Subglacial water flow strongly modulates glacier basal motion, which itself strongly
influences the contributions of glaciers and ice sheets to sea level rise. However, our …

Progress in our understanding of wave–ice interactions is currently hindered by the lack of in
situ observations and information of sea-ice properties, including the elastic modulus. Here …

Dense seismic array monitoring combined with advanced processing can help retrieve and
locate a variety of seismic sources with unprecedented resolution and spatial coverage. We …

For the release of a slab avalanche, crack propagation within a weak snowpack layer below
a cohesive snow slab is required. As crack speed measurements can give insight into …

Early borehole and surface distributed acoustic sensing (DAS) experiments have
demonstrated the viability of the method in glacial settings and allowed new insights. The …

Due to global warming, the decline in the Arctic sea ice has been accelerating over the last 4
decades, with a rate that was not anticipated by climate models. To improve these models …

Despite their high potential for accurate sea ice properties estimation, seismic methods are
still limited by the difficulty of access and the challenging logistics of polar environments …

In the perspective of upcoming seasonally ice-free Arctic, understanding the dynamics of
sea ice in the changing climate is a major challenge in oceanography and climatology. In …

This research investigates the dynamic response of offshore wind turbine (OWT) systems
subject to ice-structure-soil interaction (ISSI). To simulate the behavior of level ice sheets, a …

The rapidly warming Arctic ocean demands new ways to monitor and characterize changes
in sea-ice distribution, thickness, and mechanical properties. Upward-looking sonars …