Louisiana’s rainfall intensity creates a flat roof drainage demand that roof systems in more moderate climates rarely face. Denham Springs receives approximately 60 inches of annual rainfall, among the highest in the continental United States, delivered in a pattern of intense, high-volume events concentrated in Louisiana’s warm months rather than distributed as moderate rainfall across the year. A single Gulf storm or afternoon convective event can deliver two to four inches of rain in a matter of hours.
On a flat roof system this rainfall intensity means that drainage capacity, the number, size, and placement of drains and scuppers, is not a theoretical specification concern. It is a direct performance variable that determines whether the roof handles each rainfall event without ponding or whether water accumulates on the deck surface and remains there for extended periods after the event ends.
Ponding water on a flat roof in Louisiana is not merely a nuisance condition. Standing water accelerates roof coating and surface degradation through sustained hydrostatic pressure, chemical interaction between the water and roofing materials, and the thermal cycling between wet and dry surface temperatures that occurs as ponded water evaporates in Louisiana’s heat. A flat roof that ponds water consistently ages faster than a correctly drained flat roof, sometimes by years of service life, and is more vulnerable to failure at the ponding locations.
Beyond surface degradation, structural loading from ponded water is a real concern on flat roof decks not designed for sustained water accumulation. Water weighs approximately 5.2 pounds per square foot per inch of depth. Two inches of ponded water across a 1,000-square-foot flat roof adds over 10,000 pounds of load to the deck structure. On residential additions, carports, and covered porch roofs in Denham Springs, where the structural framing may not have been designed with significant live load reserve, this is a load that warrants attention.