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Ecliptic coordinate system

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Ecliptic coordinate system

The ecliptic coordinate system is a celestial coordinate system commonly used for representing the positions and orbits of Solar System objects. Because most planets (except Mercury), and many small solar system bodies have orbits with small inclinations to the ecliptic, it is convenient to use it as the fundamental plane. The system's origin can be either the center of the Sun or the center of the Earth, its primary direction is towards the vernal (northbound) equinox, and it has a right-handed convention. It may be implemented in spherical or rectangular coordinates.[1]

Earth-centered Ecliptic coordinates as seen from outside the celestial sphere. Ecliptic longitude (red) is measured along the ecliptic from the vernal equinox. Ecliptic latitude (yellow) is measured perpendicular to the ecliptic. A full globe is shown here, although high-latitude coordinates are seldom seen except for certain comets and asteroids.

Primary direction

The apparent motion of the Sun along the ecliptic (red) as seen on the inside of the celestial sphere. Ecliptic coordinates appear in (red). The celestial equator (blue) and the equatorial coordinates (blue), being inclined to the ecliptic, appear to wobble as the Sun advances.

The celestial equator and the ecliptic are slowly moving due to perturbing forces on the Earth, therefore the orientation of the primary direction, their intersection at the Northern Hemisphere vernal equinox, is not quite fixed. A slow motion of Earth's axis, precession, causes a slow, continuous turning of the coordinate system westward about the poles of the ecliptic, completing one circuit in about 26,000 years. Superimposed on this is a smaller motion of the ecliptic, and a small oscillation of the Earth's axis, nutation.[2][3]

In order to reference a coordinate system which can be considered as fixed in space, these motions require specification of the equinox of a particular date, known as an epoch, when giving a position in ecliptic coordinates. The three most commonly used are:

  • Mean equinox of a standard epoch (usually J2000.0, but may include B1950.0, B1900.0, etc.)
is a fixed standard direction, allowing positions established at various dates to be compared directly.
  • Mean equinox of date
is the intersection of the ecliptic of "date" (that is, the ecliptic in its position at "date") with the mean equator (that is, the equator rotated by precession to its position at "date", but free from the small periodic oscillations of nutation). Commonly used in planetary orbit calculation.
  • True equinox of date
is the intersection of the ecliptic of "date" with the true equator (that is, the mean equator plus nutation). This is the actual intersection of the two planes at any particular moment, with all motions accounted for.

A position in the ecliptic coordinate system is thus typically specified true equinox and ecliptic of date, mean equinox and ecliptic of J2000.0, or similar. Note that there is no "mean ecliptic", as the ecliptic is not subject to small periodic oscillations.[4]

Spherical coordinates

Summary of notation for ecliptic coordinates[5]
  spherical rectangular
longitude latitude distance
geocentric λ β Δ  
heliocentric l b r x, y, z[note 1]
  1. ^ Occasional use; x, y, z are usually reserved for equatorial coordinates.

Ecliptic longitude or celestial longitude (symbols: heliocentric l, geocentric \lambda) measures the angular distance of an object along the ecliptic from the primary direction. Like right ascension in the equatorial coordinate system, the primary direction (0° ecliptic longitude) points from the Earth towards the Sun at the vernal equinox of the Northern Hemisphere. Because it is a right-handed system, ecliptic longitude is measured positive eastwards in the fundamental plane (the ecliptic) from 0° to 360°.

Ecliptic latitude or celestial latitude (symbols: heliocentric b, geocentric \beta), measures the angular distance of an object from the ecliptic towards the north (positive) or south (negative) ecliptic pole. For example, the north ecliptic pole has a celestial latitude of +90°.

Distance is also necessary for a complete spherical position (symbols: heliocentric r, geocentric \mathit\Delta). Different distance units are used for different objects. Within the Solar System, astronomical units are used, and for objects near the Earth, Earth radii or kilometers are used.

Historical usage

From antiquity through the 18th century, ecliptic longitude was commonly measured using twelve zodiacal signs, each of 30° longitude, a usage that continues in modern astrology. The signs approximately corresponded to the constellations crossed by the ecliptic. Longitudes were specified in signs, degrees, minutes, and seconds. For example, a longitude of 19° 55' 58" is 19°.933 east of the start of the sign Leo. Since Leo begins 120° from the vernal equinox, the longitude in modern form is 139° 55' 58".[6]

Rectangular coordinates

Heliocentric ecliptic coordinates. The origin is the center of the Sun. The fundamental plane is the plane of the ecliptic. The primary direction (the x axis) is the vernal equinox. A right-handed convention specifies a y axis 90° to the east in the fundamental plane; the z axis points toward the north ecliptic pole. The reference frame is relatively stationary, aligned with the vernal equinox.

There is a rectangular variant of ecliptic coordinates often used in orbital calculation. It has its origin at the center of the Sun, its fundamental plane in the plane of the ecliptic, its primary direction (the x axis) toward the vernal equinox, that is, the place where the Sun crosses the celestial equator in a northward direction in its annual apparent circuit around the ecliptic, and a right-handed convention, specifying a y axis 90° to the east in the fundamental plane and a z axis perpendicular to the x-y plane in a right-handed sense.[7]

These rectangular coordinates are related to the corresponding spherical coordinates by

x = r \cos b \cos l
y = r \cos b \sin l
z = r \sin b.

Conversion between celestial coordinate systems

Converting Cartesian vectors

Conversion from ecliptic coordinates to equatorial coordinates

\begin{bmatrix} x_{equatorial} \\ y_{equatorial} \\ z_{equatorial} \\ \end{bmatrix} = \begin{bmatrix} 1 & 0 & 0 \\ 0 & \cos \epsilon & -\sin \epsilon \\ 0 & \sin \epsilon & \cos \epsilon \\ \end{bmatrix} \! \cdot \! \begin{bmatrix} x_{ecliptic} \\ y_{ecliptic} \\ z_{ecliptic} \\ \end{bmatrix} [8]

Conversion from equatorial coordinates to ecliptic coordinates

\begin{bmatrix} x_{ecliptic} \\ y_{ecliptic} \\ z_{ecliptic} \\ \end{bmatrix} = \begin{bmatrix} 1 & 0 & 0 \\ 0 & \cos \epsilon & \sin \epsilon \\ 0 & -\sin \epsilon & \cos \epsilon \\ \end{bmatrix} \! \cdot \! \begin{bmatrix} x_{equatorial} \\ y_{equatorial} \\ z_{equatorial} \\ \end{bmatrix}

where \epsilon is the obliquity of the ecliptic.

See also

External links

  • The Ecliptic: the Sun's Annual Path on the Celestial Sphere Durham University Department of Physics
  • MEASURING THE SKY A Quick Guide to the Celestial Sphere James B. Kaler, University of Illinois

Notes and references

  1. ^ Nautical Almanac Office, U.S. Naval Observatory; H.M. Nautical Almanac Office, Royal Greenwich Observatory (1961). Explanatory Supplement to the Astronomical Ephemeris and the American Ephemeris and Nautical Almanac. H.M. Stationery Office, London. pp. 24–27. 
  2. ^ Explanatory Supplement (1961), pp. 20, 28
  3. ^ U.S. Naval Observatory, Nautical Almanac Office (1992). P. Kenneth Seidelmann, ed. Explanatory Supplement to the Astronomical Almanac. University Science Books, Mill Valley, CA. pp. 11–13.  
  4. ^ Meeus, Jean (1991). Astronomical Algorithms. Willmann-Bell, Inc., Richmond, VA. p. 137.  
  5. ^ Explanatory Supplement (1961), sec. 1G
  6. ^ Leadbetter, Charles (1742). A Compleat System of Astronomy. J. Wilcox, London. p. 94. , at Google books; numerous examples of this notation appear throughout the book.
  7. ^ Explanatory Supplement (1961), pp. 20, 27
  8. ^ Explanatory Supplement (1992), pp. 555-558
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