The Lake Maracaibo estuarine system is a cooscillating coupled ocean-lake s
ystem connected through a partially mixed estuary. In this paper we examine
the low frequency movements (omega < 0.1 cycles/day) in the different wate
r bodies within this system. The harmonic and rotary spectral analyses of v
elocity data indicates the importance of tidal forcing within the whole sys
tem and its interaction with winds and fresh water discharge. In particular
, the results indicate the existence of dominant semi-monthly oscillations
in Lake Maracaibo, likely of non-linear tidal origin, and suggest that vert
ical stratificaction plays an important role in controlling the three-dimen
sional structure of tidal currents.