Physics – Geophysics
Scientific paper
Jun 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004eostr..85..249j&link_type=abstract
EOS Transactions, AGU, Volume 85, Issue 26, p. 249-253
Physics
Geophysics
Global Change: Geomorphology And Weathering (1824, 1886), History Of Geophysics: Hydrology, Hydrology: Geomorphology (1625)
Scientific paper
Lightning in the atmosphere is a transient, high current carrying electric discharge. It occurs when some region of the atmosphere reaches an electric charge sufficiently large so that the electric fields associated with the charge cause an electrical breakdown in the air. Lightning is produced in the cumulonimbus clouds; however, it can also occur in snowstorms and sandstorms. The analysis presented in this article demonstrates that there are many similarities between the celestial networks that are formed during a lighting event and the terrestrial channel networks associated with flowing surface waters in drainage basins. It begins with a preliminary analysis of the paths followed by the cloud-to-ground discharge of electric currents generated in the atmosphere during thunderstorms.
Jain Sharad K.
Singh Vijay P.
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