Arid Zone Research ›› 2025, Vol. 42 ›› Issue (11): 2117-2126.doi: 10.13866/j.azr.2025.11.14

• Ecology and Environment • Previous Articles     Next Articles

Airborne observation of the vertical distribution of atmospheric aerosols over the Qinghai-Xizang Plateau

ZHANG Yuxin1(), ZHANG Boyue2(), HOU Yonghui2, KANG Xiaoyan1   

  1. 1. Meteorological Disaster Prevention Technology Center in Qinghai Province, Xining 810000, Qinghai, China
    2. Qinghai Weather Modification Center, Xining 810000, Qinghai, China
  • Received:2025-04-07 Revised:2025-05-31 Online:2025-11-15 Published:2025-12-13
  • Contact: ZHANG Boyue E-mail:nuistzyx@126.com;rybzhk@163.com

Abstract:

To analyze the vertical variations of particle size distribution and atmospheric particulate concentrations in the middle and lower atmosphere of the Qinghai-Xizang Plateau and clarify the characteristics of the background aerosol spectra, this study utilized the aircraft-borne observational data from five flights in 2020 to analyze the size distribution and number concentration of atmospheric aerosols in the northeastern part of the Qinghai-Xizang Plateau. (1) The scattered cloud systems in the research area moved from west to east, with the cloud top height ranging from 8000 to 10000 m. The backward trajectories demonstrated that the altitude range of 6000-7000 m was primarily affected by the surrounding environmental transmission. The high-altitude aerosol particles were associated with long-distance atmospheric transport, and they originated from the edge of the Qinghai-Xizang Plateau. (2) Aerosols in the middle and lower atmospheric layers over the northeastern Qinghai-Xizang Plateau were predominantly small particles with an average effective diameter (re) of 0.68 μm and an average concentration (Na) of 102-103 cm-3. On average, Na and re reached 507.16 cm-3 and 0.40 μm, respectively, in the vertical profile, exhibiting a multi-peak structure. (3) The aerosols could be categorized into three modes, with Mode I having mean Na of 102 cm-3 and Mode II having mean Na of 101 cm-3. For Mode III, mean Na ranged 10-1-100 cm-3. Na decreased with increasing altitude. Na gradually decreased with decreasing temperature, indicating a significant positive correlation. As relative humidity increased, the aerosol spectral type remained stable, but the concentration gradually increased. (4) At vertical heights of 7000-8000 m, the relative dispersion of cloud droplet (ε) value was relatively high at approximately 0.4, suggesting that cloud droplet sizes vary more significantly at this altitude range. Linear fitting and power-law both indicated a negative correlation between ε and Na.

Key words: airborne observation, aerosols, vertical distribution, relative dispersion, Qinghai-Xizang Plateau