Mixing processes in gravity current fronts have only recently been qua
ntified due to their complex, unsteady nature. The similarity of the m
ixing processes in these pioneer works, however, has not been explored
adequately. Experiments that explore a wide range of fronts have been
performed. These experiments have used techniques that exhaustively s
ample the temporal (using a high-speed conductivity probe) and spatial
(using planar laser-induced fluorescence) density field more thorough
ly than any previous work. Both types of experiments have confirmed ea
rlier research suggesting that low Reynolds number fronts mix differen
tly and less than higher Reynolds number flows. Similarity appeared to
be achieved for Re-q>1000, where Re-q is a Reynolds number based upon
the cube root of the buoyancy flux into the front and the height of c
urrent. It appears that certain secondary mixing processes, seen by ot
her researchers studying stratified mixed layers, are responsible for
the earlier changes seen with Reynolds number and cause significant mi
xing at the front. (C) 1998 American Institute of Physics. [S1070-6631
(98)01812-1].