Periodic Time Variation of a LOW-T_<BB> Cloud Area in Typhoon
スポンサーリンク
概要
- 論文の詳細を見る
In this paper, the evolution of the cloud activities for six typhoons in 1997 is examined, utilizing T_<BB> (equivalent Black Body temperature) data of GMS (Geostationary Meteorological Satellite)-5 split window channels. As the result, periods of 24-hour and about 10-hour are found in the time variation of the cloud areas whose cloud top temperature is lower. Diurnal variation is found most distinctly in the time series of the cloud area of TBB lower than -40℃, which corresponds to the one whose cloud top gets at the upper level of the troposphere. The maximum and the minimum peaks of this variation appear around at 1500 JST (Japan Standard Time) and 0800 JST. And, the maximum appears corresponding to vigorous convections at 0600-1000 JST of all the vigorous convections. About 10-hour period time variation is found most distinctly in the time series of the cloud areas of T_<BB> lower than -60℃, which corresponds to the one whose cloud top gets at the upper level of tropopause or over. The maximum of this variation appears corresponding to a preceding vigorous convective activity which occurs in the wide region of the typhoon a few hours before.
- 社団法人日本気象学会の論文
- 2003-12-25
著者
-
Oyama Ryo
Institute For Hydrospheric Atmospheric Sciences Nagoya University
-
TAKEDA Takao
Institute for Hydrospheric Atmospheric Sciences, Nagoya University
-
Takeda Takao
Institute For Hydrospheric Atmospheric Sciences Nagoya University
関連論文
- Periodic Time Variation of a LOW-T_ Cloud Area in Typhoon
- Diurnal Variation of Cloud Features in Summer Season of 1998 in Yangtze River Basin
- Frontal Collapse and Collisions in Unbalanced Frontogenesis Model : the role of geostrophic adjustment