South China Sea Isopycnal-Surface Circulation

Abstract

This paper investigates the seasonal variabilities of the South China Sea isopycnal-surface circulations and of the Kuroshio intrusion through the Luzon Strait using the U.S. Navy?s climatological temperature and salinity dataset (public domain) with ½° ? ½° resolution by the P-vector method. The representative pattern is a persistent basin-scale cyclonic circulation away from the surface, and a seasonally varying circulation with a weak anticylonic gyre in the summer and a strong cyclonic gyre in the winter near the surface. This pattern is consistent with a classical view of mean cyclonic circulation in large stratified lakes and semienclosed marginal seas by Emery and Csanady and with a recent numerical simulation using the navy?s Layered Ocean Model by Metzger and Hurlburt. The computed monthly volume transport through the Luzon Strait is negative (inflow) all year round with a minimum value of ?13.7 Sv in February (strongest intrusion) and a maximum value of ?1.4 Sv in September (weakest intrusion). The annual mean transport is ?6.5 Sv (intrusion).