“…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%
“…To assess the likelihood for post-fire recovery to forest (i.e., resilience), we compared post-fire stem densities to local silvicultural stocking recommendations and pre-fire stem densities. On lands managed by the USDA Forest Service in the Blue Mountains, minimum stocking recommendations range from ~60 trees ha −1 in lower elevation and drier forest types to >350 trees ha −1 in higher elevation and cooler-moister forest types (Powell 1999), and these stocking rates were used in similar post-fire regeneration studies of dry to moist mixed conifer forest types in the PNW (Povak et al 2020;Boag et al 2020). Specifically, we compared postfire stem density (sum of juveniles and surviving trees) for each plot to four post-fire stem density thresholds:…”
Section: Comparing Post-fire Stem Densities To Silvicultural Stocking...mentioning
confidence: 99%
“…Increased fire activity is expected to catalyze changes in dry to moist mixed conifer forest communities, such as decreases in forested area, lower canopy cover within forested areas, and shifts toward more drought-tolerant species (Kerns et al 2018). Researchers have identified key limitations to the densities of post-fire seedling establishment (e.g., seed availability and moisture deficit) in the Blue Mountains (Downing et al 2019;Boag et al 2020), but the following aspects of post-fire ecosystem recovery have yet to be explored: (1) the influence of interannual climate on seedling establishment for multiple conifer species (but see Hankin et al 2019 in northern Rockies), (2) drivers of the spatial and temporal variability in annual height growth (but see Littlefield 2019 in the eastern Cascade Mountains), (3) shifts in post-fire tree composition and structure over time, and (4) the implications of post-fire management practices for regeneration (but see Povak et al 2020for effects of salvage logging in neighboring ecoregions).…”
Background
In seed-obligate conifer forests of the western US, land managers need a better understanding of the spatiotemporal variability in post-fire recovery to develop adaptation strategies. Successful establishment of post-fire seedlings requires the arrival of seeds and favorable environmental conditions for germination, survival, and growth. We investigated the spatiotemporal limitations to post-fire seedling establishment and height growth in dry to moist mixed conifer forests with and without post-fire forest management treatments (salvage logging, grass seeding) in areas burned from low to high severity. In 2011, we measured post-fire seedling establishment year, juvenile density (seedlings and saplings), and height growth (annual and total) in 50 plots with six conifer species in the School Fire (2005), Blue Mountains, WA, USA. In 2021, we remeasured the plots for post-fire juvenile density and height growth.
Results
Post-fire juvenile tree densities appeared sufficient for self-replacement of forest (> 60 stems ha−1) in 96% of plots in 2021 (median 3130 stems ha−1), but densities were highly variable (range 33–100,501 stems ha−1). Annual seedling establishment was positively correlated with cooler, wetter climate conditions during the summer of germination (July–September) and the growing season of the subsequent year (April–September) for multiple tree species. We found lower juvenile densities at greater distances to seed sources and with higher grass cover, while salvage logging had no effect. Annual height growth was shorter on warmer, drier topographic positions for three species, whereas annual height growth was associated with climate variability for one species. Shifts in height class structure from 2011 to 2021 were, in part, explained by differences among species in annual height growth.
Conclusions
Abundant and widespread tree seedling establishment for multiple conifer species after fire was strong evidence that most burned sites in the present study are currently on a trajectory to return to forest. However, post-fire establishment may be constrained to brief periods of cooler, wetter climate conditions following future fires. Long-term monitoring of post-fire recovery dynamics is needed to inform management activities designed to adapt forests to climate change and future disturbances, which will collectively shape future forest structure and composition.
“…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%
“…To assess the likelihood for post-fire recovery to forest (i.e., resilience), we compared post-fire stem densities to local silvicultural stocking recommendations and pre-fire stem densities. On lands managed by the USDA Forest Service in the Blue Mountains, minimum stocking recommendations range from ~60 trees ha −1 in lower elevation and drier forest types to >350 trees ha −1 in higher elevation and cooler-moister forest types (Powell 1999), and these stocking rates were used in similar post-fire regeneration studies of dry to moist mixed conifer forest types in the PNW (Povak et al 2020;Boag et al 2020). Specifically, we compared postfire stem density (sum of juveniles and surviving trees) for each plot to four post-fire stem density thresholds:…”
Section: Comparing Post-fire Stem Densities To Silvicultural Stocking...mentioning
confidence: 99%
“…Increased fire activity is expected to catalyze changes in dry to moist mixed conifer forest communities, such as decreases in forested area, lower canopy cover within forested areas, and shifts toward more drought-tolerant species (Kerns et al 2018). Researchers have identified key limitations to the densities of post-fire seedling establishment (e.g., seed availability and moisture deficit) in the Blue Mountains (Downing et al 2019;Boag et al 2020), but the following aspects of post-fire ecosystem recovery have yet to be explored: (1) the influence of interannual climate on seedling establishment for multiple conifer species (but see Hankin et al 2019 in northern Rockies), (2) drivers of the spatial and temporal variability in annual height growth (but see Littlefield 2019 in the eastern Cascade Mountains), (3) shifts in post-fire tree composition and structure over time, and (4) the implications of post-fire management practices for regeneration (but see Povak et al 2020for effects of salvage logging in neighboring ecoregions).…”
Background
In seed-obligate conifer forests of the western US, land managers need a better understanding of the spatiotemporal variability in post-fire recovery to develop adaptation strategies. Successful establishment of post-fire seedlings requires the arrival of seeds and favorable environmental conditions for germination, survival, and growth. We investigated the spatiotemporal limitations to post-fire seedling establishment and height growth in dry to moist mixed conifer forests with and without post-fire forest management treatments (salvage logging, grass seeding) in areas burned from low to high severity. In 2011, we measured post-fire seedling establishment year, juvenile density (seedlings and saplings), and height growth (annual and total) in 50 plots with six conifer species in the School Fire (2005), Blue Mountains, WA, USA. In 2021, we remeasured the plots for post-fire juvenile density and height growth.
Results
Post-fire juvenile tree densities appeared sufficient for self-replacement of forest (> 60 stems ha−1) in 96% of plots in 2021 (median 3130 stems ha−1), but densities were highly variable (range 33–100,501 stems ha−1). Annual seedling establishment was positively correlated with cooler, wetter climate conditions during the summer of germination (July–September) and the growing season of the subsequent year (April–September) for multiple tree species. We found lower juvenile densities at greater distances to seed sources and with higher grass cover, while salvage logging had no effect. Annual height growth was shorter on warmer, drier topographic positions for three species, whereas annual height growth was associated with climate variability for one species. Shifts in height class structure from 2011 to 2021 were, in part, explained by differences among species in annual height growth.
Conclusions
Abundant and widespread tree seedling establishment for multiple conifer species after fire was strong evidence that most burned sites in the present study are currently on a trajectory to return to forest. However, post-fire establishment may be constrained to brief periods of cooler, wetter climate conditions following future fires. Long-term monitoring of post-fire recovery dynamics is needed to inform management activities designed to adapt forests to climate change and future disturbances, which will collectively shape future forest structure and composition.
“…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
Juvenile tree survival will increasingly shape the persistence of ponderosa pine forests in the western United States. In contrast to severe pulse disturbances that induce widespread adult and juvenile tree mortality, moderate periods of low rainfall and warm temperatures may reduce forest persistence by killing juvenile trees at the seedling stage. Intensification of these periods in a changing climate could therefore increasingly restrict both natural regeneration and artificial regeneration of planted seedlings. We conducted a controlled field experiment at a single site in the Front Range of Colorado, USA, to determine the responses and survival of 3 Colorado subpopulations of <1 year old potted ponderosa pines to moderately dry conditions, variation in small rainfall events based on observed patterns, and shaded and unshaded microsite environments. Near surface soil moisture increased slightly following small rainfall events, but declined over the 45-day experimental period. Seedling transpiration and associated canopy cooling declined after ∼13 days, and further declines in transpiration and canopy cooling suggest that the majority of trees in lower rainfall treatments experienced hydraulic dysfunction between days ∼20–30. After 45 days, mortality across all subpopulations and treatments, inferred by relative water loss, exceeded 90–95%. Despite some uncertainty pertaining to the stress tolerance of nursery grown versus naturally germinated conifers, our results show that planted ponderosa pine seedlings <1 year old are unlikely to survive moderate dry periods of 20+ days relying on small rainfall events. Although microsite conditions and soil moisture availability shaped tree hydraulic functioning early in the experiment (days 1–13), later functioning was shaped predominately by the legacy of rainfall treatments. Our results illustrate the importance of moderate dry events that occur consistently as part of seasonal variation in climate, and show how their intensification may constitute a sustained press that limits opportunities for natural and artificial regeneration.
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