Surface transition on ice induced by the formation of a grain boundary.

In model simulations we investigated the sensitivity of the CP ratio to the dielectric constant, ice thickness, ice surface roughness, and radar incidence angle.. From the results

Ice nucleation active surface site (INAS) densities were calculated to quantify the ice nucleation efficiency as a function of temperature, humidity and the aerosol surface

results show that the coupling effect of Hf and B changes the solidifi cation structure morphology and strongly refi nes the grain size. %), the solidification

These results show that for the same grain width (0.52 mm) an increase in the grain length causes an immedi- ate increase in the fracture toughness of silicon nitride, independent

of vertical transport by measuring u ∗ directly, and under katabatic conditions, estimate boundary layer depth (Ne ff et al., 2007) as well as giving wind speed, direction

The aspects subjected to evaluation included: the grain areas, shape and elongation coefficients of grains on a non-planar surface of the blade airfoil, using measurements taken

This data is used to define the ice active surface site density per saturation interval ( k ( s ice )) by dividing the change in ice particle number by the total surface area

Over East China, when the NHS occurs at perihelion, the ice sheets reinforce the summer precipitation due to a wave train topographically induced by the Eurasian ice sheet