14 citations as recorded by crossref.

1. Storm Boris (2024) in the current and future climate: a dynamics-centered contextualization, and some lessons learnt J. Riboldi et al. https://doi.org/10.5194/wcd-7-65-2026
2. 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
3. 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
4. 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
5. 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
6. Identifying controls of extratropical cyclone intensity at genesis time and during intensification in the North Atlantic and Europe J. Cornér et al. https://doi.org/10.5194/wcd-7-873-2026
7. 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
8. 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
9. 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
10. Long‐Term Trends of Northern Hemispheric Winter Cyclones in the Extended ERA5 Reanalysis A. Karwat et al. https://doi.org/10.1029/2022JD036952
11. 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
12. Characteristics of vertical structure and intensity of spring Mongolian cyclone J. Wang et al. https://doi.org/10.1007/s00382-025-08012-z
13. Toward Eliminating the Decades‐Old “Too Zonal and Too Equatorward” Storm‐Track Bias in Climate Models S. Schemm https://doi.org/10.1029/2022MS003482
14. 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