Seismic noise can serve as an indicator of wave action and sea ice coverage offshore.

Terrestrial Radar Interferometry can help detect how rising sea levels put pressure on Greenland’s Helheim Glacier.

Two projects show how remote sensing and geodetic tools can help us study changing ecosystems and landscapes.

A new study uses the latest maps of the structure beneath Antarctica to see how important realistic crust and mantle information is to sea level rise. The answer? It’s pretty important.

Wind-driven ocean waves beat on Earth’s seafloor, creating a continuous signal for which seismic stations around the world listen—a signal that is increasing.