Abstract

Characterizing wildfire regimes where wildfires are uncommon is challenged by a lack of empirical information. Moreover, climate change is projected to lead to increasingly frequent wildfires and additional annual area burned in forests historically characterized by long fire return intervals. Western Oregon and Washington, USA (westside) have experienced few large wildfires (fires greater than 100 hectares) the past century and are characterized to infrequent large fires with return intervals greater than 500 years. We evaluated impacts of climate change on wildfire hazard in a major urban watershed outside Portland, OR, USA. We simulated wildfire occurrence and fire regime characteristics under contemporary conditions (1992–2015) and four mid-century (2040–2069) scenarios using Representative Concentration Pathway (RCP) 8.5. Simulated mid-century fire seasons expanded in most scenarios, in some cases by nearly two months. In all scenarios, average fire size and frequency projections increased significantly. Fire regime characteristics under the hottest and driest mid-century scenarios illustrate novel disturbance regimes which could result in permanent changes to forest structure and composition and the provision of ecosystem services. Managers and planners can use the range of modeled outputs and simulation results to inform robust strategies for climate adaptation and risk mitigation.

Highlights

  • Moist forests historically characterized by infrequent wildfire are projected to experience significant increases in wildfire frequency before the end of the century as a result of climate change and anthropogenic activities [1,2,3]

  • Three of four future scenarios project that the fire season as measured by ERC will expand by mid-century (Figure 4)

  • Annualized metrics are useful for illustrating the effect of climate change on fire characteristics, but results demonstrate that fire occurrence will continue to vary intra- and inter-annually

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Summary

Introduction

Moist forests historically characterized by infrequent wildfire are projected to experience significant increases in wildfire frequency before the end of the century as a result of climate change and anthropogenic activities [1,2,3]. Many of these forests are not adapted to rapid shifts in disturbance regimes and future wildfire could lead to irreversible changes in vegetation structure and composition [4,5,6,7]. Ignitions coinciding with extremely dry fuel can lead to very large fires (>5000 ha) as a result of abundant, relatively continuous fuel [2,23].Several events in mesic forests in westside forests in Oregon and Washington rank among the largest wildfire events in US history including the 1845 Great Fire (~600,000 ha) and the 1933 Tillamook Burn (~100,000 ha) both in the Oregon Coast Range and the 1865 Silverton Fire (~40,000 ha) and 1902 Yacolt Burn (~400,000 ha), both in the western Cascade Range of Oregon and Washington, respectively [24,25,26,27]

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