Abstract. This paper studies the lake dynamics for avalanche-triggered glacial lake outburst floods (GLOFs) in the Cordillera Blanca mountain range in Ancash, Peru. As new glacial lakes emerge and existing lakes continue to 10 grow, they pose an increasing risk of GLOFs that can be catastrophic to the communities living downstream. In this work, Lake Palcacocha is used as a case study to analyze the upper watershed processes that typically comprise a GLOF event, specifically the lake dynamics when an avalanche produces a large tsunami-like wave that might overtop and erode the lake-damming moraine. Dynamics of avalanche-generated impulse waves were investigated through three-dimensional hydrodynamic lake simulations of potential GLOF scenarios at Lake Palcacocha, Peru. 15Wave generation from avalanche impact was simulated using two different boundary condition methods.Representation of an avalanche as water flowing into the lake generally resulted in higher peak flows and overtopping volumes than simulating the avalanche impact as mass-momentum inflow at the lake boundary. Three different scenarios of avalanche size were simulated for the current lake conditions, and all resulted in significant overtopping of the lake-damming moraine. The lake model was evaluated for sensitivity to turbulence model and 20 grid resolution, and the uncertainty due to these model parameters is significantly less than that due to avalanche boundary condition characteristics. Although the lake model introduces significant uncertainty, the avalanche portion of the GLOF process chain is the greatest source of uncertainty. To aid in evaluation of hazard mitigation alternatives, two scenarios of lake lowering were investigated. While large avalanches produced significant overtopping waves for all lake-lowering scenarios, simulations suggest that it may be possible to contain waves 25 generated from smaller avalanches if the surface of the lake is lowered.