Thunderstorms typically develop along cold fronts, where warm, moist air is forced to rise rapidly over cooler, denser air. This lift can lead to the formation of cumulonimbus clouds and precipitation. Additionally, thunderstorms can also occur along warm fronts, but they are generally less severe compared to those developed along cold fronts. Other factors, such as topography and instability in the atmosphere, can also influence thunderstorm development.
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