Simulating Canadian Arctic Climate at Convection-Permitting Resolution

Inadequate representation and parameterization of sub-grid scale features and processes are one of the main sources for uncertainties in regional climate change projections, particularly for the Arctic regions where the climate change signal is amplified. Increasing model resolution to a couple of k...

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Published in:Atmosphere
Main Authors: Gulilat Tefera Diro, Laxmi Sushama
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/atmos10080430
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author Gulilat Tefera Diro
Laxmi Sushama
author_facet Gulilat Tefera Diro
Laxmi Sushama
author_sort Gulilat Tefera Diro
collection MDPI Open Access Publishing
container_issue 8
container_start_page 430
container_title Atmosphere
container_volume 10
description Inadequate representation and parameterization of sub-grid scale features and processes are one of the main sources for uncertainties in regional climate change projections, particularly for the Arctic regions where the climate change signal is amplified. Increasing model resolution to a couple of kilometers will be helpful in resolving some of these challenges, for example to better simulate convection and refined land heterogeneity and thus land–atmosphere interactions. A set of multi-year simulations has been carried out for the Canadian Arctic domain at 12 km and 3 km resolutions using limited-area version of the global environmental multi-scale (GEM) model. The model is integrated for five years driven by the fifth generation of the European Centre for medium-range weather forecast reanalysis (ERA-5) at the lateral boundaries. The aim of this study is to investigate the role of horizontal model resolution on the simulated surface climate variables. Results indicate that although some aspects of the seasonal mean values are deteriorated at times, substantial improvements are noted in the higher resolution simulation. The representation of extreme precipitation events during summer and the simulation of winter temperature are better captured in the convection-permitting simulation. Moreover, the observed temperature–extreme precipitation scaling is realistically reproduced by the higher resolution simulation. These results advocate for the use of convective-permitting resolution models for simulating future climate projections over the Arctic to support climate impact assessment studies such as those related to engineering applications and where high spatial and temporal resolution are beneficial.
format Text
genre Arctic
Climate change
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Climate change
geographic Arctic
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op_source Atmosphere; Volume 10; Issue 8; Pages: 430
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spelling ftmdpi:oai:mdpi.com:/2073-4433/10/8/430/ 2025-01-16T20:16:40+00:00 Simulating Canadian Arctic Climate at Convection-Permitting Resolution Gulilat Tefera Diro Laxmi Sushama agris 2019-07-26 application/pdf https://doi.org/10.3390/atmos10080430 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos10080430 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 10; Issue 8; Pages: 430 Arctic convection permitting regional climate model temperature–extreme precipitation scaling climate Text 2019 ftmdpi https://doi.org/10.3390/atmos10080430 2023-07-31T22:28:05Z Inadequate representation and parameterization of sub-grid scale features and processes are one of the main sources for uncertainties in regional climate change projections, particularly for the Arctic regions where the climate change signal is amplified. Increasing model resolution to a couple of kilometers will be helpful in resolving some of these challenges, for example to better simulate convection and refined land heterogeneity and thus land–atmosphere interactions. A set of multi-year simulations has been carried out for the Canadian Arctic domain at 12 km and 3 km resolutions using limited-area version of the global environmental multi-scale (GEM) model. The model is integrated for five years driven by the fifth generation of the European Centre for medium-range weather forecast reanalysis (ERA-5) at the lateral boundaries. The aim of this study is to investigate the role of horizontal model resolution on the simulated surface climate variables. Results indicate that although some aspects of the seasonal mean values are deteriorated at times, substantial improvements are noted in the higher resolution simulation. The representation of extreme precipitation events during summer and the simulation of winter temperature are better captured in the convection-permitting simulation. Moreover, the observed temperature–extreme precipitation scaling is realistically reproduced by the higher resolution simulation. These results advocate for the use of convective-permitting resolution models for simulating future climate projections over the Arctic to support climate impact assessment studies such as those related to engineering applications and where high spatial and temporal resolution are beneficial. Text Arctic Climate change MDPI Open Access Publishing Arctic Atmosphere 10 8 430
spellingShingle Arctic
convection permitting
regional climate model
temperature–extreme precipitation scaling
climate
Gulilat Tefera Diro
Laxmi Sushama
Simulating Canadian Arctic Climate at Convection-Permitting Resolution
title Simulating Canadian Arctic Climate at Convection-Permitting Resolution
title_full Simulating Canadian Arctic Climate at Convection-Permitting Resolution
title_fullStr Simulating Canadian Arctic Climate at Convection-Permitting Resolution
title_full_unstemmed Simulating Canadian Arctic Climate at Convection-Permitting Resolution
title_short Simulating Canadian Arctic Climate at Convection-Permitting Resolution
title_sort simulating canadian arctic climate at convection-permitting resolution
topic Arctic
convection permitting
regional climate model
temperature–extreme precipitation scaling
climate
topic_facet Arctic
convection permitting
regional climate model
temperature–extreme precipitation scaling
climate
url https://doi.org/10.3390/atmos10080430