Abstract
The mid-day dayglow intensities arising from the fluorescence of solar ionizing radiation are calculated. The predicted overhead intensities above 120 km of the O +( 2 P– 2 D) lines at λλ7319–7330, the Meinel band system of N 2 +, the first negative system of N 2 +, the first negative system of O 2 +, the Hopfield emission system of O 2 + and the second negative system of O 2 + are respectively 500 R-1 kR, 9 kR, 600 R, 2 kR, 600 R and 400 R.
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