4.7 Article

Number size distribution of aerosols at Mt. Huang and Nanjing in the Yangtze River Delta, China: Effects of air masses and characteristics of new particle formation

期刊

ATMOSPHERIC RESEARCH
卷 150, 期 -, 页码 42-56

出版社

ELSEVIER SCIENCE INC
DOI: 10.1016/j.atmosres.2014.07.020

关键词

Aerosol; Number concentration; HYSPLIT; Air masses; New particle formation

资金

  1. National Natural Science Foundation of China [41275143, 41305135]
  2. Special Fund for Public Welfare Industrial (Meteorology) Research of China [GYHY201206011]
  3. Natural Science Foundation of the Higher Education Institutions of Jiangsu Province, China [12KJA170003]
  4. Jiangsu Province 333 Project
  5. Six Talent Peaks project
  6. Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD)

向作者/读者索取更多资源

Aerosol number spectra in the range of 10 nm-10 pm were observed at Mt Huang (Aug. 15-Sep. 15) and Nanjing (Oct 13-Nov. 15) by a wide-range particle spectrometer (WFS) in 2011. Based on the backward trajectories obtained using the HYSPLIT model, the transport pathways of observed air masses during the study periods were classified into the following four groups: maritime air mass, continental air mass, marine-continental mixed air mass and local air mass. The variations in the aerosol number spectrum and the new particle formation (NPF) events for various types of air masses were discussed, along with meteorological data The results showed that the average number concentration was 12,540 cm(-3) at Nanjing and only 2791 cm(-3) at Mt. Huang. The aerosol number concentration in Nanjing was 3-7 times higher than that in Mt Huang; the large discrepancy was in the range of 10-100 nm. Different types of air masses had different effects on number concentration distribution. The number concentration of aerosols was higher in marine air masses, continental air masses and continental-marine mixed air masses at 10-50 nm, 100-500 nm and 50-200 nm, respectively. Under the four types of air masses, the aerosol size spectra had bimodal distributions in Nanjing and unimodal distributions in Mt Huang (except under continental air masses: HT1). The effects of the diverse air masses on aerosol size segments of the concentration peak in Mt Huang were stronger than those in Nanjing. The local air masses were dominant at these two sites and accounted for 44% of the total air masses. However, the aerosol number concentration was the lowest in Mt Huang and the highest in Nanjing when local air masses were present The number concentrations for foreign air masses increased at Mt Huang and decreased at Nanjing. Different types of air masses had greater effects on the aerosol spectrum distribution at Mt Huang than at Nanjing. During the NPF events, the particle growth rates at Mt Huang (65-9.0 nmh(-1)) were faster than those at Nanjing (4.8-5.6 nm h(-1)). The relative humidity at Mt. Huang (36-65%) was higher than that at Nanjing (30-47%), but the wind speed trend was the opposite. The air masses during the NPF events were clean, i.e., they were mainly from over the ocean or districts with low ultrafine particle concentrations. (C) 2014 Elsevier B.V. All rights reserved.

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