Correction of temperature influence on the wind retrieval from a mobile Rayleigh Doppler lidar*
Zhao Ruo-Cana), Xia Hai-Yuna),b), Dou Xian-Kanga),b)†, Sun Dong-Songa),b), Han Yu-Lia), Shangguan Ming-Jiaa), Guo Jiea), Shu Zhi-Fenga),b)
       
Typical raw data from the temperature measurements. An accumulating time of 30 min is adopted and the spatial resolution changes from 200 m to 1 km above 43 km (see the dotted curve).