4.0 Article

Temperature Extremes from Canadian Regional Climate Model (CRCM) Climate Change Projections

Journal

ATMOSPHERE-OCEAN
Volume 52, Issue 3, Pages 191-210

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/07055900.2014.886179

Keywords

temperature extremes; Extreme Value Theory; non-stationary fit; extremes versus averages; CRCM; CMIP3; HadEX2

Funding

  1. World Meteorological Organization (WMO) Expert Team on Climate Change Detection and Indices (ETCCDI) Linkage Project [LP100200690]

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Future climate projections of extreme events can help forewarn society of high-impact events and allow the development of better adaptation strategies. In this study a non-stationary model for Generalized Extreme Value (GEV) distributions is used to analyze the trend in extreme temperatures in the context of a changing climate and compare it with the trend in average temperatures. The analysis is performed using the climate projections of the Canadian Regional Climate Model (CRCM), under an IPCC SRES A2 greenhouse gas emissions scenario, over North America. Annual extremes in daily minimum and maximum temperatures are analyzed. Significant positive trends for the location parameter of the GEV distribution are found, indicating an expected increase in extreme temperature values. The scale parameter of the GEV distribution, on the other hand, reveals a decrease in the variability of temperature extremes in some continental regions. Trends in the annual minimum and maximum temperatures are compared with trends in average winter and summer temperatures, respectively. In some regions, extreme temperatures exhibit a significantly larger increase than the seasonal average temperatures. The CRCM projections are compared with those of its driving model and framed in the context of the Coupled Model Intercomparison Project, phase 3 (CMIP3) Global Climate Model projections. This enables us to establish the CRCM position within the CMIP3 climate projection uncertainty range. The CRCM is validated against the HadEX2 dataset in order to assess the CRCM representation of temperature extremes in the present climate. The validation is also framed in the context of CMIP3 validation results. The CRCM cold extremes validate better and are closer to the driving model and CMIP3 projections than the hot extremes.

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