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Warm-cloud seeding with spray or hygroscopic particles often dissipates small clouds but often initiates or increases rainfall from clouds that exceed 4000 ft in depth; seeding with dry ice or silver iodide in supercooled clouds; results of warm-cloud seedings in tropical clouds; new model of convective cloud fields to determine approach of individual clouds to rainstage; effects of warm and of supercooled cloud seeding on this model.
Warm-cloud seeding with spray or hygroscopic particles often dissipates small clouds but often initiates or increases rainfall from clouds that exceed 4000 ft in depth; seeding with dry ice or silver iodide in supercooled clouds; results of warm-cloud seedings in tropical clouds; new model of convective cloud fields to determine approach of individual clouds to rainstage; effects of warm and of supercooled cloud seeding on this model.
Seeding of clouds in tropical climates
ASCE -- Proc (J Irrigation Drainage Div)
Howell, W.E. (Autor:in)
1960
23 pages
Aufsatz (Zeitschrift)
Englisch
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