Laser observations of the ground-state hyperfine structure of sodium and of temperatures in the upper atmosphere
Laser observations of the ground-state hyperfine structure of sodium and of temperatures in the upper atmosphere
复制标题
钠基态超精细结构和高层大气温度的激光观测
作者:
A. J. Gibson;L. Thomas;S. K. Bhattachacharyya
The height distributions of sodium between about 80 and 100 km have been measured by several groups from observations of the resonance scattering of a tuned laser beam1–7. Furthermore, estimates of temperatures in this height range have been made4 by incorporating a sodium cell of known temperature in the receiver of the laser radar system. In all these measurements, the linewidths of the lasers employed have been comparable with, or greater than, that of the sodium D1 or D2 resonance line. The ground level of sodium atoms, 3s 2S1/2 consists of two hyperfine-structure components at −1.107 GHz and 0.664 GHz relative to the centroid8. Because of the corresponding hyperfine structure of the upper levels, 3p 2P1/2 for D1 and 3p 2P3/2 for D2, four components contribute to the D1 and six to the D2 complexes. Since the relative strengths and frequencies of the ten components are well known, the theoretical line shape can be computed9. For temperatures above about 6 K, blending of these components occurs and for temperatures below about 456 K the line profiles of both D1 and D2 complexes show two distinct peaks. In this letter preliminary measurements of the profile of the D2 line using a tunable narrow-band laser are presented and used to deduce the temperature near the peak of the sodium layer.