Snowfall in the lake (cold air above warm water) is a common cause of converting a typical thunderstorm into a thunderstorm.
In these cases – more common by people who live in northwestern Europe or near the Great Lakes region of North America and similar environments – the air rises quickly when connected to relatively warm water surface temperatures.
Air Air Aloft (near the upper part of the Cumulus cloud), as well as the levels of sharp separation where the air temperature quickly cools down, creating favorable conditions for a storm with greater destructive potential.
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