Format

Send to

Choose Destination
Proc Natl Acad Sci U S A. 2018 Sep 4;115(36):E8349-E8357. doi: 10.1073/pnas.1802316115. Epub 2018 Aug 20.

Decreasing fire season precipitation increased recent western US forest wildfire activity.

Author information

1
US Forest Service Region 1, Missoula, MT 59807; zaholden@fs.fed.us.
2
School of Public and Community Health Sciences, University of Montana, Missoula, MT 59812.
3
US Forest Service Aquatic Science Laboratory, Rocky Mountain Research Station, Boise, ID 83702.
4
US Forest Service, Fire Sciences Laboratory, Rocky Mountain Research Station, Missoula, MT 59808.
5
Department of Geosciences, University of Montana, Missoula, MT 59812.
6
Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802.
7
Department of Forestry and Conservation, University of Montana, Missoula, MT 59812.

Abstract

Western United States wildfire increases have been generally attributed to warming temperatures, either through effects on winter snowpack or summer evaporation. However, near-surface air temperature and evaporative demand are strongly influenced by moisture availability and these interactions and their role in regulating fire activity have never been fully explored. Here we show that previously unnoted declines in summer precipitation from 1979 to 2016 across 31-45% of the forested areas in the western United States are strongly associated with burned area variations. The number of wetting rain days (WRD; days with precipitation ≥2.54 mm) during the fire season partially regulated the temperature and subsequent vapor pressure deficit (VPD) previously implicated as a primary driver of annual wildfire area burned. We use path analysis to decompose the relative influence of declining snowpack, rising temperatures, and declining precipitation on observed fire activity increases. After accounting for interactions, the net effect of WRD anomalies on wildfire area burned was more than 2.5 times greater than the net effect of VPD, and both the WRD and VPD effects were substantially greater than the influence of winter snowpack. These results suggest that precipitation during the fire season exerts the strongest control on burned area either directly through its wetting effects or indirectly through feedbacks to VPD. If these trends persist, decreases in summer precipitation and the associated summertime aridity increases would lead to more burned area across the western United States with far-reaching ecological and socioeconomic impacts.

KEYWORDS:

climate change; hydrology; wildfire

PMID:
30126983
PMCID:
PMC6130364
[Available on 2019-03-04]
DOI:
10.1073/pnas.1802316115

Supplemental Content

Full text links

Icon for HighWire
Loading ...
Support Center