Thunder is the sound of the shockwave caused during a thunderstorm when lightning rapidly heats and expands the air in and directly around the lightning channel (bolt) into plasma, producing acoustic shock waves in the atmosphere indentified as thunder. It is said that the air is heated up to 30 000 °C (54 000 °F). This phenomenon happens at the same time (lightning strike/air expansion thunderclap), but we hear thunder after we see lightning due to the simple fact that light travels at a faster speed than sound. However, at a close enough distance to the actual lighting strike point, both sound and light can be heard/seen simultaneously. The exact mechanism is poorly understood.
The cause of thunder has been the subject of centuries of speculation and scientific enquiry. The first recorded theory is attributed to Aristotle in the third century BC, and an early speculation was that it was caused by the collision of clouds. Subsequently numerous other theories have been proposed. By the mid-19th century, the accepted theory was that lightning produced a vacuum along its path, and that thunder was caused by the subsequent motion of air rushing to fill the vacuum. Later in the 19th century it was believed that thunder was caused by an explosion of steam when water along the lightning channel was heated. Another theory was that gaseous materials were created by lightning and then exploded. In the 20th century a consensus evolved that thunder must begin with a shockwave in the air due to the sudden thermal expansion of the plasma in the lightning channel.
Experimental support for this theory came from spectroscopic temperature measuring up to 36000 Kelvin. Arc photography then proved that the plasma did not expand thermally in all directions, but preferentially at right angles to the electric current. According to Graneau, the mechanism for this is not yet completely understood in terms of magnetohydrodynamics.
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