The data suggested that, like mountain glaciers, melt -
induced glacier acceleration actually stops in years of intense melting once subglacial water erodes through the sediments and creates channels for water flow (Sundal et al. 2011).
Joughin and others, 2008 observed that seasonal drainage of meltwater to the
glacier bed
induces a uniform
acceleration of 50 — 150 meters / year over a ~ 300 km long section of the West Greenland margin that is not drained by outlet
glaciers, causing a large fractional
acceleration of the interior ice sheet but a small fractional change in the speed of fast - moving outlet
glaciers.