

In 1932 determination of the parallax displacement of the asteroid Eros as it made a close approach to Earth yielded what was at the time a very precise value for the astronomical unit. Later efforts made use of widely separated observations of the transit of Venus across the Sun’s disk to measure the distance between Venus and Earth. In 1672 the Italian-born French astronomer Gian Domenico Cassini made a reasonably close estimate of the astronomical unit based on a determination of the parallax displacement of the planet Mars-and thus its distance to Earth. To establish the scale for all orbits and to determine the astronomical unit, all that was needed was an accurate measurement of the distance between any two objects at a given instant. You may have heard the slang, but how much do you really know about space.cadet? Launch into this quiz and begin your journey of planets and the universe.īy the 17th century astronomers understood the geometry of the solar system and the motion of the planets well enough to develop a proportional model of objects in orbit around the Sun, a model that was independent of a particular scale. In practice, however, the method cannot be applied, because the Sun’s intense glare blots out the background stars needed for the parallax measurement. A simple trigonometric relationship incorporating this angular value and the baseline length then could be used to find the Earth-Sun distance.

Comparison of the observations would reveal an apparent shift, or angular (parallax) displacement, of the Sun against the remote stars. In this approach, two observers stationed at the ends of a long, accurately known baseline-ideally, a baseline as long as Earth’s diameter-would simultaneously record the position of the Sun against the essentially motionless background of the distant stars. In principle, the easiest way to determine the value of the astronomical unit would have been to measure the Earth-Sun distance directly by means of the parallax method. For example, stating that the planet Jupiter is 5.2 AU (5.2 Earth distances) from the Sun and that Pluto is nearly 40 AU gives ready comparisons of the distances of all three bodies. The astronomical unit provides a convenient way to express and relate distances of objects in the solar system and to carry out various astronomical calculations. Alternately, it can be considered the length of the semimajor axis-i.e., the length of half of the maximum diameter-of Earth’s elliptical orbit around the Sun.

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