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This paper gives data on the total amount of ozone above the Organ Mountain s at the White Sands Proving Ground in New Mexico from D ecember 16 to 19, 1947, and from January 6 to 8, 1948, as determined from solar ultraviolet measurements by a phototube and filter method. The measurements indicatf' ozone in the stratosphere in an amount equivalent to a Jayer about 0.19 centimeter in thickness at normal temperature and press ure for each of the two periods.
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R. Stair (1949) studied this question.
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