Atmospheric transport and photochemistry of ozone over central Southern Africa during the Southern Africa Fire-Atmosphere Research Initiative

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JournalofGeophysicalResearchAtmospheres1997TysonAtmospherictransportandphotochemistryofozoneover.pdf (1.52 MB)

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https://onlinelibrary.wiley.com/doi/abs/10.1029/97JD00170

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https://doi.org/10.1029/97JD00170
 http://hdl.handle.net/11603/34912

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https://orcid.org/0000-0002-7829-0920

Date

1997-05-01

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journal articles
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Tyson, P. D., M. Garstang, A. M. Thompson, P. D’Abreton, R. D. Diab, and E. V. Browell. “Atmospheric Transport and Photochemistry of Ozone over Central Southern Africa during the Southern Africa Fire-Atmosphere Research Initiative.” Journal of Geophysical Research: Atmospheres 102, no. D9 (1997): 10623–35. https://doi.org/10.1029/97JD00170.

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This work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
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Abstract

Vertically integrated back and forward trajectories for the 300–200, 700–500 and surface-800 hPa levels are calculated using Pretoria as point of origin for the Southern Africa Fire-Atmosphere Research Initiative (SAFARI) period September-October 1992. The transport fields are then combined to show both horizontal and vertical transport of air to and from Pretoria at the different levels. Air transport patterns in the vertical are linked to the occurrence of absolutely stable layers which are also evident in the 16 ozonesonde profiles recorded at Pretoria during SAFARI. The coherence of the stratification based on dynamical and ozone analysis permits the use of mean ozone profiles with air volume fluxes to interpret the ozone in terms of photochemistry and transport within stable layers. Extensive recirculation across the meridional plane at Pretoria implies that advection of ozone is slow and that photochemistry is responsible for the observed vertical structure over central southern Africa in September and October 1992. Requisite ozone formation rates are supported by model analysis of ozone and ozone precursors measured from SAFARI and Transport and Atmospheric Research Chemistry near the Equator-Atlantic aircraft.