* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project
Download 7. The Solar System
Outer space wikipedia , lookup
Tropical year wikipedia , lookup
Aquarius (constellation) wikipedia , lookup
Lunar theory wikipedia , lookup
Geocentric model wikipedia , lookup
Planets beyond Neptune wikipedia , lookup
Rare Earth hypothesis wikipedia , lookup
Astronomical unit wikipedia , lookup
Galilean moons wikipedia , lookup
Definition of planet wikipedia , lookup
History of Solar System formation and evolution hypotheses wikipedia , lookup
Astrobiology wikipedia , lookup
Dialogue Concerning the Two Chief World Systems wikipedia , lookup
Extraterrestrial atmosphere wikipedia , lookup
IAU definition of planet wikipedia , lookup
Solar System wikipedia , lookup
Extraterrestrial skies wikipedia , lookup
Planetary habitability wikipedia , lookup
Planets in astrology wikipedia , lookup
Formation and evolution of the Solar System wikipedia , lookup
Extraterrestrial life wikipedia , lookup
7.1 Planetary Configurations 133 7.1 Planetary Configurations The apparent motions of the planets are quite complicated, partly because they reï¬ect the motion of the Earth around the Sun (Fig. 7.3). Normally the planets move eastward (direct motion, counterclockwise as seen from the Northern hemisphere) when compared with the stars. Sometimes the motion reverses to the opposite or retrograde direction. After a few weeks of retrograde motion, the direction is changed again, and the planet continues in the original direction. It is quite understandable that the ancient astronomers had great difï¬culties in explaining and modelling such complicated turns and loops. Figure 7.4 explains some basic planetary conï¬gurations. A superior planet (planet outside the orbit of the Earth) is said to be in opposition when it is exactly opposite the Sun, i. e. when the Earth is between the planet and the Sun. When the planet is behind the Sun, it is in conjunction. In practise, the planet may not be exactly opposite or behind the Sun because the orbits of the planet and the Earth are not in the same plane. In astronomical almanacs oppositions and conjunctions are deï¬ned in terms of ecliptic longitudes. The longitudes of a body and the Sun differ by 180⦠at the moment of opposition; in conjunction the longitudes are equal. However, the right ascension is used if the other body is Fig. 7.3. (a) Apparent motion of Mars during the 1995 opposition. (b) Relative positions of the Earth and Mars. The projection of the EarthâMars direction on the inï¬nitely distant celestial sphere results in (a) Fig. 7.4. Planetary conï¬gurations. The angle α (Sunâobjectâ Earth) is the phase angle and ε (SunâEarthâobject) is the elongation not the Sun. Those points at which the apparent motion of a planet turns toward the opposite direction are called stationary points. Opposition occurs in the middle of the retrograde loop. Inferior planets (Mercury and Venus) are never in opposition. The conï¬guration occurring when either of these planets is between the Earth and the Sun is called inferior conjunction. The conjunction corresponding to that of a superior planet is called upper conjunction or superior conjunction. The maximum (eastern or western) elongation, i. e. the angular distance of the planet from the Sun is 28⦠for Mercury and 47⦠for Venus. Elongations are called eastern or western, depending on which side of the Sun the planet is seen. The planet is an âevening starâ and sets after the Sun when it is in eastern elongation; in western elongation the planet is seen in the morning sky as a âmorning starâ. The synodic period is the time interval between two successive events (e. g. oppositions). The period which we used in the previous chapters is the sidereal period, the true time of revolution around the Sun, unique