In 2008, a Polar Field Services team completed a successful overland traverse from Thule, Greenland, to Summit Station. But along the way they battled a mushy snowpack. Equipment sunk deep into the snow, sleds occasionally got stuck, progress was slow. So this year the Greenland Inland Traverse (GrIT) decided to take advantage of the long travel days and study the snowpack that had previously slowed their progress.
Using methodology developed by Bob Hawley, the team measured snow compaction by drilling a hole and taking images with an infrared camera. The photos tell scientists how much the snow layers have compacted as they've become firn, thus helping with the very precise mass balance measurements they make for satellite ground truthing.
Assume the position: placing the infrared camera into the hole to take shots that will assess the snow's firmness and compaction.
The team also took snow samples from pits to measure density. Samples were taken every 10 cm in a 1 meter pit.
The team also took measurements to detect crevasses.
All of the data will be analyzed and will help the planning for next year's GrIT. Check back soon for results.