The development of coastal sediment budgets and models for sediment tr
ansport and shoreline change require bathymetric surveys with vertical
resolution and accuracy of 5 cm or better. Horizontal resolution and
accuracy need to be at least 10 cm to quantify bedforms and bars. Sled
s are probably the most accurate, widely used system for nearshore sur
veys, but their contact with the bottom limits their speed, spatial re
solution, and ability to operate in many situations. Boat-based echo s
ounder surveys can achieve a higher spatial resolution and can operate
where sleds cannot, but waves, tides, and other water-level fluctuati
ons as well as boat dynamics and variations in the speed of sound in w
ater can greatly limit their accuracy. Problems related to a survey sl
ed's contact with the bottom cannot be overcome; therefore, echo sound
er surveys must be improved. The newly developed high-accuracy, high-r
esolution bathymetric surveying system (HARBSS) is designed to overcom
e the confounding effects of changing vessel draft, waves, and tides o
n depth soundings and to eliminate the need for measuring and modeling
water level for a particular survey. The system combines Global Posit
ioning System (GPS) receivers, an electronic motion sensor, a digital-
gyro compass, a digital-analog echo sounder, a conductivity-temperatur
e-depth probe (CTD), a computer, and custom software. The GPS antenna,
compass, and motion sensor are aligned with the echo sounder's transd
ucer. Using a bias-free phase solution from the GPS data (X,Y,Z accura
cy of better than 1 cm), attitude information from the motion sensor,
and heading information from the compass, the position and aim of the
transducer is determined for each sounding. The CTD provides data to c
alculate the speed of sound. Using the above data, the sounding depths
and horizontal locations of sounding: points are corrected in XY, and
Z with respect to an Earth-centered ellipsoid. In constant and unifor
m speed-of-sound conditions, HARBSS can provide soundings that are wit
hin 5.2 cm (mean error of 3.7 cm) of their true elevations. Horizontal
accuracy is estimated to be within 10 cm. This accuracy can be achiev
ed from a small, open boat that is rolling, pitching, heaving, or list
ing. Error analysis indicates that we may be able to decrease the erro
r by one half with better synchronization and interpolation of the var
ious data streams.