In the past century, the historical air temperature record suggests a warming trend in southern Wisconsin, particularly during winter and spring seasons. These changes should in turn have multiple effects on area lakes, such as later freezing and earlier ice breakup, warmer epilimnetic temperature, earlier onset of thermal stratification, stronger temperature gradient across thermocline, change in thermocline depth, and prolonged stratification period.To determine the consequences of these climate changes on ice cover and thermal structure of Lake Mendota, long-term, 100-year (1911-2010) simulations were performed using the DYRESM-WQI model. Results show later freezing (9.8 days/100yr), earlier ice breakup (10.8 days/100yr), and shorter ice duration ....