Project Information
NSFGEO-NERC: Collaborative Research: Two-Phase Dynamics of Temperate Ice
Start Date:
End Date:
This award supports a project to study the effect of liquid, intercrystalline water on the flow resistance of ice and the mobility of this water within ice. Water plays a central role in the flow of ice streams. It lubricates their bases and softens their margins, where flow speeds abruptly transition from rapid to slow. Within ice stream margins some ice is "temperate,” meaning that it is at its pressure-melting temperature with relatively thick water films at grain boundaries that significantly soften the ice. The amount of water in ice depends sensitively on its permeability, values of which are too poorly known to estimate the water contents of ice-stream shear margins or associated ice viscosities. This award stems from the NSF/GEO-UK NERC lead agency opportunity (NSF 14-118) and is a collaboration between Iowa State University and Oxford University in the United Kingdom. The experimental part of the project is executed at Iowa State University and is the focus herein because it has been supported by NSF. Two sets of experiments are conducted. In one set, a large ring-shear device is used to shear ice in confined compression and at its melting temperature to study the sensitivity of ice viscosity to water content. Ice is sheared at stresses and strain rates comparable to those of ice-stream margins, and water content is varied through twice the range explored in the only previous set of experiments that investigated ice softening by water. The second set of experiments required the design, fabrication, and testing of a laboratory ice permeameter that allows the permeability of temperate ice to be measured. Experiments are conducted to study the dependence of ice permeability on ice grain size and water content--the two dependencies required to model grain-scale water flow through temperate ice.
Person Role
Iverson, Neal Investigator and contact
Zoet, Lucas Co-Investigator
Antarctic Glaciology Award # 1643120
AMD - DIF Record(s)
Data Management Plan
Product Level:
1 (processed data)
Repository Title (link) Format(s) Status
USAP-DC Softening of temperate ice by interstitial water Excel exists
USAP-DC Ice permeameter experimental parameters and results Excel exists
  1. Adams, C. J. C., Iverson, N. R., Helanow, C., Zoet, L. K., & Bate, C. E. (2021). Softening of Temperate Ice by Interstitial Water. Frontiers in Earth Science, 9. (doi:10.3389/feart.2021.702761)
  2. Fowler JR and Iverson NR (in press as of 2/1/22) A permeameter for temperate ice: first results on permeability sensitivity to grain size. Journal of Glaciology.
Platforms and Instruments

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