Lifted Condensation Level Lcl Calculator
Calculate lifted condensation level lcl with our free science calculator. Uses standard scientific formulas with unit conversions and explanations.
Reviewed by Daniel Agrici, Founder & Lead Developer
Formula
T_LCL = 1/(1/(Td-56) + ln(T/Td)/800) + 56
Where T_LCL is LCL temperature in Kelvin, T is surface temp in Kelvin, Td is dew point in Kelvin. P_LCL = P*(T_LCL/T)^3.5. Height via hypsometric equation.
Worked Examples
Example 1: Summer Thunderstorm
Problem:Surface 30 C, dew point 20 C, 1013.25 hPa. Find LCL.
Solution:Depression = 10 C, Espy = 1250 m Bolton: T_LCL = 289.1K = 16.0C P_LCL = 860 hPa, Height = 1408 m
Result:LCL: 1408 m AGL | 860 hPa
Example 2: Marine Fog Layer
Problem:Coastal 15 C, dew point 14 C, 1015 hPa.
Solution:Depression = 1 C, Espy = 125 m Very low LCL - fog/stratus imminent
Result:LCL: 120 m | Fog Likely
Frequently Asked Questions
What is the Lifted Condensation Level?
The Lifted Condensation Level (LCL) is the altitude at which an air parcel becomes saturated when lifted adiabatically from the surface representing the theoretical cloud base for convective clouds. As an unsaturated parcel rises it cools at the dry adiabatic lapse rate about 9.8 C per kilometer while dew point decreases more slowly at about 1.8 C per kilometer. The LCL occurs where these profiles intersect. It is fundamental in atmospheric thermodynamics and used extensively in weather forecasting for predicting thunderstorm development.
How is the LCL calculated using the Bolton method?
The Bolton 1980 method gives an accurate empirical formula: T_LCL = 1/(1/(Td-56) + ln(Tk/Tdk)/800) + 56 where Tk and Tdk are surface temperature and dew point in Kelvin. The LCL pressure is found using P_LCL = P*(T_LCL/Tk)^3.5 and height from the hypsometric equation z = (R*Tavg/g)*ln(P/P_LCL). This method is accurate to within about 50 meters for most atmospheric conditions and preferred over simpler approximations in professional meteorology.
How does the LCL relate to thunderstorm forecasting?
The LCL is critical for thunderstorm forecasting because it determines where convective clouds begin forming and affects severe weather potential. A low LCL below 1000 meters indicates moist boundary layer favorable for tornado development. High LCL above 2500 meters suggests dry subcloud layers where downdraft evaporation produces strong outflow winds. The LCL marks the base of updraft condensation and latent heat release. Forecasters compare LCL to the Level of Free Convection to assess storm development.
What is the difference between LCL and CCL?
The LCL is the height where a surface parcel saturates when mechanically lifted while the CCL (Convective Condensation Level) is where saturation occurs through surface heating and free convection. The CCL is found by following the mixing ratio line up until it intersects the environmental temperature. The CCL is typically higher than LCL because it requires surface warming to create buoyancy. LCL applies to forced lifting such as fronts while CCL applies to afternoon solar heating over flat terrain.
References
Reviewed by Daniel Agrici, Founder & Lead Developer · Editorial policy