Scattering of Fexural Gravity Waves by a Two-Dimensional Thin Plate

extent the flow of the ice sheet. In this study we use an ide- alised lake geometry to study this impact. We employ a) an improved three-dimensional full-Stokes ice flow model with

We have performed model calculations of the plasma density perturbations caused by a gravity wave and an oscillating electric field to reproduce the daytime and nighttime

The optical phonons are usually obtained from inelastic Raman scattering or infrared spectroscopy (transmission or re fl ection), whose activities depend on several particular

Os resultados do ensaio da atividade enzimática indicam que não houve diferença relevante nos níveis de expressão de XK para as linhagens condicionadas e originais, à exceção da

The horizontal wavelengths of gravity waves in an image can be estimated by analysing the data series of the pixel inten- sities along a cross section perpendicular to the wave

the dispersion equation is then used to analyse the apillary-wave resistane, that is the drag fore.. assoiated to the emission of waves by a moving disturbane at a free

simultaneous atmospheric gravity waves and long ocean wave events, similarities of the spectral structures of both waving phenomena and the high efectiveness in the

Figure (6) displays the variation of the real and the imaginary parts of the normalized electric field on z = 0 as a function of | k3 | x , for the vertical dike model with