Articles | Volume 2, issue 4
https://doi.org/10.5194/wcd-2-991-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-2-991-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
27 Oct 2021
Research article |
| 27 Oct 2021
| 27 Oct 2021
A global analysis of the dry-dynamic forcing during cyclone growth and propagation
Philippe Besson
CORRESPONDING AUTHOR
Institute for Atmospheric and Climate Science, ETH Zürich, Zurich, Switzerland
Luise J. Fischer
Institute for Atmospheric and Climate Science, ETH Zürich, Zurich, Switzerland
Institute for Environmental Decisions, ETH Zürich, Zurich, Switzerland
Sebastian Schemm
Institute for Atmospheric and Climate Science, ETH Zürich, Zurich, Switzerland
Michael Sprenger
CORRESPONDING AUTHOR
Institute for Atmospheric and Climate Science, ETH Zürich, Zurich, Switzerland
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15 citations as recorded by crossref.
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- Case study of a long-lived Siberian summer cyclone that evolved from a heat low into an Arctic cyclone F. Schnyder et al. https://doi.org/10.5194/wcd-6-1319-2025
- The role of cyclones and potential vorticity cutoffs for the occurrence of unusually long wet spells in Europe M. Röthlisberger et al. https://doi.org/10.5194/wcd-3-733-2022
- Classification of North Atlantic and European extratropical cyclones using multiple measures of intensity J. Cornér et al. https://doi.org/10.5194/nhess-25-207-2025
- A comparison of the meridional meandering of extratropical precipitation during boreal winter: eddy momentum flux versus Eulerian storm tracks C. Yoo et al. https://doi.org/10.1038/s41612-025-00992-3
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- Warm conveyor belt characteristics and impacts along the life cycle of extratropical cyclones: case studies and climatological analysis based on ERA5 K. Heitmann et al. https://doi.org/10.5194/wcd-5-537-2024
- Stratospheric influence on the winter North Atlantic storm track in subseasonal reforecasts H. Afargan-Gerstman et al. https://doi.org/10.5194/wcd-5-231-2024
- Synoptic perspective on the conversion and maintenance of local available potential energy in extratropical cyclones M. Federer et al. https://doi.org/10.5194/wcd-6-211-2025
- Long‐Term Trends of Northern Hemispheric Winter Cyclones in the Extended ERA5 Reanalysis A. Karwat et al. https://doi.org/10.1029/2022JD036952
- Breaking Rossby waves drive extreme precipitation in the world’s arid regions A. de Vries et al. https://doi.org/10.1038/s43247-024-01633-y
- Characteristics of vertical structure and intensity of spring Mongolian cyclone J. Wang et al. https://doi.org/10.1007/s00382-025-08012-z
- Toward Eliminating the Decades‐Old “Too Zonal and Too Equatorward” Storm‐Track Bias in Climate Models S. Schemm https://doi.org/10.1029/2022MS003482
- Storm track response to uniform global warming downstream of an idealized sea surface temperature front S. Schemm et al. https://doi.org/10.5194/wcd-3-601-2022
Saved (final revised paper)
Latest update: 01 Nov 2026
Short summary
The strongest cyclone intensification is associated with a strong dry-dynamical forcing. Moreover, strong forcing and strong intensification correspond to a tendency for poleward cyclone propagation, which occurs in distinct regions in the Northern Hemisphere. There is a clear spatial pattern in the occurrence of certain forcing combinations. This implies a fundamental relationship between dry-dynamical processes and the intensification as well as the propagation of extratropical cyclones.
The strongest cyclone intensification is associated with a strong dry-dynamical forcing....
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