Abstract
The results show an increase in ozone by a factor of 5 since the beginning of the twentieth century, corresponding to an exponential increase of 1.6% per year, although this trend is probably higher (2.4% per year) for the last few decades. A stable 10 ppb ozone mixing ratio is observed during the first 20 years of the series, which is representative of the preindustrial era ozone level. The increase is seen to start around 1895. If these rates were to be maintained in the future, ozone would continue to evolve differently in the two hemispheres (maximum level in the northern hemisphere) and could make an even more significant contribution to the radiative forcing of the northern hemisphere. -from Authors
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Cite
CITATION STYLE
Marenco, A., Gouget, H., Nedelec, P., Pages, J. P., & Karcher, F. (1994). Evidence of a long-term increase in tropospheric ozone from Pic du Midi data series: consequences: positive radiative forcing. Journal of Geophysical Research, 99(D8). https://doi.org/10.1029/94jd00021