We set up a time-lapse video camera system on the southwestern shore o
f Lake Michigan for 16 days in January and February 1991 to monitor ic
e conditions. The system was used to determine longshore and cross-sho
re ice-drift rates in a zone of mobile brash and slush ice on 11 days.
Daily mean longshore ice drift was to the southeast on 10 of these da
ys at speeds ranging between 0.047 and 0.377 m s-1. Mean cross-shore i
ce drift was always offshore and varied between 0.009 and 0.126 m s-1.
Shear and strain were rare in the brash/slush zone. On 6 of the days
when drift rates were determined, we were also able to determine the w
idth of the brash/slush zone. Using these data along with published va
lues of ice thickness, ice concentration, and sediment concentration i
n ice, we were able to estimate longshore and cross-shore sand fluxes
and longshore sand transport rates. The longshore and cross-shore ice-
induced sand fluxes ranged from 0.008 to 0.760 t hr-1 and 0.0016 to 0.
096 t hr-1, respectively. Net ice-induced longshore sand transport was
to the south at rates of 1.8 to 83.7 t hr-1. Measured cross-shore san
d flux was consistently offshore. The calculated fluxes indicate that
large amounts of sand are moved alongshore and offshore by ice in sout
hernwestern Lake Michigan during the winter months.