A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2018; you can also visit the original URL.
The file type is application/pdf
.
A Relationship between the Stratospheric Circulation and the Seasonal Transition of the Ogasawara Anticyclone
成層圏循環と小笠原高気圧の季節的転移との関係
1966
Journal of the Meteorological Society of Japan
成層圏循環と小笠原高気圧の季節的転移との関係
A zonal index on the 1Omb level is defined to describe the time change of the lowlatitude easterly jet stream in the mid-stratosphere. The index shows a remarkable sudden increase on some day in June. This increase of the zonal index occurs simultaneously in the stratosphere. Further, by examining a relationship between this singular phenomenon and the seasonal transition of the Ogasawara anticyclone in the troposphere, it is found that the increase of the 1Omb zonal index occurs about a month
doi:10.2151/jmsj1965.44.3_159
fatcat:qrrrtih6szhmlke4lmevzaug2m