Measurements and simulations show that even small variations in the location of the sticks around the ridge of a mountain peak, can cause large variations in accreted ice on the sticks. A basic understanding of the air flow around isolated mountain peaks is vital to understand how complex topography and altering wind direction strongly influence icing intensity. In this case use of a micro-scale numerical model to describe the wind field around the mountain peak, or measurements at the location for a short period of time, proves to give valuable information.