In January 2016, a measurement campaign was carried out by the China Meteorological Administration, the Beijing Research Institute of Telemetry, and the Physics Department of the University of Naples “Federico II” in the Yulong Naxi Autonomous County (China) at 3200 m above sea level to evaluate the air quality in the high mountains with the lidar technique. Here we report on an interesting event that occurred on 16 January between 12.00 and 00.00 UTC, when a striking aerosol stratification was observed on the site. Aerosol transport events are studied starting from lidar characterization of different aerosol masses. From lidar signals at 355 and 532 nm, integrated on 30 min, the aerosol characterization is done in terms of aerosol depolarization ratio with a spatial resolution of 60 m and color ratio; these parameters allow for highlighting a phenomenon of aerosol transport from the Tibetan plateau planetary boundary layer and from northern India. The initial layer is composed of a mixture of aerosols characterized by average values of the aerosol depolarization ratio and the color ratio of (30 ± 2)% and (0.9 ± 0.2), respectively, indicating a large non-spherical aerosol composition. Then, the deposition of this aerosol load ensues, and aerosols with such features are progressively observed at lower altitudes.