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dc.contributor.authorRhoads, Anneen_US
dc.contributor.authorHamburg, Stevenen_US
dc.contributor.authorFahey, Timothyen_US
dc.contributor.authorSiccama, Thomasen_US
dc.contributor.authorHane, Elizabethen_US
dc.contributor.authorBattles, Johnen_US
dc.contributor.authorCogbill, Charlesen_US
dc.contributor.authorRandall, Jesseen_US
dc.contributor.authorWilson, Geoffen_US
dc.date.accessioned2006-08-18T21:23:25Zen_US
dc.date.available2006-08-18T21:23:25Zen_US
dc.date.issued2002en_US
dc.identifier.citationCanadian Journal of Forest Research 32N10 (2002) 1763-1775en_US
dc.identifier.issn0045-5067en_US
dc.identifier.urihttp://hdl.handle.net/1850/2360en_US
dc.description.abstractA major ice storm in January 1998 provided an opportunity to study the effects of a rare, intense disturbance on the structure of the northern hardwood forest canopy. Canopy damage was assessed using visual damage classes within watersheds of different ages at the Hubbard Brook Experimental Forest (HBEF) and changes in leaf area index in two of these watersheds. Ice thickness was measured, and ice loads of trees were estimated using regression equations. In the 60- to 120-year-old forests (mean basal area 26 m2•ha–1), damage was greatest in trees >30 cm diameter at breast height and at elevations above 600 m. Of the dominant tree species, beech (Fagus grandifolia Ehrh.) was the most damaged, sugar maple (Acer saccharum Marsh.) was the most resistant, and yellow birch (Betula alleghaniensis Britt.) was intermediate. Trees with advanced beech bark disease experienced heavier ice damage. Little damage occurred in the 14-year-old forest, while the 24- to 28-year-old forest experienced intense damage. In the young stands of this forest, damage was greatest between 600 and 750 m, in trees on steep slopes and near streams, and among pin cherry (Prunus pensylvanica L.). Recovery of the canopy was tracked over three growing seasons, and root growth was monitored 1 year after the storm. Because of the high density of advance regeneration from beech bark disease and root sprouting potential in ice-damaged beech, HBEF will likely see an increase in beech abundance in older forests as a result of the storm. There will also be a more rapid change from pioneer species to mature northern hardwoods in the younger forests. These predictions illustrate the ability of rare disturbances to increase heterogeneity of forest structure and composition in this ecosystem, especially through interactions with other disturbances.en_US
dc.format.extent39576 bytesen_US
dc.format.mimetypeapplication/pdfen_US
dc.language.isoen_USen_US
dc.publisherNational Research Council Canada: Canadian Journal of Forest Researchen_US
dc.titleEffects of an intense ice storm on the structure of a northern hardwood foresten_US
dc.typeArticleen_US
dc.subject.keywordBeechen_US
dc.subject.keywordIce damageen_US
dc.subject.keywordHardwood foresten_US
dc.identifier.urlhttp://dx.doi.org/10.1139/x02-089


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