Effect of Solar Activity on the Polar-night Jet Oscillation in the Northern and Southern Hemisphere Winter
スポンサーリンク
概要
- 論文の詳細を見る
Effect of the modulation of the Polar-night jet oscillation (PJO) in winter time by the 11-year solar cycle is examined by the observational data from 1979 to 1999. It is found that zonal wind and the E-P flux anomalies appear commonly in the subtropical upper stratosphere in early winter of both the Northern and Southern Hemispheres as a response to meridional UV heating contrast. These zonal wind anomalies are found to propagate poleward and downward with development as a seasonal march in both hemispheres. Although the length of the record is limited, it is suggested from the available data that the signal due to solar activity appears as the time evolution of the PJO triggered by solar forcing at early winter in both hemispheres. Differences in the signals between the Northern and Southern Hemispheres during late winter are explained in terms of the different characteristics of the PJO in each hemisphere. A significant temperature signal is also found to appear in the Southern Hemisphere in late winter under a solar maximum condition.
- 社団法人日本気象学会の論文
- 2002-09-25
著者
-
Kuroda Yuhji
Meteorological Res. Inst. Tsukuba Jpn
-
Kuroda Yuhji
Meteorological Research Institute
-
Kuroda Yuhji
Meteorological College
-
KODERA Kunihiko
Meteorological Research Institute
-
Kodera K
Meteorological Research Institute
関連論文
- Preface(JMSJ Special Edition on the Arctic Oscillation Studies)
- On the Casimir Invariant of Hamiltonian Fluid Mechanics
- Effect of Solar Activity on the Polar-night Jet Oscillation in the Northern and Southern Hemisphere Winter
- Effect of QBO and ENSO on the Solar Cycle Modulation of Winter North Atlantic Oscillation
- Time-sharing measurements of ionospheric electron temperature and electron density with the electric field using double probes: An experiment on the Antarctic sounding rocket S-310JA-7
- Interannual variation of the stratospheric circulation in the Southern Hemisphere during winter to spring -observation and simulation- (abstract)