Over the past quarter of a century the Arctic has warmed more than any other region on
Earth, causing a profound impact on the Greenland ice sheet (GrIS) and its contribution to …

This review provides updated estimates of the glacial isostatic adjustment (GIA) component
of present-day uplift at a suite of Global Navigation Satellite System (GNSS) sites in …

Abstract Digital Elevation Models (DEMs) play a prominent role in glaciological studies for
the mass balance of glaciers and ice sheets. By providing a time snapshot of glacier …

To better understand recent rapid recession of marine-terminating glaciers in Greenland, we
performed satellite and field observations near the calving front of Bowdoin Glacier, a 3 km …

Observations over the past decade show significant ice loss associated with the speed-up of
glaciers in southeast Greenland from 2003, followed by a deceleration from 2006. These …

Along the coastal areas of northwest Greenland, sea ice is crucial to people's livelihoods.
People in the region have long depended on hunting marine mammals such as seals; …

In order to model and predict future behavior of marine terminating glaciers, it is essential to
understand the different factors that control a glaciers response to climate change. Here we …

Vertical land motion (VLM) from past and ongoing glacial changes can amplify or mitigate
ongoing relative sea level change. We present a high‐resolution VLM model for the wider …

Studies of global sea level often exclude Tide Gauges (TGs) in glaciated regions due to
vertical land movement. Recent studies show that geodetic GNSS stations can be used to …

The mass flux from marine terminating glacier outlets from the Greenland ice sheet is a
significant mass budget term. Yet, glacier calving sensitivity to climate parameters is not well …