Abstract
On 13 November 1946, Vincent Schaefer scattered dry ice pellets into the top of a supercooled stratiform cloud over Pittsfield, Massachusetts. Within minutes the seeded portion of the cloud was transformed into a mass of ice crystals (New York Times 1946; Lampbright 1970). But more than the cloud was transformed! Physicists, chemists, and engineers were attracted by the prospect of benefits to be realized from cloud seeding and by the romance of in situ cloud and aerosol research. Cloud physics quickly emerged as a recognized specialty in meteorology and became much more quantitative and laboratory oriented. Laboratories devoted to the study of clouds sprang up in several nations. Clouds themselves became subjects of experimentation. More than ever before, meteorology became a multidisciplinary science.
Every occurrence in nature is preceded by other occurrences which are its causes, and succeeded by others which are its effects. The human mind is not satisfied with observing and studying any natural occurrence alone, but takes pleasure in connecting every natural fact with what has gone before it, and with what is to come after it.
(John Tyndall 1872)
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Braham, R.R. (1996). Formation of Rain: A Historical Perspective. In: Fleming, J.R. (eds) Historical Essays on Meteorology 1919–1995. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-940033-84-6_7
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