A detailed understanding of calving processes at the lacustrine margins of the Greenland ice sheet is necessary for accurately forecasting its dynamic response to ongoing climate change. However, existing data sets of lacustrine calving are limited to summer seasons and to alpine glaciers. Here, we use an integrated time-lapse and structure-from-motion approach to generate the first continuous year-round volumetric record of calving processes at a lacustrine ice sheet margin. We identify two distinct calving regimes that are associated with melt-undercutting and lake ice cover. We also find that calving rates respond rapidly to sudden lake drainage. Given that lake temperature, lake ice cover, and sudden lake drainages are controlled by air temperature and ice-margin thinning, we suggest that climate change, manifested in lengthening summer seasons, will accelerate rates of mass loss and terminus recession at lacustrine ice-margins in Greenland.Plain Language Summary Lakes situated at the margins of glaciers and ice sheets are important because they promote the detachment of large blocks of ice to form icebergs, a process known as calving. Climate change is increasing the number of lakes at the margins of the Greenland ice sheet, and many of those already present are increasing in size. Consequently, a detailed understanding of lake calving processes is needed to accurately predict the future response of the ice sheet to climate change. This study improves our knowledge of calving processes by using time-lapse cameras to record images of calving activity at a lake located in western Greenland over a continuous 14-month period. We use the images to create 3D models that illustrate how calving processes change through time and find that rates and styles of calving vary seasonally in response to lake-driven undercutting of the ice sheet margin and the presence or absence of lake ice cover. Our results suggest that ice loss via calving activity at the lake edges of the Greenland ice sheet will increase in future as summer seasons lengthen in response to climate change.