Forest disturbance in hurricane-related downbursts in the Appalachian mountains of North Carolina

We characterized five 0.21.1 ha gaps created by downbursts during Hurricane Opal in xeric oak forest at the Bent Creek Experimental Forest, Asheville. NC. Direction of windthrow was nonrandom in four of the five gaps, but differed among gaps suggesting that each was caused by an independent downburst. Windthrows reduced tree density by 19-39s and basal area (BA) by 3%53% within gaps. Most windthrows were uprooted (I 7-38% of all trees) versus broken below I .8 m height (O&3%). Most species were uprooted in proportion to their abundance regardless of canopy position. Red oaks (QUU~US c~oc~c~inra. Quercus ruhm and Quercu.r 1~lutincr~ were disproportionately uprooted, while N~ssa sylt.atica and Awr ruhrurn were resistant to uprooting. As a group, Qwrcus lost 27-47% of individuals and 41-500/c of BA. Q. coccinea lost >_ 44% of trees and > 55% of BA in sites where it occurred. Only minor shifts in canopy species dominance were evident. For several species, significantly more large-diameter individuals uprooted than their smaller counterparts. No relationship between dbh and number uprooted was detected for the red oaks, however. Canopy position appeared to have little bearing on this relationship. Uprooting disturbed I X-4.3% of the ground area and displaced I X-587 m3 of root-soil-rock masses (rootmasses) per gap. We suggest that episodic, high-intensity wind is not uncommon, and has a substantial influence on forest structure, species composition, regeneration and microtopography of the southern Appalachian mountains at variable scales.