Cloud base height, also known as cloud altitude, is the lowest level in the atmosphere where water vapor condenses to form visible cloud droplets. It's a crucial parameter in meteorology, aviation, and weather forecasting. The cloud base height marks the point where the air temperature cools to its dew point, initiating cloud formation.
The simplified formula for estimating cloud base height is:
\[H = (T - T_d) \times 125\]Where:
Let's calculate the cloud base height with:
This diagram illustrates the concept of cloud base height. The brown line represents the ground, the blue area is the atmosphere, and the white shape represents the cloud base. The dashed line indicates the altitude where the air temperature has cooled to the dew point, forming the cloud base at 1,250 meters above ground level.
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