A thermographic inspection uses an infrared camera to map the apparent surface temperature of a building or an asset, so that anomalies — a cold patch of missing insulation, a warm patch of trapped roof moisture, an overheating switchgear connection — become visible as temperature differences. Flown from a drone, it covers a whole roof or a substation yard in one pass, without anyone climbing anything.

One correction up front, because it heads off most disappointed clients. A thermal camera does not see through walls. It sees the outside surface of the wall, and everything it tells you about what is behind that surface is inferred from the pattern of heat on the face of it. That inference is often very good — but it is an inference, and it needs verifying.

What a thermal camera actually measures

Every object above absolute zero emits infrared radiation, and emits more as it gets hotter. A thermal camera collects that radiation and renders it as an image where each pixel carries an apparent temperature. The useful signal is the contrast between neighbouring areas, not any single absolute number.

“Apparent” is doing real work there. What the camera reports depends on emissivity — how efficiently a surface radiates heat compared with a perfect emitter. Most building materials are good emitters: render, brick, concrete, timber, painted steel, membrane roofing, roof tiles. They read honestly.

Shiny surfaces are the problem. Bare galvanised steel, polished aluminium, foil facings and glass are poor emitters and good reflectors, so much of what comes back is reflected radiation from the sky, the sun or nearby structures rather than the surface itself. That is why a bare metal roof can read absurdly cold on a clear night, and why an unshielded busbar can read low while running hot. Those surfaces need a different technique, or an honest note that they cannot be read.

The other limit: thermal is a locator. It tells your consultant where to look, not what to conclude.

Where aerial thermal imaging inspection earns its keep

Building envelope and insulation performance

Building thermal imaging is the classic application. Given a temperature difference across the wall or ceiling — heating on in winter, a hot day loading the fabric in summer — insulation defects show up as patterns, and the pattern is the clue.

Missing or slumped batts appear as regular voids between studs or joists. Thermal bridging shows as continuous lines tracing the structure: steel framing, lintels, balcony slab edges, uninsulated floor junctions. Air leakage shows as plumes spreading from a gap, following the draught rather than the framing, and displaced insulation in a roof cavity shows as a gradient running back from the eaves. From the air you get the roof plane and the upper storeys — the parts that matter most for heat loss and are hardest to reach from a ladder.

Flat roof moisture ingress

This is the one worth understanding properly, because nothing else finds it as quickly. Water and wet insulation hold far more heat than dry insulation. Through the day the sun loads the whole roof. After sunset the roof radiates that heat back to the sky and cools. Dry areas, holding little energy, cool quickly. Saturated areas release their heat slowly, so for a few hours after dark they sit measurably warmer than the roof around them — appearing as irregular, blotchy warm areas that follow the shape of the wetted insulation, not the shape of the roof structure.

That shape distinction is the diagnosis. Straight lines and repeating patterns are usually structure or fixings. Amoeba-shaped warm areas pooling around a penetration, a lap or a drain are the finding.

So these surveys run after sunset, once the differential has built, following a day with decent solar gain and on a clear, dry, still night. The roof also has to suit the method: it needs absorbent insulation in the build-up, and a ballasted or gravelled roof masks the signal. Not every roof is a candidate, and we would rather say so before flying than after.

Electrical infrastructure and switchgear

Thermal imaging electrical testing works on a simple principle: a bad connection has resistance, resistance under load makes heat, and heat is visible long before failure. Loose or corroded terminations, unbalanced phases, overloaded conductors and failing joints all run hotter than their healthy neighbours. From the air, that suits anything awkward or unsafe to get near — pole-top hardware, overhead spans, substation yards, rooftop plant and outdoor transformer banks. The comparison that matters is usually phase-to-phase or unit-to-unit under similar load: one of three identical things running noticeably warmer than the other two is the finding.

Two caveats. Equipment must be under meaningful load at capture or a fault will not show. And enclosed switchgear read from outside gives you the cabinet, not the connection inside it — that is a job for a licensed electrician with the panel open.

Solar arrays

Thermal is standard practice for PV, because cell-level faults are otherwise invisible: bypassed strings, hot cells, failing junction boxes and shading damage each have a distinct signature, and an aerial pass covers a large array far faster than a handheld walk. Our dedicated piece on drone solar panel inspection covers it properly.

General asset condition

Thermal is a quick screen wherever energy escapes or accumulates where it shouldn’t: cool-room envelopes, insulated pipework and tank lagging, bypassing HVAC plant, hot spots in stockpiles.

Conditions that make or break a thermographic inspection

More thermal surveys are ruined by conditions than by equipment:

  • Temperature differential. You need a meaningful difference across the element inspected. No differential, no image. For envelopes that means a decent gap between inside and outside; for roof moisture, solar loading followed by night cooling.
  • Time of day. Roof moisture surveys run after sunset; envelope surveys often pre-dawn or early evening. Midday is the worst time for anything involving a roof, because direct sun swamps the differential.
  • Recent solar loading. For roof moisture you want it. For a wall survey you often don’t — a wall that has been in sun all afternoon is still releasing that heat and masking what sits behind it. Several hours of shade first is the rule.
  • Rain. A wet surface evaporates and cools unevenly, producing convincing-looking anomalies that mean nothing. Roofs need a dry period first — a full day is a reasonable minimum, longer after heavy rain.
  • Wind and cloud. Moving air strips heat from surfaces and flattens the differences you came to measure; heavy cloud slows the night cooling a roof survey depends on. Light wind and clear sky read cleanest, and sustained wind is a flight-safety limit anyway.

Melbourne being Melbourne, we book thermal work with a reschedule window built in.

Where our work ends

We capture and deliver the thermal imagery, with anomalies located, mapped against a visual reference of the same area, and supplied alongside the capture conditions — date, time, ambient temperature, wind, cloud, time since rainfall, camera settings and emissivity assumptions. Those conditions are what make it defensible later.

We do not diagnose. A qualified building consultant, licensed electrician or roofing contractor interprets the imagery, verifies the findings and specifies the fix. That division keeps each side inside its own competence, and it is why consultants engage us rather than treat us as a competitor.

Two things to be clear about. Formal thermographic certification levels exist in the industry, and anyone commissioning a report for compliance, warranty or insurance purposes should ask their interpreting professional what level they hold. And verifying a thermal anomaly almost always requires physical investigation — a moisture meter reading, a core sample, an opened panel, a lifted section. Thermal narrows the search area dramatically. It does not close it.

Frequently asked questions

Can a thermal camera see through walls?

No. A thermal camera detects infrared radiation emitted from a surface and renders its apparent temperature. It cannot see through walls, roofs, glass or water. It shows how heat behind a surface affects the face of it — often enough to locate missing insulation, a wet area or a hot connection, but that is inference, not x-ray vision.

When is the best time to do a thermographic roof inspection?

For flat roof moisture, a couple of hours after sunset, following a sunny day, on a dry, clear, still night. The roof absorbs heat during the day and then cools; wet insulation holds its heat and stays visibly warmer. Rain the previous day, strong wind or heavy cloud will all compromise the result.

What does emissivity mean in a thermal imaging inspection?

Emissivity describes how efficiently a surface radiates infrared energy. Most building materials — brick, render, concrete, membrane, painted metal — have high emissivity and read accurately. Bare metal, foil and glass have low emissivity and reflect surrounding radiation instead, so they can read wildly wrong and should be flagged as unreadable.

Can drone thermal imaging find a roof leak?

It can locate trapped moisture in the roof build-up — which is where the water ended up, not necessarily where it got in. The entry point is often elsewhere. Thermal narrows the search to a defined area; a roofing contractor then confirms it with a moisture meter or an invasive test and identifies the defect.

Do you provide a thermographic report?

We provide the imagery, the anomaly mapping and a full record of capture conditions and methodology. We do not issue condition assessments, electrical test certificates or repair specifications — those come from your building consultant, licensed electrician or roofing contractor, who interprets the data and signs off on the conclusion.