English
 
Help Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
  Chemical characterization of air pollution in Eastern China and the Eastern United States

Tie, X., Brasseur, G. P., Zhao, C., Granier, C., Massie, S., Qin, Y., et al. (2006). Chemical characterization of air pollution in Eastern China and the Eastern United States. Atmospheric Environment, 40(14), 2607-2625. doi:10.1016/j.atmosenv.2005.11.059.

Item is

Files

show Files
hide Files
:
sdarticle.pdf (Publisher version), 3MB
 
File Permalink:
-
Name:
sdarticle.pdf
Description:
-
OA-Status:
Visibility:
Restricted (Max Planck Institute for Meteorology, MHMT; )
MIME-Type / Checksum:
application/pdf
Technical Metadata:
Copyright Date:
-
Copyright Info:
-
License:
-

Locators

show

Creators

show
hide
 Creators:
Tie, Xuexi, Author
Brasseur, Guy P.1, Author                 
Zhao, Chunsheng, Author
Granier, Claire1, Author           
Massie, Steven, Author
Qin, Yu, Author
Wang, Pucai, Author
Wang, Geli, Author
Yang, Pecai, Author
Richter, Andreas, Author
Affiliations:
1The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913550              

Content

show
hide
Free keywords: Ozone production; The Eastern US; Eastern China
 Abstract: Satellite data (MODIS, GOME, and MOPITT) together with a chemical transport global model of the atmosphere (MOZART-2) are used to characterize air pollution in Eastern China and the Eastern US to assess the differences between the photochemical conditions in these two regions. Observations show that aerosol concentrations (both fine (radius<0.5 μm) and coarse modes (radius>0.5 μm)) are higher in Eastern China than in the Eastern US. The NOx concentrations in both regions are substantially higher than in remote regions such as over the oceans (150 compared to 5 (1014 # cm−2) over the Pacific Ocean). The CO concentrations are high in both urbanized areas (30 compared to 10 (1017 # cm−2) over the Pacific Ocean). However, the concentrations of non-methane hydrocarbons from both anthropogenic and biogenic sources are considerably lower in Eastern China than in the Eastern US. As a result, the rate of photochemical ozone production and ozone concentrations during summer is significantly lower in Eastern China (daily averaged concentrations of 40–50 ppbv in summer) than in the Eastern US (daily averaged values of 60–70 ppbv). The analysis also shows that in Eastern China, the O3 production is mainly due to the oxidation of carbon monoxide (54% of total O3 production), while, in the Eastern US, the O3 production is attributed primarily to the oxidation of reactive hydrocarbons (68% of total O3 production). The results also indicate that biogenic emissions of hydrocarbons contribute substantially to the production of O3 in the Eastern US. The O3 production due to the oxidation of biogenic hydrocarbons represents approximately one third of total O3 photochemical production in this region. Measurements of surface ozone in the Eastern US and Eastern China seem to support that the summer ozone production is lower in Eastern China than in the Eastern US. However, additional surface measurements, especially of reactive hydrocarbons and ozone are needed in Eastern China in order to improve the present analysis and to confirm our current conclusions. A sensitivity study shows that with increase in anthropogenic emissions of HCs, the surface ozone concentrations significantly increase in Eastern China, indicating that the increase in the emissions of HCs plays an important role for the enhancement in surface ozone in this region.

Details

show
hide
Language(s): eng - English
 Dates: 2006-02-21
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: -
 Identifiers: eDoc: 260903
DOI: 10.1016/j.atmosenv.2005.11.059
 Degree: -

Event

show

Legal Case

show

Project information

show

Source 1

show
hide
Title: Atmospheric Environment
Source Genre: Journal
 Creator(s):
Affiliations:
Publ. Info: -
Pages: - Volume / Issue: 40 (14) Sequence Number: - Start / End Page: 2607 - 2625 Identifier: -