Now Archived! PolarConnect event with Steve Kirsche and researchers Ian Baker and Eric Wagner from Summit Station in Greenland on Tuesday, 20 June 2017. You can access this and other events on the PolarConnect Archives site.
What Are They Doing?
There is broad interest in understanding firn compaction for a number of reasons, most importantly for better interpretation of paleoclimate from air that becomes trapped within the firn (granular snow, especially on the upper part of a glacier, where it has not yet been compressed into ice). Firn densification involves a number of different mechanisms which leads to vapor movement. We will determine the mechanisms of firn densification and microstructural evolution as a function of depth using dynamic observations of the evolution of the firn using X-ray computed microtomography (µCT).
We will drill an 80-meter firn core at Summit, Greenland and transport it to Dartmouth University. After the field expedition, Steve will work with the team at the university, where we will perform experiments to observe changes based on temperature and stress (due to depth and load). In addition to observing the microstructure as a whole, we can follow the evolution of ice crystals to observe bond formation and bond-breaking under load in detail, as undertaken in some prior studies on snow.
Our project will aid in the understanding of firn and ice microstructure evolution in polar ice sheets. This will aid in understanding ice flow and interpreting paleoclimate reconstruction from ice cores.
Where Are They?
The team will travel to Summit Station, located at the peak of the Greenland ice cap atop 3200 meters of ice. Summit is a scientific research station sponsored by the National Science Foundation that supports a diversity of scientific research, including year-round measurements of air-snow interactions that provide crucial knowledge for interpreting data from deep ice cores drilled both at Summit and elsewhere. Learn more about Summit at the Summit Station website.
Ian has been on the Faculty at the Thayer School of Engineering, Dartmouth College for 34 years. He has been working on the structure, chemistry, and properties of snow, firn, and ice cores for the last 30 years. This work has ranged from fundamental studies of defect behavior in ice, studied using synchrotron X-ray topography, to studies of impurity locations in firn and ice cores and the metamorphism of snow.
Eric Wagner is currently an Engineering PhD student at Dartmouth College in Hanover, NH. His research focuses on the microstructure of firn and the mechanics of firn evolution. This is of interest in determining how firn evolution contributes to ice sheet fabric development and interpretation of paleoclimate data where coarse-grained and fine-grained firn exhibit different pore close-off depths. When not in the lab, he enjoys hiking, biking and skiing.