| Atmospheric Refraction |
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| CATEGORIES ABOUT ATMOSPHERIC REFRACTION | |
| observational astronomy | |
| atmospheric and ocean optics | |
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Atmospheric refraction causes Astronomical Object s to appear higher in the sky than they are in reality. It affects not only lightrays but all electromagnetic radiation, although in varying degrees (see Dispersion (optics) ). For example in visible light, blue is more affected than red. This may cause astronomical objects to be spread out into a spectrum in high-resolution images. Whenever possible Astronomers will always schedule their observations around the time of Culmination of an object when it is highest in the sky. Likewise sailors will never shoot a star which is not at least 20° or more above the horizon. If observations close to the horizon cannot be avoided, it is possible to equip a Telescope with control systems to compensate for the shift caused by the refraction. If the dispersion is a problem too, (in case of broadband high-resolution observations) atmospheric refraction correctors can be employed as well (made from pairs of rotating glass prisms). But as the amount of atmospheric refraction is function of temperature and pressure as well as humidity (the amount of water vapour especially important at mid-infrared wavelengths) the amount of effort needed for a successful compensation can be prohibitive. It gets even worse when the atmospheric refraction is not homogenous, when there is turbulence in the air for example. This is the cause of Twinkling of the stars and deformation of the shape of the sun at sunset and sunrise. VALUES The atmospheric refraction is zero in the zenith, is less than 1' (one one should apply additional corrections for the Horizontal Parallax of the moon, its apparent diameter and its Phase , although the latter is seldom done. The refraction is also a function of temperature and pressure. The values given above are for 10 °C and 1003 mbar. Add 1% to the refraction for every 3° C colder, subtract if hotter (hot air is less dense, and will therefore have less refraction). Add 1% for every 9 mbar higher pressure, subtract if lower. Evidently day to day variations in the weather will affect the exact times of sunrise and sunset as well as moonrise and moonset, and for that reason are never given more accurate than to the nearest whole minute in the Almanacs . Finally as the atmospheric refraction is 34' on the horizon, but only 29' half a degree above it, the setting or rising sun seems to be flattend by about 5' or 1/6 of its apparent diameter. SEE ALSO |
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