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...

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Main Authors: Poujol, Basile, Prein, Andreas F., id_orcid:0 000-0001-6250-179X, Molina, Maria J., Muller, Caroline
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2021
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
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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