Abstract

Cold temperature and associated extremes often impact adversely human health and environment and bring disruptions in economic activities during winter over Canada. This study investigates projected changes in winter (December to March) period cold extreme days (i.e., cold nights, cold days, frost days, and ice days) and cold spells over Canada based on 11 regional climate model (RCM) simulations for the future 2040–2069 period with respect to the current 1970–1999 period. These simulations, available from the North American Regional Climate Change Assessment Program, were obtained with six different RCMs, when driven by four different Atmosphere–Ocean General Circulation Models, under the Special Report on Emissions Scenarios A2 scenario. Based on the reanalysis boundary conditions, the RCM simulations reproduce spatial patterns of observed mean values of the daily minimum and maximum temperatures and inter-annual variability of the number of cold nights over different Canadian climatic regions considered in the study. A comparison of current and future period simulations suggests decreases in the frequency of cold extreme events (i.e., cold nights, cold days and cold spells) and in selected return levels of maximum duration of cold spells over the entire study domain. Important regional differences are noticed as the simulations generally indicate smaller decreases in the characteristics of extreme cold events over western Canada compared to the other regions. The analysis also suggests an increase in the frequency of midwinter freeze–thaw events, due mainly to a decrease in the number of frost days and ice days for all Canadian regions. Especially, densely populated southern and coastal Canadian regions will require in depth studies to facilitate appropriate adaptation strategies as these regions are clearly expected to experience large increases in the frequency of freeze–thaw events.

Highlights

  • According to the Intergovernmental Panel on Climate Change (IPCC 2012), significant changes in the frequency, spatial extent, and duration of temperature extremes can be expected in future climate

  • Prior to validating cold extremes indices, Tmin and Tmax series obtained from regional climate model (RCM)–NCEP2s for the 1981–2003 period are evaluated

  • The mean values of Tmax for these regions are lower than 0 °C, except for the southern parts of the western coastal (WCOAST) and western cordillera (WCRDRA), Canadian Maritimes (MRTMS), and Great Lakes (GRTLKS) regions

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Summary

Introduction

According to the Intergovernmental Panel on Climate Change (IPCC 2012), significant changes in the frequency, spatial extent, and duration of temperature extremes can be expected in future climate. Since these extremes have major effects on various human and natural systems, it is relevant to assess projected changes to temperature extremes in a future warmer climate. A decrease in the frequency of cold days and an increase in the frequency of hot days have been suggested for the twenty-first century, based on projections of global climate models contributing to the Coupled Model Intercomparison Project Phases 3 and 5 (CMIP3 and CMIP5) (IPCC 2012, 2013; Ma et al 2012; Peings et al 2013; Sillmann et al 2013). Cold temperature extremes have received less attention compared to hot temperature extremes at the regional scale (e.g., Islam et al 2009)

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