Articles | Volume 18, issue 21
https://doi.org/10.5194/acp-18-15687-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-15687-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
01 Nov 2018
Research article |
| 01 Nov 2018
| 01 Nov 2018
Particle number size distribution and new particle formation under the influence of biomass burning at a high altitude background site at Mt. Yulong (3410 m), China
Dongjie Shang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Beijing Innovation Center for Engineering Sciences and Advanced
Technology, Peking University, 100871, Beijing, China
Jing Zheng
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Yanhong Qin
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Zhuofei Du
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Mengren Li
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Jingyao Fang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Jianfei Peng
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Yusheng Wu
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
Sihua Lu
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing, 100871, China
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22 citations as recorded by crossref.
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- High frequency of new particle formation events driven by summer monsoon in the central Tibetan Plateau, China L. Tang et al. 10.5194/acp-23-4343-2023
- Unexpected High Absorption of Atmospheric Aerosols Over a Western Tibetan Plateau Site in Summer L. Zhang et al. 10.1029/2020JD033286
- Particle number size distribution and new particle formation in Xiamen, the coastal city of Southeast China in wintertime J. Wang et al. 10.1016/j.scitotenv.2022.154208
- Atmospheric particle number size distribution and size-dependent formation rate and growth rate of neutral and charged new particles at a coastal site of eastern China X. Huang et al. 10.1016/j.atmosenv.2021.118899
- Thermo-Optical and Particle Number Size Distribution Characteristics of Smoldering Smoke from Biomass Burning F. Wang et al. 10.3390/app9235259
- Measurement report: Strong light absorption induced by aged biomass burning black carbon over the southeastern Tibetan Plateau in pre-monsoon season T. Tan et al. 10.5194/acp-21-8499-2021
- Impacts of the aerosol mixing state and new particle formation on CCN in summer at the summit of Mount Tai (1534m) in Central East China Z. Wu et al. 10.1016/j.scitotenv.2024.170622
- New particle formation and its CCN enhancement in the Yangtze River Delta under the control of continental and marine air masses X. Fang et al. 10.1016/j.atmosenv.2021.118400
- New particle formation in the tropical free troposphere during CAMP2Ex: statistics and impact of emission sources, convective activity, and synoptic conditions Q. Xiao et al. 10.5194/acp-23-9853-2023
- New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al. 10.1029/2018JD029356
- Historically understanding the spatial distributions of particle surface area concentrations over China estimated using a non-parametric machine learning method Y. Qiu et al. 10.1016/j.scitotenv.2022.153849
- Mixing state of black carbon at different atmospheres in north and southwest China G. Zhao et al. 10.5194/acp-22-10861-2022
- Vigorous New Particle Formation Above Polluted Boundary Layer in the North China Plain S. Lai et al. 10.1029/2022GL100301
- Case study evaluation of size-resolved molecular composition and phase state of carbonaceous particles in wildfire influenced smoke from the Pacific Northwest G. Vandergrift et al. 10.1039/D3EA00058C
- Secondary Formation of Submicron and Supermicron Organic and Inorganic Aerosols in a Highly Polluted Urban Area Y. Zheng et al. 10.1029/2022JD037865
- Impact of aerosol–radiation interaction on new particle formation G. Zhao et al. 10.5194/acp-21-9995-2021
- Particle number size distributions and formation and growth rates of different new particle formation types of a megacity in China L. Dai et al. 10.1016/j.jes.2022.07.029
- Regional organic matter and mineral dust are the main components of atmospheric aerosols over the Nam Co station on the central Tibetan Plateau in summer H. Zhang et al. 10.3389/fenvs.2022.1055673
- Parameterization of the ambient aerosol refractive index with source appointed chemical compositions G. Zhao et al. 10.1016/j.scitotenv.2022.156573
- New Particle Formation Occurrence in the Urban Atmosphere of Beijing During 2013–2020 D. Shang et al. 10.1029/2022JD038334
- Characteristics of new particle formation events in a mountain semi-rural location in India J. Victor et al. 10.1016/j.atmosenv.2024.120414
22 citations as recorded by crossref.
- Atmospheric aerosol size distribution impacts radiative effects over the Himalayas via modulating aerosol single-scattering albedo P. Tian et al. 10.1038/s41612-023-00368-5
- High frequency of new particle formation events driven by summer monsoon in the central Tibetan Plateau, China L. Tang et al. 10.5194/acp-23-4343-2023
- Unexpected High Absorption of Atmospheric Aerosols Over a Western Tibetan Plateau Site in Summer L. Zhang et al. 10.1029/2020JD033286
- Particle number size distribution and new particle formation in Xiamen, the coastal city of Southeast China in wintertime J. Wang et al. 10.1016/j.scitotenv.2022.154208
- Atmospheric particle number size distribution and size-dependent formation rate and growth rate of neutral and charged new particles at a coastal site of eastern China X. Huang et al. 10.1016/j.atmosenv.2021.118899
- Thermo-Optical and Particle Number Size Distribution Characteristics of Smoldering Smoke from Biomass Burning F. Wang et al. 10.3390/app9235259
- Measurement report: Strong light absorption induced by aged biomass burning black carbon over the southeastern Tibetan Plateau in pre-monsoon season T. Tan et al. 10.5194/acp-21-8499-2021
- Impacts of the aerosol mixing state and new particle formation on CCN in summer at the summit of Mount Tai (1534m) in Central East China Z. Wu et al. 10.1016/j.scitotenv.2024.170622
- New particle formation and its CCN enhancement in the Yangtze River Delta under the control of continental and marine air masses X. Fang et al. 10.1016/j.atmosenv.2021.118400
- New particle formation in the tropical free troposphere during CAMP2Ex: statistics and impact of emission sources, convective activity, and synoptic conditions Q. Xiao et al. 10.5194/acp-23-9853-2023
- New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al. 10.1029/2018JD029356
- Historically understanding the spatial distributions of particle surface area concentrations over China estimated using a non-parametric machine learning method Y. Qiu et al. 10.1016/j.scitotenv.2022.153849
- Mixing state of black carbon at different atmospheres in north and southwest China G. Zhao et al. 10.5194/acp-22-10861-2022
- Vigorous New Particle Formation Above Polluted Boundary Layer in the North China Plain S. Lai et al. 10.1029/2022GL100301
- Case study evaluation of size-resolved molecular composition and phase state of carbonaceous particles in wildfire influenced smoke from the Pacific Northwest G. Vandergrift et al. 10.1039/D3EA00058C
- Secondary Formation of Submicron and Supermicron Organic and Inorganic Aerosols in a Highly Polluted Urban Area Y. Zheng et al. 10.1029/2022JD037865
- Impact of aerosol–radiation interaction on new particle formation G. Zhao et al. 10.5194/acp-21-9995-2021
- Particle number size distributions and formation and growth rates of different new particle formation types of a megacity in China L. Dai et al. 10.1016/j.jes.2022.07.029
- Regional organic matter and mineral dust are the main components of atmospheric aerosols over the Nam Co station on the central Tibetan Plateau in summer H. Zhang et al. 10.3389/fenvs.2022.1055673
- Parameterization of the ambient aerosol refractive index with source appointed chemical compositions G. Zhao et al. 10.1016/j.scitotenv.2022.156573
- New Particle Formation Occurrence in the Urban Atmosphere of Beijing During 2013–2020 D. Shang et al. 10.1029/2022JD038334
- Characteristics of new particle formation events in a mountain semi-rural location in India J. Victor et al. 10.1016/j.atmosenv.2024.120414
Latest update: 26 Apr 2024
Short summary
Biomass burning (BB) activities have a great impact on the particle number size distribution in the upper troposphere of the Tibetan Plateau (TP), which could affect regional and global climate. We found that the cloud condensation nuclei concentration was 2–8 times higher during BB influenced periods than during clean periods on the TP. An unexpectedly low new particle formation frequency was found in clean atmosphere on the TP, due to low concentrations of anthropogenic precursors, i.e., SO2.
Biomass burning (BB) activities have a great impact on the particle number size distribution in...
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