Results from an initial feasibility study to test whether Global Posit
ioning System (GPS) navigation can be combined with more traditional a
coustic methods to measure ocean current profiles are presented. A typ
ical acoustic current profiler such as PEGASUS measures currents by ra
nging on two acoustic sources (one-way beacons or two-way transponders
) as it falls or rises through the water column. These sources must be
previously deployed on the bottom, and their positions accurately det
ermined via the attending research vessel. As discussed below, this pr
ocedure introduces a number of complications. In particular, any unres
olved errors in the source deployment will remain as systematic errors
in the resulting velocity data. The method described here replaces th
e bottom-mounted sources with hydrophones drifting near the ocean surf
ace. The positions of these hydrophones are computed every few seconds
using GPS. This feasibility test shows that a combined GPS-acoustic s
ystem can approach accuracy levels found in the standard method. Furth
ermore, systematic errors can be significantly reduced. Random errors
are estimated to be approximately +/-1-2 cm s(-1) dependent on station
geometry.