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Thunderstorms develop when a mass of warm, moist air is lifted to an elevation where it becomes warmer than its surroundings. The air then rises on its own, cooling as it does so, though staying warmer than its surroundings. As it cools the moisture in it condenses into clouds, which releases energy, slowing down the cooling of the air mass. This causes it to rise even faster. As ice crystals form in the upper reaches of the cloud rain starts falling. Ice crystals and water droplets collide, creating electrical charge differences that eventually lead to lightning.

Thunderstorms can form under a number of circumstances as long as there is sufficient instability and a lifting mechanism. This can include a cold front where cold air pushes into warm air, a dry line where dry air pushes into moist air, or less often a warm front where warm air pushes into cold air.

Thunderstorms can also form along land and sea breezes, from unstable air forced up mountain slopes, or even from slight fluctuations when conditions are particularly unstable

Instability occurs when an air parcel lifted to a certain elevation becomes warmer than its surroundings and thus continues to rise.

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