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Christian Schöenbein identifies ozone in the laboratory
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Christian Schöenbein identifies ozone in the laboratory
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Auguste de la Rive and Jean-Charles de Marignac suggest ozone is a form of oxygen; confirmed by Thomas Andrews in 1856
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Auguste de la Rive and Jean-Charles de Marignac suggest ozone is a form of oxygen; confirmed by Thomas Andrews in 1856
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Andrei Houzeau finds ozone present in natural air
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Andrei Houzeau finds ozone present in natural air
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Jean-Louis Soret proves that ozone is O3
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Jean-Louis Soret proves that ozone is O3
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Marie Alfred Cornu measures solar spectrum and finds sharp cutoff in ultraviolet (UV) light
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Walter Hartley recognizes cutoff corresponds to UV absorption by ozone
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John William Strutt (Lord Rayleigh) shows absorption is not in lower atmosphere
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Charles Fabry makes first spectrometric measurements of "thickness" of ozone layer
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G.M.B. Dobson develops ozone spectrophotometer and begins regular measurements of ozone abundance (Arosa, Switzerland)
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Jean Cabannes and Jean Dufay show ozone is about 10 miles high
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Thomas Midgley synthesizes chlorofluorocarbons (CFC's)
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Sydney Chapman describes theory that explains existence of an ozone "layer"
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Ozonesonde (balloon) measurements establish the ozone concentration is maximum around 12 miles up
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David Bates and Marcel Nicolet propose catalytic (HOx) ozone destruction
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Catalytic destruction is necessary in order to explain ozone amounts
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Paul Crutzen discovers NOx catalytic cycle
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Dept of Transportation sponsors intensive program of research, The Climatic Impact Assessment Program (CIAP)
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Renewed expansion of CFC market
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CFC production ends in US and Europe
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Maximum CFC concentrations in stratosphere are reached
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CFC production ends world-wide