Mixed precipitation occurrences over southern Québec, Canada, under warmer climate conditions using a regional climate model
Autor: | René Laprise, Julie M. Thériault, Dominic Matte |
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Rok vydání: | 2018 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Climate change High resolution 010502 geochemistry & geophysics 01 natural sciences Freezing rain Climatology Precipitation types Environmental science Climate model Precipitation Ice pellets 0105 earth and related environmental sciences Winter weather |
Zdroj: | Climate Dynamics. 53:1125-1141 |
ISSN: | 1432-0894 0930-7575 |
DOI: | 10.1007/s00382-018-4231-2 |
Popis: | Winter weather events with temperatures near $$0\,^\circ\mathrm{{C}}$$ are often associated with freezing rain. They can have major impacts on the society by causing power outages and disruptions to the transportation networks. Despite the catastrophic consequences of freezing rain, very few studies have investigated how their occurrences could evolve under climate change. This study aims to investigate the change of freezing rain and ice pellets over southern Quebec using regional climate modeling at high resolution. The fifth-generation Canadian Regional Climate Model with climate scenario RCP 8.5 at $$0.11^\circ$$ grid mesh was used. The precipitation types such as freezing rain, ice pellets or their combination are diagnosed using five methods (Cantin and Bachand, Bourgouin, Ramer, Czys and, Baldwin). The occurrences of the diagnosed precipitation types for the recent past (1980–2009) are found to be comparable to observations. The projections for the future scenario (2070–2099) suggested a general decrease in the occurrences of mixed precipitation over southern Quebec from October to April. This is mainly due to a decrease in long-duration events ( $$\ge 6\,\mathrm{{h}}$$ ). Overall, this study contributes to better understand how the distribution of freezing rain and ice pellets might change in the future using high-resolution regional climate model. |
Databáze: | OpenAIRE |
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