Hygrothermal analysis models the combined movement of heat ('thermo') and moisture ('hygro') through a construction over time, to predict whether moisture will accumulate within it and whether it can dry out again. It is how a designer demonstrates, in advance, that a wall, roof or floor build-up — particularly one with added insulation — won't quietly rot from the inside. There are two levels of method.
The Glaser method (BS EN ISO 13788)
The Glaser method is the classic, steady-state condensation-risk calculation, standardised in BS EN ISO 13788. For each month of the year it computes the temperature gradient and the vapour-pressure gradient through the build-up, finds whether and where the vapour pressure reaches saturation (the condensation plane), estimates how much condensate forms in the cold months, and checks whether it evaporates again in the warm months. If annual condensation exceeds annual drying — or if it lands on a moisture-sensitive material — the build-up fails the assessment.
The limitations of Glaser
- Steady-state and vapour-only: it considers diffusion alone, ignoring liquid (capillary) transport that can redistribute and dry moisture.
- No rain: it doesn't model wind-driven rain absorbed by the outer leaf — often the dominant moisture load on a solid wall.
- No sorption / moisture storage: it treats materials as not buffering moisture, whereas real hygroscopic materials store and release it.
- No solar drying or real weather: it uses simplified monthly averages, not the actual transient climate.
- No built-in moisture or air leakage: both significant in reality.
Because of these simplifications, Glaser can be misleading for moisture-sensitive, rain-exposed or capillary-active build-ups — sometimes flagging a safe vapour-open wall as risky, or (more dangerously) missing a rain-driven failure it simply doesn't model. That's where transient simulation comes in.
Transient hygrothermal simulation (WUFI)
WUFI (Wärme und Feuchte instationär — 'heat and moisture, transient') is the leading transient hygrothermal simulation tool. Rather than monthly averages, it models heat and moisture movement hour by hour over multiple years, using real climate data and validated material datasets that include liquid (capillary) transport and moisture storage. It accounts for the things Glaser ignores:
| Factor | Glaser (ISO 13788) | WUFI (transient) |
|---|---|---|
| Time basis | Steady-state, monthly | Transient, hourly over years |
| Liquid (capillary) transport | Ignored | Modelled |
| Moisture storage / sorption | Ignored | Modelled |
| Wind-driven rain | Ignored | Modelled (with exposure) |
| Solar gain & real climate | Simplified | Real hourly weather data |
| Best for | Simple screening; diffusion-dominated walls | Solid-wall IWI, heritage, rain-exposed, high-risk |
Interpreting the results
A hygrothermal assessment isn't just 'pass/fail'. The useful output is the trend in total moisture content of the assembly and of its sensitive components (e.g. embedded timber, the masonry behind IWI) over several simulated years. The questions are: does moisture reach a stable equilibrium, or keep climbing year on year (a slow failure)? Does any component exceed the moisture level at which decay or mould becomes likely? Does the wall dry over summer? Good practice judges results against recognised assessment criteria (such as those for timber moisture content and mould-growth risk), not against a single dew-point line.
When to use which
- Simple, diffusion-dominated, low-risk build-ups (e.g. a well-detailed new cold roof or a cavity wall): Glaser is usually sufficient.
- Solid-wall internal wall insulation, heritage and traditional buildings, highly rain-exposed elevations, moisture-sensitive materials, or anything where a wrong answer is costly: transient (WUFI) analysis.
- Either way: pair the calculation with realistic inputs (local climate and rain exposure, accurate material data, sensible airtightness assumptions) — a model is only as good as what you feed it.
