TREND OF OZONE IN THE FREE TROPOSPHERE ABOVE EUROPE

被引:7
作者
SANDRONI, S
ANFOSSI, D
机构
[1] Environment Institute, Joint Research Centre, Ispra
[2] Istituto di Cosmogeofisica del CNR, Torino
来源
NUOVO CIMENTO DELLA SOCIETA ITALIANA DI FISICA C-GEOPHYSICS AND SPACE PHYSICS | 1995年 / 18卷 / 05期
关键词
Climatology;
D O I
10.1007/BF02506780
中图分类号
学科分类号
摘要
Ozone observations were made one century ago by the Schonbein technique at meteorological observatories in the alpine region. Within the intrinsic limitations of the technique, historical readings have been converted to present-time concentrations (p.p.b.v.). The evaluated ozone level in the free troposphere (17 p.p.b.v.) was twice as large as at the surface; comparable values were obtained by chemical and spectroscopic technique in the first half of our century. Furthermore, the reconstructed ozone trend in the free troposphere shows a sharp increase after the '50s, as already observed at the surface at midlatitudes of the northern hemisphere.
引用
收藏
页码:497 / 503
页数:7
相关论文
共 27 条
[1]  
Anfossi D., Sandroni S., Nuovo Cimento C, 17, (1994)
[2]  
Sandroni S., Anfossi D., Viarengo S., J. Geophys. Res., 97, (1992)
[3]  
Sandroni S., Anfossi D., Sci. Total Environ., 148, (1994)
[4]  
Anfossi D., Sandroni S., Viarengo S., J. Geophys. Res., 96, (1991)
[5]  
Bojkov R., Ozone changes at the surface and in the free troposphere, Tropospheric Ozone, pp. 83-96, (1987)
[6]  
Sandroni S., Bacci P., Boffa G., Pellegrini U., Ventura A., Sci. Total Environ., 156, (1994)
[7]  
Haller C., Z. Öst. Gesells. Meteor., 9, (1874)
[8]  
De Tierry M., Comptes Rendus, 124, (1897)
[9]  
Regener V., Meteor. Z., 55, (1938)
[10]  
Fox C.F., Ozone and Antozone. Their History and Nature, (1873)