Temporal and spatial variabilities of the South China Sea surface temperature anomaly

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Abstract

In this study we use the National Centers for Environmental Prediction (NCEP) monthly sea surface temperature (SST) fields (1982-1994) to investigate the temporal and spatial variabilities of the South China Sea (SCS) warm/cool anomalies. Three steps of analysis were performed on the data set: ensemble mean (T∼), composite analysis to obtain the monthly mean anomaly relative to the ensemble mean (T), and empirical orthogonal function (EOF) analysis on the residue data relative to (T) +(T∼). The ensemble mean SST field (T) has a rather weak horizontal gradient: 29°C near the Borneo coast to 25°-26°C near the southeast China coast. Two areas of evident SST anomalies were found in the monthly T∼ variation: west of Borneo-Palawan islands (WBP) and southeast of the southern Vietnam coast (SVC). Four patterns, monsoon and transition each with two out-of-phase structures, were found. During the spring-to-summer transition (March to May) the warm anomaly is formed in the northern SCS with T∼ > 1.8°C located at 112o-119°30'E, 15°-19°30'N. During the fall-to-winter transition (October to November) the northern SCS (north of 12°N) cool anomaly is formed in November with f

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Chu, P. C., Lu, S., & Chen, Y. (1997). Temporal and spatial variabilities of the South China Sea surface temperature anomaly. Journal of Geophysical Research: Oceans, 102(C9), 20937–20955. https://doi.org/10.1029/97JC00982

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