Sundial

As the Sun appears to move through the sky, the shadow aligns with different hour-lines, which are marked on the dial to indicate the time of day.

It is common for inexpensive, mass-produced decorative sundials to have incorrectly aligned gnomons, shadow lengths, and hour-lines, which cannot be adjusted to tell correct time.

To obtain the national clock time, three corrections are required: The principles of sundials are understood most easily from the Sun's apparent motion.

The hour-lines will be spaced uniformly if the surface receiving the shadow is either perpendicular (as in the equatorial sundial) or circular about the gnomon (as in the armillary sphere).

The corresponding light-spot or shadow-tip, if it falls onto a flat surface, will trace out a conic section, such as a hyperbola, ellipse or (at the North or South Poles) a circle.

By 240 BC, Eratosthenes had estimated the circumference of the world using an obelisk and a water well and a few centuries later, Ptolemy had charted the latitude of cities using the angle of the sun.

The motto is usually in the form of an epigram: sometimes sombre reflections on the passing of time and the brevity of life, but equally often humorous witticisms of the dial maker.

In other cases, the hour lines may be curved, or the equatorial bow may be shaped like a vase, which exploits the changing altitude of the sun over the year to effect the proper offset in time.

The Sunquest sundial, designed by Richard L. Schmoyer in the 1950s, uses an analemmic-inspired gnomon to cast a shaft of light onto an equatorial time-scale crescent.

[20] The most commonly observed sundials are those in which the shadow-casting style is fixed in position and aligned with the Earth's rotational axis, being oriented with true north and south, and making an angle with the horizontal equal to the geographical latitude.

If the shadow falls on a surface that is symmetrical about the celestial axis (as in an armillary sphere, or an equatorial dial), the surface-shadow likewise moves uniformly; the hour-lines on the sundial are equally spaced.

There is an alternative, simple method of finding the positions of the hour-lines which can be used for many types of sundial, and saves a lot of work in cases where the calculations are complex.

[citation needed] Since the hour angles are not evenly spaced, the equation of time corrections cannot be made via rotating the dial plate about the gnomon axis.

If the face of the vertical dial points directly south, the angle of the hour-lines is instead described by the formula:[30] where L is the sundial's geographical latitude,

Vertical dials that face north are uncommon, because they tell time only during the spring and summer, and do not show the midday hours except in tropical latitudes (and even there, only around midsummer).

If the style is aligned with the Earth's rotational axis, a spherical shape is convenient since the hour-lines are equally spaced, as they are on the equatorial dial shown here; the sundial is equiangular.

This pattern, built a couple of meters wide out of temperature-invariant steel invar, was used to keep the trains running on time in France before World War I.

[47] This collection of sundials and other astronomical instruments was built by Maharaja Jai Singh II at his then-new capital of Jaipur, India between 1727 and 1733.

The larger equatorial bow is called the Samrat Yantra (The Supreme Instrument); standing at 27 meters, its shadow moves visibly at 1 mm per second, or roughly a hand's breadth (6 cm) every minute.

The gnomon of a Foster-Lambert dial is neither vertical nor aligned with the Earth's rotational axis; rather, it is tilted northwards by an angle α = 45° - (Φ/2), where Φ is the geographical latitude.

In one simple version,[62] the front and back of the plate each have three columns, corresponding to pairs of months with roughly the same solar declination (June:July, May:August, April:September, March:October, February:November, and January:December).

[58] A peg gnomon is inserted at the top in the appropriate hole or face for the season of the year, and turned to the Sun so that the shadow falls directly down the scale.

Most commonly, the receiving surface is a geometrical plane, so that the path of the shadow-tip or light-spot (called declination line) traces out a conic section such as a hyperbola or an ellipse.

The collection of hyperbolae was called a pelekonon (axe) by the Greeks, because it resembles a double-bladed ax, narrow in the center (near the noonline) and flaring out at the ends (early morning and late evening hours).

The oldest example is perhaps the antiborean sundial (antiboreum), a spherical nodus-based sundial that faces true north; a ray of sunlight enters from the south through a small hole located at the sphere's pole and falls on the hour and date lines inscribed within the sphere, which resemble lines of longitude and latitude, respectively, on a globe.

With a knot or bead on the string as a nodus, and the correct markings, a diptych (really any sundial large enough) can keep a calendar well-enough to plant crops.

[77] Similar to sundials with a fixed axial style, a globe dial determines the time from the Sun's azimuthal angle in its apparent rotation about the earth.

[78] In centuries past, such dials were used to set mechanical clocks, which were sometimes so inaccurate as to lose or gain significant time in a single day.

[79] Such marks indicate local noon, and provide a simple and accurate time reference for households to set their clocks.

They typically consist of a horizontal sundial, which has in addition to a gnomon a suitably mounted lens, set to focus the rays of the sun at exactly noon on the firing pan of a miniature cannon loaded with gunpowder (but no ball).

SSW facing, vertical declining sundial on the Moot Hall in Aldeburgh , Suffolk, England. The gnomon is a rod that is very narrow, so it functions as the style. The Latin motto loosely translates as "I only count the sunny hours."
A horizontal dial commissioned in 1862, the gnomon is the triangular blade. The style is its inclined edge. [ 1 ]
A combined analemmatic -equatorial sundial in Ann Morrison Park in Boise, Idaho , 43°36'45.5"N 116°13'27.6"W
Top view of an equatorial sundial. The hour lines are spaced equally about the circle, and the shadow of the gnomon (a thin cylindrical rod) moving from 3:00 a.m. to 9:00 p.m. on or around Solstice , when the Sun is at its highest declination .
Bowstring sundial in Singapore Botanic Gardens . The design shows that Singapore is located almost at the equator .
World's oldest sundial, from Egypt's Valley of the Kings (c. 1500 BC)
Reconstruction of the 2,000 year old Phoenician sundial found at Umm al-Amad, Lebanon
A Korean sundial ( Angbu-ilgu ) first made by Jang Yeong-sil in the Joseon period, displayed in Gyeongbokgung .
A London type horizontal dial . The western edge of the gnomon is used as the style before noon, the eastern edge after that time. The changeover causes a discontinuity, the noon gap, in the time scale.
Southern-hemisphere sundial in Perth , Australia . Magnify to see that the hour marks run anticlockwise. Note graph above the gnomon of the Equation of Time , needed to correct sundial readings.
The Equation of Time – above the axis the equation of time is positive, and a sundial will appear fast relative to a clock showing local mean time. The opposites are true below the axis.
The Whitehurst & Son sundial made in 1812, with a circular scale showing the equation of time correction. This is now on display in the Derby Museum.
Sunquest sundial, designed by Richard L. Schmoyer, at the Mount Cuba Observatory in Greenville, Delaware .
Sundial on the Orihuela Campus of Miguel Hernández University , Spain, which uses a projected graph of the equation of time within the shadow to indicate clock time.
Timepiece , St Katharine Docks , London (1973) an equinoctial dial by Wendy Taylor [ 24 ]
An equatorial sundial in the Forbidden City , Beijing. 39°54′57″N 116°23′25″E  /  39.9157°N 116.3904°E  / 39.9157; 116.3904  ( Forbidden City equatorial sundial ) The gnomon points true north and its angle with horizontal equals the local latitude . Closer inspection of the full-size image reveals the "spider-web" of date rings and hour-lines.
Horizontal sundial in Minnesota . June 17, 2007 at 12:21. 44°51′39.3″N, 93°36′58.4″W
Detail of horizontal sundial outside Kew Palace in London, United Kingdom
Two vertical dials at Houghton Hall Norfolk UK 52°49′39″N 0°39′27″E  /  52.827469°N 0.657616°E  / 52.827469; 0.657616  ( Houghton Hall vertical sundials ) . The left and right dials face south and east, respectively. Both styles are parallel, their angle to the horizontal equaling the latitude. The east-facing dial is a polar dial with parallel hour-lines, the dial-face being parallel to the style.
"Double" sundials in Nové Město nad Metují , Czech Republic; the observer is facing almost due north.
Polar sundial at Melbourne Planetarium
Monumental polar sundial in Lalín ( Spain )
Effect of declining on a sundial's hour-lines. A vertical dial, at a latitude of 51° N, designed to face due south (far left) shows all the hours from 6 A.M. to 6 P.M. , and has converging hour-lines symmetrical about the noon hour-line. By contrast, a West-facing dial (far right) is polar, with parallel hour lines, and shows only hours after noon. At the intermediate orientations of south-southwest, southwest, and west-southwest , the hour lines are asymmetrical about noon, with the morning hour-lines ever more widely spaced.
Two sundials, a large and a small one, at Fatih Mosque , Istanbul dating back to the late 16th century. It is on the southwest facade with an azimuth angle of 52° N.
Vertical reclining dial in the Southern Hemisphere, facing due north, with hyperbolic declination lines and hour lines. Ordinary vertical sundial at this latitude (between tropics) could not produce a declination line for the summer solstice. This particular sundial is located at the Valongo Observatory of the Federal University of Rio de Janeiro , Brazil.
Equatorial bow sundial in Hasselt , Flanders in Belgium 50°55′47″N 5°20′31″E  /  50.92972°N 5.34194°E  / 50.92972; 5.34194  ( Hasselt equatorial bow sundial ) . The rays pass through the narrow slot, forming a uniformly rotating sheet of light that falls on the circular bow. The hour-lines are equally spaced; in this image, the local solar time is roughly 15:00 hours ( 3 P.M. ). On September 10, a small ball, welded into the slot casts a shadow on centre of the hour band.
Precision sundial in Bütgenbach, Belgium. (Precision = ±30 seconds) 50°25′23″N 6°12′06″E  /  50.4231°N 6.2017°E  / 50.4231; 6.2017  ( Belgium )
Universal ring dial. The dial is suspended from the cord shown in the upper left; the suspension point on the vertical meridian ring can be changed to match the local latitude. The center bar is twisted until a sunray passes through the small hole and falls on the horizontal equatorial ring. See Commons annotations for labels.
Analemmatic sundial on a meridian line in the garden of the abbey of Herkenrode in Hasselt ( Flanders in Belgium )
Ottoman-style sundial with folded gnomon and a compass. Debbane Palace museum, Lebanon.
19th-century Tibetan shepherd's timestick
Kraków. 50°03′41″N 19°56′24″E  /  50.0614°N 19.9400°E  / 50.0614; 19.9400  ( Kraków sundial ) The shadow of the cross-shaped nodus moves along a hyperbola which shows the time of the year, indicated here by the zodiac figures. It is 1:50 P.M. on 16 July, 25 days after the summer solstice .
Declination lines at solstices and equinox for sundials, located at different latitudes
Diptych sundial in the form of a lute , c. 1612 . The gnomons-style is a string stretched between a horizontal and vertical face. This sundial also has a small nodus (a bead on the string) that tells time on the hyperbolic pelikinon , just above the date on the vertical face.
Benoy Sun Clock showing 6:00 p.m.
Stainless steel bifilar sundial in Italy
Noon mark from the Greenwich Royal Observatory . The analemma is the narrow figure-8 shape, which plots the equation of time (in degrees, not time, 1°=4 minutes) versus the altitude of the Sun at noon at the sundial's location. The altitude is measured vertically, the equation of time horizontally.
A meridian line in the Duomo of Milan . The position of the beam of sunlight indicates that it is almost solar noon and the start of Gemini season
Angbuilgu , a portable sundial used in Korea during the Joseon period . The integrated magnetic compass aligns the instrument toward north pole.( National Museum of Korea ) [ 82 ]