| Literature DB >> 34339086 |
Paul F Hessburg1,2, Susan J Prichard2, R Keala Hagmann2,3, Nicholas A Povak1,4, Frank K Lake5.
Abstract
Forest landscapes across western North America (wNA) have experienced extensive changes over the last two centuries, while climatic warming has become a global reality over the last four decades. Resulting interactions between historical increases in forested area and density and recent rapid warming, increasing insect mortality, and wildfire burned areas, are now leading to substantial abrupt landscape alterations. These outcomes are forcing forest planners and managers to identify strategies that can modify future outcomes that are ecologically and/or socially undesirable. Past forest management, including widespread harvest of fire- and climate-tolerant large old trees and old forests, fire exclusion (both Indigenous and lightning ignitions), and highly effective wildfire suppression have contributed to the current state of wNA forests. These practices were successful at meeting short-term demands, but they match poorly to modern realities. Hagmann et al. review a century of observations and multi-scale, multi-proxy, research evidence that details widespread changes in forested landscapes and wildfire regimes since the influx of European colonists. Over the preceding 10 millennia, large areas of wNA were already settled and proactively managed with intentional burning by Indigenous tribes. Prichard et al. then review the research on management practices historically applied by Indigenous tribes and currently applied by some managers to intentionally manage forests for resilient conditions. They address 10 questions surrounding the application and relevance of these management practices. Here, we highlight the main findings of both papers and offer recommendations for management. We discuss progress paralysis that often occurs with strict adherence to the precautionary principle; offer insights for dealing with the common problem of irreducible uncertainty and suggestions for reframing management and policy direction; and identify key knowledge gaps and research needs.Entities:
Keywords: Climate Change and Western Wildfires; Indigenous fire use; climate warming; forest landscape changes; landscape realignment; landscape resilience; landscape resistance; social-ecological systems; wildfire regime changes
Mesh:
Year: 2021 PMID: 34339086 PMCID: PMC9285088 DOI: 10.1002/eap.2432
Source DB: PubMed Journal: Ecol Appl ISSN: 1051-0761 Impact factor: 6.105
Components of an active fire regime.
| Component | Definition |
|---|---|
| Amount | total amount of area burned annually or decadally |
| Distribution (severity) | distribution of severity class patch sizes |
| Distribution (event areas) | distribution of fire event patch sizes |
| Frequency | average fire return interval, and variation around the mean |
| Spatial distribution | the geographic distribution of fires |
| Intensity | the energy release from surface and crown fires at the flaming front |
| Duration | the length of time fires burn |
| Seasonality | the time of the year when fires burn |
Components may vary by climatic period.
The spatial distribution of fires is dictated by biophysical setting, climate, and weather conditions, forest or nonforest type, ignition probability, and the propensity for reburning.
The period of fires is dependent on the climate, weather, and fuel bed characteristics.
Fig. 1Map of forested areas and their primary public land management allocations in the western United States. Federal wildlands include administratively withdrawn roadless areas, congressionally designated wilderness, and terrestrial habitat reserve networks. General forest areas are those remaining that are ostensibly amenable to mechanical thinning and prescribed burning treatments. Riparian reserves are generally not shown due to map scale, but they represent a significant area in general forest. The inset map at top right shows an example of riparian reserves in the Swan sub‐basin of northwest Montana. Riparian buffers are 100 m on either side of perennial streams and 30 m on ephemeral streams. Most federal wildlands and national parks are available in concept for using managed wildfires and prescribed burning as fuel reduction treatments, but application of these tools remains uneven. Data sources for map development are (1) for forested areas, National Land Cover Database, NLCD (2006); https://www.mrlc.gov/data/nlcd‐2006‐land‐cover‐conus) for inventoried Roadless Areas (2001), https://www.fs.usda.gov/detail/roadless/2001roadlessrule/maps/?cid=stelprdb5382437, USDA‐FS internal enterprise data layer name: S_USA. InvRoadlessArea_2001; (2) for Northwest Forest Plan Land Use Allocations (2013), https://www.fs.fed.us/r6/reo/landuse/, USDA‐FS internal enterprise data layer name: S_R06.NWFP_LandUseAllocation_2013; (3) for designated Wilderness Areas (2020), USDA‐FS internal enterprise data layer name: S_USA.Wilderness; (4) for Other National Designated Areas (2020), USDA‐FS internal enterprise data layer name: S_USA.PADUS_DESIGNATION; (5) for US National Atlas Federal and Indian Land Areas (last updated 2004), USDA‐FS internal enterprise data layer name: S_USA.OtherNationalDesignatedArea.
Fig. 2Top photo: View from atop Slate Peak in northeastern Washington, looking southwest, 1934, George Clisby photograph, National Archives, Seattle, Washington, USA. The 1934 panoramic view shows extensive evidence of prior wildfires, varied age classes of cold forest, and recently burned and recovering areas. In the same view nearly eight decades later (bottom photo, 2013, John Marshall Photography), note the complete absence of recent fire evidence, widespread ingrowth creating denser forests, loss of nonforest, and lack of forest successional heterogeneity.