Hail claims on Salt Lake City commercial buildings require documentation that holds up under adjuster review, not a quick walk and a bid. We separate event damage from age-related membrane degradation, produce the dated photo record adjusters need, and deliver permanent repair - not temporary patch.

The Wasatch Front's position at the eastern edge of the Great Basin and the western slope of the Wasatch Range creates atmospheric conditions that generate significant hail events most summers. Utah's most damaging hail storms typically develop along the Wasatch Front convergence zone - where valley-floor air masses interact with orographic lift on the mountain slopes - and can produce stones above 1.5 inches in corridor events that track from south of Utah County through Salt Lake County and into Davis County. The summer of 2023 produced multiple events with documented stone sizes above 1.5 inches across the Salt Lake Valley. After each event, the documentation window that determines whether a claim is paid or contested is narrow.

Our hail damage work follows a specific sequence: independent roof walk within 48 hours of the event to establish dated, pre-adjuster documentation; adjuster walk with our project manager present; written scope distinguishing event damage from pre-existing membrane degradation; permanent repair with documented materials and installation records; and a post-repair photo record that closes out the claim file. We have worked through this sequence on commercial buildings across Salt Lake County, and we know what adjusters from the major commercial carriers look for in Utah.

We do not pursue storm-chasing sales work. We document what the event did, distinguish it from conditions that pre-dated the storm, and repair what the hail damaged. The documentation integrity we maintain is what makes our reports useful to adjusters and credible in dispute resolution.

Insurance-Grade Documentation on Utah Buildings

A commercial hail claim requires evidence of three distinct elements: that a hail event occurred, that the event caused the observed damage, and that the observed damage is distinguishable from pre-existing conditions. The first is established by NOAA storm reports and insurance weather verification services keyed to the storm date. The second requires photographs that show hail impact signatures - spatter patterns on AC condenser fins, dented pipe boot collars, fractured granules on modified bitumen surface, and bruising or splits on TPO and EPDM membrane at the impact points.

The third element - distinguishing event damage from pre-existing conditions - is where most commercial hail claims on Utah buildings generate disputes. Membrane surfaces on older Wasatch Front buildings carry UV degradation and thermal cycling damage that can be difficult to distinguish from hail-induced bruising without systematic documentation. We photograph and describe every area of membrane degradation during our pre-adjuster walk, noting whether each condition is consistent with hail impact signature or with age-related degradation. We document both honestly because our adjuster relationships depend on accuracy.

We measure hail density - impacts per 10 sq ft - in multiple locations across the roof, using a painted test square to establish a count baseline the adjuster can replicate. We also document metal components - parapet coping caps, pipe boots, skylight frames, HVAC equipment panels - because hard-surface spatter evidence is what adjusters weight most heavily when correlating roof damage to a specific event.