Researchers in the Stanford Radio Glaciology lab use radio waves to understand rapidly changing ice sheets and their contributions to global sea-level rise. This technique has revealed groundwater beneath Greenland, the long-term impacts of extreme melt, a process that could accelerate ice sheet mass loss in Antarctica, the potential instability of an ice sheet that could raise sea levels by 10 feet, and more. Researchers in the Stanford Radio Glaciology lab use radio waves to understand rapidly changing ice sheets and their contributions to global sea-level rise. This technique has revealed groundwater beneath Greenland, the long-term impacts of extreme melt, a process that could accelerate ice sheet mass loss in Antarctica, the potential instability of an ice sheet that could raise sea levels by 10 feet, and more. Earth Sciences Environment Phys.org – latest science and technology news stories
A blueprint for mapping melting ice sheets: Open-source tool can help make radar systems at a fraction of the cost
