© Matthew Clark
Prairie, Iowa, United States of America
Latitude: 40° 45' 9'' N
Longitude: 95° 33' 53'' W
31 May 2009 2200 (Local Time)
Camera direction: towards E
Image P/S code: P.14.0
Image I.D.: 5073
This photograph shows a cloud-to-ground lightning discharge from a rather high-based evening thunderstorm over Iowa, USA.
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A lightning ground discharge (cloud-to-ground lightning) from a Cumulonimbus cloud strikes the high ground of the Peak at Hong Kong (China).
A trough of low pressure brought thundery showers to the coastal areas of Guangdong. By convention, when lightning occurs the cloud is classified as Cumulonimbus.
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The main features in this picture are the lightning ground discharges at 1 and 2 (cloud-to-ground lightning). The discharges appear to follow a tortuous path between cloud and ground and are commonly known as forked lightning. Smaller branches from the main discharge at 3, 4 and 5 dissipate into clear air. The discharge on the left of the picture, from cloud to air, appears not to strike the ground and is an air discharge.
When lightning occurs, the cloud is identified as Cumulonimbus. If it is not possible to determine whether the species is calvus or capillatus, as in this picture, by convention the coding is CL = 9.
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Lightning strikes to the ground, known as ground discharges, are seen from the lower part of this Cumulonimbus cloud. The cloud is specifically identified as Cumulonimbus capillatus incus by the fibrous top to the cloud and anvil (coding CL = 9). Other lightning activity is occurring within the thundercloud cloud (intra-cloud lightning), with some cloud discharges lighting up the interior. One lightning flash – an anvil crawler – originates from the upper portion of the cloud, beneath the anvil, and travels horizontally for some distance, generating several branches.
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Lightning electrical discharges often follow a tortuous course. Here one connects with the ground as a cloud-to-ground discharge while others travel horizontally for some distance within or beneath the cloud.
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