Cloud Base Calculator helps you calculate the expected height of cloud base using atmospheric temperature and dew point data.
Learn how to use the Cloud Base Calculator and understand the atmospheric principles behind cloud formation
This calculator uses the Lifted Condensation Level (LCL) method to estimate cloud base height. The LCL is the theoretical height at which unsaturated air, when lifted, becomes saturated and condensation begins, forming clouds.
The calculation uses the following formula:
LCL Height = T + (LCL Factor × (T - Td))
Where T is the surface temperature and Td is the surface dew point. The LCL factor varies based on the temperature difference between the surface temperature and dew point:
This calculator is useful for pilots, meteorologists, and outdoor enthusiasts to understand when and where clouds might form based on current atmospheric conditions. The cloud base height information can help predict visibility conditions and potential turbulence in the lower atmosphere.
This is a simplified model and does not account for other atmospheric factors that can influence actual cloud base height, such as wind shear, atmospheric pressure variations with altitude, or the presence of atmospheric inversions. For more precise calculations, consult meteorological textbooks or advanced atmospheric science resources.