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| Titel |
Mesoscale modeling study of the interactions between aerosols and PBL meteorology during a haze episode in Jing–Jin–Ji (China) and its nearby surrounding region – Part 1: Aerosol distributions and meteorological features |
| VerfasserIn |
H. Wang, M. Xue, X. Y. Zhang, H. L. Liu, C. H. Zhou, S. C. Tan, H. Z. Che, B. Chen, T. Li |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1680-7316
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| Digitales Dokument |
URL |
| Erschienen |
In: Atmospheric Chemistry and Physics ; 15, no. 6 ; Nr. 15, no. 6 (2015-03-23), S.3257-3275 |
| Datensatznummer |
250119571
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| Publikation (Nr.) |
 copernicus.org/acp-15-3257-2015.pdf |
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| Zusammenfassung |
| The urbanized region ofJing(Beijing)-Jin(Tianjin)-Ji (alias of Hebei province) and its nearby surrounding
region (3JNS) is
becoming China's most polluted area by haze, exceeding even the Yangtze and
Pearl river deltas. Aside from pollutant emission, the meteorology of the
planetary boundary layer (PBL) is the most important factor affecting haze
pollution. Focusing on July 2008, the aerosol optical properties and PBL
meteorology features closely related to haze formation were simulated in the
3JNS region using an online atmospheric chemical transport model. The
relationship between regional PBL meteorology, PM2.5, and haze is
discussed. Model results accurately simulated the aerosol optical depth
(AOD), single scattering albedo (SSA) and asymmetry parameter (ASY),
validated by comparison with observations from the MODerate Resolution
Imaging Spectroradiometer (MODIS), the China Aerosol Remote Sensing NETwork
(CARSNET) and the Aerosol Robotic NETwork (AERONET). Modeled PBL wind speeds
showed reasonable agreement with those from the National Centers for
Environmental Prediction (NCEP) Reanalysis 2. A monthly mean AOD value as
high as 1.2 was found from both model and observations, with a daily mean
larger than 2.0 during haze episodes in the 3JNS region. Modeled and observed
SSA values of 0.90–0.96 and ASY values of 0.72–0.74 demonstrated the high
scattering characteristic of summer aerosols in this region. PBL wind speeds
from modeled and NCEP data both showed a reversing trend of PM2.5
variation, illustrating the importance of the "PBL window shadow" in haze
formation. Turbulence diffusion and PBL height had opposite phases to surface
PM2.5, indicating that lower PBL height and weaker PBL turbulence
diffusion are essential to haze formation. It is noted that homogeneous air
pressure does not occur at the surface, but at an 850–950 hPa height during
the haze episode. The momentum transmitting downward of the cold air from
above the PBL to the low PBL and surface lead to an increase in surface wind
speeds and haze dispersal. |
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