Couplingbetweenrunoff,hydrology,basalmotion,andmassloss(“hydrology-dynamics”) is a critical component of the Greenland Ice Sheet system. Despite considerable research effort, the mechanisms by which runoff inﬂuences ice dynamics and the net long-term (decadal and longer) dynamical effect of variations in the timing and magnitude of runoff delivery to the bed remain a subject of debate. We synthesise key research into land-terminating ice sheet hydrology-dynamics, in order to reconcile several apparent contradictions that have recently arisen as understanding of the topic has developed. We suggest that meltwater interaction with subglacial channels, cavities, and deforming subglacial sediment modulates ice ﬂow variability. Increasing surface runoff supply to the bed induces cavity expansion and sediment deformation, leading to early-melt season ice ﬂow acceleration. In the ablation area, drainage of water at times of low runoff from high-pressure subglacial environments toward more efﬁcient drainage pathways is thought to result in reductions in water pressure, ice-bed separation and sediment deformation, causing net slow-down on annual to decadal time-scales (ice ﬂow self-regulation), despite increasing surface melt. Further inland, thicker ice, small surface gradients and reduced runoff suppress efﬁcient drainage development, and a small net increase in both summer and winter ice ﬂow is observed. Predictingicemotionacrossland-terminatingsectorsoftheicesheetoverthetwenty-ﬁrst century is confounded by inadequate understanding of the processes and feedbacks between runoff and subglacial motion. However, if runoff supply increases, we suggest that ice ﬂow in marginal regions will continue to decrease on annual and longer timescales, principally due to (i) increasing drainage system efﬁciency in marginal areas, (ii) progressive depression of basal water pressure, and (iii) thinning-induced lowering of driving stresses. At higher elevations, we suggest that minor year-on-year ice ﬂow acceleration will continue and extend further into the interior where self-regulation mechanisms cannot operate and if surface-to-bed meltwater connections form. Based on current understanding, we expect that ice ﬂow deceleration due to the seasonal development of efﬁcient drainage beneath the land-terminating margins of the Greenland Ice Sheet will continue to regulate its future mass loss.