Dynamic and thermodynamic impacts of climate change on organized convection in Alaska
Convective storms can cause economic damage and harm to humans by producing flash floods, lightning and severe weather. While organized convection is well studied in the tropics and mid-latitudes, few studies have focused on the physics and climate change impacts of pan-Arctic convective systems. Us...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer
2021
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/695898 https://doi.org/10.3929/ethz-b-000695898 |
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author | Poujol, Basile Prein, Andreas F. id_orcid:0 000-0001-6250-179X Molina, Maria J. Muller, Caroline |
author_facet | Poujol, Basile Prein, Andreas F. id_orcid:0 000-0001-6250-179X Molina, Maria J. Muller, Caroline |
author_sort | Poujol, Basile |
collection | ETH Zürich Research Collection |
description | Convective storms can cause economic damage and harm to humans by producing flash floods, lightning and severe weather. While organized convection is well studied in the tropics and mid-latitudes, few studies have focused on the physics and climate change impacts of pan-Arctic convective systems. Using a convection-permitting model we showed in a predecessor study that organized convective storm frequency might triple by the end of the century in Alaska assuming a high emission scenario. The present study assesses the reasons for this rapid increase in organized convection by investigating dynamic and thermodynamic changes within future storms and their environments, in light of canonical existing theories for mid-latitude and tropical deep convection. In a future climate, more moisture originates from Arctic marine basins increasing relative humidity over Alaska due to the loss of sea ice, which is in sharp contrast to lower-latitude land regions that are expected to become drier. This increase in relative humidity favors the onset of organized convection through more unstable thermodynamic environments, increased low-level buoyancy, and weaker downdrafts. Our confidence in these results is increased by showing that these changes can be analytically derived from basic physical laws. This suggests that organized thunderstorms might become more frequent in other pan-Arctic continental regions highlighting the uniqueness and vulnerability of these regions to climate change. ISSN:0930-7575 ISSN:1432-0894 |
format | Article in Journal/Newspaper |
genre | Arctic Climate change Sea ice Alaska |
genre_facet | Arctic Climate change Sea ice Alaska |
geographic | Arctic |
geographic_facet | Arctic |
id | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/695898 |
institution | Open Polar |
language | English |
op_collection_id | ftethz |
op_doi | https://doi.org/20.500.11850/69589810.3929/ethz-b-00069589810.1007/s00382-020-05606-7 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-020-05606-7 http://hdl.handle.net/20.500.11850/695898 |
op_rights | info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International |
op_source | Climate Dynamics, 56 (7) |
publishDate | 2021 |
publisher | Springer |
record_format | openpolar |
spelling | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/695898 2025-03-30T15:03:16+00:00 Dynamic and thermodynamic impacts of climate change on organized convection in Alaska Poujol, Basile Prein, Andreas F. id_orcid:0 000-0001-6250-179X Molina, Maria J. Muller, Caroline 2021-04 application/application/pdf https://hdl.handle.net/20.500.11850/695898 https://doi.org/10.3929/ethz-b-000695898 en eng Springer info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-020-05606-7 http://hdl.handle.net/20.500.11850/695898 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Climate Dynamics, 56 (7) Convective systems Moisture CAPE CIN Sea ice loss Convection-permitting modeling info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftethz https://doi.org/20.500.11850/69589810.3929/ethz-b-00069589810.1007/s00382-020-05606-7 2025-03-05T22:09:16Z Convective storms can cause economic damage and harm to humans by producing flash floods, lightning and severe weather. While organized convection is well studied in the tropics and mid-latitudes, few studies have focused on the physics and climate change impacts of pan-Arctic convective systems. Using a convection-permitting model we showed in a predecessor study that organized convective storm frequency might triple by the end of the century in Alaska assuming a high emission scenario. The present study assesses the reasons for this rapid increase in organized convection by investigating dynamic and thermodynamic changes within future storms and their environments, in light of canonical existing theories for mid-latitude and tropical deep convection. In a future climate, more moisture originates from Arctic marine basins increasing relative humidity over Alaska due to the loss of sea ice, which is in sharp contrast to lower-latitude land regions that are expected to become drier. This increase in relative humidity favors the onset of organized convection through more unstable thermodynamic environments, increased low-level buoyancy, and weaker downdrafts. Our confidence in these results is increased by showing that these changes can be analytically derived from basic physical laws. This suggests that organized thunderstorms might become more frequent in other pan-Arctic continental regions highlighting the uniqueness and vulnerability of these regions to climate change. ISSN:0930-7575 ISSN:1432-0894 Article in Journal/Newspaper Arctic Climate change Sea ice Alaska ETH Zürich Research Collection Arctic |
spellingShingle | Convective systems Moisture CAPE CIN Sea ice loss Convection-permitting modeling Poujol, Basile Prein, Andreas F. id_orcid:0 000-0001-6250-179X Molina, Maria J. Muller, Caroline Dynamic and thermodynamic impacts of climate change on organized convection in Alaska |
title | Dynamic and thermodynamic impacts of climate change on organized convection in Alaska |
title_full | Dynamic and thermodynamic impacts of climate change on organized convection in Alaska |
title_fullStr | Dynamic and thermodynamic impacts of climate change on organized convection in Alaska |
title_full_unstemmed | Dynamic and thermodynamic impacts of climate change on organized convection in Alaska |
title_short | Dynamic and thermodynamic impacts of climate change on organized convection in Alaska |
title_sort | dynamic and thermodynamic impacts of climate change on organized convection in alaska |
topic | Convective systems Moisture CAPE CIN Sea ice loss Convection-permitting modeling |
topic_facet | Convective systems Moisture CAPE CIN Sea ice loss Convection-permitting modeling |
url | https://hdl.handle.net/20.500.11850/695898 https://doi.org/10.3929/ethz-b-000695898 |