Thermal Survey Conditions: Temperature Differential (ΔT)

The temperature differential — why a valid thermal survey needs a cold day.

The most common reason a thermal survey produces nothing useful is that it was done in the wrong conditions. Thermography reveals defects by the temperature patterns they create on a surface — and those patterns only appear when there is enough heat flowing through the building. Without an adequate temperature difference, even a perfect camera sees a flat, featureless wall.

A thermal camera detects where a surface is warmer or cooler than its surroundings. For a building defect — missing insulation, a thermal bridge, air leakage — to show up, heat has to be flowing through the envelope, which only happens when it is warmer inside than out (or vice versa). The driving force for that heat flow is the temperature differential, ΔT, between inside and outside. No ΔT, no heat flow, no thermal pattern, no survey.

How much ΔT is enough?

There is no single magic number, but practical and standardised guidance converges:

Inside-to-outside temperature difference (ΔT)

ΔT (inside − outside)	Survey quality
< 5 °C	Inadequate — defects won't reliably show
5–10 °C	Marginal — only gross defects visible
10–15 °C	Good — most envelope defects show clearly
> 15 °C	Ideal — subtle thermal bridges and leakage visible

In practice this means UK building thermography is largely a winter activity — heating season, when the inside is warm and the outside is cold. A survey attempted on a mild spring afternoon, with only a couple of degrees of difference, will be a waste of time however good the camera.

Conditioning the building

It is not enough for the air to be warm at the moment of the survey — the structure needs to have been in a steady, heated state long enough for the temperature patterns to establish through the fabric. Best practice is to have the building heated to a stable internal temperature for several hours (often overnight) before the survey, and to maintain that ΔT throughout. Heavyweight masonry buildings, with their thermal mass and lag, need longer conditioning than lightweight timber-frame ones.

Weather, solar loading and timing

External surveys especially are sensitive to recent weather, because the sun, wind and rain all leave thermal fingerprints that can mask or mimic defects:

Solar loading — sunshine warms surfaces unevenly and stores heat in the fabric, which then re-radiates for hours; a sun-warmed wall can completely hide (or fake) a thermal pattern. External surveys are therefore best done before dawn or after dark, and on overcast days, to avoid solar effects.
Wind — convective cooling flattens surface temperature differences and disperses the warm air plumes that reveal leakage. Strong wind degrades a survey (and a co-located blower door test).
Rain and surface wetness — evaporative cooling of a wet surface masks the underlying thermal pattern; surfaces should be dry, with no recent rain.
Time of day — early morning (after a cold night, before the sun loads the fabric) is often ideal for external work; internal surveys are less time-sensitive but still need the ΔT and no solar gain through glazing onto the surveyed surfaces.

Internal vs external surveys

The two viewpoints reveal different things and are best used together:

Internal survey — looking at the inside surfaces of the warm envelope, defects appear as cold patches/streaks (heat is escaping, so the inside surface is cooler there). Internal surveys are generally more reliable for locating defects precisely, are unaffected by solar loading, and are essential for measuring surface temperatures against the dew point. They also pair with a blower door for air-leakage detection.
External survey — looking at the outside surfaces, defects show as warm patches (heat escaping warms the outer surface). Useful for whole-elevation overviews and access, but far more vulnerable to solar loading, reflections and surface wetness, so timing and interpretation are critical.

The standards

Building thermography is guided by standards including BS EN 13187 (thermographic detection of irregularities in building envelopes) and related guidance, which set out the required conditions — adequate temperature difference, stable conditioning, avoidance of solar and weather effects — and the survey methodology. A competent surveyor records the conditions (ΔT, weather, emissivity, time) in the report, so the results can be judged and trusted. A report that omits the conditions is hiding whether the survey was even valid.

Common questions from clients.

Can you do a thermal survey in summer?

Generally no, at least not the standard heat-loss survey — there usually isn't enough inside-to-outside temperature difference, and solar loading corrupts the images. Building thermography for heat loss, insulation defects and thermal bridges is a heating-season activity, ideally on cold, overcast days or before dawn. (Some specialised surveys, e.g. reverse-ΔT in hot climates, exist, but for UK heat-loss work, winter is the time.)

Why does my house need to be heated before the survey?

Because the defects show up as temperature patterns that take time to establish through the fabric. The building should be heated to a stable temperature for several hours (often overnight) so there's a steady heat flow through the envelope when we survey. Surveying a cold house, or one only just warmed up, won't reveal the patterns reliably — especially in heavyweight masonry with thermal lag.

Is an internal or external thermal survey better?

They show different things and are best combined. Internal surveys locate defects precisely, are immune to solar loading, let us measure surface temperatures against the dew point, and pair with a blower door for air-leakage detection. External surveys give whole-elevation overviews but are far more sensitive to sun, wind and surface wetness. We typically lead with internal and use external for context.