A need exists for frequent and prompt updating of shoreline positions,
rates of shoreline movement, and volumetric nearshore changes. To eff
ectively monitor and predict these beach changes, accurate measurement
s of beach morphology incorporating both shore-parallel and shore-norm
al transects are required. Although it is possible to monitor beach dy
namics using land-based surveying methods, it is generally not practic
al to collect data of sufficient density and revolution to satisfy a t
hree-dimensional beach-change model of long segments of the coast. The
challenge to coastal scientists is to devise new beach monitoring met
hods that address these needs and are rapid, reliable, relatively inex
pensive, and maintain or improve measurement accuracy. The adaptation
of Global Positioning System (GPS) surveying techniques to beach monit
oring activities is a promising response to this challenge. An experim
ent that employed both GPS and conventional beach surveying was conduc
ted, and a new beach monitoring method employing kinematic GPS surveys
was devised. This new method involves the collection of precise shore
-parallel and shore-normal GPS positions from a moving vehicle so that
an accurate two-dimensional beach surface can be generated. Results s
how that the GPS measurements agree with conventional shore-normal sur
veys at the 1 cm level, and repeated GPS measurements employing the mo
ving vehicle demonstrate a precision of better than 1 cm. In addition,
the nearly continuous sampling and increased resolution provided by t
he GPS surveying technique reveals alongshore changes in beach morphol
ogy that are undetected by conventional shore-normal profiles. The app
lication of GPS surveying techniques combined with the refinement of a
ppropriate methods for data collection and analysis provides a better
understanding of beach changes, sediment transport, and storm impacts.