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Polarizers θ
Polarizers θ

Étendue and spectral resolution
Étendue and spectral resolution

... The finesse is a measure of the spectral resolution that can be achieved with an interferometer for a specified FSR – which is determined by experimental requirements. Ideally the interferometer plates should be illuminated by parallel rays of light and these rays should be in the wedge plane of the ...
Early Estimates of the Velocity of Light
Early Estimates of the Velocity of Light

Transmisi Optik Pertemuan 10
Transmisi Optik Pertemuan 10

... Bina Nusantara Bina Nusantara ...
Optical Broadband Angular Selectivity Yichen Shen, Dexin Ye, Ivan Celanovic,
Optical Broadband Angular Selectivity Yichen Shen, Dexin Ye, Ivan Celanovic,

Optical forces through guided light deflections
Optical forces through guided light deflections

Dunlap Institute Summer School: Fourier Transform Spectroscopy Lab
Dunlap Institute Summer School: Fourier Transform Spectroscopy Lab

Correlated diffraction and fluorescence in the backscattering
Correlated diffraction and fluorescence in the backscattering

... In this situation, the very absorbing black areas catch much of the solar illumination and frequent wing reorientation moves, observed at that moment, are likely associated with some kind of thermal control. The genus Troides has the widest distribution in Troidini, with a diversity of 17–22 species ...
PHASE CONTRAST MICROSCOPY
PHASE CONTRAST MICROSCOPY

... the incoming wavefronts but mainly changes phase relations with respect to the "unperturbed" wavefronts, newly generated spherical wave fronts that are retarded by 90° (λ/4) emanate from 'O' (see the purple area that contains now "unperturbed" plane waves and spherical wave fronts). It is important ...
Rays and Optical beams
Rays and Optical beams

Zeeman Effect - UCI Physics and Astronomy
Zeeman Effect - UCI Physics and Astronomy

... that the laser beam passes through the pinhole aperture and emerges from the collimater lens without diverging from the optical axis (this can be tedious!). Next, check the alignment of the Fabry-Perot interferometer. Set the spearation between plates to .5 cm. To make sure the beam incident on the ...
Viewpoint - Complex Photonic Systems | COPS
Viewpoint - Complex Photonic Systems | COPS

... In the current experiments the number of measured matrix elements is impressive (65536), yet the transmission matrix of the full area of the sample is even larger. Nevertheless, the matrix measured by Popoff et al. was sufficiently large to test an important baseline prediction of random matrix theo ...
Chapter 23
Chapter 23

... Atmospheric Refraction • There are many interesting results of refraction in the atmosphere • At sunsets, light rays from the sun are bent as they pass into the atmosphere • It is a gradual bend because the light passes through layers of the atmosphere, and each layer has a slightly different index ...
Computational photography with plenoptic camera and light field
Computational photography with plenoptic camera and light field

... of the monochromatic light ray. When considering color image formation, we can assume that the light field is a threecomponent vector with radiance information on the red, green, and blue components or any corresponding wavelengths. In a typical camera, the two-plane parameterization may be applied ...
HOLO TEXT
HOLO TEXT

Optical Fiber Communication
Optical Fiber Communication

... fiber are classified into two types: (i) Single mode fiber (SMF) and (ii) Multi-mode fiber (MMF) • Single-mode fibers – in single mode fiber only one mode can propagate through the fiber. This type of fiber has small core diameter(5um) and high cladding diameter(70um) and the difference between the ...
Chiroptical Spectroscopy - Ruhr
Chiroptical Spectroscopy - Ruhr

Physics II - Magnetism
Physics II - Magnetism

F - Images
F - Images

... to the surface of the mirror. Incident Ray: is the ray of light that is striking the mirror. Reflected Ray: is the ray of light that bounces off the mirror. ...
[pdf]
[pdf]

... The theory of DWS makes the connection between temporal intensity fluctuations of the speckle field emerging from the sample and the dynamics of the particles in the sample. In this section, we present the basic result of DWS and highlight some of the assumptions commonly associated with DWS. This i ...
PDF
PDF

... tectable in the unheated film,though substantial zero angle scattering is evident. This intense zero angle scattering has been observed in many ionomer samples with no agreement as to its origin. From the changes in the zero angle scattering observed in these experiments as a function of temperature ...
A new spectrally sharpened sensor basis to
A new spectrally sharpened sensor basis to

doc - IYPT Archive
doc - IYPT Archive

07 Propagation of Waves
07 Propagation of Waves

... wave. The sum of these secondary spherical “wavelets” produced the subsequent wavefronts. Huygens’ principle had the glaring disadvantage that these secondary spherical wavefronts propagated “backwards” as well as forwards. This problem was later solved by Fresnel and Kirchhoff in the 19th century. W ...
24.1 - 24.4
24.1 - 24.4

... The light from the two slits form a visible pattern on a screen The pattern consists of a series of bright and dark parallel bands called fringes Constructive interference occurs where a bright fringe appears Destructive interference results in a dark fringe ...
< 1 ... 32 33 34 35 36 37 38 39 40 ... 102 >

Atmospheric optics



Atmospheric optics deals with how the unique optical properties of the Earth's atmosphere cause a wide range of spectacular optical phenomena. The blue color of the sky is a direct result of Rayleigh scattering which redirects higher frequency (blue) sunlight back into the field of view of the observer. Because blue light is scattered more easily than red light, the sun takes on a reddish hue when it is observed through a thick atmosphere, as during a sunrise or sunset. Additional particulate matter in the sky can scatter different colors at different angles creating colorful glowing skies at dusk and dawn. Scattering off of ice crystals and other particles in the atmosphere are responsible for halos, afterglows, coronas, rays of sunlight, and sun dogs. The variation in these kinds of phenomena is due to different particle sizes and geometries.Mirages are optical phenomena in which light rays are bent due to thermal variations in the refraction index of air, producing displaced or heavily distorted images of distant objects. Other optical phenomena associated with this include the Novaya Zemlya effect where the sun appears to rise earlier or set later than predicted with a distorted shape. A spectacular form of refraction occurs with a temperature inversion called the Fata Morgana where objects on the horizon or even beyond the horizon, such as islands, cliffs, ships or icebergs, appear elongated and elevated, like ""fairy tale castles"".Rainbows are the result of a combination of internal reflection and dispersive refraction of light in raindrops. Because rainbows are seen on the opposite side of the sky as the sun, rainbows are more prominent the closer the sun is to the horizon due to their greater distance apart.
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