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《Journal of Nanjing Institute of Meteorology》 1984-02
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CIRCULATION WITH 40-50 DAY OSCILLATION AND CHANGES IN MOISTURE TRANSPORT OVER MONSOON ASIA IN 1979 SUMMER

He Jinhai;T. Murakami;T. Nakazawa Department of Meteorology, University of Hawaii  
Based on FGGE Level Ⅲb data a composite technique is employedto investigate the changes in the circulation with a 40--50 day periodand the associated moisture transport. It is found that the northwardand eastward passage of the 40--50 day perturbations is related to thephase changes between the active and break monsoons over centralSouth Asia and Southeast Asia. The active (break) monsoon is char-acterized by the maximum (minimum) cross-equatorial moisture fluxesover the western Indian Ocean. and by the maximum (minimum) east-ward moisture fluxes over the eastern Arabian Sea (75°E), the maxi-ma (minima) together with the Q_1 maximum (minimum ) and the OLRminimum (maximum), propagate eastward and northward. The fluc-tuation in cross--equatorial moisture transport related to Somali Jetexerts an influence on the summer monsoon precipitation over SouthChina via the propagation of the 40--50 day perturbation, the time lagbeing about 10--12 days.
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