Where there is lightning, there is a thunderstorm. Thunderstorms indicate a lot of air movement, up, down, and laterally. If you are taking off from or landing at an airport anywhere near a thunderstorm, you can expect wind shear.
Thunderstorms can exist inside an air mass, along frontal boundaries, or out front of a cold front in a band of weather called a squall line. Squall line thunderstorms generally produce the most intense hazard to aircraft.
Development
Three things are required for thunderstorm formation:
Sufficient water vapor
Unstable lapse rate
Lifting Force
Thunderstorm Stages
Thunderstorms have a life cycle defined by three stages of development, which are cumulus, mature, and dissipating. The cumulus stage is dominated by a continuous updraft. In this stage, the thunderstorm develops from a small cumulus cloud into a towering cumulus cloud. Precipitation indicates the mature stage of the thunderstorm. Thunderstorms reach their greatest intensity during the mature stage. Finally, the thunderstorm dissipates. The dissipating stage is characterized predominately through downdrafts.