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Since the 1940s, cloud seeding has been used to change the structure of clouds by dispersing substances into the air, potentially increasing or altering rainfall. [2] In spite of experiments dating back to at least the start of the 20th century, however, there is much controversy surrounding the efficacy of cloud seeding, and evidence that cloud seeding leads to increased precipitation on the ...
The cloudbuster was intended to be used in a way similar to a lightning rod: focusing it on a location in the sky and grounding it in some material that was presumed to absorb orgone—such as a body of water—would draw the orgone energy out of the atmosphere, causing the formation of clouds and rain.
This helps nature to form rain clouds, and it increases the potential amount of rainfall. [13] Fattening: Fattening of the rain clouds is done by scattering exothermic-hygroscopic chemicals to make droplets of water condense. [13] Attacking: Flying a plane through the heavy clouds accelerates the process of raindrop formation. [13]
High clouds having the traditional "mare's tail" appearance. These clouds are long, fibrous, and curved, with no tufts or curls at the ends. Cirrus uncinus (V-2) Filaments with up-turned hooks or curls. Cirrus spissatus (V-3) Dense and opaque or mostly opaque patches. Cirrus castellanus (V-4) A series of dense lumps, or "towers", connected by a ...
The next set of clouds are the rain-bearing nimbostratus clouds. [1] [20] [39] When cirrus clouds precede a cold front, squall line or multicellular thunderstorm, it is because they are blown off the anvil, and the next clouds to arrive are the cumulonimbus clouds. [39] Kelvin-Helmholtz waves indicate extreme wind shear at high levels. [20]