2016
DOI: 10.1109/tgrs.2016.2594828
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A Combined Rotational Raman–Rayleigh Lidar for Atmospheric Temperature Measurements Over 5–80 km With Self-Calibration

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Cited by 18 publications
(4 citation statements)
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“…The method of measuring the vertical distribution of the atmospheric temperature from the lidar signals of purely rotational spontaneous Raman spectra (SRS) of nitrogen and oxygen molecules has significant advantages over other remote methods of temperature measurement [1][2][3][4][5][6][7]. This method makes it possible to carry out actually direct temperature measurements from the population ratio of rotational levels with high accuracy and high space-time resolution [1].…”
Section: Introductionmentioning
confidence: 99%
“…The method of measuring the vertical distribution of the atmospheric temperature from the lidar signals of purely rotational spontaneous Raman spectra (SRS) of nitrogen and oxygen molecules has significant advantages over other remote methods of temperature measurement [1][2][3][4][5][6][7]. This method makes it possible to carry out actually direct temperature measurements from the population ratio of rotational levels with high accuracy and high space-time resolution [1].…”
Section: Introductionmentioning
confidence: 99%
“…At the Siberian Lidar Station (SLS), a lidar method for measuring the vertical distribution of atmospheric temperature based on the Raman scattering (RS) effect in the altitude range of 0÷40 km has been successfully developed for many years [1][2][3][4][5] . The lidar technology for remote temperature measurement is based on using the known temperature dependence of the intensity of spectral lines of rotational Raman scattering on nitrogen and oxygen molecules.…”
Section: Introductionmentioning
confidence: 99%
“…The simplest way to measure the vertical distribution profile of atmospheric temperature on lidar complexes is the Rayleigh scattering effect associated with the retrieval of the atmospheric molecular density profile and subsequent conversion to temperature, which is justified under the assumption of hydrostatic equilibrium of the atmosphere [1][2][3][4][5] . Despite the apparent technical simplicity of the method, weak dependence of the scattering coefficient on temperature imposes strict requirements on the permissible distortions of the lidar response shape.…”
Section: Introductionmentioning
confidence: 99%