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Windthrow is most common when soils are shallow
and/or water saturated. Spring is very windy throughout much of
the Southwest, and is the time when blowdown occurs in many root
diseased infected areas. Blowdown is also prevalent in winter months
when trees are loaded with snow.
More severe windthrow damage takes place with tornadoes and microbursts,
which occasionally occur in northern Arizona. Tornadoes and microbursts
both result in windthrown trees lying parallel to one another in
the same direction as the storm. Tree species with shallow root
systems (e.g. spruce) are more prone to windthrow.
Reference: 107
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