An experimental study was conducted to investigate the dynamic ice accretion process over the surface of a wind turbine blade with DU96-W-180 airfoil profile in order to elucidate the underlying physics for wind turbine icing mitigation. The experimental study was conducted in the Icing Research Tunnel of Iowa State University (ISU-IRT). Six test cases with three typical liquid water content (LWC) levels (i.e., LWC =0.3 g/m 3 , 1.1 g/m 3 , and 3.0 g/m 3) and two typical oncoming airflow temperatures (i.e., T ∞ =-5 o C, and-10 o C) were selected to represent rime icing, mixed icing and glaze icing conditions that wind turbines may experience in winter. In addition to using a high-speed imaging system to quantify the transient behavior of surface water runback and dynamic ice accretion processes over the airfoil surface, an infrared (IR) thermal imaging system was also utilized to simultaneously measure the airfoil surface temperature distributions in the course of the ice accreting process. The measurement results reveal clearly that, both the length of the surface water/ice film formed near the airfoil leading edge and the subsequent water/ice rivulet length would increase as the liquid water content level and the temperature of the oncoming airflow increase. The thickness of the ice accreted at the airfoil leading edge was found to grow rapidly with the increasing liquid water content level and decreasing oncoming airflow temperature for both glaze and mixed icing test cases. The temperature distribution over the airfoil surface was also found to vary significantly, depending on the type of ice accreted over the airfoil surface. A stream-wise 'plateau' region was observed in the measured surface temperature distributions for the glaze and mixed icing cases, due to the formation of surface water runback over the ice accreting airfoil surface.