Human influence on the recent weakening of storm tracks in boreal summer

Abstract Anthropogenic warming can alter large-scale circulation patterns in the atmosphere, which could have serious consequences for regional climate impacts and extreme weather. Observed thermodynamic changes in boreal extratropics have been attributed to human emissions with high confidence, but...

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Main Authors: Rei Chemke, Dim Coumou
Format: Article
Language:English
Published: Nature Portfolio 2024-04-01
Series:npj Climate and Atmospheric Science
Online Access:https://doi.org/10.1038/s41612-024-00640-2
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author Rei Chemke
Dim Coumou
author_facet Rei Chemke
Dim Coumou
author_sort Rei Chemke
collection DOAJ
description Abstract Anthropogenic warming can alter large-scale circulation patterns in the atmosphere, which could have serious consequences for regional climate impacts and extreme weather. Observed thermodynamic changes in boreal extratropics have been attributed to human emissions with high confidence, but most circulation changes have not. In particular, not only that in the previous suite of climate models most models do not capture the recent boreal summer storm tracks weakening, but also a quantification of the role of human emissions in the recent storm tracks weakening has not been conducted to date. Here we use the latest suite of climate models, which are found to adequately capture the recent storm tracks weakening, and show that this weakening is attributable to anthropogenic emissions. Human emissions have resulted in more-rapid warming of the high latitudes, and the associated reduction in poleward temperature gradient has weakened the storms. The physical consistency between models and reanalyses increases our confidence in the projected weakening, which presents regional risks including hot-dry extremes in summer.
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spelling doaj.art-590b7a3f85f349d59a6787f5d72babb02024-04-14T11:11:34ZengNature Portfolionpj Climate and Atmospheric Science2397-37222024-04-01711810.1038/s41612-024-00640-2Human influence on the recent weakening of storm tracks in boreal summerRei Chemke0Dim Coumou1Department of Earth and Planetary Sciences, Weizmann Institute of ScienceInstitute for Environmental Studies, VU AmsterdamAbstract Anthropogenic warming can alter large-scale circulation patterns in the atmosphere, which could have serious consequences for regional climate impacts and extreme weather. Observed thermodynamic changes in boreal extratropics have been attributed to human emissions with high confidence, but most circulation changes have not. In particular, not only that in the previous suite of climate models most models do not capture the recent boreal summer storm tracks weakening, but also a quantification of the role of human emissions in the recent storm tracks weakening has not been conducted to date. Here we use the latest suite of climate models, which are found to adequately capture the recent storm tracks weakening, and show that this weakening is attributable to anthropogenic emissions. Human emissions have resulted in more-rapid warming of the high latitudes, and the associated reduction in poleward temperature gradient has weakened the storms. The physical consistency between models and reanalyses increases our confidence in the projected weakening, which presents regional risks including hot-dry extremes in summer.https://doi.org/10.1038/s41612-024-00640-2
spellingShingle Rei Chemke
Dim Coumou
Human influence on the recent weakening of storm tracks in boreal summer
npj Climate and Atmospheric Science
title Human influence on the recent weakening of storm tracks in boreal summer
title_full Human influence on the recent weakening of storm tracks in boreal summer
title_fullStr Human influence on the recent weakening of storm tracks in boreal summer
title_full_unstemmed Human influence on the recent weakening of storm tracks in boreal summer
title_short Human influence on the recent weakening of storm tracks in boreal summer
title_sort human influence on the recent weakening of storm tracks in boreal summer
url https://doi.org/10.1038/s41612-024-00640-2
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