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Wave turbulence or convective instability induced by third-order dispersion and/or Raman scattering have also been employed to describe the formation of optical rogue waves. [ 40 ] [ 41 ] [ 49 ] Third-order dispersion and Raman scattering play a central role in the generation of large redshifts, and turbulence treats the statistical properties ...
Physical optics is also the name of an approximation commonly used in optics, electrical engineering and applied physics. In this context, it is an intermediate method between geometric optics , which ignores wave effects, and full wave electromagnetism , which is a precise theory .
In geometrical optics, light is considered to travel in straight lines, while in physical optics, light is considered as an electromagnetic wave. Geometrical optics can be viewed as an approximation of physical optics that applies when the wavelength of the light used is much smaller than the size of the optical elements in the system being ...
Fermat's principle is most familiar, however, in the case of visible light: it is the link between geometrical optics, which describes certain optical phenomena in terms of rays, and the wave theory of light, which explains the same phenomena on the hypothesis that light consists of waves.
Fourier optics begins with the homogeneous, scalar wave equation (valid in source-free regions): (,) = where is the speed of light and u(r,t) is a real-valued Cartesian component of an electromagnetic wave propagating through a free space (e.g., u(r, t) = E i (r, t) for i = x, y, or z where E i is the i-axis component of an electric field E in the Cartesian coordinate system).
[11] [12] A finite ray or real ray is a ray that is traced without making the paraxial approximation. [12] [13] A parabasal ray is a ray that propagates close to some defined "base ray" rather than the optical axis. [14] This is more appropriate than the paraxial model in systems that lack symmetry about the optical axis.
Evanescent wave; Fluorescence, also called luminescence or photoluminescence; Mie scattering (Why clouds are white) Metamerism as of alexandrite; Moiré pattern; Newton's rings; Phosphorescence; Pleochroism gems or crystals, which seem "many-colored" Rayleigh scattering (Why the sky is blue, sunsets are red, and associated phenomena) Reflection ...
Visulization of flux through differential area and solid angle. As always ^ is the unit normal to the incident surface A, = ^, and ^ is a unit vector in the direction of incident flux on the area element, θ is the angle between them.