Mechanisms for the intraseasonal variability of tropospheric ozone over the Indian Ocean during the winter monsoon-Reference-Cited by-同舟云学术

Mechanisms for the intraseasonal variability of tropospheric ozone over the Indian Ocean during the winter monsoon

Published:2007-05-17 Issue:D10 Volume:112 Page:
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res.

Author:

Chatfield R. B.¹,Guan H.¹²,Thompson A. M.³,Smit H. G. J.⁴

Affiliation:

1. Earth Science Division; NASA Ames Research Center; Moffett Field California USA

2. Bay Area Environmental Research Institute; Sonoma California USA

3. Department of Meteorology; Pennsylvania State University; University Park Pennsylvania USA

4. Forschungszentrum Jülich; Jülich Germany

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2006JD007347/fullpdf

Reference53 articles.

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3. Convection links biomass burning to increased tropical ozone: However, models will tend to overpredict O3;Chatfield;J. Geophys. Res.,1990

4. Convective lofting links Indian Ocean air pollution to paradoxical South Atlantic ozone maxima;Chatfield;Geophys. Res. Lett.,2004

5. On the origin of tropospheric O3 over the Indian Ocean during the winter monsoon: African biomass burning vs. stratosphere-troposphere exchange;de Laat;J. Atmos. Chem. Phys.,2002

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