An Overview of Climate Change Induced Hydrological Variations in Canada for Irrigation Strategies
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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. -
The Mounties and the Origins of Peace in the Canadian Prairies∗
The Mounties and the Origins of Peace in the Canadian Prairies∗ Pascual Restrepo October 2015 Abstract Through a study of the settlement of the Canadian Prairies, I examine if differences in violence across regions reflect the historical ability of the state to centralize authority and monopolize violence. I compare settlements that in the late 1880s were located near Mountie- created forts with those that were not. Data from the 1911 Census reveal that settlements far from the Mounties’ reach had unusually high adult male death rates. Even a century later the violence in these communities continues. In 2014, communities located at least 100 kilometers from former Mountie forts during their settlement had 45% more homicides and 55% more violent crimes per capita than communities located closer to former forts. I argue that these differences may be explained by a violent culture of honor that emerged as an adaptation to the lack of a central authority during the settlement but persisted over time. In line with this interpretation, I find that those who live in once-lawless areas are more likely to hold conservative political views. In addition, I use data for hockey players to uncover the influence of culture on individual behavior. Though players interact in a common environment, those who were born in areas historically outside the reach of the Mounties are penalized for their violent behavior more often than those who were not. Keywords: Culture, Violence, Culture of honor, Monopoly of violence, Institutions. JEL Classification: N32, N42, D72, D74, H40, J15, K14, K42, Z10 ∗I thank Daron Acemoglu, Abhijit Banerjee, Alberto Chong, Pauline Grosjean, Suresh Naidu, Ben Olken and Hans-Joachim Voth for their comments and helpful discussion. -
Hydrological Extremes in the Canadian Prairies in the Last Decade Due to the ENSO Teleconnection—A Comparative Case Study Using WRF
water Article Hydrological Extremes in the Canadian Prairies in the Last Decade due to the ENSO Teleconnection—A Comparative Case Study Using WRF Soumik Basu * , David J. Sauchyn and Muhammad Rehan Anis Prairie Adaptation Research Collaborative, Regina, SK S4S 0A2, Canada; [email protected] (D.J.S.); [email protected] (M.R.A.) * Correspondence: [email protected] Received: 8 September 2020; Accepted: 21 October 2020; Published: 23 October 2020 Abstract: In the Prairie provinces of Alberta, Saskatchewan, and Manitoba, agricultural production depends on winter and spring precipitation. There is large interannual variability related to the teleconnection between the regional hydroclimate and El Niño and La Niña in the Tropical Pacific. A modeling experiment was conducted to simulate climatic and hydrological parameters in the Canadian Prairie region during strong El Niño and La Niña events of the last decade in 2015–2016 and 2010–2011, respectively. The National Center for Atmospheric Research (NCAR) Weather Research and Forecasting (WRF) model was employed to perform two sets of sensitivity experiments with a nested domain at 10 km resolution using the European Centre for Medium-Range Weather Forecasts Reanalysis (ERA) interim data as the lateral boundary forcing. Analysis of the hourly model output provides a detailed simulation of the drier winter, with less soil moisture in the following spring, during the 2015–2016 El Niño and a wet winter during the La Niña of 2010–2011. The high-resolution WRF simulation of these recent weather events agrees well with observations from weather stations and water gauges. Therefore, we were able to take advantage of the WRF model to simulate recent weather with high spatial and temporal resolution and thus study the changes in hydrometeorological parameters across the Prairie during the two extreme hydrological events of the last decade. -
BREAKDOWN of SUB-REGIONS Americas
BREAKDOWN OF SUB-REGIONS Americas Atlantic Islands and Central and Canada Eastern US Latin America Southwest US Argentina Atlantic Canada Kansas City Boston Atlantic Islands British Columbia Nebraska Hartford Brazil A Canadian Prairies Oklahoma Maine Brazil B Montreal & Quebec Southwest US A New York A Central America Toronto Southwest US B New York B Chile St. Louis Philadelphia Colombia Pittsburgh Mexico Washington DC Peru Western New York Uruguay Midwest US Southeastern US Western US Chicago Florida Colorado Cleveland Greater Tennessee Desert US Indianapolis Louisville Hawaii Iowa Mid-South US Idaho Madison North Carolina Los Angeles Milwaukee Southern Classic New Mexico Minnesota Virginia Northern California Southern Ohio Orange County West Michigan Portland Salt Lake San Diego Seattle Spokane Asia Pacific Oceania Eastern Asia Southeastern Asia Southern Asia Brisbane Beijing Cambodia Bangladesh Melbourne Chengdu Indonesia India A New Zealand Hong Kong Malaysia India B Perth Japan Philippines India C Sydney Korea Singapore Nepal Mongolia Thailand Pakistan Shanghai Vietnam Sri Lanka Shenzhen A Shenzhen B Taiwan Europe, Middle East, and Africa Sub-Saharan Africa Eastern Europe Northern Europe Southern Europe Ethiopia Bulgaria Denmark & Norway Croatia Ghana Czech Republic Finland Cyprus Kenya Hungary Ireland Greece Mauritius Kazakhstan Sweden Israel Nigeria A Poland A Istanbul Nigeria B Poland B Italy Rwanda Romania Portugal South Africa Russia A Serbia Tanzania Russia B Slovenia Uganda Slovakia Spain Zimbabwe Ukraine A Ukraine B Middle East and Western Europe North Africa Austria Bahrain Benelux Doha France Egypt Germany Emirates Switzerland Jordan Kuwait Lebanon Morocco Oman Saudi Arabia . -
Weather and Climate Extremes on the Canadian Prairies: an Assessment with a Focus on Grain Production
Environment and Ecology Research 5(4): 255-268, 2017 http://www.hrpub.org DOI: 10.13189/eer.2017.050402 Weather and Climate Extremes on the Canadian Prairies: An Assessment with a Focus on Grain Production 1,* 2 E. Ray Garnett and Madhav L. Khandekar 1Agro-Climatic Consulting, Canada 2Former Environment Canada Scientist, Expert Reviewer IPCC 2007, Climate Change Documents, Canada Copyright©2017 by authors, all rights reserved. Authors agree that this article remains permanently open access under the terms of the Creative Commons Attribution License 4.0 International License Abstract The Canadian prairies are Canada’s granaries, 1 . Introduction producing up to 75 million tons of grain (primarily wheat, barley, and oats) and oilseeds (primarily canola) during the The Canadian prairie provinces have an area of about 2 summer months of June to August. Canada is a major grain million square kilometers, an area greater than Spain and exporting country; exports have a market value of about Portugal combined, and they make up about 20% of the total 30-40 billion US dollars. The Canadian prairie agricultural area of Canada. The prairie provinces are situated in western industry is a major socio-economic activity for western Canada; Canada extends from Victoria (British Columbia) in Canada, employing thousands in farming communities and the west to St John’s (Newfoundland) in the east. The current in other industries such as transportation on a year-round population of the three prairie provinces is now over 6 basis. A good grain harvest in a given year depends critically million, about 1/6th of the total population of Canada, about on various summer weather and climate extremes which can 36.5 million. -
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. -
Global and Continental Drought in the Second Half of the Twentieth Century: Severity–Area–Duration Analysis and Temporal Variability of Large-Scale Events
1962 JOURNAL OF CLIMATE VOLUME 22 Global and Continental Drought in the Second Half of the Twentieth Century: Severity–Area–Duration Analysis and Temporal Variability of Large-Scale Events J. SHEFFIELD Department of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey K. M. ANDREADIS Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington E. F. WOOD Department of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey D. P. LETTENMAIER Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington (Manuscript received 10 July 2008, in final form 15 October 2008) ABSTRACT Using observation-driven simulations of global terrestrial hydrology and a cluster algorithm that searches for spatially connected regions of soil moisture, the authors identified 296 large-scale drought events (greater than 500 000 km2 and longer than 3 months) globally for 1950–2000. The drought events were subjected to a severity–area–duration (SAD) analysis to identify and characterize the most severe events for each continent and globally at various durations and spatial extents. An analysis of the variation of large-scale drought with SSTs revealed connections at interannual and possibly decadal time scales. Three metrics of large-scale drought (global average soil moisture, contiguous area in drought, and number of drought events shorter than 2 years) are shown to covary with ENSO SST anomalies. At longer time scales, the number of 12-month and longer duration droughts follows the smoothed variation in northern Pacific and Atlantic SSTs. Globally, the mid-1950s showed the highest drought activity and the mid-1970s to mid-1980s the lowest activity. -
Meltwater Run-Off from Haig Glacier, Canadian Rocky Mountains, 2002–2013
Hydrol. Earth Syst. Sci., 18, 5181–5200, 2014 www.hydrol-earth-syst-sci.net/18/5181/2014/ doi:10.5194/hess-18-5181-2014 © Author(s) 2014. CC Attribution 3.0 License. Meltwater run-off from Haig Glacier, Canadian Rocky Mountains, 2002–2013 S. J. Marshall Department of Geography, University of Calgary, 2500 University Dr NW, Calgary AB, T2N 1N4, Canada Correspondence to: S. J. Marshall ([email protected]) Received: 14 June 2014 – Published in Hydrol. Earth Syst. Sci. Discuss.: 21 July 2014 Revised: 18 October 2014 – Accepted: 1 November 2014 – Published: 12 December 2014 Abstract. Observations of high-elevation meteorological 1 Introduction conditions, glacier mass balance, and glacier run-off are sparse in western Canada and the Canadian Rocky Moun- Meltwater run-off from glacierized catchments is an inter- tains, leading to uncertainty about the importance of glaciers esting and poorly understood water resource. Glaciers pro- to regional water resources. This needs to be quantified so vide a source of interannual stability in streamflow, supple- that the impacts of ongoing glacier recession can be eval- menting snow melt, and rainfall (e.g. Fountain and Tangborn, uated with respect to alpine ecology, hydroelectric opera- 1985). This is particularly significant in warm, dry years (i.e. tions, and water resource management. In this manuscript drought conditions) when ice melt from glaciers provides the the seasonal evolution of glacier run-off is assessed for an main source of surface run-off once seasonal snow is de- alpine watershed on the continental divide in the Canadian pleted (e.g. Hopkinson and Young, 1998). -
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 ..................................................................................................