Radio-echo sounding (RES), or radar, is an established geophysical techniqu
e that has been, and continues to be, applied to investigate a variety of i
ce-mass properties. This review presents the physical theory and principles
of radio-glaciology, and describes the various types of radar equipment co
mmonly used, including modern, ground-penetrating radar (GPR) systems. The
range of glaciological applications these systems have been used to investi
gate is summarized, along with promising avenues of current and future rese
arch.