Laboratory experiments inform iceberg-calving forces

Globally detected glacial earthquakes are produced during cubic-kilometer scale calving events. The mechanism producing these earthquakes and the dependence of the seismic moment on iceberg size and glacial calving front geometry are not well established. We use a laboratory-scale model of the post-fracture calving process to measure aspects of the calving process not observable in nature. In our experiments, buoyant plastic blocks rest against against a force plate (glacial terminus) which measures both the total force and the torque exerted during the calving process. The blocks are gravitationally unstable, so that they will spontaneously capsize and rotate away from the terminus. We find that hydrodynamics are crucial when considering the coupling between the calving process and the solid earth. There is both a pushing contact force and a simultaneous pulling hydrodynamic force created by a reduced pressure along the terminus face. This suggests that a single couple force mechanism is a more appropriate mode for glacial earthquakes than the commonly used centroid single force model.