Damp and mould are fundamentally about the relationship between surface temperature and the moisture in the air (see the Building Physics guide). Surface condensation forms where a surface is colder than the dew point of the room air; mould grows where the surface relative humidity stays high. A thermal camera maps surface temperature across a room — so it directly reveals the cold surfaces where these problems will occur. That's its role in damp work: locating the cold, not detecting the water.

Locating surfaces below the dew point

The core technique is quantitative: measure the room air's temperature and relative humidity (giving the dew point), then use the thermal camera to read surface temperatures across walls, corners, reveals and lintels. Wherever a surface sits at or below the dew point, condensation will form; wherever it sits within the mould-risk margin (surface RH above ~80%), mould can grow — even without visible water. The thermal image and the psychrometrics together produce a map of risk.

The evaporative-cooling signature of damp

There is a second, subtler way thermography helps with actual moisture: evaporation cools a surface. Where a material is genuinely wet — from a leak, penetrating damp or drying-out — water evaporating from it draws latent heat and leaves the surface cooler than the surrounding dry area. So a damp patch can show as a distinctly cool, often irregularly-shaped region. Its boundary frequently follows the spread of the moisture (a tide-line, a run-down from a leak) rather than the geometry of the construction, which is a clue to its nature.

The interpretation problem — three cold things

Here is the crucial limitation. Three different problems all produce cold areas on a thermal image, and the camera alone often can't separate them:

Three causes of a cold thermal area
CauseTypical patternHow we confirm it
Missing/poor insulationCold patch matching construction geometryStatic; ignores blower door
Air leakageCold fingers/fans from a gapBlooms under blower-door depressurisation; smoke trace
Evaporating moisture (damp)Irregular cool area following moisture spreadMoisture meter, humidity data, source survey

The combined damp survey

  1. Log room temperature and RH over a representative period to characterise the indoor air and derive the dew point.
  2. Thermal-image the affected surfaces to map cold spots and read surface temperatures.
  3. Calculate surface RH at the cold locations and compare surface temperature against the dew point — confirming condensation/mould risk with numbers.
  4. Use moisture meters (with the hygroscopic-salt caveat in mind) and, where needed, true moisture-content sampling to test for liquid moisture.
  5. Run a blower door if air leakage is suspected, to separate leakage from insulation and moisture.
  6. Survey the exterior for penetrating-damp sources (pointing, render, flashings, drainage).
  7. Only then write the diagnosis — which mechanism(s), where, and the targeted remedy.

This is the measured approach that distinguishes condensation from penetrating and rising damp — the subject of our 'condensation vs damp' article — and it is why a RetrofitIQ damp diagnosis rests on data from several instruments, not on a single dramatic thermal image.