The core idea
Valleys, gutters, scuppers and roof transitions concentrate water and can exceed local drainage capacity.
How the mechanism works
Flow depth and pressure increase where runoff converges or debris restricts the path.
When it becomes relevant
Typical trigger: Heavy rain, leaf fall or snowmelt.
Evidence that supports this interpretation
- Only intense events reproduce the symptom
- Overflow or ponding is visible
- Damage aligns below a concentration point
Evidence that weakens it
- Light rain causes identical leakage
- Drainage remains free and oversized
- The mark follows indoor water use
What this concept cannot prove alone
A single observation, image or meter reading cannot confirm the complete failure pathway. Use this concept to form better questions, compare alternatives and decide which safe observation would be most informative next.
Safety and professional boundary
Wet, icy or steep roof drainage components require professional access.
Primary references for this topic family
These references ground the general building-science or safety context. They do not diagnose a specific house, replace local requirements or certify a repair.