Titlebook: Natural Disturbances and Historic Range of Variation; Type, Frequency, Sev Cathryn H. Greenberg,Beverly S. Collins Book 2016 Springer Inter

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neutrophils

Gap-Scale Disturbances in Central Hardwood Forests with Implications for Management, fine-scale biophysical conditions, these localized canopy disturbances promote heterogeneity and biodiversity in forest ecosystems. Forest management based on natural disturbance processes should consider elements of the gap-scale disturbance regime, such as frequency, size, shape, and closure mech

世俗

Oak Decline in Central Hardwood Forests: Frequency, Spatial Extent, and Scale,eriods of drought that occur in combination with repeated spring defoliations by leaf-feeding insects exacerbate decline. Past disturbances have shaped current forest species composition and age structure, favoring physiologically mature stands with a large oak component, and are thus inextricably l

畢業(yè)典禮

Southern Pine Beetles in Central Hardwood Forests: Frequency, Spatial Extent, and Changes to Forestgion in the past 65 years occurred 1974–1976 and 1997–2003, with the most recent impacting more than 405,000 ha, and caused an estimated economic loss of more than $1 billion across six states. In this chapter we examine the spatial extent and frequency of SPB outbreaks in the CHR. We also discuss t

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Ruptured-Disk

Multi-millennial Record of Erosion and Fires in the Southern Blue Ridge Mountains, USA, no indication that pre-settlement Mississippian and Cherokee agricultural activities accelerated erosion and sedimentation in the region. A continuous 11,244 years before present (BP) vertical accretion record from a meander scar in the Upper Little Tennessee River valley indicates abundant charcoa

pacifist

Frequency and Magnitude of Selected Historical Landslide Events in the Southern Appalachian Highlaneinforcing roots. Precipitation and hillslope-scale landforms have a controlling effect on soil moisture, root strength, and debris flow hazards. Anthropogenic influences have increased the frequency of mass wasting for a given storm event above historical natural levels through changes in vegetatio