Ozone formation in the greater Cairo area.

Abstract

Ozone formation in the greater Cairo area was studied in 1990 in a 3-week measurement period performed at three sites (Shoubra El-Kheima, Mokattam Hill, Helwan), covering a north-south direction of 27 km, and in 1991, from the beginning of April until the end of October, by measurement of the seasonal variation of ozone at one site at El-Kobba. The sinusoidal shape in the diurnal volume fraction plots with peak values of 120 ppb and daily mean value of 50 ppb throughout the year indicate a substantial contribution of photochemistry to the ozone content of the atmosphere. Ozone is produced predominantly over the industrial area in the north and in the centre of Cairo and transported southward by the prevailing northerly winds. Contrary to many urban areas in Europe and in North America, fairly high average ozone levels of 40 ppb are observed during the night throughout the spring and the summer. This may imply that health hazards and crop damage are higher in the greater Cairo area than in Central Europe.

Cite this paper

@article{Gsten1994OzoneFI, title={Ozone formation in the greater Cairo area.}, author={Hans G{\"{u}sten and Gert Heinrich and Justin Weppner and Mohamed M Abdel-Aal and Fouad Abdel-Hay and Abou Bakr Ramadan and F S Tawfik and Dorria M. Ahmed and Gehan K. Hassan and T Civitas}, journal={The Science of the total environment}, year={1994}, volume={155 3}, pages={285-95} }