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The far ultraviolet vehicle glow of the S3‐4 satellite
Author(s) -
Conway R. R.,
Meier R. R.,
Strobel D. F.,
Huffman R. E.
Publication year - 1987
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl014i006p00628
Subject(s) - airglow , excited state , altitude (triangle) , daytime , atmospheric sciences , satellite , atomic physics , ultraviolet , atmosphere (unit) , physics , meteorology , optics , astronomy , geometry , mathematics
Nadir‐viewing far ultraviolet observations obtained on the S3‐4 satellite show that during the daytime the N 2 Lyman‐Birge ‐Hopfield (LBH) emission exhibits a change in vibrational distribution and becomes substantially brighter than predicted from photoelectron theory when the satellite is near perigee. At night, the intensity depends on altitude and no emission is detected when the vehicle is above 230 km. The altitude variation of the signal is proportional to the cube of the N 2 density or the product of the square of the N 2 density and the O density. We conclude that there is an LBH emission which is excited by the interaction of the vehicle with the ambient atmosphere, and that it is this emission which was previously interpreted as nightglow. The vibrational distribution is sharply peaked at v′ = 0. The altitude variation of the emission suggests a three stage excitation process in which N 2 is adsorbed, collisionally excited, and finally electronically excited and desorbed by ambient N 2 collisions, but physically reasonable reaction rates fail to account for the observed intensities.