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《Chinese Journal of Atmospheric Sciences》 1992-01
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A Primary Analysis of the Process of the 1960s Northern Hemispheric Summer Climatic Jump

Yan Zhongwei(Institute of Atmospheric Physics, Chinese Academy of Sciences , Bejing, 100080)  
The paper aimed at the recognition of the origin of the large-scale jump signal of the sixties' event. The result from the major signal analysis suggests that the jump happened systematically and earlier (about 1962- 1963) in the fields of the 500hPa height and near-surface temperatures, and later (about 1965-1967) in the fields of the rainfall, sea level pressure and 500hPa ridge-and-trough. The precedent large-scale jump signal occured in the late fifties on the 500 hPa height of the mid-latitudinal Atlantic region-the south edge of the area where the Polar Vortex expands. The signal of height decreasing, accompanied with that of surface temperature decreasing, propagated northward in a few years, leading to a sharp deepening of the Polar Vortex and cooling in the near-polar regions . It was suggested that the atmosphere-oceanic disturbance structure needs much attention in the study of the climatic jump in the long-term climatic process.
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