The apparent daily motion of celestial bodies across the sky from east to west. It results from the Earth's rotation from west to east, the axis of the diurnal motion coinciding with the Earth's axis. The apparent path of a celestial body arising from diurnal motion is a circle parallel to the celestial equator and is termed a diurnal circle.
Telephoto lenses increase the length of the trails, since they effectively magnify the sky's diurnal motion on the film, while wide-angle lenses diminish it.
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