Rain that gets in after the wind has been through

Storm losses are usually two events. Wind lifts shingles, tears a ridge, drives a limb through the decking or pulls a vent boot loose, and then rain uses the opening for as long as it takes to get a tarp on. Most of the water damage on the interior is the second event, and the amount depends almost entirely on how fast the envelope got closed.

December 25, 1987, in West Memphis

There is a local example that makes the sequence unmistakable. A tornado touched down southwest of West Memphis at 9:40 p.m. on December 14, 1987 and tracked northeast through the city with a path up to three hundred feet wide before crossing into Tennessee. It killed six people, destroyed 235 homes and 153 apartments across three complexes, leveled 35 businesses and Maddux Elementary School, and left fifteen hundred people homeless. Eleven days later, on December 25, twelve inches of rain fell on the same city and compounded the damage that was already there.

Every building still standing with a compromised roof took that rain into an assembly that had no cover. That is the ordinary pattern in miniature after every wind event: the storm damage estimate written on day one is not the loss, it is the beginning of the loss, and the roof tarp is a water mitigation step, not a cosmetic one.

1. You callOne number per county. The dispatcher takes the address, the ZIP and a short description of what happened.
2. A local crew calls backAn independent restoration contractor already working that county rings you directly and sets a time.
3. They look, then scope itNothing is priced from a phone call. The crew walks the building, takes readings, and writes a scope you can hand to your adjuster.

Water does not fall where the hole is

Rain entering a roof opening rarely drops straight down into the room below it. It lands on the top of the decking or runs down the underside of the sheathing along the rafter, follows the rafter to the top plate of an exterior wall, and travels along that plate until it finds a path. The path is usually a ceiling penetration: a can light, a bath fan housing, a supply register, or the seam between two sheets of drywall. That is why a hole above a back bedroom shows up as a wet spot over the kitchen sink.

Blown-in attic insulation makes it worse in a specific way. It absorbs and holds the water, spreads it laterally across the ceiling by capillary action, and keeps feeding it into the drywall for days after the rain has stopped. Wet insulation also loses its loft permanently, so it comes out over the wetted area whether or not the ceiling below is saved.

A ceiling holding water will sag before it fails, and the sag is a useful warning. The right response is a deliberate relief hole at the low point with a bucket under it, cut by someone standing to the side, rather than waiting to see whether the assembly holds. A saturated ceiling that lets go at once takes the light fixtures, the insulation and whatever is on the floor beneath it.

Hail, and the leak that arrives months later

Hail does something different from wind. It bruises asphalt shingles, fracturing the mat and knocking granules loose without necessarily opening a hole the same day. The roof looks intact from the ground and leaks the following spring, once ultraviolet exposure has worked on the damaged mat. Franklin County saw a line of storms drop hail from one inch to two inches across the county between roughly 11:10 p.m. on April 4 and 1:45 a.m. on April 5, 2025, with damage to homes and vehicles reported near Webb City, near Meg and northwest of Peter Pender, at an estimated fifteen to twenty-five thousand dollars per event.

That delay is why a hail inspection after a storm is worth doing even when nothing is dripping. It is also why a slow ceiling stain in a house that took hail a year earlier should be traced to the roof before anyone assumes it is plumbing.

The events this footprint has actually seen

Van Buren sits on the eastern edge of the region called Tornado Alley, and it has the record to match. An F3 tornado with winds near 200 miles per hour touched down near the Garrison Street Bridge in Fort Smith at 11:12 p.m. on April 21, 1996, crossed the Arkansas River into Van Buren around 11:18 p.m., and ran about seven more miles before dissipating east of US-59. In Van Buren it heavily damaged the Vista Ridge subdivision, Morrison Elementary School, Coleman Junior High School and a newly built fire station, part of a nearly ten-mile, half-mile-wide path that destroyed or severely damaged about eighteen hundred homes.

Franklin County's worst was the low-end EF4 that touched down at 11:53 p.m. on May 24, 2011 and tracked 45.71 miles overnight across Franklin, Logan and Johnson counties, growing nearly a mile wide, bending large metal transmission poles to the ground at Denning and killing two people there before dissipating in the Ozark National Forest. A smaller EF1 on May 18, 2019 ran 4.6 miles along Jetton Road and Highway 217 near Charleston, uprooting trees and damaging home roofs and chicken houses. In Baxter County, a February 2008 tornado cut a destructive path through Gassville, killing one person and injuring many others.

Winter storms produce the same category of loss by a different route. A system on January 24 and 25, 2023 dropped four to ten inches of heavy wet snow across Franklin County, snapping tree limbs onto power lines and causing about $320,000 in property damage. Limbs come down on roofs, and the resulting openings sit unattended while the power is out.

Drying a building the power has left

Storm losses have a constraint that plumbing losses do not: the electricity is usually gone, often across a whole neighborhood, and drying equipment needs current. That shapes the first day of work. Water gets extracted mechanically, standing water gets pumped, saturated insulation and pad come out, and the building gets closed in with tarp and board. Dehumidifiers and air movers go in when there is power to run them, from a generator if the outage is going to be long.

Closing the envelope is the step that protects everything else. A roof tarp fastened properly at the ridge and battened at the edges will hold through the next round of rain; a sheet of plastic weighted with lumber will not. Broken glazing gets boarded, because wind-driven rain through a window opening wets an interior wall faster than a roof leak does.

What people ask before calling

Everything above is background. The call is what starts the work.