Storm Damage Repair in Cleveland, OH

Cleveland's storm damage environment is dominated by Lake Erie's enormous influence on regional weather — the lake generates lake-effect snowstorms, intense nor'easters, and autumn gale events that give Cleveland some of the most extreme storm damage exposure of any major Midwestern city. Lake-effect snowstorms, which develop when cold Arctic air masses traverse the unfrozen lake surface in November through January and absorb enormous moisture before dumping heavy snow on downwind Cleveland communities, can deposit 2 to 3 feet of snow in 24 hours in the snow belts of eastern Cuyahoga County and Lake, Geauga, and Ashtabula Counties. The resulting snow loads on commercial and residential rooftops — particularly flat commercial roofs in the eastern Cleveland suburbs — can exceed design capacity, causing partial or full collapses. Lake Erie nor'easters, which direct northeast winds and waves against the Cleveland shoreline, can generate wave heights of 10 to 15 feet and storm surge conditions that damage lakefront bulkheads, seawalls, and beachfront properties from Bay Village to Euclid. Cleveland's autumn and winter windstorms — which track from the west across the open lake surface and arrive at the south shore with maximum fetch and intensity — regularly produce 50 to 65 mph sustained wind conditions that damage commercial signage, strip roofing from flat-roofed commercial buildings, and topple large trees throughout the metro.