Restoration Lab · Free tool

Glaser method condensation calculator

Build a wall from inside to outside and check whether moisture will condense inside it for the indoor and outdoor conditions you enter.

Check a wall assembly for condensation inside the wall with the Glaser method. List the layers from inside to outside; the tool compares the vapor pressure at each layer with the saturation pressure there.

Inside air
Outside air
Layers, inside → outside
Condensation risk at between fiberglass batt and osb sheathing. Vapor reaching that point is above what the air can hold at its temperature (22.5°F). Add a vapor retarder on the warm side, or exterior insulation to keep that layer warmer.
InsideOutside (x = vapor resistance, sd)— saturation— actual vapor pressure
PointTemp °FSaturation kPaVapor kPa
Inside surface67.42.291.00
Between gypsum board and fiberglass batt66.42.210.97
Between fiberglass batt and osb sheathing22.50.390.94
Between osb sheathing and housewrap20.80.360.26
Outside face of housewrap20.80.360.24
Assembly R-14.4 (U = 0.40 W/m²K), total sd 2.46 m. Steady-state screening per the Glaser method; it ignores moisture storage, rain and air leaks, which often matter more. Use hygrothermal modeling (WUFI) for design decisions.

How the Glaser method works

The method treats the wall as a stack of layers. Each layer’s thermal resistance sets the temperature at its faces, and each layer’s vapor resistance (sd = μ × thickness) sets how fast vapor pressure falls through it. Where the actual vapor pressure would rise above the saturation pressure at that temperature, condensation is predicted.

Worked example

A 2×4 wall with drywall, 3.5 in fiberglass batts, 7/16 in OSB and housewrap, with 70°F / 40% RH inside and 20°F outside, predicts condensation on the back of the OSB. The OSB is cold and resists vapor far more than the drywall and batts in front of it. Add a vapor retarder on the warm side, or move insulation to the outside, and the risk clears.

Why restorers use it

It explains moisture found inside walls with no plumbing or roof leak: cold-weather condensation on sheathing. It also checks a rebuild before the walls close, for example whether adding exterior foam or a poly layer moves the wet spot.

Frequently asked

What is the Glaser method?

A steady-state calculation (used in standards such as ISO 13788) that compares vapor pressure with saturation pressure through each layer of a building assembly to predict interstitial condensation.

What are the limits of the Glaser method?

It ignores moisture stored in materials, liquid water movement, rain, solar heating and air leakage, and it assumes steady conditions. It is a screening tool; use hygrothermal modeling such as WUFI for design decisions.

What does sd value mean?

sd is the equivalent air-layer thickness in meters: a layer’s vapor resistance factor μ times its thickness. A higher sd means a tighter vapor retarder; polyethylene sheet is around 15 m, drywall well under 0.1 m.

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This knowledge, built into the software

RestoredOS runs the whole job on the same field knowledge behind these tools — drying logs, moisture mapping, scope, and billing.

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