Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei, 230031, China
Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei, 230031, China
Department of Precision Machinery and Precision Instruments, University of Science and Technology of China, Hefei, 230026, China
Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China
Key Laboratory of Precision Scientific Instrumentation of Anhui Higher Education Institutes, University of Science and Technology of China, Hefei, 230026, China
College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
Jingkai Xue
School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei, 230026, China
Hongyu Wu
School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei, 230026, China
Xiangguang Ji
Institute of Physical Science and Information Technology, Anhui University, Hefei, 230601, China
Jinping Ou
Department of Health Promotion and Behavioral Sciences, School of Public Health, Anhui Medical University, Hefei, 230032, China
Qihou Hu
Key Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei, 230031, China
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Total article views: 509 (including HTML, PDF, and XML)
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We identified the contributions of ozone (O3) and nitrous acid (HONO) to the production rates of hydroxide (OH) in vertical space on the Tibetan Plateau (TP). A new insight was offered: the contributions of HONO and O3 to the production rates of OH on the TP are even greater than in lower-altitudes areas. This study enriches the understanding of vertical distribution of atmospheric components and explains the strong atmospheric oxidation capacity (AOC) on the TP.
We identified the contributions of ozone (O3) and nitrous acid (HONO) to the production rates of...