Satellite radar interferometry data reveals that the grounding line of Petermann Glacier,
Greenland migrates by several kilometers during the tidal cycle, bringing pressurized …

Warming of the ocean waters surrounding Greenland plays a major role in driving glacier
retreat and the contribution of glaciers to sea level rise. The melt rate at the junction of the …

Understanding grounding line dynamics is critical for projecting glacier evolution and sea
level rise. Observations from satellite radar interferometry reveal rapid grounding line …

We update observationally based estimates of subaqueous melt, Qm, beneath Petermann
Glacier Ice Shelf (PGIS), Greenland, and model its sensitivity to oceanic thermal forcing, TF …

Ice velocity variations near the terminus of Jakobshavn Isbræ, Greenland, were observed
with a terrestrial radar interferometer (TRI) during three summer campaigns in 2012, 2015 …

We have developed an automatic method to identify changes in the position of calving
glacier margins using daily MODIS imagery. Application of the method to 32 ocean …

Petermann Glacier is a major outlet glacier of northern Greenland that drains a marine‐
based basin vulnerable to destabilization from enhanced oceanic and atmospheric forcings …

We present three‐dimensional, high‐resolution simulations of ice melting at the calving face
of Store Glacier, a tidewater glacier in West Greenland, using the Massachusetts Institute of …

Seafloor topography shapes the pathways of ocean currents transporting ocean heat and,
thus, is a fundamental boundary condition for modeling ocean‐ice interactions. However …

Marine‐terminating glaciers control most of Greenland's ice discharge into the ocean, but
little is known about the geometry of their frontal regions. Here we use side‐looking …