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Exploring Sundials

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Introduction

A Sundial of sorts can quite easily be made by pushing a pencil through the centre of a paper plate and placing it in a sunny position such that the pencil casts a shadow.


If the paper plate is divided into 24 equal segments (i.e. each 15 degrees) then this would work quite well at the North Pole, since the Sun appears to do a full 3600 rotation of the Earth every 24 hours (i.e. 360 ÷ 24 = 15). If placed anywhere other than the North Pole, however, it would soon become apparent that equal segments are not the answer if the pencil is vertical.


Equatorial Sundial

The rod or edge projecting the shadow (e.g. the pencil in this case), known as the Gnomon, must be arranged always to point North and be parallel to the Earth's axis for a Sundial to maintain good time throughout the year. In this orientation, the Sun can appear to be rotating around it as if it were placed at the North Pole (see Sundials and Gnomons).


The correct orientation can be achieved simply by tilting the paper plate and pencil until the pencil is lying at an angle equal to the Latitude of where the Sundial is to be positioned (e.g. approximately 51.50 for London).


It can be imagined that a Sundial designed to sit at the North Pole would be identical to one placed at the centre of the Earth on the Equator, if that were possible, and so Sundial with equally spaced divisions as shown are known as Equatorial Sundials. These can be regarded as ‘master sundials’ from which designs for others may be generated.

Horizontal Sundial


Horizontal Sundial

The tilted dial of an Equatorial Sundial is not always convenient and so consideration must be given to designing a Sundial with a horizontal dial. This is achieved by imagining the shadows cast to be projected on to a horizontal plate. Lines are drawn from where the Gnomon rests on the plate, along the lines of each shadow, to generate a series of hour lines on the horizontal dial.


As is the case with other Sundials, the Gnomon remains pointing North and at an angle equal to the Latitude of where the Sundial is to be positioned. Note that the angles between the hour lines increase as the Sun's shadow deviates away from Noon during both morning and afternoon. This gives rise to the familiar splayed lines on a modern Horizontal Sundial and as seen on the face of the Ancient Egyptian sundial discovered in the Valley of the Kings around 1500 BC.


Horizontal Sundial

The calculation of the angles for the hour lines requires some quite advanced Trigonometry as follows: Horizontal dial shadow angle θ = Arctan (Sin Latitude(L) x Tan H)

Where:

  • θ = the hour angle (i.e. the deviation away from the North-facing Noon line);
  • L = the Latitude of the sundial location;
  • H = the number of hours either side of Noon x 150.


The results will show that Horizontal Sundials work best at higher Latitudes rather than near the Equator.


Horizontal Sundial
Vertical Sundial

As with a Horizontal Sundial the Gnomon remains pointing North and set at an angle to the horizontal equal to the Latitude of the Sundial location. The Gnomon therefore must be set at an angle to the 'dial' of 900. minus Latitude.


Ideally, the 'dial' of a Vertical Sundial should be fixed to a South-facing wall or surface. In this situation the Gnomon is located in a plane at right angles to the 'dial' and will cast a vertical shadow at Noon. If placed on a wall which is not South-facing (e.g. S.E. or S.W.) then the Gnomon will need to be angled to the 'dial' such that the shadow cast at Noon remains vertical and is said to be Declined East or West as appropriate.


The calculation of the angles for the hour lines requires similar advanced Trigonometry as for Horizontal Sundials:

Horizontal dial shadow angle θ = Arctan (Cos Latitude(L) x Tan H)

Vertical Sundial

Where the variables are the same as given above for the Horizontal Sundial but note that it is the Cosine of Latitude which is used rather than the Sine.


The results will show that Vertical Sundials work well if nearer to the Equator than the North Pole.



Note: A DT Online Tool is available here which completes the calculation of the angle of each hour line for any given Latitude which is input.


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