By Julian Heicklen (Auth.)
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Ranges of data are shown for each date, and authors' uncertainty for a single measurement is shown as a double arrow. R* Ridley et al. (1974), aircraft 9-34° N, afternoon IX 73, and 65^75° N, polar low sun XI 73, chemiluminescence. Range of data is shown. SL Savage et al. (1974), aircraft 25-49° N, midday XI 73-V 74, chemiluminescence. ixHiii 10" Particle»/cm3 Fig. I'll. Semilog plots of estimated concentrations of the oxides of nitrogen versus altitude for an overhead sun. and Fontanella et al.