The spatial resolution of a ground penetrating radar (GPR) system using tra
ditional interpretation methods is largely dependent on the isolations of e
choes. It is difficult to identify weak echoes that are mixed with either d
irect waves or other larger echoes; especially, when the media is absorptiv
e, the reflections cannot be identified from the tail of the direct wave. I
n this paper, we present an iterative algorithm to reconstruct the image of
the subsurface using time-domain waveforms, The forward modeling employed
in the algorithm is derived from the transmission line matrix (TLM) method
with a perfect matched layer (PML) absorbing boundary. One-dimensional (1-D
) inversion algorithm is briefly described, based on which, a two-dimension
al (2-D) inversion method is developed. The inversion algorithm proceeds it
eratively in space and time step by step. The inversion algorithm is tested
in cases in which both 1-D and 2-D variations exist. The developed inversi
on method is used to reconstruct the images of buried objects using GPR dat
a with echoes buried in the direct waves. The results show a superior resol
ution and stability.