Glaciers and parts of ice sheets that end in the ocean are the most rapidly shrinking glaciers on earth, but are so poorly understood that they are also a dominant source of uncertainty in sea level rise projections.  My research identifies the factors that control the rate at which these glaciers calve icebergs, melt, and flow into the ocean.

Icequakes
Representative icequakes produced by calving events observed at Yahtse Glacier, AK. (Bartholomaus et al., 2012)

My research is focused on understanding glacier dynamics, such as the controls on flow speed and terminus position. Changes in speed and terminus position have a major influence on glacier and ice sheet mass balance, and therefore the contribution of glaciers and ice sheets to sea level rise. I have addressed these topics at Alaskan glaciers as well as the Greenland and Antarctic Ice Sheets.  Within this framework, iceberg calving, subglacial processes, and glacier-generated seismicity are particular focuses of my recent studies.

More information on my most significant projects to date can be found through the links below the “Research” menu item, above.  These include: