Comprehensive wind correction for a Rayleigh Doppler lidar from atmospheric temperature and pressure influences and Mie contamination

Shangguan Ming-Jia^a), Xia Hai-Yun†^a),^b),^c), Dou Xian-Kang^a),^b), Wang Chong^a), Qiu Jia-Wei^a), Zhang Yun-Peng^a), Shu Zhi-Feng^a),^b), Xue Xiang-Hui^a),^b)

The RBS calculated with the Tenti S6 model at 1013 hPa and 288 K (black dots). The red line represents the superposition of a central Gaussian line (dashed blue line) and two shifted Gaussian lines (dashed grey line) according to the Witschas’s model.