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International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Concurrent and antecedent soil moisture relate positively or negatively to probability of large wildfires depending on season

Erik S. Krueger A E , Tyson E. Ochsner A , J. D. Carlson B , David M. Engle C , Dirac Twidwell C D and Samuel D. Fuhlendorf C
+ Author Affiliations
- Author Affiliations

A Department of Plant and Soil Sciences, 371 Agricultural Hall, Oklahoma State University, Stillwater, OK 74078, USA.

B Department of Biosystems and Agricultural Engineering, 111 Agricultural Hall, Oklahoma State University, Stillwater, OK 74078, USA.

C Department of Natural Resource Ecology and Management, 011 Agricultural Hall, Oklahoma State University, Stillwater, OK 74078, USA.

D Department of Agronomy and Horticulture, 202 Keim Hall, University of Nebraska-Lincoln, Lincoln, NE 68588, USA.

E Corresponding author. Email: erik.krueger@okstate.edu

International Journal of Wildland Fire 25(6) 657-668 https://doi.org/10.1071/WF15104
Submitted: 28 May 2015  Accepted: 3 February 2016   Published: 27 April 2016

Abstract

Measured soil moisture data may improve wildfire probability assessments because soil moisture is physically linked to fuel production and live fuel moisture, yet models characterising soil moisture–wildfire relationships have not been developed. We therefore described the relationships between measured soil moisture (concurrent and antecedent), as fraction of available water capacity (FAW), and large (≥405 ha) wildfire occurrence during the growing (May–October) and dormant (November–April) seasons from 2000 to 2012 in Oklahoma, USA. Wildfires were predominantly grass and brush fires but occurred across multiple fuel types including forests. Below-average FAW coincided with high wildfire occurrence each season. Wildfire probability during the growing season was 0.18 when concurrent FAW was 0.5 (a threshold for plant water stress) but was 0.60 when concurrent FAW was 0.2 (extreme drought). Dormant season wildfire probability was influenced not only by concurrent but also by antecedent FAW. Dormant season wildfire probability was 0.29 and 0.09 when FAW during the previous growing season was 0.9 (near ideal for plant growth) and 0.2, respectively. Therefore, although a wet growing season coincided with reduced wildfire probability that season, it also coincided with increased wildfire probability the following dormant season, suggesting that the mechanisms by which soil moisture influences wildfire probability are seasonally dependent.


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