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Thunder

From Wikipedia, the free encyclopedia
For other uses, see Thunder (disambiguation). Not to be confused with lightning.
Rain
Typical sound of rain with thunder
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Thunder is the sound caused by lightning.[1][2][3] Depending upon the distance from and nature of the lightning, it can range from a long, low rumble to a sudden, loud crack. The sudden increase in temperature and hence pressure caused by the lightning produces rapid expansion of the air in the path of a lightning bolt.[4] In turn, this expansion of air creates a sonic shock wave, often referred to as a "thunderclap" or "peal of thunder". The scientific study of thunder is known as brontology and the irrational fear (phobia) of thunder is called brontophobia.

Etymology

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The d in Modern English thunder (from earlier Old English þunor) is epenthetic, and is now found as well in Modern Dutch donder (cf. Middle Dutch donre; also Old Norse þorr, Old Frisian þuner, Old High German donar, all ultimately descended from Proto-Germanic *þunraz). In Latin the term was tonare "to thunder". The name of the Nordic god Thor comes from the Old Norse word for thunder.[5]

The shared Proto-Indo-European root is *tón-r̥ or *tar-, also found in Gaulish Taranis.[6]

Cause

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The cause of thunder has been the subject of centuries of speculation and scientific inquiry.[7] Early thinking was that it was made by deities, but the ancient Greek philosophers attributed it to natural causes, such as wind striking clouds (Anaximander, Aristotle) and movement of air within clouds (Democritus).[8] The Roman philosopher Lucretius held it was from the sound of hail colliding within clouds.[8] By the mid-19th century, the accepted theory was that lightning produced a vacuum and that the collapse of that vacuum produced what is known as thunder.[7]

Scientists have agreed since the 20th century that thunder must begin with a shock wave in the air due to the sudden thermal expansion of the plasma in the lightning channel.[9][8] 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 20,400 K (20,100 °C; 36,300 °F).[10] 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,[11] similar in principle to the shock wave formed by an explosion, or at the front of a supersonic aircraft. Near the source, the sound pressure level of thunder is usually 165 to 180 dB, but can exceed 200 dB in some cases.[12]

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.[13][9] Other causes have also been proposed, relying on electrodynamic effects of the enormous current acting on the plasma in the bolt of lightning.[14]

Consequences

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The shock wave in thunder is sufficient to cause property damage[7] and injury, such as internal contusion, to individuals nearby.[15] Thunder can rupture the eardrums of people nearby, leading to permanently impaired hearing.[7] Even if not, it can lead to temporary deafness.[7]

A thunder originating from a Positive Cloud-to-Ground lightning, known in short as +CG, producing such a loud blow like a Bomb, as loud as 135-180 decibels, is mainly responsible for the above listed bad consequences. This lightning is, however, quite rare and makes up only less than or equal to 5% of a Thunderstorm, and occurs only sometimes. This loud noise occurs due to a Large mass of air being heated and blown up all the way from the Anvil, the peak of the Cumulonimbus cloud, to the ground, along the path of the lightning. The lightning's electricity can go upto 3-4 Mega Amperes (300,000-400,000 Amps)

Types

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Vavrek et al. (n.d.) reported that the sounds of thunder fall into categories based on loudness, duration, and pitch.[7] Claps are loud sounds lasting 0.2 to 2 seconds and containing higher pitches. Peals are sounds changing in loudness and pitch. Rolls are irregular mixtures of loudness and pitches. Rumbles are less loud, last for longer (up to more than 30 seconds), and are of low pitch.[16]

Inversion thunder results when lightning strikes occur between the cloud and ground during a temperature inversion. The resulting thunder sounds have significantly greater acoustic energy than those produced from the same distance in non-inversion conditions. In a temperature inversion, the air near the ground is cooler than the air higher up. Inversions often happen when warm, moist air passes above a cold front. Within a temperature inversion, sound energy is prevented from dispersing vertically as it would in non-inversion conditions, and is thus concentrated in the near-ground layer.[17]

Cloud-to-ground lightning (CG) typically consists of two or more return strokes, from ground to cloud. Later return strokes have greater acoustic energy than the first.[18]

Perception

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Thundercracks
Sample of sharp cracking sounds of thunder heard immediately after nearby lightning strikes
Crack of thunder
A crack of thunder during the sound of falling rain
Thunder boom
A thunder boom
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The most noticeable aspect of lightning and thunder is that the lightning is seen before the thunder is heard. This is a consequence of the speed of light being much greater than the speed of sound. The speed of sound in dry air is approximately 343 m/s (1,130 ft/s) or 1,236 km/h (768 mph) at 20 °C (68 °F; 293 K).[19]

This translates to approximately 3 s/km (4.8 s/mi); saying "one thousand and one... one thousand and two..." is a useful method of counting the seconds from the perception of a given lightning flash to the perception of its thunder (which can be used to gauge the proximity of lightning for the sake of safety). To estimate the distance from the lightning strike, divide the counted seconds by five for miles,[20] or three for kilometers.

A very bright flash of lightning and an almost simultaneous sharp "crack" of thunder, a thundercrack, therefore indicates that the lightning strike was very near.

Close-in lightning has been described first as a clicking or cloth-tearing sound, then a cannon shot sound or loud crack/snap, followed by continuous rumbling.[7] The early sounds are from the leader parts of lightning, then the near parts of the return stroke, then the distant parts of the return stroke.[7]

See also

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References

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  1. ^ "Severe Weather 101: Lightning Basics". nssl.noaa.gov. Retrieved October 23, 2019.
  2. ^ "Thunder Facts". factsjustforkids.com. Retrieved October 23, 2019.
  3. ^ "The Sound of Thunder". weather.gov. Retrieved October 23, 2019.
  4. ^ "What Causes Lightning and Thunder?". NOAA. 2022.
  5. ^ "thunder". Oxford English Dictionary (2 ed.). Oxford, England: Oxford University Press. 1989.
  6. ^ Matasovic, Ranko. Etymological Dictionary of Proto Celtic. Leiden, The Netherlands: Brill. 2009. p. 384. ISBN 978-90-04-17336-1
  7. ^ a b c d e f g h Vavrek, R. J.; Kithil, R.; Holle, R. L.; Allsopp, J.; Cooper, M. A. (17 July 2006) [4 April 2006]. "Section 6.1.8: The Science of Thunder". National Lightning Safety Institute. Archived from the original on 17 July 2006. Retrieved 11 June 2022.
  8. ^ a b c Heidorn, K. C. (1999). Thunder: Voice of the heavens. Retrieved from http://www.islandnet.com/~see/weather/elements/thunder1.htm
  9. ^ a b Rakov, Vladimir A.; Uman, Martin A. (2007). Lightning: Physics and Effects. Cambridge, England: Cambridge University Press. p. 378. ISBN 978-0-521-03541-5.,
  10. ^ Cooray, Vernon (2003). The lightning flash. London: Institution of Electrical Engineers. pp. 163–164. ISBN 978-0-85296-780-5.
  11. ^ "Thunder". Encyclopædia Britannica. Archived from the original on 2008-06-07. Retrieved 2008-09-12.
  12. ^ "Ultimate Sound Pressure Level Decibel Table". Retrieved 2020-12-13.
  13. ^ MacGorman, Donald R.; Rust, W. David (1998). The Electrical Nature of Storms. Oxford University Press. pp. 102–104. ISBN 978-0195073379. Archived from the original on 2014-06-28. Retrieved 2012-09-06.
  14. ^ P Graneau (1989). "The cause of thunder". J. Phys. D: Appl. Phys. 22 (8): 1083–1094. Bibcode:1989JPhD...22.1083G. doi:10.1088/0022-3727/22/8/012. S2CID 250836715.
  15. ^ Fish, Raymond M (2021). "Thermal and mechanical shock wave injury". In Nabours, Robert E (ed.). Electrical injuries: engineering, medical, and legal aspects. Tucson, AZ: Lawyers & Judges Publishing. p. 220. ISBN 978-1-930056-71-8.
  16. ^ "Thunder Facts". Fast Facts for Kids. 2022.
  17. ^ Dean A. Pollet and Micheal M. Kordich (2013-04-08). "User's guide for the Sound Intensity Prediction System (SIPS) as installed at the Naval Explosive Ordnance Disposal Technology Division (Naveodtechdiv)" (PDF). Systems Department February 2000. dtic.mil. Archived from the original on April 8, 2013.
  18. ^ "Lightning Types". NOAA National Severe Storms Laboratory. 2022.
  19. ^ Handbook of Chemistry and Physics, 72nd edition, special student edition. Boca Raton: The Chemical Rubber Co. 1991. p. 14.36. ISBN 978-0-8493-0486-6.
  20. ^ "Understanding Lightning: Thunder". National Weather Service. 2022.
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