Valley leaks
Where two roof slopes meet
Wet insulation with a dry ceiling below is one of the more useful diagnostic findings, because it means the water is being caught before it gets through — and it usually points at flashing or a pipe boot rather than the field of the roof. It can also be condensation, which is a ventilation problem and needs a completely different fix. Telling them apart matters: sealing the roof on a condensation problem achieves nothing and often makes it worse by reducing airflow further.
Clay County is far enough south to take the inland remnants of Gulf and Atlantic hurricane systems, and that is the storm profile that matters here. By the time these systems reach Clay County the wind has dropped below the headline numbers but is still sustained for hours, which does something different to a roof than a short violent gust — it works shingle tabs loose over an extended period and drives rain horizontally under courses that would shed a normal downpour. The heat and humidity do the rest. Roofs here run hot for most of the year, which ages the shingle and hardens every rubber and sealant component, and the humidity means anything that gets wet inside the roof stays wet.
Leaks track rain — they appear or worsen during and just after it. Condensation tracks cold snaps and is usually spread evenly across the underside of the decking rather than concentrated at one point. Frost on the nails in winter is condensation, every time.
If it has been properly wet, yes. Fibre insulation compresses when saturated and does not recover its R-value when it dries, so it goes on looking fine while performing at a fraction of its rating.
Where two roof slopes meet
Fasteners, washers and seams
The secondary barrier under the covering
Natural slate, repaired not replaced
Algae streaking and moss growth
Scheduled checks instead of emergencies
You will get a straight answer on whether Clay County needs someone out today or whether it can wait — before anyone quotes you for anything.
Call (229) 592-0097