Glacier Perito Moreno, in the southern Patagonian Icefields, is now experiencing accelerated thinning, flow acceleration, and unprecedented frontal retreat, indicating the potential for buoyancy-driven retreat once it passes a subglacial ridge, according to observational data, bathymetric surveys, and satellite time series of surface elevation and velocity.
- Moritz Koch
- Christian Sommer
- Matthias H. Braun