@article{oai:nipr.repo.nii.ac.jp:00003518,
 author = {セキグチ, ヨシロウ and SEKIGUCHI, Yoshiro},
 journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology},
 month = {Sep},
 note = {P(論文), Data of total ozone obtained by the ground-based measurements (Dobson spectrophotometer) at Japanese Antarctic Station, Syowa (69°00′S, 39°35′E), are analysed together with data of stratospheric temperature at the same site. The period of analysis is 21 years from 1966 to 1986,covering almost two solar cycles. The time series of monthly averages of the both quantities for October, November and December is compared with the time series of the relative sunspot numbers. A relatively high correlation is found between the relative sunspot number, and the total ozone and the stratospheric temperature at Syowa for the 21-year period inclusive. A peak negative correlation with respect to the present-day 11-year sunspot cycle is found at a lag of 3years of ozone (or temperature) relative to the sunspots. This result will be discussed in connection with the results obtained by H. C. WILLETT (J. Geophys. Res., 67,661,1962) and H. C. WILLETT and J. PROHASKA (J. Atmos. Sci., 22,493,1965).},
 pages = {18--23},
 title = {ANTARCTIC OZONE CHANGE CORRELATED TO THE STRATOSPHERIC TEMPERATURE FIELD AND THE SOLAR ACTIVITY},
 volume = {1},
 year = {1987}
}