This paper describes the spatial and temporal variability of strength
in a typical river-ice cover during the pre-breakup period affected by
radiation decay. Strength was determined using the borehole jack - a
field-portable ice indentor system. Two cover types were analyzed: a g
ranular white-ice/freeze-up jam and a columnar black-ice cover. Despit
e a protracted period of intense radiation, the strength of the highly
-reflective ice in the freeze-up jam experienced no measurable change.
The low-albedo, highly-transparent columnar cover, however, decreased
in strength by approximately 50 % due primarily to the development of
inter-granular void space. Changes are related to porosity and a comp
arison made to previous theoretical and laboratory work. Spatial varia
tions in strength are discussed with respect to break-up advance and i
ce jamming. Possible control of break-up through modification of freez
e-up processes is also presented.