Climate indices to characterize climatic changes across southern Canada

Abstract The present study analyses the impacts of past and future climate change on extreme weather events for southern parts of Canada from 1981 to 2100. A set of precipitation and temperature‐based indices were computed using the downscaled Coupled Model Intercomparison Project Phase 5 (CMIP5) mu...

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Published in:Meteorological Applications
Main Authors: Hussein Wazneh, M. Altaf Arain, Paulin Coulibaly
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2020
Subjects:
Online Access:https://doi.org/10.1002/met.1861
https://doaj.org/article/158c04164a60422bb7bd208e365429fa
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spelling ftdoajarticles:oai:doaj.org/article:158c04164a60422bb7bd208e365429fa 2023-05-15T16:35:30+02:00 Climate indices to characterize climatic changes across southern Canada Hussein Wazneh M. Altaf Arain Paulin Coulibaly 2020-01-01T00:00:00Z https://doi.org/10.1002/met.1861 https://doaj.org/article/158c04164a60422bb7bd208e365429fa EN eng Wiley https://doi.org/10.1002/met.1861 https://doaj.org/toc/1350-4827 https://doaj.org/toc/1469-8080 1469-8080 1350-4827 doi:10.1002/met.1861 https://doaj.org/article/158c04164a60422bb7bd208e365429fa Meteorological Applications, Vol 27, Iss 1, Pp n/a-n/a (2020) climate change climate indices CMIP5 extreme events future climate projection Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.1002/met.1861 2023-02-26T01:35:55Z Abstract The present study analyses the impacts of past and future climate change on extreme weather events for southern parts of Canada from 1981 to 2100. A set of precipitation and temperature‐based indices were computed using the downscaled Coupled Model Intercomparison Project Phase 5 (CMIP5) multi‐model ensemble projections at 8 km resolution over the 21st Century for two representative concentration pathway (RCP) scenarios: RCP4.5 and RCP8.5. The results show that this region is expected to experience stronger warming and a higher increase in precipitation extremes in future. Generally, projected changes in minimum temperature will be greater than changes in maximum temperature, as shown by respective indices. A decrease in frost days and an increase in warm nights will be expected. By 2100 there will be no cool nights and cool days. Daily minimum and maximum temperatures will increase by 12 and 7°C, respectively, under the RCP8.5 scenario, when compared with the reference period 1981–2000. The highest warming in minimum temperature and decrease in cool nights and days will occur in Ontario and Quebec provinces close to the Great Lakes and Hudson Bay. The highest warming in maximum temperature will occur in the southern parts of Alberta and Saskatchewan. Annual total precipitation is expected to increase by about 16% and the occurrence of heavy precipitation events by five days. The highest increase in annual total precipitation will occur in the northern parts of Ontario and Quebec and in western British Columbia. Article in Journal/Newspaper Hudson Bay Directory of Open Access Journals: DOAJ Articles British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canada Hudson Hudson Bay Meteorological Applications 27 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic climate change
climate indices
CMIP5
extreme events
future climate projection
Meteorology. Climatology
QC851-999
spellingShingle climate change
climate indices
CMIP5
extreme events
future climate projection
Meteorology. Climatology
QC851-999
Hussein Wazneh
M. Altaf Arain
Paulin Coulibaly
Climate indices to characterize climatic changes across southern Canada
topic_facet climate change
climate indices
CMIP5
extreme events
future climate projection
Meteorology. Climatology
QC851-999
description Abstract The present study analyses the impacts of past and future climate change on extreme weather events for southern parts of Canada from 1981 to 2100. A set of precipitation and temperature‐based indices were computed using the downscaled Coupled Model Intercomparison Project Phase 5 (CMIP5) multi‐model ensemble projections at 8 km resolution over the 21st Century for two representative concentration pathway (RCP) scenarios: RCP4.5 and RCP8.5. The results show that this region is expected to experience stronger warming and a higher increase in precipitation extremes in future. Generally, projected changes in minimum temperature will be greater than changes in maximum temperature, as shown by respective indices. A decrease in frost days and an increase in warm nights will be expected. By 2100 there will be no cool nights and cool days. Daily minimum and maximum temperatures will increase by 12 and 7°C, respectively, under the RCP8.5 scenario, when compared with the reference period 1981–2000. The highest warming in minimum temperature and decrease in cool nights and days will occur in Ontario and Quebec provinces close to the Great Lakes and Hudson Bay. The highest warming in maximum temperature will occur in the southern parts of Alberta and Saskatchewan. Annual total precipitation is expected to increase by about 16% and the occurrence of heavy precipitation events by five days. The highest increase in annual total precipitation will occur in the northern parts of Ontario and Quebec and in western British Columbia.
format Article in Journal/Newspaper
author Hussein Wazneh
M. Altaf Arain
Paulin Coulibaly
author_facet Hussein Wazneh
M. Altaf Arain
Paulin Coulibaly
author_sort Hussein Wazneh
title Climate indices to characterize climatic changes across southern Canada
title_short Climate indices to characterize climatic changes across southern Canada
title_full Climate indices to characterize climatic changes across southern Canada
title_fullStr Climate indices to characterize climatic changes across southern Canada
title_full_unstemmed Climate indices to characterize climatic changes across southern Canada
title_sort climate indices to characterize climatic changes across southern canada
publisher Wiley
publishDate 2020
url https://doi.org/10.1002/met.1861
https://doaj.org/article/158c04164a60422bb7bd208e365429fa
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
geographic British Columbia
Canada
Hudson
Hudson Bay
geographic_facet British Columbia
Canada
Hudson
Hudson Bay
genre Hudson Bay
genre_facet Hudson Bay
op_source Meteorological Applications, Vol 27, Iss 1, Pp n/a-n/a (2020)
op_relation https://doi.org/10.1002/met.1861
https://doaj.org/toc/1350-4827
https://doaj.org/toc/1469-8080
1469-8080
1350-4827
doi:10.1002/met.1861
https://doaj.org/article/158c04164a60422bb7bd208e365429fa
op_doi https://doi.org/10.1002/met.1861
container_title Meteorological Applications
container_volume 27
container_issue 1
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