Spatial and temporal oscillation and long-term variation in sea surface temperature field of the South China Sea
Qinghua Qi
Abstract
Qinghua Qi
Abstract
Based on monthly mean sea surface temperature(SST),850hPa wind and subtropical high index over the western Pacific during 1950~2006,the spatial and temporal oscillation and long-term variation in SST field of the South China Sea(SCS) are analyzed by using empirical orthogonal function(EOF),polynomial function and spectrum analysis,and then the causes of SST interannual and long-term variation are discussed by using correlation and composite analysis.The results show that SST anomaly fields have two major patterns.SSTs over the South China Sea have spatially in-phase interannual variation and seasonal oscillation with out-of-phases between the west and east South China Sea.The SST in the central South China Sea exhibit significant interannual and interdecadal variations,and experienced a climate jump in 1981.The annual mean SST in the central South China Sea has increased by 0.92℃ from 1950 to 2006.It is also suggested that the interannual and long-term variations in SST of the South China Sea may be resulted from the meridional wind anomaly and zonal migration of the subtropical high over the western Pacific.
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Based on monthly mean sea surface temperature(SST),850hPa wind and subtropical high index over the western Pacific during 1950~2006,the spatial and temporal oscillation and long-term variation in SST field of the South China Sea(SCS) are analyzed by using empirical orthogonal function(EOF),polynomial function and spectrum analysis,and then the causes of SST interannual and long-term variation are discussed by using correlation and composite analysis.The results show that SST anomaly fields have two major patterns.SSTs over the South China Sea have spatially in-phase interannual variation and seasonal oscillation with out-of-phases between the west and east South China Sea.The SST in the central South China Sea exhibit significant interannual and interdecadal variations,and experienced a climate jump in 1981.The annual mean SST in the central South China Sea has increased by 0.92℃ from 1950 to 2006.It is also suggested that the interannual and long-term variations in SST of the South China Sea may be resulted from the meridional wind anomaly and zonal migration of the subtropical high over the western Pacific.
Key concepts: Empirical orthogonal functions, Climatology, Sea surface temperature, Anomaly (physics), Subtropical ridge, Environmental science, Subtropics, Pacific decadal oscillation