On the accuracy of a spherical gnomon's shadow readings
by Aimo Niemi
Introduction
In my previous work I was trying to observe the east-west direction using the well known equal length shadow method described also on many pages in the internet. I then found that an accuracy of ±3' was easily achieved or even better, if a spherical gnomon had been used. In the present work the use of a spherical gnomon and it's accuracy in the shadow readings was studied in a more detailed way.

Equipment
The gnomon consisted of a 3447 mm high plumb line and a 40 mm diameter sphere at the top of it. The dimensions were so chosen that the angular diameter of the sphere, as seen from the center of the shadow, corresponded that of the sun. The arrangement used is shown in the Figures 1. and 8.

Plumb line gnomon and details. Click to enlarge. Figure 1.

Observations
The shadow of the sphere was cast onto a millimeter paper from which it's place was photographed for a later analysis. On some observations the shadow's place was also marked with a template which was then photographed as well (fig.  2). Note that the shadow on the template in fig 2 doesn't coincide with the template's midpoint because the picture was taken only 4 to 7 seconds later than the template was set.

Click to enlarge. Figure 2.

The observations were carried out at Turku (lat 60.°369 N) at noon on 26 july 2008. Alltogether 207 observations were made from which 72 were template observations. As an extra precaution the time of the observation was also recorded. The result of the templates xy-coordinate analysis is shown in the figure 3. In it the mean error of one observation is ±1.023 mm and  the accuracy of the best fit curve through the points is about ±0.5 mm.
Templates x-coordinate was compared also against time at wich the mean error of one observation was ±0.933 mm (Fig. 4). Correspondingly, when the same analysis was made to the shadow observations, the mean errors were ±0.709 mm  and ±0.735 mm (Fig. 5  and 6).

Click for shadow
Figure 3.

Click for residuals
Figure 4. Click the picture to see the residuals.

Points in the brackets were omitted from the analysis
Figure 5.

Click for residuals
Figure 6. Click the picture to see the residuals.

In fig. 5 an interesting phenomenon is also visible. In two points the sun was behind a thin cloud, which caused the shadow's distance from the plumb to lengthen about 15 mm. This means that the sun's apparent altitude was decreased more than 8', which is much more than the standard refraction (52�) at that altitude (49°). Figure 7 shows a composite photograph of the phenomenon.

Figure 7.

At noon, when the sun crossed the meridian, also the shadow's distance from the plumb line was measured. The result was 3001±1 mm and the heigth of the gnomon 3447±2 mm. Here the lesser accuracy in the gnomon was caused by the uncertainty in the levelling but nevertheless, sun's observed altitude 48°.957 was in a good agreement with it's calculated apparent altitude 48°.944.

Conclusions
The experiment shows clearly that with the equal length method an accuracy of ±1' in the east-west direction is easily achieved. And, in the sundial of this scale a reading accuracy of ±2 mm or better (Fig. 4b) is easily achieved, too. In the time this corresponds to an accuracy of ±6 seconds.

Last edited 2008-09-04
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