Relative Humidity from Dew or Frost Point
Calculate relative humidity from air temperature and a documented dew or frost point, with explicit liquid-water and ice saturation conventions.
Use this result well
- Inputs that matter
- Air temperature (°C), Dew/frost saturation point (°C), Sources and assumptions
- Output to expect
- Humidity from dew or frost point
- Check the units and required inputs before comparing results.
- Keep the assumptions with a copied result so you can reproduce the calculation later.
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Reference & details
How it works
Updated September 2026
How it works
Updated September 2026Humidity from dew or frost point
Calculate relative humidity from air temperature and a documented saturation point. Below the triple point, the entered point is interpreted as a frost point and the saturation reference is ice.
RH = 100 × es(saturation point) / es(air temperature).Updated: September 2026
Example Scenarios
Inspect the example and its input basis, then substitute your own documented measurements or matched cases.
→ 53.812916% relative humidity
Common Mistakes to Avoid
Common Mistakes to Avoid
Mixing observation and model inputs
Use the exact units, timestamp, level and measurement or model basis stated by the selected mode. A similar quantity from another instrument or product is not automatically interchangeable.
Treating an illustrative case as a measurement
Replace the example with your own sourced inputs. Retain missing values and method limits, and keep raw source data alongside a saved calculation.
FAQ
About Relative Humidity from Dew or Frost Point
Calculate relative humidity from air temperature and a documented saturation point. Below the triple point, the entered point is interpreted as a frost point and the saturation reference is ice.