Guide

Why this window gets wet first

Window condensation is a surface-temperature problem and a moisture problem at the same time. Indoor vapor reaches the glass, frame edge or reveal; if that surface is cold enough, local RH rises toward saturation and droplets can form.

Three inputs matter most

Indoor temperature and RH determine dew point. Outdoor temperature affects how cold the inside surface becomes. Glazing and frame performance determine how much of that outdoor cold reaches the room-facing surface.

Try your window

Window condensation quick check

Use one current room reading. The model estimates the room-side surface from outdoor temperature and a glazing preset, then solves backwards for the cold-weather breakpoint.

°C
% RH
°C at roughly the same time
Simplified whole-surface estimate

Planning estimate only. Real glass edges, spacers, frames and reveals can be colder. For a measured coldest-surface override and saved history, use the full window preset.

How to read the quick check

ResultWhat it meansUseful next check
Surface RH below the caution bandThe modeled center surface still has moisture margin in this snapshot.Repeat during colder weather if condensation is seasonal.
Surface RH around or above 80%The selected preset surface is modeled as moisture-loaded even before saturation.Measure the actual glass edge/frame if possible and test a lower room RH.
Surface at or below dew pointCondensation is physically possible on the modeled surface under these air conditions.Check both indoor moisture sources and why the local surface is so cold.

Center glass is not always the coldest place

Edges, spacers, frames, reveals and thermal bridges can be colder than the center of the pane. Curtains and blinds can also reduce warm room air reaching the glass. That is why the Lab lets you override its glazing estimate with a measured cold-surface temperature.

If your measured coldest surface is 10°C and the room dew point is 12°C, the calculator flags a condensation condition even if the room RH number by itself does not look extreme.

At what outdoor temperature does the modeled window become risky?

The calculator now solves the preset window model backwards. With your current indoor temperature and RH held constant, it estimates the outdoor temperature where the selected interior surface would reach about 80% RH, and the colder breakpoint where it reaches saturation. This is useful for testing a coming cold snap, but it remains a model: real glass edges, frames and reveals may be colder than the preset surface.

What to compare

Test the same window under current RH and a lower target RH. Then compare a second room at the same outdoor temperature. This helps distinguish a whole-home moisture load from one unusually cold assembly.

Measurement protocol for one troublesome window

  1. Measure room temperature and RH away from the glass.
  2. Record outdoor temperature at the same time.
  3. If possible, measure the coldest accessible interior point: edge, frame or reveal, not only center glass.
  4. Repeat on a drier or colder day and save both snapshots.

The whole-home tool also reports the approximate room RH corresponding to 80% surface RH and saturation for the selected surface, so the result changes with both weather and construction.

Condensation is a moisture-control signal, not a diagnosis by itself. EPA guidance recommends moisture-source control, ventilation/air movement where appropriate and attention to cold surfaces; see the primary moisture guidance or EPA's mold and moisture guide.

Run the numbers for your room

Open the window preset