We attribute this difference to an effective anisotropy due to fine layering. The layered structure of firn, ice, water and the seafloor results in a characteristic dispersion curve below 7 Hz.

In ice, water molecules are arranged in a repeating pattern that gives ice its crystal structure. Even though ice is at 0 °C, the molecules still vibrate. After freezing, the water molecules are ...

This repository includes VUMAT and VUSDFLD subroutines for simulating the elastoplastic behaviour of ice crushed in ice-structure collision simulations. They are both written in Fortran for the Abaqus ...

In making this study, two lines of investigation have been followed. In one, controlled laboratory measurements were made of the permittivity and loss tangent of ice and snow of varying density and ...

Department of Chemistry and Biochemistry, University of California San Diego, La Jolla, California 92093, United States Materials Science and Engineering, University of California San Diego, La Jolla, ...

Each January, when the haze of a new year clears, a hotel appears from the snow and ice outside Quebec City. As Hôtel de ...