Vertical Profiles of Particle Number Size Distribution and Variation Characteristics at the Eastern Slope of the Tibetan Plateau

Author:

Shu Chenyang1,Zhu Langfeng2,Yang Yinshan3,Zhao Xingbing4,Jiang Xingwen4,Hu Hancheng5,Pu Dongyang2,Liu Mengqi2,Wu Hao2ORCID

Affiliation:

1. Plateau Atmospheres and Environment Key Laboratory of Sichuan Province & School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225, China

2. Key Laboratory of China Meteorological Administration Atmospheric Sounding, School of Electrical Engineering, Chengdu University of Information Technology, Chengdu 610225, China

3. Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China

4. Institute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072, China

5. College of Optoelectronic Engineering, Chengdu University of Information Technology, Chengdu 610225, China

Abstract

An unmanned aerial vehicle (UAV) observation platform obtained the first vertical profiles of particle number size distribution (PNSD) from 7 to 16 July 2022 on the eastern slope of the Tibetan Plateau (ESTP). The results were from two flanks at the Chuni (CN) and Tianquan (TQ) sites, which are alongside a mountain (Mt. Erlang). The observations revealed a significant negative correlation between the planetary boundary layer height (PBLH) and the particle number concentration (PNC), and the correlation coefficient was −0.19. During the morning, the rise in the PBLH at the CN and TQ sites caused decreases of 16.43% and 58.76%, respectively, in the PNC. Three distinct profile characteristics were classified: Type I, the explosive growth of fine particles with a size range of 130–272 nm under conditions of low humidity, strong wind shear, and northerly winds; Type II, the process of particles with a size range of 130–272 nm showing hygroscopic growth into larger particles (e.g., 226–272 nm) under high humidity conditions (RH > 85%), with a maximum vertical change rate of about −1653 # cm−3 km−1 for N130–272 and about 3098 # cm−3 km−1 for N272–570; and Type III, in which during the occurrence of a surface low-pressure center and an 850 hPa low-vortex circulation in the Sichuan Basin, polluting air masses originating from urban agglomeration were transported to the ESTP region, resulting in an observed increase in the PNC below 600 nm. Overall, this study sheds light on the various factors affecting the vertical profiles of PNSD in the ESTP region, including regional transport, meteorological conditions, and particle growth processes, helping us to further understand the various features of the aerosol and atmospheric physical character in this key region.

Funder

National Natural Science Foundation of China (NSFC) research project

Heavy Rain and Drought-Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province

Project of the Sichuan Department of Science and Technology

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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