Parallactic Angle
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In
spherical astronomy Spherical astronomy, or positional astronomy, is a branch of observational astronomy used to locate astronomical objects on the celestial sphere, as seen at a particular date, time, and location on Earth. It relies on the mathematical methods o ...
, the parallactic angle is the angle between the great circle through a
celestial object An astronomical object, celestial object, stellar object or heavenly body is a naturally occurring physical entity, association, or structure that exists in the observable universe. In astronomy, the terms ''object'' and ''body'' are often u ...
and the
zenith The zenith (, ) is an imaginary point directly "above" a particular location, on the celestial sphere. "Above" means in the vertical direction ( plumb line) opposite to the gravity direction at that location ( nadir). The zenith is the "high ...
, and the
hour circle In astronomy, the hour circle, which together with declination and distance (from the planet's centre of mass) determines the location of any celestial object, is the great circle through the object and the two celestial poles. As such, it is a ...
of the object. It is usually denoted ''q''. In the triangle zenith—object—celestial pole, the parallactic angle will be the
position angle In astronomy, position angle (usually abbreviated PA) is the convention for measuring angles on the sky. The International Astronomical Union defines it as the angle measured relative to the north celestial pole (NCP), turning positive into the ...
of the zenith at the celestial object. Despite its name, this angle is unrelated with parallax. The parallactic angle is zero or 180° when the object crosses the meridian.


Uses

For ground-based observatories, the Earth atmosphere acts like a prism which disperses light of different wavelengths such that a star generates a
rainbow A rainbow is a meteorological phenomenon that is caused by reflection, refraction and dispersion of light in water droplets resulting in a spectrum of light appearing in the sky. It takes the form of a multicoloured circular arc. Rainbows c ...
along the direction that points to the zenith. So given an astronomical picture with a coordinate system with a known direction to the
Celestial pole The north and south celestial poles are the two points in the sky where Earth's axis of rotation, indefinitely extended, intersects the celestial sphere. The north and south celestial poles appear permanently directly overhead to observers a ...
, the parallactic angle represents the direction of that prismatic effect relative to that reference direction. Knowledge of that angle is needed to align Atmospheric Dispersion Correctors with the beam axis of the telescope Depending on the type of mount of the
telescope A telescope is a device used to observe distant objects by their emission, absorption, or reflection of electromagnetic radiation. Originally meaning only an optical instrument using lenses, curved mirrors, or a combination of both to observ ...
, this angle may also affect the orientation of the celestial object's disk as seen in a telescope. With an equatorial mount, the cardinal points of the celestial object's disk are aligned with the vertical and horizontal direction of the view in the telescope. With an altazimuth mount, those directions are rotated by the amount of the parallactic angle. The cardinal points referred to here are the points on the limb located such that a line from the center of the disk through them will point to one of the celestial poles or 90° away from them; these are not the
cardinal points The four cardinal directions, or cardinal points, are the four main compass directions: north, east, south, and west, commonly denoted by their initials N, E, S, and W respectively. Relative to north, the directions east, south, and west are at ...
defined by the object's axis of rotation. The orientation of the disk of the Moon, as related to the horizon, changes throughout its
diurnal motion Diurnal motion (, ) is an astronomical term referring to the apparent motion of celestial objects (e.g. the Sun and stars) around Earth, or more precisely around the two celestial poles, over the course of one day. It is caused by Earth's ro ...
and the parallactic angle changes equivalently. This is also the case with other celestial objects. In an ephemeris, the
position angle In astronomy, position angle (usually abbreviated PA) is the convention for measuring angles on the sky. The International Astronomical Union defines it as the angle measured relative to the north celestial pole (NCP), turning positive into the ...
of the midpoint of the bright limb of the Moon or planets, and the position angles of their
North pole The North Pole, also known as the Geographic North Pole or Terrestrial North Pole, is the point in the Northern Hemisphere where the Earth's rotation, Earth's axis of rotation meets its surface. It is called the True North Pole to distingu ...
s may be tabulated. If this angle is measured from the North point on the limb, it can be converted to an angle measured from the zenith point (the vertex) as seen by an observer by subtracting the parallactic angle. The position angle of the bright limb is directly related to that of the subsolar point.


Derivation

The vector algebra to derive the standard formula is equivalent to the calculation of the long derivation for the compass course. The sign of the angle is basically kept, north over east in both cases, but as astronomers look at stars from the inside of the celestial sphere, the definition uses the convention that the is the angle in an image that turns the direction to the NCP
counterclockwise Two-dimensional rotation can occur in two possible directions. Clockwise motion (abbreviated CW) proceeds in the same direction as a clock's hands: from the top to the right, then down and then to the left, and back up to the top. The opposite ...
into the direction of the zenith. In the equatorial system of right ascension and declination the star is at ::\mathbf = \left(\begin \cos\delta \cos \alpha \\ \cos \delta\sin\alpha\\ \sin\delta\end \right). In the same coordinate system the zenith is found by inserting , into the transformation formulas ::\mathbf = \left(\begin \cos\varphi \cos l\\ \cos\varphi \sin l\\ \sin\varphi\end \right), where is the observer's geographic latitude, the star's altitude, the zenith distance, and the local sidereal time. The North Celestial Pole is at ::\mathbf = \left(\begin0 \\ 0 \\ 1 \end\right). The normalized cross product is the rotation axis that turns the star into the direction of the zenith: ::\mathbf_z = \frac\mathbf\times \mathbf = \frac\left(\begin \cos\delta\sin\alpha\sin\varphi -\sin\delta\cos\varphi\sin l\\ -\cos\delta\cos\alpha\sin\varphi +\sin\delta \cos\varphi\cos l\\ \cos\delta \cos\varphi \sin(\alpha-l) \end \right). Finally is the third axis of the tilted coordinate system and the direction into which the star is moved on the great circle towards the zenith. The plane tangential to the celestial sphere at the star is spanned by the unit vectors to the north, ::\mathbf_\delta = \left(\begin -\sin\delta\cos\alpha\\ -\sin\delta\sin\alpha\\ \cos\delta \end\right), and to the east ::\mathbf_\alpha = \left(\begin -\sin\alpha \\ \cos\alpha\\ 0 \end\right). These are orthogonal: ::\mathbf_\delta \cdot \mathbf_\alpha=0;\quad \mathbf^2_\delta = \mathbf^2_\alpha=1. The parallactic angle is the angle of the initial section of the great circle at s, east of north, ::\omega_z\times \mathbf = \cos q\, \mathbf_\delta + \sin q \, \mathbf_\alpha. ::\cos q = (\omega_z\times \mathbf)\cdot \mathbf_\delta = \frac(\cos\delta\sin\varphi -\sin\delta \cos\varphi \cos h), ::\sin q = (\omega_z\times \mathbf)\cdot \mathbf_\alpha = \frac\sin h \cos\varphi. (The previous formula is the ''sine formula'' of
spherical trigonometry Spherical trigonometry is the branch of spherical geometry that deals with the metrical relationships between the sides and angles of spherical triangles, traditionally expressed using trigonometric functions. On the sphere, geodesics are grea ...
.) The values of and of are positive, so using atan2 functions one may divide both expressions through these without losing signs; eventually ::\tan q = \frac= \frac yields the angle in the full range . The advantage of this expression is that it does not depend on the various offset conventions of ; the uncontroversial offset of the hour angle takes care of this. For a sidereal target, by definition a target where and are not time-dependent, the angle changes with a period of a
sidereal day Sidereal time (as a unit also sidereal day or sidereal rotation period) (sidereal ) is a timekeeping system that astronomers use to locate celestial objects. Using sidereal time, it is possible to easily point a telescope to the proper coor ...
. Let dots denote time derivatives; then the hour angle changes as ::\dot h =\frac and the time derivative of the expression is ::\dot q \frac= \frac \dot h; ::\dot q = \frac\dot h = \frac\dot h =\frac\dot h. The value derived above always refers to the North Celestial Pole as the origin of coordinates, even if that is not visible (i.e., if the telescope is south of the Equator). Some authors introduce more complicated formulas with variable signs to derive similar angles for telescopes south of the Equator that use the South Celestial Pole as the reference. eq. (27)


See also

* Libration * Equatorial mount * Altazimuth mount


Further reading

* *


References

{{Reflist Astronomical coordinate systems Angle Observational astronomy