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A System to Create Stable Nanoparticle Aerosols from Nanopowders
Published on: July 26, 2016
Aerosol structure and vertical distribution in a multi-source dust region
Jie Zhang1, Qiang Zhang, Congguo Tang
1Key Laboratory of Meteorological Disaster, Ministry of Education and Jiangsu Province, Nanjing University of Information Science & Technology, Nanjing 210044, China. gs-zhangjie@163.com
Surface micro-pulse lidar observed aerosol vertical distribution in China. Aerosols were classified into three layers, influenced by atmospheric conditions and sources, with distinct extinction coefficient profiles.
Area of Science:
- Atmospheric Science
- Remote Sensing
- Environmental Monitoring
Background:
- Aerosols significantly impact climate and air quality.
- Understanding vertical aerosol distribution is crucial for atmospheric studies.
- Limited data exists on free troposphere aerosol profiles in western China.
Purpose of the Study:
- To investigate the vertical distribution of aerosols in the free troposphere over Zhangye, China.
- To analyze the sources and characteristics of different aerosol layers.
- To examine the relationship between aerosol distribution and atmospheric conditions.
Main Methods:
- Direct observation of aerosol vertical distribution using surface micro-pulse lidar (MPL4).
- Data collection at Zhangye Station (39.08° N, 100.27° E) during spring 2008.
- Analysis of aerosol layers, extinction coefficients, and diurnal variations.
Main Results:
- Aerosols were classified into upper (4.5-9 km), middle (2.5-4.5 km), and lower (<2.5 km) layers.
- Upper layer aerosols originated from external, high-altitude sources; middle and lower layers had mixed origins.
- Aerosol extinction coefficients varied with altitude and atmospheric stability, indicating aerosol mixing in the middle layer.
- Diurnal variation showed a single peak, higher in the afternoon, influenced by the atmospheric boundary layer.
Conclusions:
- Vertical aerosol distribution is layer-dependent, influenced by altitude, atmospheric conditions, and source regions.
- Aerosol mixing processes are significant in the middle atmospheric layer.
- Micro-pulse lidar is effective for characterizing free troposphere aerosol profiles.
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