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2020
DOI: 10.1016/j.foreco.2020.118312
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Topography and fire legacies drive variable post-fire juvenile conifer regeneration in eastern Oregon, USA

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Cited by 21 publications
(20 citation statements)
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“…Abundant, natural post-fire tree establishment and fast height growth rates of juvenile trees in most plots imply that dry to moist mixed conifer forests are rapidly recovering following the School Fire. High abundances of post-fire regeneration, similar to those observed in the School Fire, were also found following multiple fires in the southern Blue Mountains (Downing et al 2019;Boag et al 2020). However, we did observe very low abundances of post-fire regeneration (<60 stems ha −1 ) 16 years following high-severity fire in plots (4%) near the forest-grassland ecotone where forests in the Blue Mountains and western US appear to be more vulnerable to conversion from forest to non-forest or require longer periods to recover (Downing et al 2019;Stevens-Rumann and Morgan 2019;Boag et al 2020).…”
Section: Discussionmentioning
confidence: 52%
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“…Abundant, natural post-fire tree establishment and fast height growth rates of juvenile trees in most plots imply that dry to moist mixed conifer forests are rapidly recovering following the School Fire. High abundances of post-fire regeneration, similar to those observed in the School Fire, were also found following multiple fires in the southern Blue Mountains (Downing et al 2019;Boag et al 2020). However, we did observe very low abundances of post-fire regeneration (<60 stems ha −1 ) 16 years following high-severity fire in plots (4%) near the forest-grassland ecotone where forests in the Blue Mountains and western US appear to be more vulnerable to conversion from forest to non-forest or require longer periods to recover (Downing et al 2019;Stevens-Rumann and Morgan 2019;Boag et al 2020).…”
Section: Discussionmentioning
confidence: 52%
“…The annual precipitation is ~700mm, and the mean monthly maximum temperatures are ~18°C in July and August and the mean monthly minimum temperatures are −0.4°C in December and January 1 Predictor variables and expected direction of effect in analyses of annual post-fire establishment, post-fire juvenile stem density, and annual height growth (HG) increment with median and range of plot data. Expected effects ("+" positive, "-" negative, "NT" not tested) were based on prior studies (see superscript numbers and footnotes) in the Blue Mountains ecoregion or neighboring ecoregions a (Boag et al, 2020) b (Downing et al, 2019) c (Povak et 2013, and global climate models project temperatures will increase an additional 2.4 to 3.1 °C by 2050 relative to 1970-1999 (Halofsky et al 2018). Annual precipitation has not significantly changed, and model projections do not agree on the direction of change in future annual precipitation (Clifton et al 2018).…”
Section: Study Areamentioning
confidence: 99%
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“…Forest recovery following wildfire is declining and becoming increasingly challenging to achieve through management interventions that seek to replicate past post-wildfire regeneration patterns [7,49,50]. The unfavorability of post-wildfire landscapes for tree recovery (when seed sources are available) has been well-documented [5,14,51], and recent studies point to the further impact of climate change in making post-wildfire environments inhospitable for recovery, both across broad burned areas and within specific microenvironments such as south-facing aspects [1,4,7,49,52]. Additionally, high soil temperatures and complete removal of the litter layer during high severity wildfire are associated with a large decline in post-fire soil water infiltration [53,54].…”
Section: Environmental Effects Shaping Dry Period Severitymentioning
confidence: 99%