Practical guide and verification
Pressure belongs with the moist-air state
Humidity ratio, wet-bulb temperature, enthalpy and specific volume depend on station pressure. Use pressure appropriate to the site rather than assuming sea-level pressure when altitude is significant, and keep that pressure with any exported or copied state.
Use the mini plot to see relationships, not to replace the numeric result
The state marker and relative-humidity guide curves help show where the air lies relative to saturation. Read exact values from the calculated properties; the compact chart is an approximate visualization rather than a standards-certified psychrometric chart.
Dew point is the direct condensation comparison
For a surface-condensation check, compare the calculated dew point with the measured surface temperature. A surface below dew point can support condensation even when room relative humidity does not appear unusually high.
Different input pairs should resolve to one consistent state
Dry bulb plus RH, dry bulb plus dew point and other supported pairs describe the same moist-air state when measurements are consistent. Solving from an alternate measured pair is a useful cross-check when independent sensors are available.
Measurement uncertainty can dominate formula precision
Sensor calibration, air stratification, radiation, response time and pressure error can exceed the rounding shown by the browser. Keep instrument quality and sampling location in mind before interpreting small differences between two calculated states.