This paper gives the results of some preliminary measurements on the ul traviolet spectral energy distribution of direct solar radiation at Washington , D . C. Data are give n for wave l e ng~hs extending below 300 millimicrons for air masses approximating M = 1.4. T~e ne'y equipment and method employed in this work permit the rapid acquire ment of a prismatic ultraYlOlet sp ec~ral e nergy curve at sea level showing greater Fraunhofer struct ure than prevIOusly obtamed e ven at d esert and mountain stations.
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R. Stair (1951) studied this question.
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