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Journal of the International Association of Wildland Fire
RESEARCH ARTICLE (Open Access)

Climate and weather drivers in southern California Santa Ana Wind and non-Santa Wind fires

Jon E. Keeley A B * , Michael Flannigan C , Tim J. Brown D , Tom Rolinski E , Daniel Cayan F , Alexandra D. Syphard G , Janin Guzman-Morales H and Alexander Gershunov F
+ Author Affiliations
- Author Affiliations

A U.S. Geological Survey, Western Ecological Research Center, Sequoia-Kings Canyon Field Station, Three Rivers, CA 93271, USA.

B Department of Ecology and Evolutionary Biology, University of California, Los Angeles, CA 90095, USA.

C Thompson Rivers University, Natural Resource Science, BC V2C 0C8, Canada.

D Western Regional Climate Center, Reno, NV 89512, USA.

E Southern California Edison, Los Angeles, CA, USA.

F Climate, Atmospheric Science and Physical Oceanography Division, Scripps Institution of Oceanography, University of California, San Diego, CA 92093, USA.

G Conservation Biology Institute, 136 SW Washington Avenue, Corvalis, OR 97333, USA.

H Department of Geography, University of California, Santa Barbara, CA 93106, USA.

* Correspondence to: jon_keeley@usgs.gov

International Journal of Wildland Fire 33, WF23190 https://doi.org/10.1071/WF23190
Submitted: 5 December 2023  Accepted: 10 July 2024  Published: 15 August 2024

© 2024 The Author(s) (or their employer(s)). Published by CSIRO Publishing on behalf of IAWF. This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License (CC BY-NC-ND)

Abstract

Background

Autumn and winter Santa Ana Winds (SAW) are responsible for the largest and most destructive wildfires in southern California.

Aims

(1) To contrast fires ignited on SAW days vs non-SAW days, (2) evaluate the predictive ability of the Canadian Fire Weather Index (CFWI) for these two fire types, and (3) determine climate and weather factors responsible for the largest wildfires.

Methods

CAL FIRE (California Department of Forestry and Fire Protection) FRAP (Fire and Resource Assessment Program) fire data were coupled with hourly climate data from four stations, and with regional indices of SAW wind speed, and with seasonal drought data from the Palmer Drought Severity Index.

Key results

Fires on non-SAW days were more numerous and burned more area, and were substantial from May to October. CFWI indices were tied to fire occurrence and size for both non-SAW and SAW days, and in the days following ignition. Multiple regression models for months with the greatest area burned explained up to a quarter of variation in area burned.

Conclusions

The drivers of fire size differ between non-SAW and SAW fires. The best predictor of fire size for non-SAW fires was drought during the prior 5 years, followed by a current year vapour pressure deficit. For SAW fires, wind speed followed by drought were most important.

Keywords: aiutumn fires, Canadian Fire Weather Index, drought, summer fires, vapour pressure deficit, VPD, wind speed.

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