Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program

Ozone (O<sub>3</sub>) profiles recorded over Beijing from 1995 to 2005 by the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC) program were analyzed to provide a first climatology of tropospheric O<sub>3</sub> over Be...

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Main Authors: A. J. Ding, T. Wang, V. Thouret, J.-P. Cammas, P. Nédélec
Format: Article
Language:English
Published: Copernicus Publications 2008-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/1/2008/acp-8-1-2008.pdf
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author A. J. Ding
T. Wang
V. Thouret
J.-P. Cammas
P. Nédélec
author_facet A. J. Ding
T. Wang
V. Thouret
J.-P. Cammas
P. Nédélec
author_sort A. J. Ding
collection DOAJ
description Ozone (O<sub>3</sub>) profiles recorded over Beijing from 1995 to 2005 by the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC) program were analyzed to provide a first climatology of tropospheric O<sub>3</sub> over Beijing and the North China Plains (NCPs), one of the most populated and polluted regions in China. A pooled method was adopted in the data analysis to reduce the influence of irregular sampling frequency. The tropospheric O<sub>3</sub> over Beijing shows a seasonal and vertical distribution typical of mid-latitude locations in the Northern Hemisphere, but has higher daytime concentrations in the lower troposphere, when compared to New York City, Tokyo, and Paris at similar latitude. The tropospheric O<sub>3</sub> over Beijing exhibits a common summer maximum and a winter minimum, with a broad summer maximum in the middle troposphere and a narrower early summer (June) peak in the lower troposphere. Examination of meteorological and satellite data suggests that the lower tropospheric O<sub>3</sub> maximum in June is a result of strong photochemical production, transport of regional pollution, and possibly also more intense burnings of biomass in Central-Eastern China. Trajectory analysis indicates that in summer the regional pollution from the NCPs, maybe mixed with urban plumes from Beijing, played important roles on the high O<sub>3</sub> concentrations in the boundary layer, but had limited impact on the O<sub>3</sub> concentrations in the middle troposphere. A comparison of the data recorded before and after 2000 reveals that O<sub>3</sub> in the lower troposphere over Beijing had a strong positive trend (approximately 2% per year from 1995 to 2005) in contrast to a flat or a decreasing trend over Tokyo, New York City, and Paris, indicating worsening photochemical pollution in Beijing and the NCPs.
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spelling doaj.art-c3eac5a034d8422ba34e5736471578b52022-12-22T03:11:17ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-01-0181113Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC programA. J. DingT. WangV. ThouretJ.-P. CammasP. NédélecOzone (O<sub>3</sub>) profiles recorded over Beijing from 1995 to 2005 by the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC) program were analyzed to provide a first climatology of tropospheric O<sub>3</sub> over Beijing and the North China Plains (NCPs), one of the most populated and polluted regions in China. A pooled method was adopted in the data analysis to reduce the influence of irregular sampling frequency. The tropospheric O<sub>3</sub> over Beijing shows a seasonal and vertical distribution typical of mid-latitude locations in the Northern Hemisphere, but has higher daytime concentrations in the lower troposphere, when compared to New York City, Tokyo, and Paris at similar latitude. The tropospheric O<sub>3</sub> over Beijing exhibits a common summer maximum and a winter minimum, with a broad summer maximum in the middle troposphere and a narrower early summer (June) peak in the lower troposphere. Examination of meteorological and satellite data suggests that the lower tropospheric O<sub>3</sub> maximum in June is a result of strong photochemical production, transport of regional pollution, and possibly also more intense burnings of biomass in Central-Eastern China. Trajectory analysis indicates that in summer the regional pollution from the NCPs, maybe mixed with urban plumes from Beijing, played important roles on the high O<sub>3</sub> concentrations in the boundary layer, but had limited impact on the O<sub>3</sub> concentrations in the middle troposphere. A comparison of the data recorded before and after 2000 reveals that O<sub>3</sub> in the lower troposphere over Beijing had a strong positive trend (approximately 2% per year from 1995 to 2005) in contrast to a flat or a decreasing trend over Tokyo, New York City, and Paris, indicating worsening photochemical pollution in Beijing and the NCPs.http://www.atmos-chem-phys.net/8/1/2008/acp-8-1-2008.pdf
spellingShingle A. J. Ding
T. Wang
V. Thouret
J.-P. Cammas
P. Nédélec
Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program
Atmospheric Chemistry and Physics
title Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program
title_full Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program
title_fullStr Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program
title_full_unstemmed Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program
title_short Tropospheric ozone climatology over Beijing: analysis of aircraft data from the MOZAIC program
title_sort tropospheric ozone climatology over beijing analysis of aircraft data from the mozaic program
url http://www.atmos-chem-phys.net/8/1/2008/acp-8-1-2008.pdf
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AT vthouret troposphericozoneclimatologyoverbeijinganalysisofaircraftdatafromthemozaicprogram
AT jpcammas troposphericozoneclimatologyoverbeijinganalysisofaircraftdatafromthemozaicprogram
AT pnedelec troposphericozoneclimatologyoverbeijinganalysisofaircraftdatafromthemozaicprogram