Free convective clouds generally form at the altitude of the convective condensation level ( CCL ).
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Both condensation levels indicate the altitude ( or pressure ) where relative humidity reaches 100 %.
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Alternatively, the cloud base can be estimated from surface measurements of air temperature and humidity by calculating the lifted condensation level.
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Compare this to the Lifting Condensation Level ( LCL ) where the air is lifted and cooled without first increasing the surface temperature.
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In the lower troposphere, more moisture ( small dew point depression ) results in lower cloud bases and lifted condensation levels ( LCL ).
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An absence of sufficient condensation particles at and above the condensation level causes the rising air to become supersaturated and the formation of cloud tends to be inhibited.
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The droplets would normally evaporate below the condensation level, but strong updrafts buffer the falling droplets, and can keep them aloft much longer than they would otherwise.
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However, since the actual condensation level depends on the availability of condensation nuclei, clouds typically do not form until the relative humidity is somewhat above 100 %.
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With the help of these lines, parameters such as cloud condensation level, level of free convection, onset of cloud formation . etc . can be derived from the soundings.
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For non-convective cloud, the altitude at which condensation begins to happen is called the lifted condensation level ( LCL ), which roughly determines the height of the cloud base.
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