A cross-validated three-dimensional model of an englacial and subglacial drainage system in a High-Arctic glacier
Recent speleological surveys of meltwater drainage systems in cold and polythermal glaciers have documented dynamic englacial and in some cases subglacial conduits formed by the ‘cut-and- closure’ mechanism. Investigations of the spatial distribution of such conduits often require a combination of different methods. Here, we studied the englacial drainage system in the cold gla- cier Longyearbreen
