It is commonplace in Wisconsin for cranberry growers to flood their beds to form thick ice during winter to protect the uprights from dangerously low winter air temperatures. However, the specifics of ice thickness and zone temperature within and below the ice vs. surface air temperature have not been studied. We have developed several models using finite element analysis, a process by which a complex system is divided into finite segments and analyzed individually. All pieces are then recombined into the complete system so a comprehensive picture of the activity of the freezing cranberry bed may be visualized. It was determined that cold surface air temperatures of -25 °C and thin ice of 15 cm, soil and gap air temperatures do not drop lower then -5 °C, which is congruent with data collected from the field. Models on sand beds and peat beds did not show enough difference to be of concern. Temperatures within the ice, where the uprights would be encased, reached -15 °C under the cold air regime, which has been proven to be well within the survival range of the dormant buds.