 4.10 Post-wildfire hazard mitigation . 57 4.10.1 Post-wildfire flood mitigation . 58 4.10.1.1 Post-wildland fire flood risk management in Kelowna . 59 4.10.1.1.1 Mitigation works and appeal for funding . 60 4.11 Post-disaster policy window . 62 4.12 General perceptions of OMPF . 64 4.12.1 Time taken to recover from OMPF . 64 4.12.2 Risk perceptions associated with recurrence of fire events . 65 4.12.2.1 Impacts of beetle kill . 66 4.12.3 Impact of OMPF experience on management of future disasters . 67 4.12.4 The role of higher levels of government . 68 4.12.5 Emergency response, evacuations . 70 4.12.5.1 Evacuation . 71 4.13 Barriers to wildfire hazard mitigation in Kelowna . 72 4.13.1 Litigation and the window of opportunity . 74 5. Resilience characteristics, recommendations, further work and conclusions . .76 5.1 Characteristics of resilience in Kelowna . 76 5.1.1 Redundant . 76 5.1.2 Diverse . 76 5.1.3 Efficient . 77 5.1.4 Autonomous . 77 5.1.5 Resistant . 78 5.1.6 Interdependent . 78 5.1.7 Adaptable . 81 5.1.8 Collaborative . 81 5.2 Recommendations . 81 5.2.1 Adoption of adjustments by private property owners . 81 5.2.2 Identification of vulnerable individuals . 83 5.2.3 Collaboration with insurance companies . 84 5.2.4 Incentives for municipal governments . 85 5.2.5 The Role of the provincial government . 87 5.2.6 The Role of the federal government . 88 5.3 Limits to the study and suggestions for future work . 89 5.4 Conclusion . 90 Works Cited . .92 Appendix A: Summary of November 20, 2007 meeting in Kelowna . 105 Appendix B: Participants . 106 Appendix C: Interview survey . 107 Appendix D: Blackwell & Needoba (2006) recommendations . 113 List of tables Table 1 U.S. insured catastrophic losses from 1987 to 2006 . 5 Table 2 Ten most catastrophic wildfire events in the United States . 5 Table 3 WUI fire management by level of government . 8 Table 4 Characteristics of resilient systems . 11 Table 5 Components of vulnerability . 13 Table 6 Vulnerability categories and example factors . 14 Table 7 Components of emergency management . 15 Table 8 Progression of community level wildfire mitigation adjustments during the Lost Creek fire . 19 Table 9 DFAA funding shares . 25 Table 10 Comparison of population changes in Kelowna and B.C. 35 Table 11 Comparison of population and population change amongst local municipalities . 35 Table 12 Number, area burned and average size of fires in B.C. 36 Table 13 Timeline of events for OMPF . 37 Table 14 Priority actions for 2007 . 43 Table 15 Responses to: “Please use the scale below to rate how likely it is that the City of Kelowna would experience another wildfire event, similar to that of the OMPF?” . 65 Table 16 Responses to: “If the fire were to occur again in the next 10 years, how would you rate the impacts, in comparison to the OMPF?” and “If the OMPF were to occur again in the next 10 years, how would you rate the amount of time it would take to recover, in comparison to the OMPF?” . 66 Table 17 Progression of actions . 80 List of figures Figure 1 Reported number of disasters from 1900 to 2005 . 3 Figure 2 Resilience . 10 Figure 3 Fire Guard . 54 Figure 4 Larger Crossing at Chute Lake Road and Frost Road, Kelowna . 61 Figure 5 Larger Crossing at Lebanon Creek and Lakeshore Road, Kelowna . 62 Executive summary Resilience is the ability of a community to “bounce back” from adversity. A disaster resilient community employs tools and strategies to mitigate the impacts of, and quickly and effectively recover from disasters. The City of Kelowna suffered significant adversity during the Okanagan Mountain Park Fire (OMPF) of 2003, including significant damage to private property, homes, infrastructure, as well as an evacuation of a significant portion of the City’s population. The OMPF was a severe Wildland-Urban Interface (WUI) fire event that resulted in the destruction of 238 homes, the evacuation of approximately one third of the population of the City of Kelowna, and was considered the most destructive WUI fire in Canadian history. Damages to the City of Kelowna alone were estimated at $100 million. This paper provides a discussion of a resilient community, through the exploration of impacts, reactions and mitigative adjustments adopted by the City of Kelowna before, during and after the OMPF. The paper provides context for disaster mitigation decision making in Canada and British Columbia, including a review of relevant legislation and government programs related to emergency management. This paper discusses the adoption.
Load more

Recommended publications
  • Appendix 1 Chronology of the Okanagan Mountain Fire Events Extracted from Castanet.Net Okanagan Mountain Fire Watch 2005
    Health, Safety and Workload Challenges of the Okanagan Mountain Fire 2003 Submitted to the Vancouver Foundation University of British Columbia Okanagan Faculty of Health and Social Development School of Nursing September 2005 Copyright © 2005 University of British Columbia Okanagan Faculty of Health and Social Development 1 Funding Vancouver Foundation BC Canada Research Team Principal Investigator Dr Penny Cash RN (Vic.Aust), DipAppSci (NsgEd), BEd, MEdAdmin, PhD, FRCNA. Associate Professor, School of Nursing, University of British Columbia Okanagan Co-Investigators Ms Linda Daviss RN, BSN, MSN. Associate Professor, School of Nursing, Okanagan University College, Kelowna Ms Donna Kurtz RN, BSN, MSN. Associate Professor, School of Nursing, University of British Columbia Okanagan Ms Susan Van Den Tillaart RN, BSN, MSN. Assistant Professor, School of Nursing, University of British Columbia Okanagan Research Assistants Ms Anne Bregeda RN, BSN. Ms Rhonda Croft RN, BSN. Ms Jean McKenzie RN, BSN. Advisory Committee Dr Joan Bassett-Smith RN, BSN, MA, PhD. Director School of Nursing, University of British Columbia Okanagan Dr Claire Budgen RN, BSN, MSN, PhD. Director Campus Health, University of British Columbia Okanagan Dr Colin Reid BA, MA, PhD. Senior Fellow, Centre for Population Health and Social Services, University of British Columbia Okanagan Ms Sharon Wammer RN, BSN, MNS. Director Community Care, Interior Health, Kelowna, British Columbia Dedication The Research Team would like to gratefully thank HCOs who participated in this research. The legacy of the challenges and success of your work is deeply reflected in the community's healing. It is your courage and dedication that has made recovery possible for many people.
    [Show full text]
  • Technical Report for Naramata Bench Sub-GI
    Naramata Bench Sub-Geographic Indication January 2018 Technical Description and Geographic Extent Documentation in support of a formal application to the BC Wine Authority for the creation of a new Sub-GI named Naramata Bench. Scott Smith, Eterrna Consulting Pat Bowen, Summerland Research and Development Centre, Agriculture and Agri-Food Canada Naramata Bench Sub-Geographic Indication Naramata Bench Sub- Geographic Indication TECHNICAL DESCRIPTIO N AND GEOGRAPHIC EXT ENT EXECUTIVE SUMMARY The ‘Naramata Bench’ brand is firmly established in a regional socioeconomic context and particularly within the BC wine and wine tourism industry. The proposed sub-Geographic Indication (sub-GI) covers an area of just under 3,650 ha along the east side of the Okanagan Valley from Okanagan Mountain Provincial Park in the north to Penticton Creek within the City of Penticton in the south. The area includes approximately 250 ha of vineyards and some 50 wineries. The proposed sub-GI is composed of two landscape elements – the glaciolacustrine landscape and the mixed sediments landscape. The glaciolacustrine landscape is characterized by a gullied, gently undulating land surface and is the signature landform of the Naramata Bench. The second landscape element is the mixed deposits that lie above the glaciolacustrine landscape. At higher elevations are common outcrops of coarse grained metamorphic rocks (gneiss) which have been altered through geologic faulting and are termed ‘mylonite’ The soil used extensively for agriculture on the Naramata Bench sub-GI is the Penticton silt loam. This stone-free soil has a well-developed profile with a distinct organic matter-rich topsoil underlain by a highly favourable rooting zone up to 60 cm thick over the unweathered calcareous parent material.
    [Show full text]
  • Monitoring Impacts of the Okanagan Mountain Park Fire on Hydrological
    EvaluationsEvaluations ofof ImpactsImpacts ofof thethe OkanaganOkanagan MountainMountain ParkPark FireFire onon InIn--streamstream WoodWood andand OtherOther WatershedWatershed ProcessesProcesses Adam Wei Earth and Environmental Science University of British Columbia Okanagan Kelowna, British Columbia, Canada (Presentation at the Watershed Conference, South Carolina, USA, 2006) TopicsTopics toto bebe coveredcovered • Rationale for the project • Long-term monitoring approach • Preliminary results RationaleRationale forfor thethe projectproject • A big picture: forest-water-fish interaction for BC • Disturbance ecology – Wildfire and pine beetle infestation – Emulation of natural disturbance? – Need to know impacts of natural disturbance • In-stream wood (LWD) ecological importance – LWD--morphology—aquatic habitat—fish – Large LWD variability in space and time – Lack of long-term LWD studies There are about 9000 forest fires recorded annually in Canada. An average of 2.1 million hectares are burned every year; virtually all of it is boreal forest. On average, 2000 occurred each year, 50% by man and 50% by lighting Total Area Affected by Mountain Pine Beetle in Western Canada 2001: Mountain pine beetle damage LWD as cover, Salmon Arm fire, 1998 Channel morphology, 90 years after fire, Upper Penticton cr. LWDLWD rolerole && managementmanagement paradigmparadigm • Aquatic environment – Channel morphology & fish habitat – Diversity of hydraulic flows – Sediment trapping – Nutrients & its long-term release – Bank erosion prevention – Paradigm
    [Show full text]
  • Okanagan Mountain Master Plan
    Okanagan Mountain Provincial Park M ASTER LAN P Prepared by Southern Interior Region Kamloops, B.C. Canadian Cataloguing in Publication Data Main entry under title: Okanagan Mountain Park master plan Cover title: Master Plan for Okanagan Mountain Provincial Park ISBN 0-7726-1150-5 1. Okanagan Mountain Provincial Park (B.C.) 2. Parks – British Columbia – Planning. 3. Parks – British Columbia – Management. I. British Columbia. Ministry of Parks. Southern Interior Region. II. Title: Master plan for Okanagan Mountain Provincial Park. FC3815.032032 1990 333.78”3”097115 C90-092180-3 F1089.032032 1990 Table of Contents Plan Highlights........................................................ 7 Introduction ............................................................. 9 Purpose of the Plan Background Summary ...................................................................12 The Role of the Park......................................................16 Regional and Provincial Significance Conservation Role Recreation Role ............................................................................17 Park Zoning Intensive Recreation Zone Natural Environment Zone.............................................................18 Wilderness Recreation Zone Natural and Cultural Resource Management Lands Water ...........................................................................................22 Vegetation.....................................................................................23 Fish and Wildlife ..........................................................................24
    [Show full text]
  • Kelowna 17 AIRPORT International BOOTH RD WAY Airport
    10 to Vernon Airport to Vernon. Lake & Drive time approximately SilverStar 30 minutes. Country Mountain Resort See Lake Country Map QUAIL RIDGE 10 (LKM) on reverse BLVD to reserve to 8 7 9 Kelowna 17 AIRPORT International BOOTH RD WAY Airport COUNTRY CLUB DR 18 28 59 Ellison 3 Centennial Park North Glenmore JOHN HINDLE DR Dog Park 14 South Ellison Dog Park RD ANDERSON pickup service in Kelowna. pickup 8 INNOVATION WAY ANDERSON RD UPPER BOOTH RD S Bear Creek 13 CLIFTON RD 11 9 bcbudget.com GLENMORE RD N FREE Traders Cove 97 ACCOMMODATIONS PRIMARY HIGHWAY BOAT LAUNCH UBC Regional Park Okanagan 250-491-7368 & Beach Robert BULMAN RD MAJOR HIGHWAY Bear Main FSR ACTIVITIES & ATTRACTIONS SWIMMING / BEACH* Lake MAJOR ROAD Call Call ARTS, EVENTS, & ENTERTAINMENT LOOKOUT POINT your car. car. your 50 SCOTTY CREEK RD MINOR ROAD SCENIC RD Robert Lake DINING & NIGHTLIFE Bear Creek Regional Park BIRDWATCHING SITE Provincial Park GRAVEL ROAD 84 Carney RD VERNON OLD GOLF 15 UPPER CANYON DRIVE Pond OKANAGAN RAIL TRAIL PERFORMANCE VENUE UNION RD Paul’s Tomb 71 VALLEY RD WILDEN GUIDED TOURS PADDLE TRAIL HIKING/WALKING TRAILS* SNOWSELL ST TRAIL* BEAR CREEK RD Brigade Trail NEAVE RD 8 HERITAGE SITES & MUSEUMS CROSS RD BIKING TRAILS* 7 5 APPALOOSA RD PENNO RD BIKE ROUTE ADAMS RD LAKE ACTIVITIES RIO DR LONGHILL RD BUS: TRANSIT EXCHANGE MULTI-USE PATHWAY SEXSMITH RD OLD VERNON RD FARMS, ORCHARDS, & MARKETS Raymer Beach GLENMORE RD 80 WATERFRONT PARKING Regional Park KANE RD SHOPPING AND WELLNESS BOARDWALK VALLEY RD ELECTRIC CHARGING CORNISH RD 78 LONGHILL RD
    [Show full text]
  • Corrugated Architecture of the Okanagan Valley Shear Zone and the Shuswap Metamorphic Complex, Canadian Cordillera
    Corrugated architecture of the Okanagan Valley shear zone and the Shuswap metamorphic complex, Canadian Cordillera Sarah R. Brown1,2,*, Graham D.M. Andrews1,3, and H. Daniel Gibson2 1DEPARTMENT OF GEOLOGICAL SCIENCES, CALIFORNIA STATE UNIVERSITY–BAKERSFIELD, 9001 STOCKDALE HIGHWAY, BAKERSFIELD, CALIFORNIA 93311, USA 2DEPARTMENT OF EARTH SCIENCE, SIMON FRASER UNIVERSITY, 8888 UNIVERSITY DRIVE, BURNABY, BRITISH COLUMBIA V5A 1S6, CANADA 3DEPARTMENT OF GEOLOGY AND GEOGRAPHY, WEST VIRGINIA UNIVERSITY, 98 BEECHURST AVENUE, MORGANTOWN, WEST VIRGINIA 26506, USA ABSTRACT The distribution of tectonic superstructure across the Shuswap metamorphic complex of southern British Columbia is explained by east-west– trending corrugations of the Okanagan Valley shear zone detachment. Geological mapping along the southern Okanagan Valley shear zone has identified 100-m-scale to kilometer-scale corrugations parallel to the extension direction, where synformal troughs hosting upper-plate units are juxtaposed between antiformal ridges of crystalline lower-plate rocks. Analysis of available structural data and published geological maps of the Okanagan Valley shear zone confirms the presence of≤ 40-km-wavelength corrugations, which strongly influence the surface trace of the detachment system, forming spatially extensive salients and reentrants. The largest reentrant is a semicontinuous belt of late Paleozoic to Mesozoic upper-plate rocks that link stratigraphy on either side of the Shuswap metamorphic complex. Previously, these belts were considered by some to be autochthonous, implying minimal motion on the Okanagan Valley shear zone (≤12 km); conversely, our results suggest that they are allochthonous (with as much as 30–90 km displacement). Corrugations extend the Okanagan Valley shear zone much farther east than previously recognized and allow for hitherto separate gneiss domes and detachments to be reconstructed together to form a single, areally extensive Okanagan Valley shear zone across the Shuswap metamorphic complex.
    [Show full text]
  • Riding the Kettle Valley Railway
    BC Ballast Riding the Kettle Valley Railway Story and photos by Chuck Haney BC Ballast ith chains lubed, tires topped In past cycling trips to the backroads and off with air, and water in the trails of Colorado, Utah, and Oregon, Mike packs, another two-wheeled and I seemed destined to follow a dubious Wadventure was set in motion as the morning pattern of unpredictable weather leading sunlight began to filter through thick stands to various misadventures from incessant of coniferous forest. The cool of the morn- rain, wind, or even snow mucking up our ing air slowly dissipated to the warmth of planned itinerary. Throw in car troubles, a lengthy June summer day. Ravens called tow trucks, raccoons setting off car alarms out to each other from opposing sides of in the middle of the night in a full camp- the trail, their squawking banter and the ground, and getting lost, and it seemed we gravel ballast crunched constantly below had been through it all. But for this particu- our tires. This was the soundtrack of our lar trip, the skies remained clear, the winds first day of riding. In south central British were calm, and even annoying things like Columbia, mighty locomotives were once mosquitoes stayed mostly at bay. the undeniable kings of the Kettle Valley. Our British Columbia adventure on I’m once again paired up with Adventure the KVR began near the remote town of Cyclist editor, Mike Deme, for a cycling Westbridge, which is small enough to be view of the rapids below. For the first excursion in a far-flung location.
    [Show full text]
  • Origins of Lake Okanagan
    ORIGINSORIGINS OFOF LAKELAKE OKANAGANOKANAGAN By Murray A. Roed, PhD, PEng Information provided is primarily from a book entitled “Okanagan Geology, British Columbia” published in 2004 by the Kelowna Geology Committee. 05/12/2005 1 INTRODUCTIONINTRODUCTION z Precambrian Time – Vast granitic Continental Crust, Pangaea z Paleozoic Time – Oceanic shelf environment, major mountain building z Mesozoic Time – Island Arc archipelago, plate tectonic structure, Continental Drift, obduction, Interior Mountain Building, Massive Stream Erosion z Cenozoic Time…the valley begins 05/12/2005 2 TheThe CenozoicCenozoic EraEra (Tertiary(Tertiary andand QuaternaryQuaternary Periods)Periods) z Initiation of the Okanagan Rift System z Eocene Volcanic activity, explosive type – Knox Mountain, Mount Boucherie z Development of White Lake River System z Erosion of Highlands, Deposition onto Alberta Plains z The rise of the Rocky Mountains z Folding and Faulting in the Okanagan z Mission Creek Fault z Peneplanation of the Interior of BC 05/12/2005 3 PlateauPlateau VulcanismVulcanism z Uplift, Rifting, and Erosion, regional near- surface magma chamber. z Widespread fluid basaltic flows erupt along fractures and inundate low relief valley system (200 to 300 metres local relief) including part of the Okanagan Valley (Wrinkly Faced Cliff, Oyama). z Continued Uplift, Cooling of the Earth, High 05/12/2005Precipitation, Erosion 4 PreglacialPreglacial ValleyValley SystemSystem z Massive deep erosion along fractured and fault- bounded rocky terrain in the Canadian Cordillera and Interior Plains. z Development of major valleys; topography highly rugged with sharp bold profiles. z Incision or dissection of the Thompson Plateau and Okanagan Highland 05/12/2005 5 THETHE ICEICE AGEAGE z Ice accumulation from massive snowfall z Development of Cordilleran Ice Sheets -beginning with valley glaciers and ending with ice so thick, it overtopped mountains.
    [Show full text]
  • Climate Projections for the Okanagan Region
    Climate Projections for the Okanagan Region February 2020 In partnership with Chapter 3 – Summer Temperature Indicators ..................... 17 Days Above 30°C ......................................................................................................18 Table of Contents Hottest Days .............................................................................................................. 20 1-in-20 Hottest Day ..................................................................................................21 Growing Season Length.......................................................................................21 Chapter 1 – Introduction ............................................................ 5 Cooling Degree Days ............................................................................................22 How Much Will the Climate Change? .......................................................... 6 Shifting Seasons .........................................................................................................7 Chapter 4 – Winter Temperature Indicators .......................23 A Note on Data Interpretation ............................................................................7 Average Spring Nighttime Low Temperatures ....................................24 Coldest Night ..............................................................................................................26 Chapter 2 – Regional Impacts ..................................................9 Frost Days .....................................................................................................................26
    [Show full text]
  • Okanagan-Kettle Subregion Connectivity Assessment
    Providing a Regional Connectivity Perspective to Local Connectivity Conservation Decisions in the British Columbia–WAshington Transboundary Region: Okanagan-Kettle Subregion Connectivity Assessment Transboundary Connectivity Group March 2016 Providing a Regional Connectivity Perspective to Local Connectivity Conservation Decisions in the British Columbia–Washington Transboundary Region: Okanagan-Kettle Subregion Connectivity Assessment Transboundary Connectivity Group March 2016 March 2016 Transboundary Connectivity Group This report has been prepared by Rachel Holt (Independent), Tory Stevens (BC Ministry of the Environment), Gregory Kehm (Independent), Andrew Shirk (University of Washington), Peter Singleton (US Forest Service–Pacific Northwest Research Station), Meade Krosby (University of Washington- Climate lead), Jen Watkins (Conservation Northwest), and Leslie Robb (Independent). Assistance was given by Bill Gaines (Washington Conservation Science Institute). Acknowledgements The findings presented in this report are the collaborative effort among the Washington Wildlife Habitat Connectivity Working Group member organizations and partners in British Columbia. We would like to thank the many individuals who generously contributed their time, expertise, and support during the development of this report and associated products. Workshops with partners for each of the operational-scale linkages and to integrate climate change considerations were essential to the success of this project. We appreciate the organizers and participants
    [Show full text]
  • Nuttall's Cottontail Sylvilagus Nuttallii Nuttallii (British Columbia Population) and Sylvilagus Nuttallii Pinetis (Prairie Population) in Canada
    COSEWIC Assessment and Update Status Report on the Nuttall’s Cottontail nuttallii subspecies Sylvilagus nuttallii nuttallii in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION DES ENDANGERED WILDLIFE IN ESPÈCES EN PÉRIL CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Nuttall’s Cottontail nuttallii subspecies Sylvilagus nuttallii nuttallii in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. Previous reports: Carter, D. and M. Merkens. 1994. Update COSEWIC status report on the Nuttall's cottontail Sylvilagus nuttallii nuttallii (British Columbia population) and Sylvilagus nuttallii pinetis (Prairie population) in Canada. Committee on the Status of Endangered Wildlife in Canada. 1-38 pp. Production note: COSEWIC would like to acknowledge David Nagorsen for writing the update status report on the Nuttall’s Cottontail nuttallii subspecies Sylvilagus nuttallii nuttallii in Canada prepared under contract with Environment Canada, overseen and edited by Marco Festa-Bianchet, Co-chair (Terrestrial Mammals), COSEWIC Terrestrial Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur le lapin de Nuttall de la sous- espèce nuttallii (Sylvilagus nuttallii nuttallii) au Canada – Mise à jour.
    [Show full text]
  • Osps Newsletter
    OSPSOKANAGAN NEWSLETTER SIMILKAMEEN PARKS SOCIETY Spring P.O. Box 787, Summerland, B.C. V0H 1Z0 2010 Phone: 250-494-8996 • Email: [email protected] Editorial 45th ANNUAL GENE L MEETING of the kanagan Mountain Park is the fea- ture of our 45th Annual General OKANAGAN SIMILKAMEEN Meeting. It was an early success Oof this society, the first Provincial Park in PARKS SOCIETY the Okanagan Similkameen. The Park has so much to offer – hiking trails, wild life visions of all sorts and gorgeous vistas. presenting Harold Baumborough’s slides and talk shows his enthusisan for his neighbour, “New Life in Okanagan Mountain Park” Okanagan Mountain Park. A Record of Growth and Change Much has been written about the lack of support – budget and staff of BC’s wonder- ful parks. Perhaps, we hope, some of the much talked about Olympics Legacy will be directed towards improving the condi- tions of protected areas and the people who manage them. BEFORE THE DISASTER Parks are valuable. They generate growth. They generate funds. They preserve natural life and resources, they encourage healthy activity. They are living classrooms for all and can promote love of the land among children. A Slide Show by Parks deserve our unqualified support. Harold Baumbrough of Naramata We must agree with resolutions of the ‘naturalist extraordinaire’ Outdoor Recreation Council regarding Off AFTER THE DISASTER Road Vehicle use our trails and in natural Since the Okanagan Mountain Park re in 2003, Harold has made areas. The first steps of long requested leg- islation regarding licensing and regulations numerous trips into an area he knew well.
    [Show full text]