Uplift, Seal Failure, and Vulnerable Areas
Understanding the mechanics of wind damage helps explain why
professional inspection after a significant wind event is
genuinely necessary even when a roof looks intact.
Uplift Force
Wind does not simply blow shingles horizontally off a roof. It
creates uplift. As wind moves over a roof surface, it creates a
low pressure zone above the roof plane that pulls upward. This
uplift force is highest at the edges of the roof, at the ridge,
along the rakes, and at any point where the geometry creates
accelerated wind flow.
The starter course at the eave edge is the roofing system first
line of defense against this uplift. From the eaves, uplift
pressure tries to work its way up the roof by lifting each shingle
tab and putting stress on the adhesive seal that holds the tab to
the shingle beneath it. When that seal breaks, the tab lifts
freely. When the wind stops, the tab lays back down. The break is
invisible.
Adhesive Seal Failure
Factory applied asphalt shingles include an adhesive strip along
the back of the tab that seals the shingle to the course beneath
it when exposed to adequate temperature. Once a wind event breaks
that adhesive bond, the tab is functionally unsealed even though
it appears attached.
In Bismarck’s climate, a shingle tab that has lost its
adhesive seal in a September wind event may lay flat throughout
the cold months, appearing completely intact. The first warm
spring rain drives water underneath it along the path that the
broken seal would have blocked.
Ridge Caps, Hips, and Rake Edges
Ridge cap shingles sit at the peak of the roof and receive uplift
pressure from both directions simultaneously. Hip sections, where
two roof slopes meet at an angled ridge running from peak to eave,
face similar exposure. Rake edges face direct wind pressure from
the side and uplift from the leading shingle edges. We inspect
every linear foot of ridge cap and hip treatment after a wind
event, and we look at rake edges specifically for shingles lifting
back from the roof edge.
Valley Exposure
Valleys, where two roof planes meet at an inward angle, experience
concentrated wind flow as air is funneled through the geometry of
the valley. After a high wind event, valley conditions are worth
specific inspection attention.