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- W2370362803 abstract "The two years with large differences of monthly mean flow(i.e.,1985 and 1988) are chosen to study the propagation of 30—60-day oscillation and its interaction with monthly mean flow over the East Asia and western Pacific.The results show that 30—60-day oscillation in the East Asia and western Pacific is influenced by two branches of low frequency eddy,one of which originates from the tropical eastern Indian Ocean,another comes from the Central Pacific.During most of the summertime,they converge at 20—30°N and exert a further influence on geopotential height over this region.When the low frequency cyclone(anticyclone) moves into the western Pacific,geopotential height tends to be reduced(enhanced).Moreover,there exist an interannual variability of 30—60-day oscillation.In 1985,the wave trains are active and the low frequency eddies over middle and high latitudes move to the south of Japan.In 1988,the low frequency eddies over middle and high latitudes propagate southward to the South China Sea although the wave train is not so active as in 1985.As far as the conversion of kinetic energy and available potential energy between 30—60-day oscillation and mean flow is concerned,the barotropic process,the moist baroclinic process and the dry baroclinic process may play a role in the conversion because the three processes possess the same magnitude.However,the intensity of conversion in 1985 is much larger than that in 1988.It is also shown that 30—60-day oscillation in the warm pool transports energy into the monthly mean flow while it gains energy from the monthly mean flow region in middle and high latitudes." @default.
- W2370362803 created "2016-06-24" @default.
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- W2370362803 date "2005-01-01" @default.
- W2370362803 modified "2023-09-23" @default.
- W2370362803 title "The Propagation of 30—60-Day Oscillation and Its Interaction with the Monthly Mean Flow over East Asia and the Western Pacific During the Northern Summer" @default.
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