Kadri says the typical water
wave equations used to characterize ocean wave interactions do not apply to acoustic - gravity waves, as they do not factor in compressibility and gravity effects.
Not exact matches
«When the physical model of
wave - motion in a material medium had to be abandoned in physics», writes Mary Hesse, «it left its traces in the kind of mathematics which was
used, for this was still a mathematical language derived from the
wave equations of fluid motion, and so, for the mathematician, it carried some of the imaginative associations of the original physical picture.»
Polkinghorne's scientific background is everywhere evident; often he
uses examples from the laboratory: the historical appearance of Jesus in the world is seen in terms of the apparently undramatic discovery of penicillin on a windowsill; the two natures in Christ find a possible parallel in the
wave / particle duality of light, and Dirac's
equation concerning quantum mechanics is
used in reference to the doctrine of the Trinity.
This relation of the Schrödinger
equation to classical
waves is already revealed in the way that a variant called the nonlinear Schrödinger
equation is commonly
used to describe other classical
wave systems — for example in optics and even in ocean
waves, where it provides a mathematical picture of unusually large and robust «rogue
waves.»
Schrödinger drew on his deep knowledge of classical mechanics, and his
equation in many ways resembles those
used for ordinary
waves.
In this story, and in his latest book, 17
Equations that Changed the World, Ian Stewart
uses Maxwell's
equation for electromagnetic
waves propagating in a vacuum.
The seven I focus on here — the
wave equation, Maxwell's four
equations, the Fourier transform and Schrödinger's
equation — illustrate how empirical observations have led to
equations that we
use both in science and in everyday life.
In the accompanying video, we
use the longer version of the
equation that doesn't depend on the
waves moving through a vacuum.
Perhaps most importantly, the approach
used can be applied to other physical phenomena that are described by
wave equations, such as acoustics.
Simmons, with the help of the Arctic Region Supercomputer Center, which is part of the UAF Geophysical Institute,
used math
equations to make detailed numerical simulations, or high - resolution models, of under - ocean
wave processes.
First, they spotted clusters of
waves that tend to roll along together, then they analyzed each cluster's length and height, and they finally
used a combination of statistics and dynamical
equations to determine which of those clusters was most likely to go rogue.
«
Using data and
equations, we've determined for any given sea state the
wave groups that can evolve into rogue
waves,» Sapsis says.
Propagation of
waves through an astrophysical disk can be understood
using Schrödinger's
equation - a cornerstone of quantum mechanics.
An engaging activity introducing students to the
wave equation, giving them an understanding of some of the vocabulary and concepts
used.
The
equations for Rossby
waves (Calculation of the Meridional
Wave Number, Physics of the Parameter, and Calculation of the Amplitudes) show that this can occur if a set of necessary conditions are met: u ¯ > 0 in the midlatitude region; the highest value of l within the waveguide is in the range of the meridional
wave numbers lm dominantly contributing to the external forcing with a given m, which provides closeness of the k
waves to respective m
waves not only in terms of the zonal but also the meridional
wave numbers, favoring the QRA of the m
waves; the total latitudinal width of the waveguide is no less than the characteristic spatial scale of the relevant Airy function (25), which is
used as the boundary condition at its southern and northern boundaries; and latitudinal distribution of l is sufficiently smooth in the waveguide, and both TPs lie within a midlatitude region of ∼ 25 ° N — 30 ° N and ∼ 65 ° N − 70 ° N, as the necessary condition for the application of quasilinear Wentzel − Kramers − Brillouin (WKB) method (25) when solving the
equations for Rossby
waves.
To obtain the
equation for A˜m, b, we
use the parameterization of the
wave activity A during the
wave breaking proposed in ref.