Tatum Forensic Weather & Hail Impact Report

Look, I’ve been replacing roofs out here for over twenty years, and Tatum sits right in that nasty little corridor where the Piney Woods meet the open prairie. That mix of flat, hot land and the tree line to the east creates a funnel effect for spring storms. When those supercells roll in from the southwest, usually March through May, they don’t just pass over—they spin up. We get these tight, rotating winds that can hit sixty or seventy miles an hour in a heartbeat, and they’ll peel shingles right off a slope like they’re nothing. The hail is the real kicker, though. It’s not that we get bigger stones than Dallas, but they come down at an angle, driven by that wind, so they slam into the face of your roof instead of just bouncing off the top. That’s what busts up the granules and leaves those little black bruises you can’t see from the ground.

And it’s not just the spring. We get those pop-up thunderstorms in late summer and early fall, too, the kind that brew up in the afternoon heat with zero warning. Those are sneaky because they’ll drop marble-sized hail for ten minutes, then clear off, and you won’t think twice about it. But that hail, mixed with the straight-line winds that come with those cells, is what does the slow damage. The wind lifts the edges of your shingles, and the hail drives water up under them. Before you know it, you’ve got a leak that shows up in the living room ceiling three months later. The geography here—the red clay soil, the scattered pines, the open fields—just makes the air heat up unevenly, and that’s the recipe for these violent, short-lived storms. I tell folks all the time, if you live in Tatum, you’re not asking *if* you’ll need a roof, you’re asking *when*.