2010
DOI: 10.2980/17-1-3247
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Fire disturbance, forest structure, and stand dynamics in montane forests of the southern Cascades, Thousand Lakes Wilderness, California, USA

Abstract: We examined tree diameter, age structure, and successional trends in 100 montane forest plots to identify the effects of variation in the return interval, severity, and extent of fires on forest structure and dynamics in the southern Cascade Range, California. We classified 100 forest plots into 8 groups based on stand structural characteristics. Median point fire return intervals were shortest in lower montane mixed conifer and Jeffrey pine-white fir stands (13-25 y) and upper montane red fir-white fir stands… Show more

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Cited by 53 publications
(38 citation statements)
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“…With respect to the species distribution, Figure 4 shows that jóvenes como adultos, promoviendo el desarrollo de masas forestales de distintas edades y dimensiones (Bekker & Taylor, 2010). Sin embargo, otros mecanismos también influyen en la distribución espacial de los árboles; por ejemplo, la heterogeneidad microambiental es un conductor potencialthe correlation function of mark indicates that in the area with low severity, the species mix almost in all distances analyzed; however , in medium and high severities, the correlation was positive (K mm [r] > 1).…”
Section: Spatial Interaction Of Trees With the Variable Speciesunclassified
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“…With respect to the species distribution, Figure 4 shows that jóvenes como adultos, promoviendo el desarrollo de masas forestales de distintas edades y dimensiones (Bekker & Taylor, 2010). Sin embargo, otros mecanismos también influyen en la distribución espacial de los árboles; por ejemplo, la heterogeneidad microambiental es un conductor potencialthe correlation function of mark indicates that in the area with low severity, the species mix almost in all distances analyzed; however , in medium and high severities, the correlation was positive (K mm [r] > 1).…”
Section: Spatial Interaction Of Trees With the Variable Speciesunclassified
“…De acuerdo con las estadísticas nacionales, la cantidad de incendios va en aumento; tan sólo hasta el mes de septiembre de 2013, cerca de 415,000 ha se han visto afectadas registrándose más de 10,000 incendios distribuidos en todo el país (Comisión Nacional Forestal [CONAFOR], 2013). Sin embargo, en ecosistemas como los bosques de coníferas, la presencia y la severidad con que un incendio se desarrolla contribuyen a mantener o eliminar la dinámica de crecimiento de las especies, modificar su composición, diversificar la estructura de dimensiones y crear un mosaico heterogéneo de edades (Collins, Everett, & Stephens, 2011;Omi, 2005;Phillips & Waldrop, 2008;Pomerenning, 2006) no sólo a escala de rodal sino también de paisaje (Alanís et al, 2010;Bekker & Taylor, 2010;Gill, Woinarski, & York, 1999;González, Szejner, Muñoz, & Silva, 2011). De esta forma, después de un incendio, los bosques experimentan cambios inmediatos en los patrones de distribución del arbolado (Beaty & Taylor, 2008;Lecomte, Simard & Bergeron, 2006;Li-Juan & Jian-Ping, 2003;Stephens & Fry, 2005;Taylor, 2010) y en la variación de características de la estructura forestal (Ávila et al, 2012;Yu, Wiegand, & Yang, 2009).…”
Section: Introductionunclassified
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“…Whether climate has warmed to historical levels and potentially, precipitation has decreased (or the length between precipitation events has increased), or counter-intuitively, growing season temperatures have cooled and growing season precipitation has increased (McEwan et al 2011), tree species that have increased in current forests show a range of shade and drought tolerance, from early-successional eastern redcedar to mesic, near-riparian tree species (Hanberry et al 2012a). Further patterns that conflict with climate change as a driving factor of forest change include (1) historically dominant oaks and pine are decreasing and contracting in range, not shifting in range to track climate, (2) although climate outlines species distributions, most species do not realize their potential distribution, as evidenced by naturalization outside of ranges, (3) tree establishment and growth do not always match with weather oscillations (e.g., Bekker and Taylor 2010, Kaye et al 2010, Schoennagel et al 2011. However, changes that (1) began at least a century ago, (2) occur across a continent, (3) operate on a temporal scale of tree generations, (4) and have little documentation make experimental and even correlational studies difficult.…”
Section: Climate and Forestsmentioning
confidence: 99%