halo(redirected from Halo (meteorology))
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halo,in art: see nimbusnimbus
, in art, the luminous disk or circle or other indication of light around the head of a sacred personage. It was used in Buddhist and other Asian art and by the early Greeks and Romans to designate gods and heroes and appeared in Christian art in the 5th cent.
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halo,in meteorology, short-lived circles or arcs, and less commonly spikes and crosses, of colored or whitish light surrounding the moon or sun or in clouds as seen from above. A halo occurs when the light from the sun or the moon is refracted and reflected by ice crystals in the atmosphere, usually in a thin layer of high cirrostratus clouds. Under certain circumstances a second, or outer, halo appears, which is fainter than the inner one. At times white or colored luminous arcs are also seen lying somewhat parallel to the horizon and passing through the source of light, called mock suns, parhelia, or sun dogs for the sun, and paraselenae for the moon. A single mock sun, the anthelion, directly opposite the sun, may be added. In general a white halo results from the reflection of light by ice crystals, while one which appears as colored rings results from the refraction of light by ice crystals. Halos are more brilliant and complex near the poles than in other parts of the world. The theory attributing their formation to the presence of ice crystals was first suggested by the 17th cent. French philosopher Descartes. Similar to a halo and sometimes confused with it is the sun's coronacorona,
luminous envelope surrounding the sun, outside the chromosphere. Its density is less than one billionth that of the earth's atmosphere. The corona is visible only at the time of totality during a total eclipse of the sun.
..... Click the link for more information. . In X-ray electron diffraction, the term halos refers to the broad rings that appear on a photographic film as a result of the diffraction of a monoenergetic beam of X rays or electrons from a crystalline powder located at the center of the camera.
several optical phenomena in the atmosphere that are due to the refraction and reflection of light by ice crystals forming cirrus clouds and fogs.
There is a great variety of halo phenomena: they take the form of iridescent (for refraction) and white (for reflection) bands, spots, arcs, and circles in the firmament. The most common forms are iridescent circles around the disk of the sun or moon at an angular radius of either 22° or 46°; parhelia, or “mock suns,” which are bright iridescent spots to the right and left of the sun or moon at distances of 22°, rarely at 46°; a circumzenithal arc, which is a segment of an iridescent arc touching the upper point of a 46-degree circle that turns its convex side toward the sun; a parhelic circle, which is a white horizontal circle passing across the disk of the luminary; a column, which is part of a white vertical circle passing across the luminary’s disk; and a white cross formed by the combination of the parhelic circle with the column. Halos differ from coronas, which, though outwardly alike, have other origins related to diffraction.
In order for certain halos to occur, ice crystals, which have the shape of six-sided prisms, must be oriented the same way or predominantly the same way with respect to the vertical. The theory of halos has been developed in detail. Thus, the 22-degree parhelia occur because of the refraction of rays in the vertically oriented crystals when a ray passes through the faces forming angles of 60°; the 46-degree circle is created by refraction when the faces form angles of 90°; and the vertical and horizontal circles are obtained as a result of reflection from horizontal and vertical faces of the crystals.
REFERENCEMinnaert, M. Svet i tsvet v prirode. Moscow, 1958. (Translated from English.)
(in optics), the light background around the image of a source of optical radiation that can be observed by the eye or recorded by a light detector. Halos are caused by light scattering at small angles in the medium through which the light is passing.
The size, color, and brightness of a halo depend on the dimensions and physical nature of the particles of the medium and on the optical thickness of the medium. Scattering at small angles, resulting in the formation of halos, is especially strong in media of small optical thickness with particles whose dimensions are greater than the wavelength λ of the radiation (the Mie effect). If the dimensions of the particles greatly exceed λ, the intensity of scattering is independent of λ. This explains, for example, the “white” color of the halo surrounding the solar disk (the combination of rays with different λ gives white light). Halos significantly affect the resolving power of photographic materials and luminescent screens and, consequently, the quality of the images produced by them. The character of a halo is taken into account in measuring the transparency of scattering media; in particular, the change in the brightness and spectral distribution of light in the solar halo is a criterion of atmospheric purity and transparency.
L. N. KAPORSKII
What does it mean when you dream about a halo?
A dream of oneself with a halo may signify that perfection is a goal for the dreamer. Alternatively, it may represent an exaggerated “holier than thou” attitude.
ii. A high-altitude, low-opening (HALO) paradrop system. The paratroopers jump from aircraft at very high altitudes and open their parachutes at very low heights. This technique ensures rapid infiltration and tactical surprise. The latter is achieved as the paratroopers can jump from the aircraft, which is flying some distance away from the drop zone.
iii. The reflection of cockpit instruments seen in a canopy at night.
iv. The colored ring seen on clouds in the direction away from the sun (i.e., with the aircraft's shadow at the center). Also called a pilot's halo.
v. A bright ring around the spot produced by a beam of electrons striking the fluorescent coating in a cathode-ray tube.