@article{Stewart-2019-A,
title = "A Review and Synthesis of Future Earth System Change in theInterior of Western Canada: Part I {--} Climate and Meteorology",
author = "Stewart, Ronald E. and
Szeto, Kit K. and
Bonsal, Barrie and
Hanesiak, John and
Kochtubajda, Bohdan and
Li, Yanping and
Th{\'e}riault, Julie M. and
DeBeer, C. M. and
Tam, Benita Y. and
Li, Zhenhua and
Liu, Zhuo and
Bruneau, Jennifer and
Marinier, S{\'e}bastien and
Matte, Dominic",
journal = "",
year = "2019",
publisher = "Copernicus GmbH",
url = "https://gwf-uwaterloo.github.io/gwf-publications/G19-9010",
doi = "10.5194/hess-2019-51",
abstract = "Abstract. The Interior of Western Canada, up to and including the Arctic, has experienced rapid change in its climate, hydrology, cryosphere and ecosystems and this is expected to continue. Although there is general consensus that warming will occur in the future, many critical issues remain. In this first of two articles, attention is placed on atmospheric-related issues that range from large scales down to individual precipitation events. Each of these is considered in terms of expected change organized by season and utilizing climate scenario information as well as thermodynamically-driven future climatic forcing simulations. Large scale atmospheric circulations affecting this region are generally projected to become stronger in each season and, coupled with warming temperatures, lead to enhancements of numerous water-related and temperature-related extremes. These include winter snowstorms, freezing rain, drought as well as atmospheric forcing of spring floods although not necessarily summer convection. Collective insights of these atmospheric findings are summarized in a consistent, connected physical framework.",
}
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<abstract>Abstract. The Interior of Western Canada, up to and including the Arctic, has experienced rapid change in its climate, hydrology, cryosphere and ecosystems and this is expected to continue. Although there is general consensus that warming will occur in the future, many critical issues remain. In this first of two articles, attention is placed on atmospheric-related issues that range from large scales down to individual precipitation events. Each of these is considered in terms of expected change organized by season and utilizing climate scenario information as well as thermodynamically-driven future climatic forcing simulations. Large scale atmospheric circulations affecting this region are generally projected to become stronger in each season and, coupled with warming temperatures, lead to enhancements of numerous water-related and temperature-related extremes. These include winter snowstorms, freezing rain, drought as well as atmospheric forcing of spring floods although not necessarily summer convection. Collective insights of these atmospheric findings are summarized in a consistent, connected physical framework.</abstract>
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%0 Journal Article
%T A Review and Synthesis of Future Earth System Change in theInterior of Western Canada: Part I – Climate and Meteorology
%A Stewart, Ronald E.
%A Szeto, Kit K.
%A Bonsal, Barrie
%A Hanesiak, John
%A Kochtubajda, Bohdan
%A Li, Yanping
%A Thériault, Julie M.
%A DeBeer, C. M.
%A Tam, Benita Y.
%A Li, Zhenhua
%A Liu, Zhuo
%A Bruneau, Jennifer
%A Marinier, Sébastien
%A Matte, Dominic
%D 2019
%I Copernicus GmbH
%F Stewart-2019-A
%X Abstract. The Interior of Western Canada, up to and including the Arctic, has experienced rapid change in its climate, hydrology, cryosphere and ecosystems and this is expected to continue. Although there is general consensus that warming will occur in the future, many critical issues remain. In this first of two articles, attention is placed on atmospheric-related issues that range from large scales down to individual precipitation events. Each of these is considered in terms of expected change organized by season and utilizing climate scenario information as well as thermodynamically-driven future climatic forcing simulations. Large scale atmospheric circulations affecting this region are generally projected to become stronger in each season and, coupled with warming temperatures, lead to enhancements of numerous water-related and temperature-related extremes. These include winter snowstorms, freezing rain, drought as well as atmospheric forcing of spring floods although not necessarily summer convection. Collective insights of these atmospheric findings are summarized in a consistent, connected physical framework.
%R 10.5194/hess-2019-51
%U https://gwf-uwaterloo.github.io/gwf-publications/G19-9010
%U https://doi.org/10.5194/hess-2019-51
Markdown (Informal)
[A Review and Synthesis of Future Earth System Change in theInterior of Western Canada: Part I – Climate and Meteorology](https://gwf-uwaterloo.github.io/gwf-publications/G19-9010) (Stewart et al., GWF 2019)
ACL
- Ronald E. Stewart, Kit K. Szeto, Barrie Bonsal, John Hanesiak, Bohdan Kochtubajda, Yanping Li, Julie M. Thériault, C. M. DeBeer, Benita Y. Tam, Zhenhua Li, Zhuo Liu, Jennifer Bruneau, Sébastien Marinier, and Dominic Matte. 2019. A Review and Synthesis of Future Earth System Change in theInterior of Western Canada: Part I – Climate and Meteorology.
