Jakobshavn Isbræ is is the most active Greenland outlet glacier. We have studied its dynamics and calving in several projects.

• (2014) Quantifying velocity response to ocean tides and calving near the terminus of Jakobshavn Isbræ, Greenland
• (2012) Observing calving-generated ocean waves with coastal broadband seismometers, Jakobshavn Isbræ, Greenland
• (2009) Calving icebergs indicate a thick layer of temperate ice at the base of Jakobshavn Isbræ, Greenland
• (2008) Glacier, fjord, and seismic response to recent large calving events, Jakobshavn Isbræ, Greenland
• (2003) Indication of active overthrust faulting along the Holocene-Wisconsin transition in the marginal zone of Jakobshavn Isbræ
• (2002) Mechanisms of fast flow in Jakobshavn Isbræ, West Greenland: Part III. Measurements of ice deformation, temperature and cross-borehole conductivity in boreholes to the bedrock