Other
Scientific paper
Dec 2005
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005georl..3223812z&link_type=abstract
Geophysical Research Letters, Volume 32, Issue 23, CiteID L23812
Other
2
Global Change: Climate Variability (1635, 3305, 3309, 4215, 4513), Global Change: Climate Dynamics (0429, 3309), Atmospheric Processes: Climate Change And Variability (1616, 1635, 3309, 4215, 4513), Atmospheric Processes: Climatology (1616, 1620, 3305, 4215, 8408), Atmospheric Processes: Polar Meteorology
Scientific paper
The merged TOMS/SBUV ozone data for 1979-2002 are used to analyze, with a linear regression model and the other approaches, the zonal distribution of ozone variations between 50° and 60°N, the seasonal cycle and trends, and the responses to the solar cycle, quasi-biennial oscillation (QBO), El Niño-Southern Oscillation (ENSO) and Arctic Oscillation (AO). The seasonal ozone cycle shows ozone high over the north Pacific and low over the north Atlantic in winter, with a variability of 180 DU between 50° and 60°N. The maximum ozone trend obtained is over -5.3 +/- 0.8%/decade at around 95°E in March. The anti-phase ozone response to the equatorial QBO is about 8 DU, with a 28-month period, in zonal average. In addition, the ozone responses to ENSO and AO are detected as 5 and 8 DU, respectively, between 95° and 190°E. The zonal inhomogeneity of ozone variations between 50° and 60°N is also discussed in this study.
Chen Xiaowei
Gao Dengyi
Gao Yongqi
Ji Chongping
Li Peng
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