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...
Published in: | Atmosphere |
---|---|
Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2019
|
Subjects: | |
Online Access: | https://doi.org/10.3390/atmos10080430 |
_version_ | 1821810930404556800 |
---|---|
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 |
genre_facet | Arctic Climate change |
geographic | Arctic |
geographic_facet | Arctic |
id | ftmdpi:oai:mdpi.com:/2073-4433/10/8/430/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/atmos10080430 |
op_relation | Meteorology https://dx.doi.org/10.3390/atmos10080430 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Atmosphere; Volume 10; Issue 8; Pages: 430 |
publishDate | 2019 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
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 |