Reverse humidity limit
For each selected surface, the tool calculates the approximate room RH that would correspond to 80% surface RH and to saturation. This turns “is 55% RH okay?” into a surface-specific answer.
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Compare several rooms at once instead of judging one humidity number. Calculate dew point, estimated or measured surface RH, condensation margin, the maximum room RH each surface can tolerate, and the outdoor-temperature breakpoint where that surface is modeled to enter the high-RH or condensation zone.
Use readings from a hygrometer. Surface temperature is optional: if you leave it blank, the tool estimates it from outdoor temperature and the selected construction preset.
| Date | Worst room | Highest dew point | Highest surface RH | Score |
|---|
A single calculator can tell you the dew point. The harder question is whether your problem comes from high indoor moisture, an unusually cold surface, or both — and which room is actually the priority.
For each selected surface, the tool calculates the approximate room RH that would correspond to 80% surface RH and to saturation. This turns “is 55% RH okay?” into a surface-specific answer.
Each room is classified as mainly moisture-driven, cold-surface-driven, mixed, or lower concern from the values you entered. It is a prioritization aid, not a defect diagnosis.
For preset surfaces, the tool estimates the outdoor temperature at which today’s indoor conditions would push that surface to about 80% RH or to saturation. This makes a coming cold spell testable instead of generic.
Save snapshots locally and compare the worst room, highest dew point and surface RH over time. Repeated measurements are more useful than a single morning reading.
Start with indoor temperature, RH, outside temperature and a window preset.
Compare a cool basement with the warmer rooms above instead of relying on RH alone.
Compare evening and morning snapshots to see whether dew point actually rose.
Save a post-shower snapshot, then another after ventilation to compare the drying response.
EPA guidance says indoor relative humidity should be kept below 60% and ideally around 30–50% where possible. It also emphasizes fixing the moisture source and drying wet materials quickly. WHO guidance likewise focuses on preventing persistent dampness and microbial growth rather than treating one humidity percentage as a complete diagnosis.
Because condensation depends on the coldest surface, not only room RH. If the surface falls to the room dew point, saturation can occur there. Enter the window or measured surface temperature to see the margin directly.
They answer different questions. RH depends strongly on air temperature; dew point is a better indicator of the actual vapor level. For condensation, compare dew point with the coldest surface temperature.
There is no universal number for every window and weather condition. The lab calculates a surface-specific RH limit from your indoor temperature, outside temperature and selected or measured surface.
For preset window and wall types, the lab estimates the outdoor-temperature breakpoint at which your current indoor temperature and RH would push the modeled interior surface to about 80% RH, and separately to saturation. Treat it as a planning estimate because real edges, frames and thermal bridges can be colder.
Cooler air can show higher RH even with a similar vapor level. Compare dew points upstairs and downstairs; a much higher basement dew point suggests a larger moisture load, while a similar dew point points more strongly toward temperature.
No. It can identify conditions that deserve closer moisture investigation. It cannot inspect materials, determine duration of dampness, identify growth, or provide a health assessment.
Use it for comparisons. Real edges, frames, thermal bridges, curtains, air movement and installation details can make local surfaces colder. A careful measured surface temperature is better when the result matters.
What glazing estimates can and cannot tell you, and where the coldest point may be.
Separate cool-air RH from a genuinely higher moisture load.
Use repeated morning/evening readings instead of one overnight percentage.
Focus on the drying response after a shower rather than only the peak.