2000
DOI: 10.1016/s0378-1127(99)00082-1
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Catastrophic windthrow in the southern Appalachians: characteristics of pits and mounds and initial vegetation responses

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Cited by 157 publications
(111 citation statements)
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“…vulnerable to wind damage because of its high elevation, steep slopes, and shallow soils on numerous scree sites. Moreover, when strong winds are accompanied by heavy rainfall, as it happened in October of 2006, the saturated soil becomes unstable, causing tall trees to fall, as they act as masts (Clinton and Baker 2000). In both of our forest types, canopy gaps tended to form on the slopes, suggesting that such locations are more affected by strong winds than mountain ridges or flat areas (Kim 1996).…”
Section: Characteristics Of Gap-maker Speciesmentioning
confidence: 88%
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“…vulnerable to wind damage because of its high elevation, steep slopes, and shallow soils on numerous scree sites. Moreover, when strong winds are accompanied by heavy rainfall, as it happened in October of 2006, the saturated soil becomes unstable, causing tall trees to fall, as they act as masts (Clinton and Baker 2000). In both of our forest types, canopy gaps tended to form on the slopes, suggesting that such locations are more affected by strong winds than mountain ridges or flat areas (Kim 1996).…”
Section: Characteristics Of Gap-maker Speciesmentioning
confidence: 88%
“…When large trees are uprooted, the forest floor is significantly altered because seeds lying within the soil become exposed and germinate, and the physical and chemical nature of the soil is changed by penetrating light (Greenberg and McNab 1998). In addition, soil gaps such as pits and mounds (Peterson and Pickett 1990) may lead to new microsites that can support the development of vegetation, ultimately changing the overall forest structure (Clinton and Baker 2000).…”
Section: Study Sitesmentioning
confidence: 99%
“…Koivula and Spence [123] reported increased activity-abundance and species richness with increasing salvage logging intensity (low: 23-30% timber removed, moderate: Severe wind storms generally fell a high proportion of canopy trees forming large, patchy gaps, although some trees lose only branches and remain standing [96]. Tipped trees form pits and mounds that mix organic and mineral layers, expose rocks and roots, and create distinct microsites that differ from neighboring undisturbed soil [97][98][99][100][101]. Trees fall nearly simultaneously and often in the same direction, resulting in accumulation of CWD of different species, types, and sizes [36,96].…”
Section: Windmentioning
confidence: 99%
“…The risk of windthrow is greatest on thin or waterlogged soils and is more common for species with shallow roots or low-density wood (Whitney 1961, Mitchell 1995, Auclair et al 1996, Clinton and Baker 2000, Ruel 2000, Ruel et al 2001. The time of occurrence of windstorms likely plays a role in the tree mortality rate.…”
Section: Windthrowmentioning
confidence: 99%