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- W2354518251 abstract "The interdecadal changes of both the East Asia summer monsoon(EASM) and the pressure system anomalies over China-Mongolia areas(30°~55°N, 70°~120°E) as well as their relationship have been analysed, utilizing NCEP/NCAR reanalysed gridded data from 1958 to 2000, the result show that, in the lower and middle layers of troposphere, from the surface to 500 hPa or more, the negative correlation between EASM and the pressure system anomalies is quite clear. The coefficients are -0.67 (for sea level pressure) and -0.69 (for geopotential height on 500 hPa) respectively, which is significant at 99.9% confidence level. A clear change appears in the late of 1970′s. In the period of 1960_1976, both the surface and 500 hPa, the pressure system anomalies were negative centre over the China-Mongolia areas. It indicates that the areas dominate low pressure trough or cyclone activities. The strong southerly wind enhances the EASM and result in wet summer in North China. However, in the period of 1977_2000, in the China-Mongolia areas dominate the high pressure ridge or anticyclone activities, the stronger northerly wind over North China preveates the EASM flow form moving northward, and causes the weak EASM and the dry North China. Interestingly, on 100 hPa, mean geopotential height anomaly appears a dipole pattern: During the period of 1960_1976 it was higher in the east, lower in the west; vise versa during the period of 1977_2000. It would be needed further to study." @default.
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- W2354518251 date "2005-04-24" @default.
- W2354518251 modified "2023-09-24" @default.
- W2354518251 title "Impact of Pressure System Anomaly over Mid-High Latitude on the Interdecadal Change of East Asia Summer Monsoon" @default.
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