geometric albedo oor Sjinees

geometric albedo

Vertalings in die woordeboek Engels - Sjinees

幾何反照率

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albedo subtype
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Vertoon algoritmies gegenereerde vertalings

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The geometric albedo of the ring particles does not exceed 5–6%, while the Bond albedo is even lower—about 2%.
本版本只能处理传真文件LASER-wikipedia2 LASER-wikipedia2
This is in contrast to other definitions of albedo such as the geometric albedo, which can be above 1.
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In general, though, the Bond albedo may be greater or smaller than the geometric albedo, depending on surface and atmospheric properties of the body in question.
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^ The geometric albedo of an astronomical body is the ratio of its actual brightness at zero phase angle (i.e. as seen from the light source) to that of an idealized flat, fully reflecting, diffusively scattering (Lambertian ) disk with the same cross-section.
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The Bond albedo is a value strictly between 0 and 1, as it includes all possible scattered light (but not radiation from the body itself). This is in contrast to other definitions of [[albedo]] such as the geometric albedo, which can be above 1.
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Puck and Mab are the two outermost inner satellites of Uranus. All inner moons are dark objects; their geometrical albedo is less than 10%.[21] They are composed of water ice contaminated with a dark material—probably radiation-processed organics.[22] The small inner moons constantly perturb each other.
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Puck and Mab are the two outermost inner satellites of Uranus. All inner moons are dark objects; their geometrical albedo is less than 10%.[21] They are composed of water ice contaminated with a dark material—probably radiation-processed organics.[22] The small inner moons constantly perturb each other.
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All of Neptune's inner moons are dark objects: their geometric albedo ranges from 7 to 10%.[18] Their spectra indicate that they are made from water ice contaminated by some very dark material, probably complex organic compounds . In this respect, the inner Neptunian moons are similar to the inner moons of Uranus .[5]
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There is a snag when using these expressions to estimate the temperature of a particular asteroid. The calculation requires the Bond albedo A (the proportion of total incoming power reflected, taking into account all directions), while the IRAS and MSX albedo data that is available for asteroids gives only the geometric albedo p which characterises only the strength of light reflected back to the source (the Sun).
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Some complicated modelling of surface and thermal properties can lead to estimates of the Bond albedo given the geometric one, but this far is beyond the scope of a quick estimate for these articles. It can be obtained for some asteroids from scientific publications.
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10 sinne gevind in 4 ms. Hulle kom uit baie bronne en word nie nagegaan nie.