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Cloud base calculator: estimate cloud height from the dew point

Estimate the height of the base of cumulus clouds from the temperature and dew point at the ground, the rule of thumb used by pilots and glider pilots.

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Results

Cloud base above the ground

4,101 ft

Typical base of fair-weather cumulus

Cloud base above sea level

4,101 ft

In meters
1,250 m
Temperature and dew point spread
18.0 °F

Why clouds have a flat base

On a sunny day, bubbles of warm air rise from the ground and cool as they expand. Their temperature falls by about 9.8 °C per kilometer (5.4 °F per 1,000 ft), the dry adiabatic lapse rate. Their dew point falls much more slowly, about 1.8 °C per kilometer. When the two meet, water vapor condenses and a cumulus cloud forms. Because all the bubbles start from similar air, they condense at almost the same height, which gives fair-weather cumulus their flat bases.

The rule of thumb

The gap between temperature and dew point closes by about 8 °C per kilometer, so:

  • Cloud base (m) ≈ 125 × (T − Td) with temperatures in °C
  • Cloud base (ft) ≈ 400 × (T − Td) with temperatures in °C
  • Cloud base (ft) ≈ 228 × (T − Td) with temperatures in °F, often rounded to 222 to 230

The result is the height above the ground. Add the station elevation to get the height above mean sea level.

Worked example

At an airport at sea level, the afternoon METAR reports a temperature of 25 °C (77 °F) and a dew point of 15 °C (59 °F):

  1. Spread = 25 − 15 = 10 °C (18 °F).
  2. Cloud base ≈ 10 × 125 = 1,250 m, or about 4,100 ft above the ground.
  3. At an airport at 1,000 ft, the same spread would put the base near 5,100 ft above sea level.

Typical results

Spread Approximate base
2 °C (4 °F) 250 m (800 ft): low clouds, possible mist
5 °C (9 °F) 625 m (2,000 ft)
10 °C (18 °F) 1,250 m (4,100 ft): typical summer cumulus
15 °C (27 °F) 1,875 m (6,200 ft)
20 °C (36 °F) 2,500 m (8,200 ft): dry air, high bases or no clouds

Who uses it

Glider and paraglider pilots estimate how high thermals will carry them. Private pilots check whether a VFR flight can stay below the clouds with the required clearance. Hikers and photographers use it to guess whether summits will be in the clouds.

Limits

The estimate assumes a well-mixed layer near the ground, which is true on sunny afternoons but not in the early morning, at night or over cool water. It does not apply to stratus, fog, high clouds or clouds lifted by fronts and mountains. Always check the official forecast and the reported ceiling before a flight.

Frequently asked questions

How do you estimate the cloud base?

Subtract the dew point from the temperature at the ground and multiply by about 400 ft per °C (about 222 ft per °F, or 125 m per °C). A spread of 18 °F gives a cumulus base near 4,000 ft above the ground.

Why does the rule work?

Rising air cools by about 9.8 °C per km while its dew point drops by only about 1.8 °C per km. The gap closes by about 8 °C per km, and clouds form where the two meet.

Does it work for all clouds?

It works best for fair-weather cumulus on sunny afternoons, when air near the ground is well mixed. It does not predict fog, stratus layers, high clouds or cloud bases set by fronts and sea breezes.

Is the result above ground or above sea level?

The formula gives the height above the station. Add the station elevation to get the height above mean sea level, as pilots use on charts and in METAR reports.

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Results are estimates provided for information purposes. They do not replace professional advice.