This paper presents an approach to array element localization (AEL) for tow
ed marine seismic arrays based on regularized inversion of direct and botto
m-reflected acoustic ray travel times picked from recorded seismic sections
. Depth-sensor measurements at a number of points along the array are inclu
ded as a priori estimates (with uncertainties) in the inversion. The smooth
est array shape consistent with the acoustic data and prior estimates is de
termined by minimizing the array curvature or roughness. A smooth array sha
pe is physically reasonable; in addition, minimizing curvature provides a p
riori information about the correlation between hydrophone positions that a
llows the estimation of both the offset and depth of hydrophones that recor
d only one (or even no) acoustic arrival due to the shadowing effects of wa
ter-column refraction or reflection from arbitrary bathymetry. The AEL inve
rsion is applied to a 102-sensor, 1.2-km towed array to correct receiver po
sitions in the seismic velocity analysis of a seabed gas hydrate survey. (C
) 2001 Acoustical Society of America.