کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4454103 1620823 2015 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Numerical study of the effects of local atmospheric circulations on a pollution event over Beijing–Tianjin–Hebei, China
موضوعات مرتبط
علوم زیستی و بیوفناوری علوم محیط زیست علوم زیست محیطی (عمومی)
پیش نمایش صفحه اول مقاله
Numerical study of the effects of local atmospheric circulations on a pollution event over Beijing–Tianjin–Hebei, China
چکیده انگلیسی

Currently, the Chinese central government is considering plans to build a trilateral economic sphere in the Bohai Bay area, including Beijing, Tianjin and Hebei (BTH), where haze pollution frequently occurs. To achieve sustainable development, it is necessary to understand the physical mechanism of the haze pollution there. Therefore, the pollutant transport mechanisms of a haze event over the BTH region from 23 to 24 September 2011 were studied using the Weather Research and Forecasting model and the FLEXible-PARTicle dispersion model to understand the effects of the local atmospheric circulations and atmospheric boundary layer structure. Results suggested that the penetration by sea-breeze could strengthen the vertical dispersion by lifting up the planetary boundary layer height (PBLH) and carry the local pollutants to the downstream areas; in the early night, two elevated pollution layers (EPLs) may be generated over the mountain areas: the pollutants in the upper EPL at the altitude of 2–2.5 km were favored to disperse by long-range transport, while the lower EPL at the altitude of 1 km may serve as a reservoir, and the pollutants there could be transported downward and contribute to the surface air pollution. The intensity of the sea–land and mountain–valley breeze circulations played an important role in the vertical transport and distribution of pollutants. It was also found that the diurnal evolution of the PBLH is important for the vertical dispersion of the pollutants, which is strongly affected by the local atmospheric circulations and the distribution of urban areas.

The vertical cross section of the simulated tracer concentration field (ng/m3), (a) 1600 LST 24 September, (b) 2130 LST 24 September. The black arrows in (b) indicate the schematic transport paths of the tracer.Figure optionsDownload as PowerPoint slide

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Environmental Sciences - Volume 30, 1 April 2015, Pages 9–20
نویسندگان
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