A. Talkkari et al., Integration of component models from the tree, stand and regional levels to assess the risk of wind damage at forest margins, FOREST ECOL, 135(1-3), 2000, pp. 303-313
This work aims at integrating component models from the tree, stand and reg
ional levels to produce a means of assessing the risk of wind damage at for
est margins. This is done by employing (i) a mechanistic model for predicti
ng the critical wind speed needed to cause damage, (ii) a regional airflow
model simulating the relative wind climates for sites, (iii) a geographical
database on forest stands in the area concerned, and (iv) the probability
distribution of long-term extremes in wind speed at the sites.
Critical wind speeds needed for uprooting of trees at the margins of Scots
pine-dominated stands in an area of north-eastern Finland (which had suffer
ed wind damage in 1995) were predicted using stand level data on mean tree
height, diameter at breast height and stand density for the operational man
agement units. The relative wind climate at the forest margins was calculat
ed from inputs indicating stand location, topography (terrain) and surface
roughness. Annual average wind speed statistics for the area were obtained
from a nearby weather station, and the annual probabilities of critical win
d speeds for the edge conditions prevailing in each stand were then calcula
ted by correcting the probabilities of these critical wind speeds by refere
nce to the relative wind climate for each stand.
The area predicted to be at risk was larger than the area of Scots pine sta
nds which had actually suffered damage. This was because it had been assume
d in the computations that all the stands were at the forest margin. The ca
lculations demonstrate that the area at risk is very sensitive to wind spee
d, and that risk predictions are also especially sensitive to the ratio of
tree height to diameter at breast height. The probabilities of wind damage
were relatively low, however, since the annual wind climate for the area co
ncerned involves mainly speeds of less than 15 m s(-1), whereas in most cas
es higher wind speeds are required to cause damage to stands.
Integration of these component models seems to have great potential for pre
dicting areas with a risk of damage in a given wind climate. Once this info
rmation can be integrated with data on silviculture, it may be possible to
allocate thinnings and new clear fellings, for example, to forest areas usi
ng a strategy that minimises such risks. (C) 2000 Elsevier Science B.V. All
rights reserved.