2018
DOI: 10.1016/j.foreco.2018.01.017
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Intra- and inter-specific variation of the maximum size-density relationship along an aridity gradient in Iberian pinewoods

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Cited by 42 publications
(46 citation statements)
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“…where represents the number of trees per hectare (trees ha −1 ), and is the quadratic mean diameter over bark (cm) measured at the height level of 1.30 m. For analysis purposes, the maximum density lines for the species estimated in previous studies namely by Luis and Fonseca [28], Aguirre et al [21], Ríofrio et al [30], and Charru et al [26] were also considered, as shown in Figure 5, (coded as L&F, a, b, and c, respectively). (Equation (1)) and the quadratic model (Equation (2)).…”
Section: Maximum Size-density Trajectory Over All the Stages Of Develmentioning
confidence: 99%
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“…where represents the number of trees per hectare (trees ha −1 ), and is the quadratic mean diameter over bark (cm) measured at the height level of 1.30 m. For analysis purposes, the maximum density lines for the species estimated in previous studies namely by Luis and Fonseca [28], Aguirre et al [21], Ríofrio et al [30], and Charru et al [26] were also considered, as shown in Figure 5, (coded as L&F, a, b, and c, respectively). (Equation (1)) and the quadratic model (Equation (2)).…”
Section: Maximum Size-density Trajectory Over All the Stages Of Develmentioning
confidence: 99%
“…For analysis purposes, the maximum density lines for the species estimated in previous studies namely by Luis and Fonseca [28], Aguirre et al [21], Ríofrio et al [30], and Charru et al [26] were also considered, as shown in Figure 5, (coded as L & F, a, b, and c, respectively). Fonseca [28]; a-Aguirre et al [21]; b-Ríofrio et al [30]; c-Charru et al [26]) and in the current study-line in red. The points represented in the graph refer to the four data subsets.…”
Section: Maximum Size-density Trajectory Over All the Stages Of Develmentioning
confidence: 99%
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“…Therefore, the change trend of ALT was negative in early burned areas. However, self-thinning becomes an active process when a young even-aged forest grows to maturity [51], resulting in a relatively open forest cover, which may increase the amount of solar radiation reaching the ground. The interannual variation of ALT is considered to be the result of the interaction between air temperature, wildfire, vegetation recovery, and self-thinning in early burned areas.…”
Section: Spatio-temporal Variations In Active Layer Thicknessmentioning
confidence: 99%