Articles | Volume 25, issue 3
https://doi.org/10.5194/nhess-25-1037-2025
https://doi.org/10.5194/nhess-25-1037-2025
Research article
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10 Mar 2025
Research article | Highlight paper |  | 10 Mar 2025

Characterizing the scale of regional landslide triggering from storm hydrometeorology

Jonathan Perkins, Nina S. Oakley, Brian D. Collins, Skye C. Corbett, and W. Paul Burgess

Data sets

Landslides triggered by th February 2019 atmospheric river storm in the vicinity of Bee Canyon, Riverside County, CA, USA Skye C. Corbett and Jonathan P. Perkins https://doi.org/10.5066/P92XCRSZ

Landslides triggered by the January 11th, 2005 storm in the vicinity of La Conchita, Ventura County, CA, USA Skye C. Corbett and Jonathan P. Perkins https://doi.org/10.5066/P9K6E6MW

QPE (6-Hour Observed Precipitation) California Nevada River Forecast Center https://www.cnrfc.noaa.gov/arc_search.php?product=netcdfqpe

IEM Cow (NSW storm based warning verification) Iowa Environmental Mesonet https://mesonet.agron.iastate.edu/cow/

Shuttle Radar Topography Mission (SRTM) Global NASA https://doi.org/10.5069/G9445JDF

30-Year Normals PRISM https://prism.oregonstate.edu/

Precipitation-Frequency Atlas of the United States, Version 2.3, California Sanja Perica et al. https://repository.library.noaa.gov/view/noaa/22614

Model code and software

PyGMT: A Python interface for the Generic Mapping Tools Dongdong Tian et al. https://doi.org/10.5281/zenodo.14868324

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Executive editor
This paper presents a method for characterizing regional landslide potential, which the authors suggest as an improved basis for landslide hazard forecasting during storms. It discusses the advantage of using considering the relative soil-saturation rather than a rainfall recurrence interval to understand landsliding triggered by rainfall, focusing on data from California.
Short summary
Rainfall-induced landslides result in deaths and economic losses annually across the globe. However, it is unclear how storm severity relates to landslide severity across large regions. Here we develop a method to dynamically map landslide-affected areas, and we compare this to meteorological estimates of storm severity. We find that preconditioning by earlier storms and the location of rainfall bursts, rather than atmospheric storm strength, dictate landslide magnitude and pattern. 
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