Gnomonics
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Gnomonics (from the
ancient Greek Ancient Greek (, ; ) includes the forms of the Greek language used in ancient Greece and the classical antiquity, ancient world from around 1500 BC to 300 BC. It is often roughly divided into the following periods: Mycenaean Greek (), Greek ...
word γνώμων, , meaning 'interpreter, discerner') is the study of the design, construction and use of
sundials A sundial is a horology, horological device that tells the time of day (referred to as civil time in modern usage) when direct sunlight shines by the position of the Sun, apparent position of the Sun in the sky. In the narrowest sense of the ...
. The foundations of gnomonics were known to the ancient Greek
Anaximander Anaximander ( ; ''Anaximandros''; ) was a Pre-Socratic philosophy, pre-Socratic Ancient Greek philosophy, Greek philosopher who lived in Miletus,"Anaximander" in ''Chambers's Encyclopædia''. London: George Newnes Ltd, George Newnes, 1961, Vol. ...
(ca. 550 BCE), which augmented the science of shadows brought back from Egypt by
Thales of Miletus Thales of Miletus ( ; ; ) was an Ancient Greek pre-Socratic philosopher from Miletus in Ionia, Asia Minor. Thales was one of the Seven Sages, founding figures of Ancient Greece. Beginning in eighteenth-century historiography, many came to ...
. Gnomonics was used by Greek and Roman architects from 25 BCE for the design of buildings. Modern gnomonics has its root in the nascent European astronomy of the 16th Century. The first works, in Latin, were published by
Sebastian Münster Sebastian Münster (20 January 1488 – 26 May 1552) was a German cartographer and cosmographer. He also was a Christian Hebraist scholar who taught as a professor at the University of Basel. His well-known work, the highly accurate world map, ...
in 1531 and Oronce Fine in 1532, rapidly followed by books in French. At the end of the 17th century, gnomonics developed notably in the application of
spherical trigonometry Spherical trigonometry is the branch of spherical geometry that deals with the metrical relationships between the edge (geometry), sides and angles of spherical triangles, traditionally expressed using trigonometric functions. On the sphere, ge ...
. Several methods, both graphical and analytical, were published in books which allowed the creation of
sundials A sundial is a horology, horological device that tells the time of day (referred to as civil time in modern usage) when direct sunlight shines by the position of the Sun, apparent position of the Sun in the sky. In the narrowest sense of the ...
of greater or lesser precision to be placed on buildings and in gardens. In his ''Histoire de la Gnomonique ancienne et moderne'', Jean-Étienne Montucla sums up gnomonics in these words:


Analytical gnomonics


Coordinate system transforms - Change of bases

The
Cartesian coordinates In geometry, a Cartesian coordinate system (, ) in a plane is a coordinate system that specifies each point uniquely by a pair of real numbers called ''coordinates'', which are the signed distances to the point from two fixed perpendicular o ...
of the Sun in the
horizontal coordinate system The horizontal coordinate system is a celestial coordinate system that uses the observer's local horizon as the fundamental plane to define two angles of a spherical coordinate system: altitude and ''azimuth''. Therefore, the horizontal coord ...
can be determined by successive changes of bases.


Expression as transformation matrices

A
transformation matrix In linear algebra, linear transformations can be represented by matrices. If T is a linear transformation mapping \mathbb^n to \mathbb^m and \mathbf x is a column vector with n entries, then there exists an m \times n matrix A, called the transfo ...
from a system B to a system B' allows for calculating the coordinates of a point or
vector Vector most often refers to: * Euclidean vector, a quantity with a magnitude and a direction * Disease vector, an agent that carries and transmits an infectious pathogen into another living organism Vector may also refer to: Mathematics a ...
in system B' when its coordinates are known is system B. For example, to change the system by rotating by an angle α around the Z axis, the coordinates in the new system can be calculated from those in the old system as: \begin\mathrm' \\ \mathrm'\\ \mathrm'\\ \end = \begin \cos \alpha & \sin \alpha & 0 \\ -\sin \alpha & \cos \alpha & 0 \\ 0 & 0 & 1 \\ \end \cdot \begin \mathrm\\ \mathrm\\ \mathrm\\ \end Similarly, for rotation of an angle α around the X axis: \begin\mathrm' \\ \mathrm'\\ \mathrm'\\ \end = \begin 1 & 0 & 0 \\ 0 & \cos \alpha & \sin \alpha \\ 0 & -\sin \alpha & \cos \alpha \\ \end \cdot \begin \mathrm\\ \mathrm\\ \mathrm\\ \end And for rotation by the angle α around the Y axis: \begin\mathrm' \\ \mathrm'\\ \mathrm'\\ \end = \begin \cos \alpha & 0 & -\sin \alpha \\ 0 & 1 & 0 \\ \sin \alpha & 0 & \cos \alpha \\ \end \cdot \begin \mathrm\\ \mathrm\\ \mathrm\\ \end


Model of the apparent movement of the Sun

The Cartesian coordinates of the Sun in the horizontal system of coordinates can be calculated using
change of basis In mathematics, an ordered basis of a vector space of finite dimension allows representing uniquely any element of the vector space by a coordinate vector, which is a sequence of scalars called coordinates. If two different bases are conside ...
matrices: \begin\mathrm_h \\ \mathrm_h\\ \mathrm_h\\ \end = \begin \cos (\frac-\phi) & 0 & -\sin (\frac-\phi) \\ 0 & 1 & 0 \\ \sin (\frac-\phi) & 0 & \cos (\frac-\phi) \\ \end \cdot \begin \cos (LMST) & \sin (LMST) & 0 \\ -\sin (LMST) & \cos (LMST) & 0 \\ 0 & 0 & 1 \\ \end \cdot \begin 1 & 0 & 0 \\ 0 & \cos (-\epsilon) & \sin (-\epsilon) \\ 0 & -\sin (-\epsilon) & \cos (-\epsilon) \\ \end \begin \cos(l_\odot)\\ \sin(l_\odot)\\ 0\\ \end where: \phi :
Latitude In geography, latitude is a geographic coordinate system, geographic coordinate that specifies the north-south position of a point on the surface of the Earth or another celestial body. Latitude is given as an angle that ranges from −90° at t ...
of the place of observation LMST : Local mean
sidereal time Sidereal time ("sidereal" pronounced ) is a system of timekeeping used especially by astronomers. Using sidereal time and the celestial coordinate system, it is easy to locate the positions of celestial objects in the night sky. Sidereal t ...
\epsilon :
Axial tilt In astronomy, axial tilt, also known as obliquity, is the angle between an object's rotational axis and its orbital axis, which is the line perpendicular to its orbital plane; equivalently, it is the angle between its equatorial plane and orbita ...
l_\odot :
Ecliptic longitude In astronomy, the ecliptic coordinate system is a celestial coordinate system commonly used for representing the apparent positions, orbits, and pole orientations of Solar System objects. Because most planets (except Mercury) and many small So ...
of the Sun


Projection of the shadow of a vertical gnomon

Let \begin 0\\ 0\\ L\\ \end be the Cartesian coordinates, in the local coordinate system, of the end of a vertical gnomon of length L . The coordinates of the extremity of the shadow in the horizontal plane can be obtained with an
affine transform In Euclidean geometry, an affine transformation or affinity (from the Latin, '' affinis'', "connected with") is a geometric transformation that preserves lines and parallelism, but not necessarily Euclidean distances and angles. More generally ...
parallel to the line by \begin\mathrm_h \\ \mathrm_h\\ \mathrm_h\\ \end and \begin 0\\ 0\\ L\\ \end .


Inclined and declined sundial

The Cartesian coordinates of the Sun in the system of coordinates bound to an inclined sundial of given declination are: * \begin\mathrm'_h \\ \mathrm'_h\\ \mathrm'_h\\ \end = \begin \cos i & 0 & -\sin i \\ 0 & 1 & 0 \\ \sin i & 0 & \cos i \\ \end \cdot \begin \cos (-D) & \sin (-D) & 0 \\ -\sin (-D) & \cos(-D) & 0 \\ 0 & 0 & 1 \\ \end \cdot \begin \mathrm_h\\ \mathrm_h\\ \mathrm_h\\ \end where: D :
declination In astronomy, declination (abbreviated dec; symbol ''δ'') is one of the two angles that locate a point on the celestial sphere in the equatorial coordinate system, the other being hour angle. The declination angle is measured north (positive) or ...
of the plane of the sundial i : inclination of the sundial, that is, the angle of the normal with respect to the zenith


Other uses

Gnomonic projection A gnomonic projection, also known as a central projection or rectilinear projection, is a perspective projection of a sphere, with center of projection at the sphere's center, onto any plane not passing through the center, most commonly a tan ...
is a
map projection In cartography, a map projection is any of a broad set of Transformation (function) , transformations employed to represent the curved two-dimensional Surface (mathematics), surface of a globe on a Plane (mathematics), plane. In a map projection, ...
where the vanishing point is in the centre of a spheroid.


References


Sources

* * * * * *


External links

* at the Société Astronomique de France website * , Minutes of meetings of the ''Commission des Cadrans solaires du Québec (CCSQ)'' from 1995 to 2014, available as PDF files * In May 2018, a French-language {{cite web, url=http://www.cadrans-solaires.info, title=online learning course on the theory and construction of sundials was launched by a member of the Sundials Commission of the
Société astronomique de France The Société astronomique de France (SAF; ), the France, French astronomical society, is a non-profit association in the public interest organized under French law (Association loi de 1901). Founded by astronomer Camille Flammarion in 1887, its ...
. Sundials