Storm Damage Repair in Tucson, AZ

Tucson's storm damage environment is dominated by three weather phenomena unique to the Sonoran Desert: the monsoon convective storms of summer, the haboobs (massive dust storms) that precede monsoon fronts, and the high-wind events that accompany both systems across the city's flat, open terrain. Monsoon convective storms generate hail — occasionally golf-ball-sized in the most intense supercells — that is particularly damaging to Tucson's flat-roofed residential construction: gravel ballast roofing systems, which are ubiquitous in the metro, are vulnerable to hail-driven gravel displacement that exposes the underlying membrane to UV degradation. Haboobs — the dramatic wall-of-dust phenomena that reach 3,000-foot heights above the desert floor — carry sand particles that abrade window screens, weatherstripping, and building exterior finishes, while also driving sharp gravel and debris at vehicle and structure surfaces at 40 to 60 mph. Tucson's historically flat terrain and open desert exposure also concentrate the destructive potential of monsoon downburst winds: microbursts associated with collapsing convective cells can generate straight-line winds of 80 to 100 mph in the Tucson Valley, causing rooftop damage to flat-roofed commercial and residential structures and toppling mature saguaro cacti that crash through roofs and vehicles.