Lightning (nonfiction): Difference between revisions

From Gnomon Chronicles
Jump to navigation Jump to search
No edit summary
No edit summary
Line 5: Line 5:
The charged regions in the atmosphere temporarily equalize themselves through this discharge referred to as a strike if it hits an object on the ground, and a flash if it occurs within a cloud.
The charged regions in the atmosphere temporarily equalize themselves through this discharge referred to as a strike if it hits an object on the ground, and a flash if it occurs within a cloud.


Lightning causes [[light (nonfiction)]] in the form of plasma, and sound in the form of thunder.
Lightning causes [[light]] in the form of plasma, and sound in the form of thunder.


Lightning may be seen and not heard when it occurs at a distance too great for the sound to carry as far as the light from the strike or flash.
Lightning may be seen and not heard when it occurs at a distance too great for the sound to carry as far as the light from the strike or flash.

Revision as of 11:53, 4 June 2016

Lightning striking the Eiffel Tower, June 3, 1902, at 9:20 P.M. This is one of the earliest photographs of lightning in an urban setting.

Lightning is a sudden electrostatic discharge during an electrical storm between electrically charged regions of a cloud (called intra-cloud lightning or IC), between that cloud and another cloud (CC lightning), or between a cloud and the ground (CG lightning).

Description

The charged regions in the atmosphere temporarily equalize themselves through this discharge referred to as a strike if it hits an object on the ground, and a flash if it occurs within a cloud.

Lightning causes light in the form of plasma, and sound in the form of thunder.

Lightning may be seen and not heard when it occurs at a distance too great for the sound to carry as far as the light from the strike or flash.

Nonfiction cross-reference

Fiction cross-reference

External links