Calibrating relative-humidity sensors
Saturation vapour pressure climbs about 6 % per degree, so half a degree between sensor and reference costs more RH error than most whole budgets.
Relative humidity is the ratio of the actual water vapour pressure to the saturation vapour pressure at that temperature. The numerator is a property of the air; the denominator is a property of the thermometer reading. Saturation vapour pressure rises steeply with temperature — from 23.33 kPa at 20.0 °C to 24.07 kPa at 20.5 °C, a 3 % change for half a degree — so any temperature disagreement between the sensor and the reference turns straight into an RH disagreement, whatever the humidity generator is doing.
How much a half-degree costs
Hold the actual moisture content fixed and move only the sensor's temperature. The table below is that calculation run against the Magnus relation, for a sensor reading 0.5 °C warmer than the reference.
| Reference condition | Dew point | Sensor reads | Error | dRH/dT |
|---|---|---|---|---|
| 20 °C, 30 %rh | 1.89 °C | 29.09 %rh | −0.91 %rh | −1.86 %rh/°C |
| 20 °C, 50 %rh | 9.26 °C | 48.48 %rh | −1.52 %rh | −3.10 %rh/°C |
| 20 °C, 80 %rh | 16.44 °C | 77.57 %rh | −2.43 %rh | −4.95 %rh/°C |
| 25 °C, 50 %rh | 13.86 °C | 48.53 %rh | −1.47 %rh | −2.98 %rh/°C |
| 25 °C, 80 %rh | 21.31 °C | 77.65 %rh | −2.35 %rh | −4.77 %rh/°C |
Two things follow. The error is proportional to the humidity, so a chamber qualified comfortably at 50 %rh can fail at 80 %rh for no reason other than thermal lag. And at 2.43 %rh, a half-degree at the high end is already larger than the 1–2 %rh calibration uncertainty a good laboratory would quote — which means the thermal condition, not the reference hygrometer, is setting the result.
Methods, in order of achievable uncertainty
- Humidity generator (two-pressure or two-temperature): the reference method, generating a known RH from first principles. Best uncertainty, highest cost.
- Comparison in a humidity chamber against a chilled-mirror hygrometer: the usual laboratory approach. Around 1–2 %rh at k = 2 with a good reference and proper stabilisation.
- Saturated salt solutions in a sealed jar (LiCl ≈ 11 %, MgCl₂ ≈ 33 %, NaCl ≈ 75 %, K₂SO₄ ≈ 97 %): cheap, portable, and strongly temperature-dependent — the quoted RH of each salt shifts with temperature, so the jar needs its own thermometer. Typically 2–3 %rh.
- One-point field check against a hand-held reference: a verification, not a calibration. Useful for catching gross failure, not for a certificate.
Stabilisation is the measurement
A capacitive RH sensor responds to humidity in seconds but to temperature in minutes, and the mass of its housing and cable slows it further. If you step the chamber and read at ten minutes, you are recording the sensor's thermal lag rather than its calibration error. Allow the whole assembly — sensor, sheath, cable gland — to come to equilibrium, and demonstrate that it has by showing a flat trace rather than by assuming a settling time.
Read down rather than up where you can. A capacitive sensor that has been held at 80 %rh carries hysteresis for some time afterwards; approaching each point from the same direction at least makes the effect consistent, and approaching from both quantifies it.
What goes on the certificate
- The RH value and its uncertainty at each point — and the temperature at which that point was realised.
- The direction of approach, if hysteresis was not separately evaluated.
- The stabilisation criterion actually used, not a nominal one.
- As-found and as-left values where an adjustment was made, so drift history survives the adjustment.
Capacitive sensors drift with contamination and exposure rather than with time on a shelf, so the interval should come from as-found history in the environment of use. A sensor in a clean laboratory and the same model in a warehouse loading bay do not deserve the same interval.
Frequently asked questions
- What uncertainty is typical for humidity sensor calibration?
- Around 1–2 %rh at k = 2 in a good chamber against a chilled-mirror reference, and 2–3 %rh with saturated salt solutions or a lower-grade reference. If your thermal control is worse than about 0.2 °C, that term alone will exceed these figures at high humidity.
- Why does a small temperature error cause such a large RH error?
- Because relative humidity is measured against saturation, and saturation vapour pressure rises about 6 % per degree near room temperature — 23.33 kPa at 20.0 °C against 24.07 kPa at 20.5 °C. Change the temperature and you change the denominator of the ratio without touching the moisture in the air.
- Does the error get worse at high humidity?
- Yes, roughly in proportion to the RH. A 0.5 °C difference costs 0.91 %rh at 30 %rh, 1.52 %rh at 50 %rh and 2.43 %rh at 80 %rh, all at 20 °C. It is why chambers that qualify easily at mid-range fail at the top of their envelope.
- Can I calibrate humidity sensors with salt solutions?
- Yes, for 2–3 %rh work. Use sealed jars, give them hours not minutes to equilibrate, and measure the jar's temperature — each salt's nominal RH shifts with temperature, so an assumed 75 % for NaCl at an unmeasured temperature is a guess dressed as a reference.
- How often should humidity sensors be calibrated?
- Annually is common for capacitive sensors because they drift with contamination and exposure rather than age. Set the interval from as-found history in the actual environment: a sensor in a dusty or solvent-laden atmosphere will need it more often than the same model on a laboratory bench.
References
- [1]JCGM 100:2008 — Guide to the expression of uncertainty in measurement (GUM)
- [2]EURAMET cg-20: Calibration of Climatic Chambers
- [3]ISO/IEC 17025:2017 — General requirements for the competence of testing and calibration laboratories
General technical guidance written against the cited sources. It is not regulatory or legal advice and does not replace the applicable standard, guideline or a qualified reviewer's judgement.
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