Abstract
THE (0,1) band of the (1Δg−3σg−) system of oxygen was first observed from the ground in the twilight airglow in 1958 (ref. 1). This band, at 1.58µ, was subsequently observed often in the evening twilight, but never in the morning twilight.
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References
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EVANS, W., LLEWELLYN, E. & VALLANCE JONES, A. Balloon-borne Observations of Brightness Variations in the (0,0) Band of the (1Δg−3σg−) System of Oxygen in the Day and Twilight Airglow. Nature 213, 352–353 (1967). https://doi.org/10.1038/213352a0
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DOI: https://doi.org/10.1038/213352a0
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