Huffman Forensic Weather & Hail Impact Report

Look, I’ve been roofing in this part of Texas for over twenty years, and I can tell you Huffman gets hit from a perfect storm of bad luck. We sit right in that corridor between the Gulf and the Piney Woods, which means when those spring squall lines roll through, they don’t just pass over—they spin up. The heat off the bayou and the cooler air from the forests to the north create that instability that turns a normal thunderstorm into a hail factory. I’ve pulled golf-ball-sized ice out of gutters here that looked like they’d been shot out of a cannon, and it’s not just the size. The wind that comes with those cells, especially in April and May, whips through the river bottoms and funnels between the trees, so you get these sudden 60 to 70 mile-per-hour gusts that catch the edge of a shingle and just peel it back like a sardine can.

And it’s not just the spring. We get those pop-up supercells in the late summer and early fall, too, when the humidity is still thick and the afternoon sun heats the blacktop roads and concrete pads. That’s when you get the sideways rain and the microbursts that drop straight down. The problem is, most homes here have that architectural shingle that’s rated for 110 mph, but that rating assumes the nails are driven perfectly and the underlayment is fresh. After a few years of that Texas sun baking the asphalt, the granules get loose, and then a hailstone doesn’t bounce—it dents. Once the granule layer is compromised, the mat underneath is exposed, and the next windstorm doesn’t even need to be that strong to lift a tab. I’ve seen roofs that looked fine from the street, but up close, they were just one good gust away from losing half their covering. It’s a double whammy: the storms are violent, but the real damage is that they keep coming back, year after year, wearing down what’s already there.