1. Regional Microclimate Dynamics & Severe Storm Exposure in Salt Lake City
Salt Lake City's high-altitude elevation of 4,226 feet (rising to over 5,000 feet in foothill areas like Sandy and Draper) creates extreme diurnal temperature differentials during winter months. Heavy snowfall melts under midday high-altitude sunlight and warm attic heat bypasses, flowing downward toward the cold, unheated eave overhangs and aluminum gutters. As evening temperatures plunge into the teens, this meltwater refreezes into an impermeable ice dam. Backed-up meltwater pools behind the ice barrier and is drawn upward via capillary suction beneath asphalt shingles, saturating cellulose attic insulation and causing ceiling collapses and toxic mold colonization within 48 to 72 hours. Furthermore, repeated freeze-thaw cycles expand trapped water inside micro-fissures by 9 percent, physically tearing nail shanks from plywood decks and delaminating standard organic roofing felts.