Roof Notes · Storm Damage
Wind damage on a Kentucky roof has a direction, and the direction is the most useful thing about it. The National Weather Service separates straight-line wind from tornado damage by asking which way the debris is lying, and a homeowner standing in the yard the morning after can read the same evidence on the same roof before anyone climbs it.
This is the survey method, not a rule of thumb. The NWS office in Northern Indiana states the distinction in two words: “IN – all wind flows INTO a tornado” and “OUT – all wind flows OUT from a downburst.” With a tornado, “debris is often laying at angles due to the curving of the inflow winds.” With a downburst, “debris is often laying in straight lines (hence the term ‘straight line winds’) parallel to the outward wind flow.”
How do you tell wind damage from ordinary wear on a Kentucky roof?
Wear is scattered and random across the whole roof. Wind damage is directional and edge-first: it concentrates on one or two slopes, starts at a perimeter or a ridge, and points the same way.
That is the practical value of the NWS framing. A roof that has simply aged loses granules and seals unevenly everywhere. A roof that met a downburst shows a consistent story: lifted or creased shingles on the windward slope, a clean line where the failure started, and everything downstream of it pointing away from the same origin. If the pattern on your roof has no direction, the storm probably is not the explanation.
Why does wind damage start at the edge of the roof?
Because the edge is where wind first gets underneath. Uplift needs a lever, and an unsealed perimeter shingle, a lifted ridge cap or a poorly terminated rake gives it one.
Once the first course lifts, the failure runs with the wind rather than against it, which is why a wind event so often reads as a stripe rather than a patch. It is also why the perimeter details are code-regulated in the first place — see our note on what the Kentucky code requires at the drip edge, which is the specific detail most often missing where a wind stripe begins.
Hail leaves a pattern you have to be on the roof to see. Wind leaves one you can photograph from the driveway — and the photograph is worth more the same day than it is a month later.
What is worth photographing the morning after a Central Kentucky windstorm?
Four things: the direction everything in the yard is lying, the affected slope from the ground, any shingles or caps on the ground with their position, and the date.
- The yard, not just the roof. Lawn furniture, branches and fence sections lying in one consistent direction is the same evidence the NWS uses. Photograph it before anyone tidies up.
- The whole elevation from the ground, then the detail. A wide shot establishes which slope and which direction; close-ups without it establish neither.
- Anything that came off, where it landed. A shingle in the yard downwind of the slope it came from is a directional fact. In a bag by the garage it is just a shingle.
- The date, from the camera. The event date is what ties your roof to the public storm record, and the record is searchable — the NOAA Storm Events Database logs thunderstorm wind events by county and date.
Does a wind event have to be a tornado to damage a roof?
No. Straight-line thunderstorm wind is the ordinary case in Central Kentucky, not the exception, and it is the category most of the county record is made of.
We counted that record ourselves for fourteen Central and Eastern Kentucky counties: the federal log carries far more thunderstorm wind events than hail events across 2022 through 2024. The county-by-county numbers, with the source files, are in our comparison of the Central Kentucky wind and hail record. The reason it matters for a roof is that the damage signature nobody is looking for is the one that shows up most often.
A note on how this goes in practice, as a matter of craft. The single most common thing that weakens a homeowner’s own account of a wind event is cleanup. The yard gets cleared, the loose shingles get stacked, and by the time anyone is looking at the roof the direction — the one piece of evidence the National Weather Service itself relies on — has been thrown away. Ten minutes of photographs before the cleanup is worth more than any amount of description afterwards, and it costs nothing.
Can I tell the wind speed from the damage on my roof?
Not yourself. The NWS assigns a maximum wind speed after a survey, “based on the degree of damage and damage indicators,” which is a trained judgement against a published scale. What you can do is record the direction and the date accurately and let the public record supply the event.
Is a lifted shingle that settled back down still damage?
It can be, because the seal strip does not re-bond once it has been broken. A shingle that looks flat again may no longer be sealed to the course below it, which is why creasing along the seal line matters more than whether the shingle is currently lying down.
My roof is on a rental — who handles a wind repair?
That is a landlord-and-tenant question set by the lease and by Kentucky law rather than by the roof, and we cover it separately in who repairs a roof leak in a Kentucky rental.
Last updated: September 28, 2026. The IN/OUT distinction, the debris-direction wording and the wind-speed assignment method are quoted from the National Weather Service Northern Indiana page on straight-line winds versus tornadoes, read 28 September 2026. Event counts referenced above come from the NOAA NCEI Storm Events Database as reported in our own earlier note, retrieved 27 September 2026.
By Marcos Gil, REALTOR® — Keller Williams Commonwealth · KY Real Estate License No. 296259 · Call or text (859) 310-1209.
Central Roof Repair is owned by Marcos Gil, who also publishes marcosgilrealty.com and investinthegorge.com. This note is general information about reading storm evidence. It is not a damage assessment, an insurance opinion, or a promise about any claim outcome.

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