The Cost of Climate Adaptation at the Local Level
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For the Canadian Transportation Sector 2016 (Pp
3 · Northern Territories CHAPTER 3: NORTHERN TERRITORIES LEAD AUTHOR: KALA PENDAKUR1 CONTRIBUTING AUTHORS: JACKIE DAWSON (UNIVERSITY OF OTTAWA), KATERINE GRANDMONT (UNIVERSITY OF MONTREAL), DOUG MATTHEWS (MATTHEWS ENERGY CONSULTING), ART STEWART (GOVERNMENT OF NUNAVUT) RECOMMENDED CITATION: Pendakur, K. (2017). Northern Territories. In K. Palko and D.S. Lemmen (Eds.), Climate risks and adaptation practices for the Canadian transportation sector 2016 (pp. 27-64). Ottawa, ON: Government of Canada. 1 The Conference Board of Canada, Ottawa, ON Climate Risks & Adaptation Practices - For the Canadian Transportation Sector 2016 TABLE OF CONTENTS Key Findings .........................................................................................................................................................29 1.0 Introduction ..................................................................................................................................................29 1.1 Regional overview .............................................................................................................................30 2.0 An introduction to Canada’s northern transportation system...............................................................31 2.1 System overview ................................................................................................................................31 2.2 Road transportation ..........................................................................................................................33 2.3 -
Future Possible Dry and Wet Extremes in Saskatchewan, Canada
!"#"$%&'())*+,%&-$.&/01&2%#& 34#$%5%)&*0&6/)7/#89%:/0;& </0/1/&& '$%=/$%1&>($	%&2/#%$&6%8"$*#.&?@%08.;&6/)7/#89%:/0& 3&29%/#(0;&A&A(0)/,;&B&2*##$(87&&CDEF&& 6G<&'"+&H&EFIJCKE3EF& & Future Possible Dry and Wet Extremes in Saskatchewan, Canada Prepared for the Water Security Agency, Saskatchewan E Wheaton Adjunct Professor, University of Saskatchewan and Emeritus Researcher, Saskatchewan Research Council Box 4061 Saskatoon, SK, 306 371 1205 B Bonsal Research Scientist, Environment Canada Adjunct Professor, University of Saskatchewan Saskatoon, SK V Wittrock Research Scientist, Saskatchewan Research Council Saskatoon, SK November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�$4! 56! 7$#4+89&4(!,-+#(.(!)*+*#(!"#(/010+&+0$2!3/(2�$4! 56! .,*8)-2*.2')*'8"+"%2':%,12.+),*!' =9! -)!."!!),*'$*-'.,*.6"!),*!' =>! $.?*,@62-;2#2*+!' AB! %282%2*.2!' A<! 3 6MNN?GO& Droughts and extreme precipitation are extreme climate events and among the most costly and disruptive environmental hazards. -
Aviation Investigation Report A06w0002 In-Flight Engine Fire Buffalo Airways Limited Douglas C-54G-Dc (Dc-4) C-Gxkn Norman Well
AVIATION INVESTIGATION REPORT A06W0002 IN-FLIGHT ENGINE FIRE BUFFALO AIRWAYS LIMITED DOUGLAS C-54G-DC (DC-4) C-GXKN NORMAN WELLS, NORTHWEST TERRITORIES (CYVQ) 05 JANUARY 2006 The Transportation Safety Board of Canada (TSB) investigated this occurrence for the purpose of advancing transportation safety. It is not the function of the Board to assign fault or determine civil or criminal liability. Aviation Investigation Report In-Flight Engine Fire Buffalo Airways Limited Douglas C-54G-DC (DC-4) C-GXKN Norman Wells, Northwest Territories (CYVQ) 05 January 2006 Report Number A06W0002 Summary The Buffalo Airways Limited Douglas C-54G-DC (DC-4), registration C-GXKN, serial number 36090, departed from Norman Wells, Northwest Territories, at 1749 mountain standard time for a visual flight rules flight to Yellowknife, Northwest Territories, with a crew of four and 2000 pounds of cargo. While climbing through an altitude of approximately 3500 feet above sea level, the crew experienced a failure of the number 2 engine and a nacelle fire. The crew carried out the Engine Fire Checklist, which included discharging the fire bottles and feathering the number 2 propeller. The fire continued unabated. During this period, an uncommanded feathering of the number 1 propeller and an uncommanded extension of the main landing gear occurred. The crew planned for an emergency off-field landing, but during the descent to the landing area, the fuel selector was turned off as part of the Engine Securing Checklist, and the fire self-extinguished. A decision was made to return to the Norman Wells Airport where a successful two-engine landing was completed at 1804 mountain standard time. -
Adapting Infrastructure to Climate Change in Canada's
Infrastructure Canada Part of the Transport, Infrastructure and Communities Portfolio ADAPTING INFRASTRUCTURE TO CLIMATE CHANGE IN CANADA’S CITIES AND COMMUNITIES A Literature Review Research & Analysis Division Infrastructure Canada December 2006 Table of Contents Section 1: Introduction..................................................................................................... 1 Context and overview of the report.............................................................................. 3 Section 2: Adaptation Processes .................................................................................... 5 Section 3: Adaptation Responses ................................................................................... 7 3.1 Literature by Type of Infrastructure........................................................................ 8 3.1.1 Water Supply and Wastewater Infrastructure................................................. 8 3.1.2 Transportation Infrastructure........................................................................ 11 3.2 Regionally Specific Literature .............................................................................. 12 3.3 Literature on Climate Change Adaptation for Cities and Communities................ 15 3.4 Literature Related to Engineering Needs............................................................. 18 Section 4: Conclusion.................................................................................................... 20 Adapting Infrastructure to Climate Change in Canada’s -
Evolution of Winter Temperature in Toronto, Ontario, Canada: a Case Study of Winters 2013/14 and 2014/15
15 JULY 2017 A N D E R S O N A N D GOUGH 5361 Evolution of Winter Temperature in Toronto, Ontario, Canada: A Case Study of Winters 2013/14 and 2014/15 CONOR I. ANDERSON AND WILLIAM A. GOUGH Department of Physical and Environmental Sciences, University of Toronto Scarborough, Scarborough, Ontario, Canada (Manuscript received 29 July 2016, in final form 27 March 2017) ABSTRACT Globally, 2014 and 2015 were the two warmest years on record. At odds with these global records, eastern Canada experienced pronounced annual cold anomalies in both 2014 and 2015, especially during the 2013/14 and 2014/15 winters. This study sought to contextualize these cold winters within a larger climate context in Toronto, Ontario, Canada. Toronto winter temperatures (maximum Tmax, minimum Tmin,andmeanTmean)for the 2013/14 and 2014/15 seasons were ranked among all winters for three periods: 1840/41–2015 (175 winters), 1955/56–2015 (60 winters), and 1985/86–2015 (30 winters), and the average warming trend for each temperature metric during these three periods was analyzed using the Mann–Kendall test and Thiel–Sen slope estimation. The winters of 2013/14 and 2014/15 were the 34th and 36th coldest winters in Toronto since record-keeping began in 1840; however these events are much rarer, relatively, over shorter periods of history. Overall, Toronto winter temperatures have warmed considerably since winter 1840/41. The Mann–Kendall analysis showed statistically significant monotonic trends in winter Tmax, Tmin,andTmean over the last 175 and 60 years. These trends notwithstanding, there has been no clear signal in Toronto winter temperature since 1985/86. -
NWT/NU Spills Working Agreement
NORTHWEST TERRITORIES–NUNAVUT SPILLS WORKING AGREEMENT Updated October 2014 This page intentionally left blank. TABLE OF CONTENTS Section Content Page Cover Front Cover 1 Cover Inside Front Cover 2 Introductory Table of Contents 3 Introductory Record of Amendments 3 1. Introduction/Purpose/Goals 4 2. Parties to the Agreement 5 3. Letter of Agreement 6 - Background 6 - Lead Agency Designation and Contact 6 - Lead Agency Responsibilities 6 - General 7 4. Signatures of Parties to the Agreement 8 5. Glossary of Terms 9 Table 1A Lead Agency Designation for Spills in the NT and NU 10 Table 1B Lead Agency Designation for NT Airport Spills 14 Table 1C Lead Agency Designation for NU Airport Spills 14 Table 1D Territorial Roads and Highways in the NT 15 Table 1E Territorial Roads in NU 15 Table 2 General Guidelines for Assessing Spill Significance and Spill File Closure 16 Table 3 Spill Line Contract and Operation 17 Appendix A Schedule 1 - Reportable Quantities for NT-NU Spills 18 Appendix B Spill Line Report Form 20 Appendix C Instructions for Completing the NT/NU Spill Report Form 21 Appendix D Environmental Emergencies Science Table (Science Table) 22 RECORD OF AMENDMENTS * No. Amendment Description Entered By / Date Approved By / Date 1 GNWT spills response structure changed on April 1. 2014 to reflect the changes of devolution. Departments of Industry Tourism and Investment and Lands were added to the NT/NU SWA 2 Environment Canada nationally restructured their spill response structure in 2012. 3 4 5 6 7 8 9 10 * Starting in 2015, the NT/NU SWA will be reviewed and updated annually during the Fall NT/NU Spills Working Group meeting. -
Decolonizing Climate Policy in Canada Phase 1
March 2021 Indigenous Climate Action Decolonizing Climate Policy in Canada Report from Phase One Table of Contents About Indigenous Climate Action ..................................................................................................................................... 3 Acknowledgments ................................................................................................................................................................. 4 Executive Summary .............................................................................................................................................................. 5 1. Introduction ........................................................................................................................................................................ 8 1.1 The Methods we Used for Phase 1.........................................................................................................................10 1.2 What we Found ...........................................................................................................................................................11 2. Overview of Climate Policy and Plans in Canada ...................................................................................................12 2.1 The Pan-Canadian Framework (PCF) ....................................................................................................................12 2.2 A Healthy Environment, A Healthy Economy (HEHE) .......................................................................................12 -
THE CLIMATE of the CANADIAN ARCTIC 59 Recorded Temperature in Canada
THE CLIMATE OF THE CANADIAN ARCTIC 59 recorded temperature in Canada. Mean daily temperatures for March of —36°F at Eureka, — 25°F at Resolute and — 15°F at Baker Lake are indicative of the great length of the period of severe cold at Arctic stations. The frequencies of occurrence of low temperatures at these stations provide further evidence of the coldness of the Arctic. During the four coldest months—December, January, February and March—temperatures may be expected to drop as low as — 10°F on 85 to 100 p.c. of the days, -20°F on 70 to 95 p.c. of the days and -30°F on 30 to 90 p.c. of the days (the lower frequencies apply to southern sections of the Arctic and the higher values to the northern islands of the Archipelago). Readings of — 50°F are about as frequent at stations in the high Arctic as in the recognized cold spots of the Yukon in December and January but are considerably more frequent in February and March. At the high Arctic stations of Eureka and Isachsen the longest uninterrupted spells with temperatures —50°F or lower, during the decade 1951-60, were four and five days respec tively. On one occasion, temperatures remained below — 40°F at Eureka during ten consecutive days. Several northern Arctic stations have failed to record temperatures higher than —30°F for periods up to 22 consecutive days. Sheltered interior locations on the larger islands are subject to greater cooling than are the coastal sites of the weather stations. -
Saskatchewan's Natural Capital in a Changing Climate
Saskatchewan’s Natural Capital in a Changing Climate: An Assessment of Impacts and Adaptation PARC PARAIRIE DAPTATIONRC ESEARCH OLLABORATIVE Lead Author: Dave Sauchyn Contributing Authors: Elaine Barrow, X. Fang, Norm Henderson, Mark Johnston, John Pomeroy, Jeff Thorpe, Elaine Wheaton, B. Williams Saskatchewan’s Natural Capital in a Changing Climate: An Assessment of Impacts and Adaptation Lead Author: Dave Sauchyn1 Contributing Authors: Elaine Barrow2, X. Fang3, Norm Henderson1, Mark Johnston4, John Pomeroy3, Jeff Thorpe4, Elaine Wheaton4, B. Williams3 1 Prairie Adaptation Research Collaborative 2 Climate Research Services, Regina 3 University of Saskatchewan 4 Saskatchewan Research Council This document is available for download from the PARC website (www.parc.ca). PARC acknowledges the funding support of Saskatchewan Environment April 2009 Citation: Sauchyn, Dave; Barrow, Elaine; Fang, X., Henderson, Norm; Johnston, Mark; Pomeroy, John; Thorpe, Jeff; Wheaton, Elaine; and Williams, B. 2009. Saskatchewan’s Natural Capital in a Changing Climate: An Assessment Of Impacts And Adaptation. Report to Saskatchewan Ministry of Environment from the Prairie Adaptation Research Collaborative, 162 pp. CONTENTS Executive Summary........................................................................................................................ 8 Introduction................................................................................................................................... 13 Past Climate and Recent Trends .................................................................................................. -
Carbon Pricing, Fairness, and Fiscal Federalism: a Cost-Sharing Proposal for Canada
Queen’s Policy Review Volume 2, No. 2 (Fall 2011) Carbon Pricing, Fairness, and Fiscal Federalism: A Cost-Sharing Proposal for Canada Monica Tang Carleton University, Freie Universität Berlin ABSTRACT Carbon pricing has been proposed as a mechanism to reduce carbon emissions in the efforts to mitigate the impacts of climate change. However, the potentially uneven distribution of costs between provinces and regions across Canada has stalled progress on the issue. This paper examines the possibility of implementing cost-sharing arrangements and revenue recycling within the Canadian intergovernmental context to address issues of fairness and fiscal capacity and recommends the coupling of ecological tax reforms with adjustments in intergovernmental transfers. Introduction The setting is a First Ministers Conference, where the Prime Minister and provincial and territorial ministers have gathered to discuss what Canada’s approach should be for reducing carbon and other greenhouse gas emissions in order to mitigate and adapt to the effects of global climate change. Similar to other intergovernmental discussions on issues such as healthcare or education, the questions of fiscal capacity, distribution, and fairness will likely arise. There may be heated debate about which level of government should be responsible for service provision. There may be pleas for special accommodation or exemption for particular provinces. Past disagreements may be revisited about real or perceived unfair treatment of provinces in previous First Ministers Conferences. 17 Queen’s Policy Review Volume 2, No. 2 (Fall 2011) This scenario, while fictional, is certainly plausible. The challenges with addressing climate change on a national level arise from differing provincial economies, emissions profiles, and fiscal capacities. -
Calgary ALBERTA
of Canada Calgary ALBERTA Calgary and Climate Change The climate determines almost everything about how we design, build, and live in our cities. As the climate changes, the safety and High-Carbon prosperity of our cities is put at risk. Climate change is a Climate Change Projections* challenge that requires us to work together, locally, nationally, and globally. With technical know-how, political will, targeted 1976-2005 2051-2080 investments, and collective commitment, we can mitigate the Change Mean Low Mean High severity of climate change and build resilience to its impacts. Typical Climate Change and Health hottest 31.6 °C 33.0 °C 36.6 °C 40.1 °C High temperatures in urban centres can be hazardous, especially summer day for the elderly, the chronically ill, and those without air conditioning. High and prolonged heat can also impact air Typical quality, facilitate the spread of harmful diseases, inhibit outdoor coldest -33.2 °C -31.7 °C -26.0 °C -19.5 °C winter day activities, and cause stress and anxiety. We can adapt with measures such as shaded areas, green roofs, and supports for those who need help during heat waves. Number of +30 °C days 5 11 32 55 per year Climate Change and Extreme Weather A warmer climate may increase the chance of more extreme weather, including high winds, flash floods, hail, lightning, Spring 103 mm 89 mm 129 mm 199 mm tornadoes, drought, and wildfires. Cities must improve their precipitation planning and engineering, emergency preparedness, and water management to cultivate resilience. Summer 201 mm 97 mm 202 mm 333 mm Climate Change and Infrastructure precipitation Climate change may threaten the integrity of infrastructure such as roads, bridges, water supply, and telecommunications, most of Number of which has not been built to withstand future extremes. -
Is 2019 Spring Ottawa Flood Caused by Climate Change?
IS 2019 SPRING OTTAWA FLOOD CAUSED BY CLIMATE CHANGE? Xuebin Zhang, Climate Research Division Is this due to climate change? • A short answer: we don’t know. • A longer answer: there is no simple answer to this question (but this is not that useful at all). • What do we know? Canada has warmed, faster than the global average Annual • Annual average temperature in Canada has increased by 1.7◦C between 1948 and 2016. • Canada has warmed about two times the global rate. • Warming is not uniform across Canada. Northern Canada has warmed by 2.3◦C, about three times global warming. • Most of the observed increase in annual average temperature in Canada can be attributed to human influence 3 THE EFFECTS OF WIDESPREAD WARMING ARE EVIDENT ACROSS MANY INDICATORS. Changes in annual precipitation Length of growing season (days) 1948-2012 • Annual precipitation has increased in many regions since 1948. • Averaged over the country, normalized precipitation has increased by about 20% from 1948 to 2012. • An increase in growing season length of about 15 days between 1948 and 2016 has been observed. 9 The seasonal timing of peak streamflow has shifted, driven by warming temperatures. • Over the last several decades, spring peak streamflow following snowmelt has occurred earlier, with higher winter and early spring flows. In some areas, reduced summer flows have been observed. • Seasonal changes projected to continue, with shifts from more snowmelt-dominated regimes toward rainfall-dominated regimes. Most of the observed temperature increase can be attributed to human influence • Anthropogenic (human) activities explain most of the historical warming trend in annual average temperature, as well as for the hottest and coldest temperatures of the year • Natural external factors (solar and volcanic activity) play a very minor role 6 ANTHROPOGENIC CLIMATE CHANGE HAS INCREASED THE LIKELIHOOD OF SOME TYPES OF EXTREME EVENTS.