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Density
Windbreak
density is based on the a view of the long side of a windbreak. It is
the ratio of the solid portion of the windbreak to the total area of the
windbreak. Density is a very important component of windbreak structure
because it affects the length of the protected zone, both upwind and
downwind from the windbreak. Windbreak density is usually divided into
rather broad ranges:
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<20% - Young, establishing
windbreaks or old, mostly-dead single-row windbreaks. Minimal protection
provided.
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20-40% - Established single row
windbreaks consisting of deciduous trees (Fig. 2-1).
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40-60% - Established single row
windbreaks consisting of conifers.
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60-80% - Multiple-row
windbreaks, usually consisting of a mixture of conifers and deciduous
trees (Fig. 2-2A and B).
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>80% - Multiple-row windbreaks
often including more than one row of densely-branched conifers such as
spruces (Fig. 2-3).
Figure 2-1.
Single-row deciduous windbreak, 20-40% density. This density is effective
in crop protection, but the higher density at the bottom of the windbreak
will not allow much snow spreading across the field. Photo by Joe Zeleznik.

Figure 2-2. Multiple-row, mixed deciduous and conifer windbreaks,
in summer and winter. A. Summer density is 50-70% at the top, >80% at the
bottom of the windbreak. B. Winter density in a similar
windbreak is 40-60% at the top, 60-80% near the bottom. These
windbreaks are vital in controlling snow placement and
are both used as "living snow fences" along roads and highways.
Photos by Joe Zeleznik.


Figure 2-3. Very-high-density mixed deciduous and conifer windbreak,
>80% density. Wind protection in winter is outstanding, but remains
for only a short distance downwind of the windbreak. Summer temperatures
behind this windbreak may be stifling, as winds will barely penetrate the
tree canopy. Photo by Joe
Zeleznik.

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