Seasonality of the Water Balance of the Sooke Reservoir, BC, Canada

Total Page:16

File Type:pdf, Size:1020Kb

Seasonality of the Water Balance of the Sooke Reservoir, BC, Canada Seasonality of the Water Balance of the Sooke Reservoir, BC, Canada by Arelia Taymen Werner B.Sc., University of British Columbia, 2000 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in the Department of Geography Arelia Taymen Werner, 2007 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. ii Supervisory Committee _____________________________________________________________________ Dr. Terry D. Prowse, Co-Supervisor (Department of Geography) _____________________________________________________________________ Dr. John J. Gibson, Co-Supervisor (Department of Geography) _____________________________________________________________________ Dr. Dan L. Peters, Departmental Member (Department of Geography) _____________________________________________________________________ Dr. Barrie R. Bonsal, Departmental Member (Department of Geography) Examining Committee All members of the Supervisory Committee and _____________________________________________________________________ Dr. Garth van der Kamp, External Examiner (University of Saskatchewan) iii Supervisory Committee Dr. Terry D. Prowse, Co-Supervisor (Department of Geography) Dr. John J. Gibson, Co-Supervisor (Department of Geography) Dr. Dan L. Peters, Departmental Member (Department of Geography) Dr. Barrie R. Bonsal, Departmental Member (Department of Geography) Abstract Climate change and population growth is putting increased pressure on water supply. However, detailed water-balance information, which would assist with management is lacking for major reservoirs around the world. This information is particularly critical in mid- latitude northern Mediterranean climates where evaporation is a potentially important water- balance component. This study examines the seasonality of the water balance for the Sooke Reservoir in western Canada, a major water supply for the City of Victoria, British Columbia. Evaporation is estimated with three evaporation models, Penman, Priestley-Taylor, and Hamon and the results are compared. Inflows are estimated with the contributing-area approach and the HBV- EC, hydrologic model. Finally, a worst-case drought scenario is created. If conditions of low precipitation and high evaporation like those found in the study period were to persist, water levels would become critically low during the third dry season and by the fifth season if water restrictions were put in place. iv Table of Contents Supervisory Committee ................................................................................................ ii Abstract........................................................................................................................iii Table of Contents......................................................................................................... iv LIST OF TABLES....................................................................................................... vi LIST OF FIGURES .................................................................................................... vii Acknowledgments......................................................................................................... x CHAPTER 1: INTRODUCTION................................................................................. 1 1 BACKGROUND .............................................................................................. 1 2 STUDY AREA................................................................................................. 3 3 PREVIOUS STUDIES OF THE SOOKE RESERVOIR ................................. 5 4 RESEARCH PROBLEM.................................................................................. 6 5 RESEARCH OBJECTIVES............................................................................. 7 REFERENCES ........................................................................................................... 11 CHAPTER 2: STUDY AREA.................................................................................... 14 1 INTRODUCTION .......................................................................................... 14 2 REGIONAL HYDROCLIMATIC SETTING................................................ 14 3 PHYSICAL CHARACTERISTICS............................................................... 16 4 RESERVOIR HISTORY AND LIMNOLOGY ............................................. 21 5 DATA HISTORY SUMMARY ..................................................................... 22 REFERENCES ........................................................................................................... 28 CHAPTER 3: ESTIMATING EVAPORATION FROM THE SOOKE RESERVOIR, BC, CANADA ............................................................................................................ 32 ABSTRACT................................................................................................................ 32 1 INTRODUCTION .......................................................................................... 33 2 STUDY AREA............................................................................................... 38 3 METHODOLOGY AND DATA.................................................................... 40 3.1 Observational Data......................................................................................41 3.2 The Penman Estimate ................................................................................. 42 3.3 Priestley-Taylor Estimate............................................................................ 44 3.4 The Hamon Estimate and an Adjustment Factor ........................................ 51 4 RESULTS AND DISCUSSION..................................................................... 52 4.1 The Penman Estimate ................................................................................. 52 4.2 The Priestley-Taylor Estimate .................................................................... 58 4.3 Heat-Storage Flux....................................................................................... 62 4.4 The Hamon and Monthly Adjustment Factors............................................ 67 5 CONCLUSIONS AND RECOMMENDATIONS ......................................... 73 REFERENCES ........................................................................................................... 77 CHAPTER 4: SEASONALITY OF THE WATER BALANCE OF THE SOOKE RESERVOIR, BC, CANADA.................................................................................... 83 ABSTRACT................................................................................................................ 83 1 INTRODUCTION .......................................................................................... 84 2 STUDY AREA............................................................................................... 87 v 3 METHODOLOGY AND DATA.................................................................... 90 3.1 Total Inputs................................................................................................. 90 3.1.1 Surface Water Inflows ........................................................................ 91 3.1.1.1 Primary Data................................................................................... 91 3.1.1.2 Secondary Data............................................................................... 92 3.1.1.3 Methods for Discharge Estimate..................................................... 93 3.1.1.3.1 Modelled Total Inflows.............................................................94 3.1.1.3.2 Scaling Inflows from Individual Catchments up to the Total Inflow Estimate........................................................................................... 96 3.1.1.3.3 Estimates of Total Inflows Based on Contributing Area Approach 97 3.1.2 Diversions ........................................................................................... 99 3.1.3 Groundwater ....................................................................................... 99 3.2 Total Outputs............................................................................................ 100 3.2.1 Evaporation....................................................................................... 100 3.2.2 Spill................................................................................................... 101 3.2.3 Fisheries Release............................................................................... 101 3.2.4 Consumption..................................................................................... 102 3.3 Change in Storage..................................................................................... 103 3.4 Closure of the Water balance.................................................................... 103 3.5 Seasonal Trends and Extremes ................................................................. 103 4 RESULTS AND DISCUSSION................................................................... 105 4.1 Total Inputs............................................................................................... 105 4.1.1 Surface Water Inflows ...................................................................... 105 4.1.1.1 Validity of HBV-EC Model.......................................................... 105 4.1.1.2 Comparison of Total Inflow Estimates......................................... 108 4.1.1.2.1
Recommended publications
  • Drought Planning and Adaptation
    Running Head: DROUGHT PLANNING AND ADAPTATION Drought Disaster Planning and Adaptation in Rural British Columbia by Evan Lloyd A Thesis Submitted to the Faculty of Social and Applied Sciences in Partial Fulfillment of the Requirements for the Degree of Master of Arts In Disaster and Emergency Management Royal Roads University Victoria, British Columbia, Canada Supervisor: Professor Ann Dale June, 2017 Evan Lloyd, 2017 DROUGHT PLANNING AND ADAPTATION 2 COMMITTEE APPROVAL The members of Evan Lloyd’s Thesis Committee certify that they have read the thesis titled Drought Disaster Planning and Adaptation in Rural British Columbia and recommend that it be accepted as fulfilling the thesis requirements for the Degree of Master of Arts in Disaster and Emergency Management: Dr. Ross Pink [signature on file] Dr. Julie Drolet [signature on file] Final approval and acceptance of this thesis is contingent upon submission of the final copy of the thesis to Royal Roads University. The thesis supervisor confirms to have read this thesis and recommends that it be accepted as fulfilling the thesis requirements: Dr. Ann Dale [signature on file] DROUGHT PLANNING AND ADAPTATION 3 Creative Commons Statement This work is licensed under the Creative Commons Attribution-NonCommercial- ShareAlike 2.5 Canada License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/2.5/ca/. Some material in this work is not being made available under the terms of this licence: • Third-Party material that is being used under fair dealing or with permission. • Any photographs where individuals are easily identifiable. DROUGHT PLANNING AND ADAPTATION 4 Abstract Drought is one of the more devastating climate-driven hazards across the world.
    [Show full text]
  • Assessment of the Influence of Nonstationary Climate on Extreme Hydrology of Southwestern Canada
    ASSESSMENT OF THE INFLUENCE OF NONSTATIONARY CLIMATE ON EXTREME HYDROLOGY OF SOUTHWESTERN CANADA A Thesis Submitted to the Faculty of Graduate Studies and Research For the Degree of Special Case Doctor of Philosophy in Geography University of Regina By Sunil Gurrapu Regina, Saskatchewan January 2020 Copyright 2020: S. Gurrapu UNIVERSITY OF REGINA FACULTY OF GRADUATE STUDIES AND RESEARCH SUPERVISORY AND EXAMINING COMMITTEE Sunil Gurrapu, candidate for the degree of Special Case Doctor of Philosophy in Geography, has presented a thesis titled, Assessment of the Influence of Nonstationary Climate on Extreme Hydrology in Southwestern Canada, in an oral examination held on November 7, 2019. The following committee members have found the thesis acceptable in form and content, and that the candidate demonstrated satisfactory knowledge of the subject material. External Examiner: *Dr. Stephen Jacques Dery, University of Northern British Columbia Co-Supervisor: Dr. David Sauchyn, Department of Geography & Environmental Studies Co-Supervisor: *Dr. Kyle Hodder, Department of Geography & Environmental Studies Committee Member: *Dr. Jeannine St. Jacques, Adjunct Committee Member: Dr. Peng Wu, Environmental System Engineering Committee Member: Dr. Ulrike Hardenbicker, Department of Geography & Environmental Studies Chair of Defense: Dr. Fanhua Zeng, Faculty of Graduate Studies & Research *Via ZOOM conferencing ABSTRACT The demand for water supplies across southwestern Canada has increased substantially over the past century with growing population and economic activities. At the same time, the region’s resilience to the impacts of hydrological extremes, floods and droughts is challenged by the increasing frequency of these extreme events. In addition, increased winter temperatures over the past century have led to declines in winter snowpack and caused earlier snowmelt, leading in some years to a substantial shortage of water during late summer and fall seasons.
    [Show full text]
  • Sooke Watersheds, Inlet, Harbour and Basin Water Quality Assessment and Proposed Objectives
    ENVIRONMENTAL PROTECTION DIVISION MINISTRY OF ENVIRONMENT AND CLIMATE CHANGE STRATEGY Water Quality Assessment and Proposed Objectives for Sooke Watersheds, Inlet, Harbour and Basin TECHNICAL REPORT January 2019 WATER QUALITY ASSESSMENT AND PROPOSED OBJECTIVES: SOOKE WATERSHEDS/INLET/HARBOUR/BASIN Prepared by: Rosie Barlak Environmental Impact Assessment Biologist Environmental Protection Division MINISTRY OF ENVIRONMENT AND CLIMATE CHANGE STRATEGY ii WATER QUALITY ASSESSMENT AND PROPOSED OBJECTIVES: SOOKE WATERSHEDS/INLET/HARBOUR/BASIN EXECUTIVE SUMMARY This document presents a summary of the ambient water quality of Sooke Inlet, Harbour and Basin, and the streams in the surrounding watersheds that drain into these marine areas, near the District of Sooke, British Columbia (BC). The water quality assessment conducted here forms the basis for proposed water quality objectives (WQOs) to protect existing and future water uses. The WQOs have recently been approved and can be found in the following document “Water Quality Objectives for Sooke Inlet, Harbour, and Basin, and Tributary Streams” (BC ENV, 2019). There are 12 major watersheds that drain into the Sooke Inlet, Harbour and Basin. Nine are designated community watersheds, including four that are part of the Greater Victoria Water Supply Area (GVWSA). The T’Sou-ke Nation traditionally used to harvest shellfish in the Sooke marine areas; however the area has been closed to harvesting for many years. The designated water values/uses to be protected are shellfish harvesting, recreation and wildlife in the marine waters of the inlet/harbour/basin; and drinking water, aquatic life, recreation, irrigation and wildlife in the freshwater rivers and streams. There are many activities that can potentially affect water quality both in the marine and freshwater environments, such as rural and urban development, industry, agriculture, forestry, recreation and wildlife.
    [Show full text]
  • Significant Watersheds in the District of Sooke and Surrounding Areas
    Shawnigan Lake C O W I C H A N V A L L E Y R E G I O N A L D I S T R I C T Significant Watersheds in the District of Sooke Grant Lake and Surrounding Areas North C o w i c h a n V a l l e y Saanich R e g i o n a l D i s t r i c t Sidney OCelniptrahl ant Lake Saanich JdFEA H a r o S t r a Highlands it Saanich View Royal Juan de Fuca Langford Electoral Area Oak Bay Esquimalt Jarvis Colwood Victoria Lake Sooke Weeks Lake Metchosin Juan de Fuca Electoral Area ca SpectaFcu le Lake e d it an ra STUDY Ju St AREA Morton Lake Sooke Lake Butchart Lake Devereux Sooke River Lake (Upper) Council Lake Lubbe Wrigglesworth Lake Lake MacDonald Goldstream Lake r Lake e iv R e k o Bear Creek o S Old Wolf Reservoir Boulder Lake Lake Mavis y w Lake H a G d Ranger Butler Lake o a l n d a s Lake Kapoor Regional N C t - r i a s Forslund Park Reserve e g n W a a a o m r l f C r a T Lake r e R e k C i v r W e e e r a k u g h C r e Mount Finlayson e k Sooke Hills Provincial Park Wilderness Regional Park Reserve G o ld s Jack t re a Lake m Tugwell Lake R iv e r W augh Creek Crabapple Lake Goldstream Provincial Park eek Cr S ugh o Wa o Peden k Sooke Potholes e Lake C R Regional Park h i v a e Sheilds Lake r r t e r k e s re C ne i R ary V k M e i v e r e r V C Sooke Hills Table of Significant Watersheds in the e d i t d c Wilderness Regional h o T Charters River C Park Reserve District of Sooke and Surrounding Areas r e e k Watershed Name Area (ha) Sooke Mountain Sooke River (Upper) 27114.93 Boneyard Provincial Park Lake DeMamiel Creek 3985.29 Veitch Creek 2620.78
    [Show full text]
  • East Sooke Management Plan Engagement Process
    REPORT TO CAPITAL REGIONAL DISTRICT BOARD MEETING OF WEDNESDAY, JUNE 24, 2020 SUBJECT Management Plans for East Sooke and Roche Cove/Matheson Lake Regional Parks ISSUE SUMMARY To initiate management planning processes for East Sooke Regional Park and for Roche Cove and Matheson Lake regional parks. BACKGROUND East Sooke Regional Park (East Sooke) is located in the Juan de Fuca Electoral Area in East Sooke (Appendix A). The park was established in 1970 and is 1,456.6 hectares in size. East Sooke is classified as a Regional Wilderness Area because of its large size and remote and rugged nature. It features 48.9 kilometres of trails through forest, marsh and old fields, including the challenging 10-kilometre coast trail with its outstanding views of the Strait of Juan de Fuca and the Olympic Mountains. In addition to a developed trail system, the park features other facilities, including parking lots, rest areas, a group shelter and information kiosks. Roche Cove and Matheson Lake regional parks are located in East Sooke within the Juan de Fuca Electoral Area, District of Sooke and District of Metchosin, and are adjacent to Sooke Basin and the Galloping Goose Regional Trail (Appendix A). Roche Cove Regional Park was originally acquired by Capital Regional District (CRD) Regional Parks in 1985 and additional lands were acquired through a Crown Grant in 1990 and through private purchase in 1994. Adjacent Matheson Lake Regional Park was transferred from BC Parks to the CRD in 1994. Combined, Roche Cove and Matheson Lake regional parks comprise approximately 320 hectares. These parks are classified as Regional Natural Areas and feature opportunities for hiking, equestrian, fishing and nature appreciation.
    [Show full text]
  • Uvic Thesis Template
    ‗That Immense and Dangerous Sea‘: Spanish Imperial Policy and Power During the Exploration of the Salish Sea, 1790-1791. by Devon Drury BA, University of Victoria, 2007 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF ARTS in the Department of History Devon Drury, 2010 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. ii Supervisory Committee ‗That Immense and Dangerous Sea‘: Spanish Imperial Policy and Power During the Exploration of the Salish Sea, 1790-1791. by Devon Drury BA, University of Victoria, 2007 Supervisory Committee Dr. John Lutz, Department of History Supervisor Dr. Eric W. Sager, Department of History Departmental Member Dr. Patrick A. Dunae, Department of History Departmental Member iii Abstract Supervisory Committee Dr. John Lutz, Department of History Supervisor Dr. Eric W. Sager, Department of History Departmental Member Dr. Patrick A. Dunae, Department of History Departmental Member In the years between 1789 and 1792 the shores of what is now British Columbia were opened to European scrutiny by a series of mostly Spanish expeditions. As the coastline was charted and explored by agents of European empires, the Pacific Northwest captured the attention of Europe. In order to carry out these explorations the Spanish relied on what turned out to be an experiment in ‗gentle‘ imperialism that depended on the support of the indigenous ―colonized‖. This thesis examines how the Spanish envisioned their imperial space on the Northwest Coast and particularly how that space was shaped through the exploration of the Salish Sea.
    [Show full text]
  • Access to Water
    ACCESS TO WATER 301 CONTEXT FOR WATER ACCESS There is a considerable amount of waterfront property in East Sooke. The Strait of Juan de Fuca forms the southern boundary of East Sooke while Sooke Harbour and Basin act as the northern and western boundaries. The shoreline fronting the Strait is rugged and steep with two rocky beaches: Becher Bay and Iron Mine Bay; both of which are accessible by foot. Along Sooke Harbour and Basin, there is a combination of low and high bank shoreline where shingle beaches, muddy shoreline, and small coves are prevalent. QUESTION: Are there names for any of the beaches in the Sooke Basin & Harbour? When waterfront properties are subdivided, provincial land title legislation has long required the dedication of a 20 metre wide strip as highway at specified intervals. The purpose of this dedication is to facilitate future subdivision and provide access to water. This requirement can be waived by the Province if there are compelling reasons. Often when a high bank is involved, the right of way is not suitable as a road and it remains undeveloped. In East Sooke, the right of ways are owned and administered by the Province. The Province is not obligated to develop the right of ways as road or to maintain them. When properties adjacent to the right of ways are subdivided, a developer can be required to construct a public road. Organizations and individuals can also request permission from the Province to develop the right of ways. TABLE ###: Status of Foreshore Accesses in East Sooke 2014 DEVELOPED BY PROVINCE
    [Show full text]
  • Drought Preparedness
    -- CHECK AGAINST DELIVERY -- Statement by the Delegation of Canada to the Sixteenth Session of the United Nations Commission on Sustainable Development Wednesday, May 7 2008, 10:00 am – Drought Preparedness Mr/Madame Chairperson, Canada experienced serious land degradation and severe drought in the 1930s. In response, Canada developed soil and water conservation initiatives and converted fragile lands into grassland to inhibit land degradation. Despite these efforts drought can still cause loss of income and pose adaptation challenges. This was seen in the 2001 - 2002 drought, which affected regions not normally affected by drought such as parts of Eastern Canada and northern areas of Canada’s prairies. This drought cost an estimated $6 billion, in total, to the agriculture, forestry, petroleum and mining, hydro power, and water supply sectors. Climate change experts are anticipating greater variability and shifts in timing of available water supplies in the future, with a predicted increase in the frequency and duration of droughts. Because droughts are expensive, efforts are being applied to deal with drought proactively as a part of a comprehensive Canadian approach. Canada has established a range of drought identification activities. These activities require partnerships across jurisdictions and sectors. One example of drought monitoring and reporting is ‘Drought Watch’. This is a national program that provides timely information about climatic impacts on water supply and agriculture. Drought Watch products combine physical information, such as precipitation and soil moisture, with historic climate information to assess the status of drought in Canada’s agricultural regions. During each growing season, the Climate Production Risk Committee uses Drought Watch maps and regional information supplied by representatives from provinces and other government departments to assess drought impacts on soil conservation, crop and livestock management, and range, pest and water supply management.
    [Show full text]
  • 2019 Annual Report
    Greater Victoria Drinking Water Quality 2019 Annual Report Parks & Environmental Services Department Environmental Protection Prepared By Water Quality Program Capital Regional District 479 Island Highway, Victoria, BC, V9B 1H7 T: 250.474.9680 F: 250.474.9691 www.crd.bc.ca May 2020 Greater Victoria Drinking Water Quality 2019 Annual Report EXECUTIVE SUMMARY This report provides the annual overview of Capital Regional District (CRD) Water Quality Monitoring program and its results on water quality in 2019 within the Greater Victoria Drinking Water System (GVDWS) and its individual system components (Map 1). The results indicate that Greater Victoria’s drinking water continues to be of good quality and is safe to drink. The monitoring program is designed to meet the requirements of the provincial regulatory framework, which is defined by the BC Drinking Water Protection Act and Drinking Water Protection Regulation, and follow the federal guidelines for drinking water quality. The approximately 11,000 hectares of the Sooke and Goldstream watersheds comprise the source of our regional drinking water supply area. Water flows from the reservoirs to the Sooke and Goldstream (formerly called Japan Gulch) water treatment plants and then through large-diameter transmission mains and a number of storage reservoirs into eight different distribution systems, which in turn deliver the drinking water to the consumers. The monitoring program covers the entire system to anticipate any issues (i.e., source water monitoring), ensure treatment is effective (i.e., monitoring at the treatment facilities), and confirm a safe conveyance of the treated water to customers (i.e., transmission and distribution system monitoring).
    [Show full text]
  • Media Kit | Truekey.Ca
    MEDIA KIT | TRUEKEY.CA SOOKEPOINT OCEAN COTTAGE RESORT IS SET AWAY FROM THE VILLAGE OF SOOKE ON POSSESSION POINT, THE MOST SOUTHWEST TIP OF BRITISH COLUMBIA’S VANCOUVER ISLAND. THIS PREMIUM LUXURY RESORT IS SURROUNDED BY NATURE – PERCHED CLIFFSIDE ABOVE THE PACIFIC OCEAN AND HUGGED BY THE FORESTED LANDS OF THE POINT. This is your destination for unparalleled and abundant Orca whales and other ocean life watching opportunities right from your suite; plus you’re conveniently located near world class fishing charters in Sooke, endless scenic hikes and trails, sea kayaking, biking and more. SookePoint Ocean Cottage Resort’s oceanside suites offer an unrivaled oceanic vacation experience. An ideal home base for any traveler, each beautifully fully furnished studio, 1 and 2 bedroom suites offer breathtaking and undisturbed ocean views, fully equipped gourmet kitchens and overhanging ocean decks. MEDIA CONTACT [email protected] 403.614.6175 FACTS • The Resort offers 14 fully furnished, fully equipped studio, 1 and 2 bedroom vacation homes with incredible panoramic ocean views (more suites coming soon)! • Currently under development, the resort’s future amenities will include a pool, spa, marina, whale research centre, shops, restaurants, and more! • SookePoint Resort is located beside East Sooke Park which offers many hikes and hidden beaches. The village of Sooke is only 30 minutes away along with many other Sooke adventures. LINKS Website: www.sookepointresort.ca @SookePointResort Email: [email protected] @SookePointResort Trip Advisor: SookePoint Ocean Cottage Resort MEDIA CONTACT [email protected] 403.614.6175 ACTIVITIES || TRUEKTRUEKEEY.CA FISHING CHARTERS Experience the thrill of reeling in a 40-50 lb.
    [Show full text]
  • “A Multi-Millennia Perspective on Drought and Implications for the Future"
    CLIVAR/PAGES/IPCC Workshop “A multi-millennia perspective on drought and implications for the future" November 18-21, 2003 Tucson, AZ Organized by: Jonathan Overpeck, University of Arizona Kevin Trenberth, National Center For Atmospheric Research Sponsored by: US National Science Foundation US National Oceanographic and Atmospheric Administration Intergovernmental Panel on Climate Change For full background materials, venue, agenda, speakers and participants see: http://ipcc-wg1.ucar.edu/meeting/wg1/Drght/ also: Trenberth, K., J. Overpeck and S. Solomon, 2004: Exploring drought and its implications for the future. Eos, 85, No. 3, 20 Jan. 2004, p27. 1 Table of Contents 1. Organizational Acronyms Used..............................................................................3 2. Introduction ...........................................................................................................3 3. Initial Plenary Talks and Discussion.......................................................................4 3.1. Opening session.......................................................................................4 3.2. Instrumental and paleoclimatic records of drought...................................6 3.3. Drought processes and modeling .............................................................8 4. Breakout Working Groups ...................................................................................10 4.1. Introduction...........................................................................................10 4.2. Summary
    [Show full text]
  • Canadian Drought Monitor Conditions As of March 31, 2014
    Canadian Drought Monitor Conditions as of March 31, 2014 The frigid Canadian winter continued into March, with monthly mean temperatures more than 5 degrees Celsius below-normal from Alberta all the way to the Atlantic region. This continued to delay snowmelt across the country, resulting in little change in drought conditions. However, between February and March, the amount and severity of drought in Canada did decrease slightly. Some new abnormally dry areas were identified in central British Columbia and northwestern Alberta, but other dry areas showed improvement. The areas of Moderate Drought (D1) and Severe Drought (D2) were smaller in March than in February. Precipitation in March was above-average in southern British Columbia, east central Alberta, and the Atlantic region, average in northern Ontario and Quebec, and below-average throughout the Prairie region and southern Ontario. Over the winter season, the areas receiving the least precipitation were east central Alberta and southern Manitoba. As a result, an area of Moderate Drought (D1) has been declared in east central Alberta, as precipitation has been record dry to extremely low since September 2013 in that area. In southern Manitoba, the area of Moderate Drought (D1) expanded slightly. The other area of concern was southern British Columbia, but this area has improved since February due to significant precipitation. There remains some Moderate Drought (D1) and a small strip of Severe Drought (D2), but provincial records are showing average to above-average snow water content in that area, which should bring further improvements upon snowmelt. High elevation snowmelt in British Columbia typically begins in the middle of April.
    [Show full text]