Romijn et al. (2026) Shifting Northern Hemisphere snowfall extremes and their physical drivers
Identification
- Journal: Weather and Climate Extremes
- Year: 2026
- Date: 2026-07-31
- Authors: Nick Romijn, Richard Bintanja, Eveline C. van der Linden, Marlen Kolbe
- DOI: 10.1016/j.wace.2026.100939
Research Groups
- Royal Netherlands Meteorological Institute (KNMI)
- Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology
- University of Groningen (RUG)
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia
Short Summary
This study examines the changes in extreme snowfall across the Northern Hemisphere under a 2K warming scenario using the Large ENsemble TIme Slice (LENTIS) model. The results show that while light snowfall is projected to decline significantly, particularly in maritime and mid-latitude regions near the melting point, increases are expected in high-latitude maritime, select high-altitude and continental areas.
Objective
- Investigate the changes in extreme snowfall frequency and amount across the Northern Hemisphere under a 2K warming scenario.
- Examine the physical drivers of these changes, including thermodynamic and dynamic processes.
Study Configuration
- Spatial Scale: Global, with a focus on the Northern Hemisphere.
- Temporal Scale: Present-day (2000-2009) and future projection (2075-2084).
Methodology and Data
- Models used: Large ENsemble TIme Slice (LENTIS) model.
- Data sources: LENTIS dataset, ERA-5 reanalysis dataset, MERRA-2 reanalysis dataset, JRA-3Q reanalysis dataset.
Main Results
- Light snowfall is projected to decline significantly in maritime and mid-latitude regions near the melting point.
- Extreme snowfall is expected to increase in high-latitude maritime, select high-altitude and continental areas.
- The sign and magnitude of change depend on the region's present-day seasonal mean climatological temperature.
Contributions
- This study provides new insights into the changes in extreme snowfall across the Northern Hemisphere under a 2K warming scenario.
- The results highlight the importance of considering both thermodynamic and dynamic processes in understanding these changes.
Funding
- This research was funded by the Royal Netherlands Meteorological Institute (KNMI) and the University of Groningen (RUG).
Citation
@article{Romijn2026Shifting,
author = {Romijn, Nick and Bintanja, Richard and Linden, Eveline C. van der and Kolbe, Marlen},
title = {Shifting Northern Hemisphere snowfall extremes and their physical drivers},
journal = {Weather and Climate Extremes},
year = {2026},
doi = {10.1016/j.wace.2026.100939},
url = {https://doi.org/10.1016/j.wace.2026.100939}
}
Original Source: https://doi.org/10.1016/j.wace.2026.100939