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Ozone effect on solar radiation

Ozone flames burning at 6 cc. per second

Ozone formation from compound X

Ozone formation in irradiated scrubbed Pasadena air

Ozone formation in irradiated treated Pasadena air

Ozone formation with various organics and nitrogen dioxide

Ozone generating equipment and control panel

Ozone generator

Ozone generator header and tubes

Ozone history along the 1030 trajectory

Ozone hole observed in March above the Arctic in March from 1996 to 2000 by GOME compared to the average TOMS March values for 1979 to 1983. Mean polar vortex position is indicated by the 38PVU isoline at the 47SK potential temperature surface

Ozone hole observed in September above the Antarctic by GOME from 1995 to 1999 compared to the average TOMS September values for 1979 to 1992.

Ozone is a major component of smog. Source

Ozone isopleth diagram for 18th July 2006 at the EMEP GB0036R Harwell station plotted from the results of VOC and NOx emission sensitivity experiments performed with a Photochemical Trajectory Model

Ozone isopleth diagram showing the dependencies of ozone on varying levels of initial VOCs and NO,. Concentrations are given in ppb. Adapted from M.S. Bergin et at, Enc. ofEnv. Analysis and Remediation, 29, 3029,

Ozone isopleth diagram showing the dependeneies of ozone on varying levels of initial VOCs and NO,. Concentrations are given in ppb. Adapted fiom MS. Bergin et al., Enc. ofEnv. Analysis and Remediation, 29,3029,

Ozone isopleth diagram showing the dqiendencies of ozone on varying levels of initial VOCs and NO. Concentrations are given in ppb. Adapted from M.S. Bergin et al., Enc. ofEnv. Analysis and Remediation, 29,3029, .

Ozone isopleths for the maximum concentration of O3 obtained by

Ozone layer profile for the Earth Reproduced by permission of Ozone Profiles at Lauder, NZ June 1, 1994.

Ozone mini-hole event was observed on the edge of a polar vortex exhibiting chemical depletion in

Ozone mixing ratio , averaged over December-January-February months of winter 1991-1992. Latitudes are in degrees and from Southern to Northern Pole as well as everywhere further.

Ozone mixing ratio at height 40 km. Longitudes are ip degrees and from Greenwich to east

Ozone mixing ratio vertical profiles at latitude 62.5N and at longitude 60 solid line and 220 marked line

Ozone mixing ratios in the present atmosphere as calculated by the 2-D model for August 1

Ozone mixing ratios in the upper troposphere as a function of latitude, from aircraft observations. Top



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