2003
DOI: 10.2737/rmrs-gtr-105
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Coarse woody debris: Managing benefits and fire hazard in the recovering forest

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Cited by 133 publications
(140 citation statements)
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References 30 publications
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“…This is consistent with a pulse of new logs into the system, many of which (46.8%) were in decay class 1 when sampled in 2009, as well as with greater decay of logs in decay class 3; 100% of logs lost to decay between 2004 and 2009 in mixedconifer forest were in decay class 3 in 2004. Changes in decay status can affect fire behavior, with flammability and probability of ignition generally increasing as logs progress from sound to rotten (Brown et al, 2003). Thus, this large pulse of new logs has implications for fire behavior not only in terms of fuel loads (see below), but also with respect to fuel type.…”
Section: Discussionmentioning
confidence: 99%
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“…This is consistent with a pulse of new logs into the system, many of which (46.8%) were in decay class 1 when sampled in 2009, as well as with greater decay of logs in decay class 3; 100% of logs lost to decay between 2004 and 2009 in mixedconifer forest were in decay class 3 in 2004. Changes in decay status can affect fire behavior, with flammability and probability of ignition generally increasing as logs progress from sound to rotten (Brown et al, 2003). Thus, this large pulse of new logs has implications for fire behavior not only in terms of fuel loads (see below), but also with respect to fuel type.…”
Section: Discussionmentioning
confidence: 99%
“…Brown et al (2003) provided recommendations for optimal ranges of CWD in warm dry coniferous forests, based on factors such as resistance of fires to control, fire duration, soil heating, wildlife values, and historical ranges. Recent studies by Hoffman et al (2011) and Stevens-Rumann et al (2012) documented increases in surface fuel loads in ponderosa pine forests following disturbance by bark beetles and wildfire, respectively.…”
Section: Discussionmentioning
confidence: 99%
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“…Fire temperatures and burn times were modeled for the surface of v www.esajournals.org the mineral soil without a duff layer. While the exclusion of duff from consideration may cause the fire to appear hotter than it actually was, removal served to standardize the soil exposure, and was deemed an equitable means of comparison between fuel loadings (Brown et al 2003) since the relative change in fire characteristics along the interaction gradient was the phenomenon of interest. A map of burn severity was used to estimate distance to the edge of high-severity burned areas for the spatial scale analysis and neighborhood burn severity.…”
Section: Sitementioning
confidence: 99%
“…As Kennedy et al (2010) noted, management effects on deadwood may not appear for 100-200 years due to the potentially long persistence of legacy deadwood. Based on this fact, a rule of thumb might be that a model needs to run at least twice as many years as it takes for an average freshly killed tree to fully decompose, although Brown et al (2003) argue that with uncertainty increasing with time, reasonable projections of deadwood can only be simulated for 50-100 years. If live tree models are used to grow trees for future deadwood inputs, upper time bounds for growth models may limit the maximum number of years that can be projected.…”
Section: H) Temporal Projectionmentioning
confidence: 99%