Ball Lightning and Bead Lightning: Extreme Forms of Atmospheric Electricity

1984 ◽  
Vol 52 (8) ◽  
pp. 764-765
Author(s):  
James Dale Barry ◽  
Glenn M. Schmieg
Keyword(s):  
Atmospheric Electricity ◽  
Ball Lightning

Current problems in ball lightning science

1990 ◽  
Vol 160 (4) ◽  
pp. 95 ◽  
Author(s):  
Boris M. Smirnov
Keyword(s):  
Ball Lightning

Analysis of observational ball lightning by correlation methods

1994 ◽  
Vol 50 (5) ◽  
pp. 606-608 ◽  
Author(s):  
B M Smirnov ◽  
A Ju Strizhev
Keyword(s):  
Ball Lightning ◽  
Correlation Methods

Dust, Clouds, Rain Types, and Climatic Variations in Tropical North Africa

1982 ◽  
Vol 18 (1) ◽  
pp. 1-16 ◽  
Author(s):  
Jean Maley
Keyword(s):  
North Africa ◽  
Atmospheric Electricity ◽  
Thunderstorm Activity ◽  
Tropical Africa ◽  
Tropical Zone ◽  
Climatic Variations ◽  
Dust Clouds ◽  
Climatic Evolution ◽  
Cloud Thickness ◽  
Second Period

AbstractDust and processes of raindrop formation in the clouds play a very important role in the climatic evolution of tropical north Africa. Sedimentologic, stratigraphic, pedologic, geomorphologic, and palynologic data converge to show that a major environmental change occurred in tropical Africa about 7000 yr B.P. In the Sudanian and Sudano–Guinean zones (wet tropical zone), from 15,000 to 7000 yr B.P., rivers deposited mostly clay, while from 7000 to 4000 yr B.P. they deposited mostly sand. During the first period, pedogenesis was vertisolic (montmorillonite dominant), associated with pollen belonging mostly to vegetation typical of hydromorphic soils, while during the second period pedogenesis was of ferruginous type (kaolinite dominant) with pollen belonging mostly to vegetation typical of well-drained soils. The great change near 7000 yr B.P. is linked chiefly to a major hydrological change that appears related to a change in the size of raindrops: from fine rains associated with considerable atmospheric dust (raindrop diameter essentially less than 2 mm) to the second period associated with thunderstorm rains (raindrop diameter mostly greater than 2 mm). The size of raindrops is related particularly to cloud thickness and dust concentration in the troposphere. Thunderstorm activity is influenced also by fluctuations of the atmospheric electricity, modulated by the sun.

Sign in / Sign up

Export Citation Format

Share Document