Jarvis Glacier, Alaska
For my MS research, I developed a novel cost-effective borehole tilt sensor (along with its corresponding sensor network for data transmission and storage) that we deployed in 2 boreholes drilled close to the shear margin of Jarvis Glacier in Alaska to measure ice kinematics through recording borehole deformation. Jarvis is a polythermal glacier, characterized by strong shearing and wet-based beds and is one of two major glacier groups, along with temperate glaciers, where streaming flow occurs. Regions of streaming flow are responsible for draining the major ice sheets and alpine regions.
Our project goals aimed to improve our understanding of flow dynamics at glacier shear margins and how streaming flow relates to the constitutive flow law for ice (Glen’s Flow Law). Applying borehole geophysics, microstructure analysis, ice core analysis, and radar surveys, we completed a rare systematic in-situ study in a natural setting of streaming flow, from which we were able to gain valuable insights into the region’s flow dynamics. In addition to providing the field data, the successful deployment of our tilt sensor served as proof-of-concept of its viability for similar borehole geophysics endeavors.