کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4440076 1311046 2011 13 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Impacts of aerosols on summertime tropospheric photolysis frequencies and photochemistry over Central Eastern China
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علم هواشناسی
پیش نمایش صفحه اول مقاله
Impacts of aerosols on summertime tropospheric photolysis frequencies and photochemistry over Central Eastern China
چکیده انگلیسی

Aerosols in the troposphere influence photolysis frequencies and hence the concentrations of chemical species. We used a three-dimensional regional chemical transport model (NAQPMS) coupled with an accurate radiative transfer model to examine the impacts of aerosols on summertime photochemistry in Central Eastern China (CEC) via changing photolysis frequencies. In addition to looking at changes in concentrations as previous studies have done, we examined the changes in ozone (O3) budgets and the uncertainties related to our estimations. The 1st–12th June 2006 was selected as the simulation period when high aerosol optical depth at 550 nm (AOD550) and O3 were found. A comparison of measurements showed that the model was capable of reproducing the spatial and temporal variations in photolysis frequencies, ultraviolet (UV) radiation, AOD550, cloud optical depth, O3 and other chemical constitutes in CEC. Aerosols have important impacts on atmospheric oxidation capacity in CEC. On a regional scale, aerosols decreased the average O3→O (1D) photolysis frequency by 53%, 37% and 21% in the lower, middle and upper troposphere in CEC. The uncertainties of these estimations were 37%, 25% and 14%, respectively. Mean OH concentrations decreased by 51%, 40% and 24% in layers below 1 km, 1–3 km and 3–10 km, with uncertainties of 39%, 28% and 9%, respectively. The changes in HO2 concentrations were smaller but significant. In contrast, NOx showed a significant increase at 0–1 km and 1–3 km in CEC, with magnitudes of 6% and 8%. The largest relative enhancement occurred in downwind regions below 1 km. Summertime boundary layer O3 (below 1 km and 1–3 km) was reduced by 5% with a maximum of 9% in highly polluted regions. The reduced ozone production (P (O3)) was responsible for this reduction below 3 km.


► A 3D chemical transport model was coupled with an accurate radiative transfer model.
► The siginificant impacts of aerosols on summertime photochemistry in Central China.
► Summertime boundary layer ozone reduced by 5% in polluted regions.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Atmospheric Environment - Volume 45, Issue 10, March 2011, Pages 1817–1829
نویسندگان
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