Scientists believe increased water depth, and therefore pressure, inside moulins lubricates the base of the ice sheet and increases the speed of its movement toward the sea, the way an ice cube slides easily on a thin film of water.
But until now, little was known about the actual size of moulins and how much water they can hold.
“We compared our models with in-the-field observations of the water levels and it seemed like we would need really huge volumes inside moulins to produce the relatively smaller water variations that we were seeing,” said Matt Covington, associate professor of geosciences and first author of the study published in the journal Geophysical Research Letters.University of Arkansas associate professor of geosciences Matt Covington climbs into a moulin on the Greenland ice sheet.During each trip, they used ropes and other climbing equipment to rappel 100 meters into two separate moulins, almost reaching the water level.
The team’s findings add to the knowledge of how water interacts with the base of the ice sheetD
University of Arkansas associate professor of geosciences Matt Covington investigates a moulin on the Greenland ice sheet.“We’re trying to understand the way the meltwater is interacting with the ice motion, and the main thing that we found is that the water pressure within these moulins is not as variable as was previously observed, and that this seems to result from really large volumes in the moulins,” Covington said.Reference: “Moulin Volumes Regulate Subglacial Water Pressure on the Greenland Ice Sheet” by M.November 19, 2020November 18, 2020