
Researchers have deployed distributed acoustic sensing, or DAS, technology to study rapid ice deterioration in alpine glaciers. The method uses fiber optic cables to detect vibrations caused by fractures in ice, providing detailed real-time monitoring of glacial conditions. Scientists at ETH Zurich laid cables in a grid pattern on a Swiss glacier and used laser pulses to identify thousands of small seismic events, known as icequakes, that occur when meltwater forces its way into cracks and fractures the frozen structure.
The DAS approach offers significant advantages over traditional monitoring methods. A single fiber optic cable can function as thousands of individual strain sensors, effectively equivalent to deploying numerous seismometers across a glacier. The technology is also more cost-effective and safer for researchers, allowing them to collect continuous data without maintaining a permanent presence in dangerous terrain. During one week of fieldwork, researchers detected more than a thousand icequakes, demonstrating the sensitivity of the system.
The findings have important implications for understanding glacier stability. When meltwater seeps into cracks, it creates internal pressure that compromises structural integrity. This process, called hydrofracturing, is believed to contribute to potential catastrophic collapse of ice shelves and ice sheets in regions like Antarctica and Greenland, though the mechanism has not been previously studied in such detail. The research suggests that monitoring crack depth and density could provide early warning of dangerous changes.
Scientists envision developing DAS into an early-warning system for glacial hazards that threaten infrastructure and populated areas. The technology could also help track ice loss in Greenland and Antarctica, where warming waters and other dynamic processes accelerate melting. By providing unprecedented visibility into subsurface cracks and fractures, DAS offers a tool to better understand how quickly glaciers may break apart and contribute to sea level rise.
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