INTERANNUAL CHANGES OF UPPER STRATOSPHERIC TEMPERATURES BASED ON RECENT SATELLITE OBSERVATIONS
スポンサーリンク
概要
- 論文の詳細を見る
Interannual changes of zonal mean temperature in the upper stratosphere are investigated for the period from 1979 to 1986 with the aid of TIROS-N/NOAA satellite observations. It is found that a systematic interannual change of the temperature with a maximum in 1980 and a minimum in 1985 is predominant in the upper stratospheric summer of the Northern Hemisphere. The magnitude of the difference between the maximum and minimum temperature is about 2 K at the 1 mb level. This interannual change seems to be in phase with sunspot number index and may be caused by the 11-year solar cycle. In the Southern Hemisphere, however, such a systematic interannual change is unclear even in the summer season of the upper stratosphere, which is probably related to irregular occurrence of final warmings.
- 国立極地研究所の論文
著者
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HIROOKA Toshihiko
Department of Earth and Planetary Sciences, Kyushu University
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Hirooka T
Department Of Earth And Planetary Sciences Kyushu University
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Hirooka Toshihiko
Meteorological College
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- YEAR-TO-YEAR CHANGES OF MONTHLY MEAN ZONAL WINDS IN THE ANTARCTIC STRATOSPHERE : A RELATION TO THE OZONE HOLE
- Stratospheric Circulation of the Northern Hemisphere Winter during 1989-90
- INTERANNUAL CHANGES OF UPPER STRATOSPHERIC TEMPERATURES BASED ON RECENT SATELLITE OBSERVATIONS