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The cause of thunder has been the subject of centuries of speculation and scientific inquiry. The first recorded theory is attributed to the Greek philosopher Aristotle in the fourth century BC, and an early speculation was that it was caused by the collision of clouds. Subsequently, numerous other theories were proposed. By the mid-19th century, the accepted theory was that lightning produced a vacuum.

In the 20th century a consensus evolved that thunder must begin with a shock wave in the air due to the sudden thermal expansion of the plasma in the lightning channel.<ref name="UmanVladimir A. Rakov2007">{{#invoke:citation/CS1|citation |CitationClass=book }}</ref> The temperature inside the lightning channel, measured by spectral analysis, varies during its 50 μs existence, rising sharply from an initial temperature of about 20,000 K to about 30,000 K, then dropping away gradually to about 10,000 K. The average is about {{safesubst:#invoke:convert|convert}}.<ref>{{#invoke:citation/CS1|citation |CitationClass=book }}</ref> This heating causes a rapid outward expansion, impacting the surrounding cooler air at a speed faster than sound would otherwise travel. The resultant outward-moving pulse is a shock wave,<ref name="britannica"></ref> similar in principle to the shock wave formed by an explosion, or at the front of a supersonic aircraft.

Experimental studies of simulated lightning have produced results largely consistent with this model, though there is continued debate about the precise physical mechanisms of the process.<ref>{{#invoke:citation/CS1|citation |CitationClass=book }}</ref><ref name="UmanVladimir A. Rakov2007"/> Other causes have also been proposed, relying on electrodynamic effects of the massive current acting on the plasma in the bolt of lightning.<ref>{{#invoke:Citation/CS1|citation |CitationClass=journal }}</ref> The shockwave in thunder is sufficient to cause injury, such as internal contusion, to individuals nearby.<ref>{{#invoke:citation/CS1|citation |CitationClass=book }}</ref>

Inversion thunder results when lightning strikes between cloud and ground occur during a temperature inversion. In such an inversion, the air near the ground is cooler than the higher air. The sound energy is prevented from dispersing vertically as it would in a non-inversion and is thus concentrated in the near-ground layer. Inversions often occur when warm moist air passes above a cold front; the resulting thunder sound is significantly louder than it would be if heard at the same distance in a non inversion condition.<ref>Dean A. Pollet and Micheal M. Kordich, User's guide for the Sound Intensity Prediction System (SIPS) as installed at the Naval Explosive Ordnance Disposal Technology Division (Naveodtechdiv). Systems Department February 2000. dtic.mil</ref>

Thunder is the sound produced by lightning.

Thunder sections
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Cause
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