Laura Kehrl, working with the glaciological team at Victoria University have reported on their precise measurements of the surface velocity of the Franz Josef glacier. They put a whole lot of GPS sensors on the glacier and left them to log their position during March of 2011 and then again over late summer in 2013. They found the glacier sped up and slowed down every day and sped up following rain. The movement propagated from up glacier down to the terminus. When comparing the movement to their best estimates of rainfall and melt water they concluded the glacier speed was related to the change in liquid water, not just the quantity of water. They attribute this to the sub-glacial conduits closing during low flows leading to high pressure when the next high flows occurred. This high water pressure reduced friction between the glacier and the rock beneath it letting the glacier speed up. The research is published the Journal of Glaciology.