The overnight storms (and this is pretty common for nighttime storms and some during the day as well) were what we call "elevated thunderstorms." Basically, we had a very strong temperature inversion in place, in which the temperature rises with height rather than cooling. It was about 45° F at the surface during last night's storms, but 57° F at just 4,000 feet up! That inversion creates a stable layer in the atmosphere at the low levels and basically acts like a lid at 4,000 feet above us.
When lightning discharges under that lid, the sound of the thunder is trapped close to the ground. Since the sound can't escape UP ↑, it bounces around between the ground and the stable layer above (the lid), amplifying the noise. It's like setting off firecrackers in grandma's pressure cooker!
Erik Proseus
MWN Meteorologist
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