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Weather

Cloud Base Calculator

Estimate the convective cloud base from the temperature/dewpoint spread.

Inputs

ft

Result

Cloud base (AGL)

4,000ft

Spread 10 °C × 400 ft

Cloud base (MSL)

Includes 500 ft field elevation

4,500ft

Temp / dewpoint spread

10°C

Cloud base ≈ 4,000 ft AGL (4,500 ft MSL), spread 10 °C

Formula

Ref
  • Spread = temperature − dewpoint [°C]
  • Base (ft AGL) ≈ spread × 400
  • Base (ft MSL) = base AGL + field elevation

Worked example

Ref

Surface temp 25 °C, dewpoint 15 °C, field elevation 500 ft.

  1. 1.Spread = 25 − 15 = 10 °C.
  2. 2.Base AGL ≈ 10 × 400 = 4,000 ft.
  3. 3.MSL = 4,000 + 500 = 4,500 ft.

Cloud base ≈ 4,000 ft AGL (4,500 ft MSL).

How it works

Ref

Rising air cools at the dry adiabatic rate while its dewpoint falls more slowly; they converge at about 2.5 °C per 1,000 ft, so every degree of temperature/dewpoint spread lifts the convective cloud base by roughly 400 ft. It estimates cumulus bases on a thermally active day, not layered stratus.

DGCA student tip

Exam

The 400 ft-per-degree rule (from the 2.5 °C/1000 ft convergence) is worth instant recall. A small spread means a low base and possible fog; a large spread means high, well-defined cumulus.

Common mistakes

Watch
  • Applying the rule to stratus/layer cloud — it is for convective cumulus.
  • Mixing temperature in °C with dewpoint in °F.
  • Forgetting to add field elevation when an MSL base is needed.