Sea surface elevation in the South China Sea is examined in the Topex/Posei
don altimeter data from 1992 to 1995. Sea level anomalies are smoothed alon
g satellite tracks and in time with tidal errors reduced by harmonic analys
is. The smoothed data are sampled every ten days with an along-track separa
tion of about 40 km. The data reveal significant annual variations in sea l
evel. In winter, low sea level is over the entire deep basin with two local
lows centred off Luzon and the Sunda Shelf. In summer, sea level is high o
ff Luzon and off the Sunda Shelf, and a low off Vietnam separates the two h
ighs. The boundary between the Vietnam low and Sunda high coincides with th
e location of a jet leaving the coast of Vietnam described in earlier studi
es. Principal component analysis shows that the sea level variation consist
s mainly of two modes, corresponding well to the first two modes of the win
d stress curl. Mode 1 represents the oscillation in the southern basin and
shows little inter-annual variation. The mode 2 oscillation is weak in the
southern basin and is strongest off central Vietnam. During the winters of
1992-1993 and 1994-1995 and the following summers, the wind stress curl is
weak, and the mode 2 sea level variation in the northern basin is reduced,
resulting in weaker winter and summer gyres. Weakening of the Vietnam low i
n summer implies diminishing of the eastward jet leaving the coast of Vietn
am. The results are consistent with model simulations. (C) Elsevier, Paris
/ Ifremer / Cnrs / Ird.