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Submitted by jdp on Sat, 11/01/2014 - 12:21 pm


Hot off the press, our (myself, Dan Marion, Chad Yocum, Stephanie Mehlhope, and Jeff Olson) study of geomorphic impacts of a tornado blowdown event. You can get a copy here:

The abstract is below:

Geomorphological Impacts of a tornado disturbance in a subtropical forest.

We studied tree uprooting associated with an EF2 tornado that touched down in portions of the Ouachita Moun- tains in western Arkansas in 2009. In the severe blowdown areas all trees in the mixed shortleaf pine–hardwood forest were uprooted or broken, with no relationship between tree species or size and whether uprooting or breakage occurred. There was also no significant relationship between tree species and amount of soil displaced, and only a weak relationship between tree size and rootwad size. Uprooting resulted in a mean bioturbation rate of 205 m3 ha1 (about 240 t ha1). Direct transfer of wind energy via tree uprooting to geomorphic work of soil displacement was about 75 to 190 J m2. Given the infrequency of tornadoes, this energy subsidy is minor with respect to the long-term energetics of pedogenesis and landscape evolution. However, it does represent a highly significant pulse of geomorphically-significant energy relative to other mechanical processes. Tornadoes such as that of April, 2009—not atypical for the region—are disturbances causing severe, non-selective impacts within the affected area. At a broader, landscape scale, tornadoes are highly localized disturbances, and occur infrequently within any given landform element or forest stand. Only about a third of the uproots revealed root penetration of bedrock, compared to about 90% in other areas of the Ouachita Mountains. This is attributable to the thicker colluvial soils at the study site, and is consistent with the idea that root–bedrock interaction is more likely in thinner regolith covers.