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Scan ceilings, walls, floors and reveals with a locked span of about 8 to 10 °C around room temperature, looking for cool areas with irregular or trailing edges that do not follow studs and joists, and for warm plumes near hot-water and heating runs. Do it in dry room air (which strengthens evaporative cooling) and not in sunlight. Mark every anomaly, then pass a pinless moisture meter over it and a dry reference area; a raised reading confirms water. Confirm the wettest point with pins, trace toward the highest readings to find the source, and record everything before anyone opens a surface.
Why damp is visible
- Evaporative cooling: water leaving a damp surface cools it 1 to 4 °C below dry neighbors; stronger in dry air.
- Thermal mass: wet material warms and cools slowly, so after any temperature change it lags and shows contrast.
- Conduction: wet insulation conducts heat; the surface over it is cooler in winter.
- Hot leaks: a leaking hot pipe or heating loop warms the surface above it.
See can thermal imaging find water leaks.
Conditions and settings
- Room air dry rather than humid; run a dehumidifier for an hour if needed.
- A recent temperature change helps: image after the heating comes on, or after a cool night.
- No sun on the surface.
- For hot leaks, run the hot water or heating for 15 to 30 minutes first.
- Span locked at roughly ±4 to 5 °C around room temperature; ironbow or grayscale; emissivity 0.95.
Where to look
| Location | Likely source | Signature |
|---|---|---|
| Ceilings below bathrooms and roofs | Shower trays, waste pipes, roof and flashing leaks | Cool irregular patch, often larger than any stain; a trail along a joist |
| Window reveals and below sills | Failed seals, sill drainage | Cool area widening downward from the sill or corner |
| Base of external walls | Rising damp, bridged damp course, external ground levels | Cool band with a ragged upper edge |
| Walls behind kitchen and bathroom fittings | Plumbing joints, appliance hoses | Vertical cool trail from a fitting |
| Floors along pipe runs | Heating and hot-water leaks | Warm plume off the pipe line |
| Corners and behind furniture | Condensation | Cool corner geometry matching cold bridges; see why condensation forms |
| Chimney breasts | Flue condensation, failed flashing, hygroscopic salts | Cool patch on the breast, often mid-height |
Distinguishing damp from lookalikes
- Insulation gaps follow framing bays and have straight edges; see finding insulation gaps.
- Drafts feather from joints and change when doors open or fans run.
- Thermal bridges are linear at structural elements.
- Emissivity differences follow material or paint boundaries exactly.
- Damp has irregular, organic edges, sits below a plausible source, and reads high on a moisture meter.
Confirming and tracing
- Pass a pinless moisture meter over the anomaly and a dry reference of the same material; note both readings.
- Map the wet extent with the pinless meter on a grid; mark the edges.
- Take pin readings at the wettest point where marks are acceptable.
- Follow rising readings toward the source; water travels down and along, so the source is usually above or upstream of the highest reading.
- Use a borescope through a small hole to see the cavity if the source is hidden.
See pin vs pinless moisture meters and thermal camera vs borescope. After repair, re-image and re-meter to confirm drying. Cameras for moisture work need good sensitivity; see best thermal cameras for home inspection.
Recommended Tools
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Frequently Asked Questions
What does damp look like on a thermal camera?
Usually a cooler patch with an irregular, often rounded or trailing edge that does not follow the framing pattern, appearing below a likely source: a window, a roof junction, a bathroom above, a pipe run.
Can a thermal camera find a leak under a floor?
Hot water and heating leaks show as a warm plume through the floor surface. Cold-water leaks are harder; they may show as a cool area or only through a moisture meter reading on the surface.
Why must I use a moisture meter as well?
Because cool patches also come from missing insulation, thermal bridges, drafts and emissivity differences. The meter proves water is present and maps how far it extends.
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