apparent magnitude
Quick Summary
In astronomy, apparent magnitude is a measure of how bright a celestial object appears from Earth. The brighter an object, the lower its magnitude number. This system, refined by Norman Robert Pogson in 1850, uses a scale where one magnitude difference equates to a brightness ratio of approximately 2.512. A difference of five magnitudes represents a 100:1 brightness ratio. Negative magnitudes are used for objects brighter than the traditional scale's brightest stars.12
For example, the Sun has an apparent magnitude of -26.7, the full Moon is around -11, and Sirius, a bright star, is -1.5. The faintest objects detectable by the Hubble Space Telescope have an apparent magnitude of about 30. This measurement is a key aspect of photometry, the science of measuring celestial brightness to understand objects' properties like temperature and distance.13
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