K. Kita et al., ROCKET OBSERVATION OF ATOMIC OXYGEN AND NIGHT AIRGLOW - MEASUREMENT OF CONCENTRATION WITH AN IMPROVED RESONANCE FLUORESCENCE TECHNIQUE, Annales geophysicae, 14(2), 1996, pp. 227-237
An improved resonant fluorescence instrument for measuring atomic oxyg
en concentration was developed to avoid the Doppler effect and the aer
odynamic shock effect due to the supersonic motion of a rocket. The sh
ock effect is reduced by adopting a sharp wedge-shaped housing and by
scanning of the detector field of view to change the distance between
the scattering volume and the surface of the housing. The scanning ena
bles us to determine absolute values of atomic oxygen concentration fr
om relative variation of the scattered light signal due to the self-ab
sorption. The instrument was calibrated in the laboratory, and the num
erical simulation reproduced the calibration result. Using the instrum
ent, the altitude profile of atomic oxygen concentration was observed
by a rocket experiment at Uchinoura (31 degrees N) on 28 January 1992.
The data obtained from the rocket experiment were not perfectly free
from the shock effect, but errors due to the effect were reduced by th
e data analysis procedure. The observed maximum concentration was 3.8
x 10(11) cm(-3) at altitudes around 94 km. The systematic error is est
imated to be less than +/- 0.7 x 10(11) cm(-3) and the relative random
error is less than +/- 0.07 x 10(11) cm(-3) at the same altitudes. Th
e altitude profile of the OI 557.7-nm airglow was also observed in the
same rocket experiment. The maximum volume emission rate was found to
be 150 photons cm(-3) s(-1) at 94 km. The observed altitude profiles
are compared with the MSIS model and other in situ observations.