The Geometry of Sunlight

Marissa Romano

Laser Teaching Center
Stony Brook University



Introduction

My mentor, Dr. Noé, concluded one of our first meetings by showing me how the shadow of an object becomes increasingly blurred with increasing distance, as shown in this picture of a flagpole shadow. Although I have seen this effect almost every day I had never thought about why this happens. To help me find an explanation he showed me a related phenomenon. He let some sunlight pass through a small hole made with his hand and pointed out that the disk of light projected onto a piece a paper grows in size as the paper is moved further and further away. I estimated that the diameter of the disk was about 1, 2 or 3 cm at about 1, 2 or 3 meters away. He then used a small pocket mirror to illustrate that the size of a spot of reflected sunlight also increases with distance in a similar way. When the spot was directed to the wall between the physics and math buildings it was about 30 cm in diameter, much bigger than the 6 cm mirror. That evening I thought about what I'd seen and came to the conclusion that the observed spreading of sunlight must be due to diffraction. I drew diagrams like this one and was completely convinced of my reasoning.



It's Just Geometry !!

At our next meeting Dr. Noé suggested I think about light rays (geometry) instead of waves (diffraction) and had me draw this diagram.



This diagram makes it clear that sunlight enters the pinhole at slightly different angles and this causes the "spreading" effect after the pinhole. The angular spread is just due to simple geometry of light rays and has little or nothing to do with diffraction. The earlier estimation that the image is 1 cm in diameter at 1 meter away is actually the angular spread of the sunlight. Similarly, sunlight reflected off a small mirror diverges, therefore resulting in a larger spot of light on the wall or screen with increasing distance.

Geometry also explains why shadows blur. A majority of the sunlight is blocked out by the object causing a defined dark shadow to be projected behind the object. As the object's distance from the screen increases a small amount of sunlight is able to "get behind" the object. The intensity (brightness) of this amount of sunlight is less than what a person would observe in unobstructed sunlight producing a "fuzzy" outline.


Angular Size and Time

The angular spread of sunlight is also known as the sun's angular diameter and can be determined using simple geometry. From the small angle approximation the sun's angular size is its diameter divided by its distance from the earth, therefore the esitmated angular size is 1/100 radians.

Dr. Noé and I then decided to experiment further with the angular size of the sun. First we calculated the estimated time for the sun to move its diameter across the sky. Since we know that 1/100 radian is equivalent to 0.5 degree and that there is a total of 360 degrees in a day, we can say that this is proportional to a certain time, t, in a day[1440 minutes]. In fact, angular measurements can be expressed in units known as an arcminute and an arcsecond which are 1/60th of a degree and 1/60th of an arcminute respectively. Our calculated t is equivalent to 2 minutes, thus we estimated that it took 2 minutes for the sun to move its own diameter. To observe this quantative result, we went into a hallway that allowed in a lot of sunlight and taped a black sheet of paper with a hole to the window. The sunlight entered through the hole and was projected as a circular image onto a white piece of paper several meters away. The initial image's outline was traced and after 2 minutes the image moved a certain distance and its outline was traced again. Our quantative estimate was similar to the results we observed: the sun moves its own diameter every 2 minutes.



     

     




Measuring Angular Size

As mentioned previously, when sunlight is reflected off a mirror the size of the image increases with increasing distance. In this part of the project we made careful measurements of this effect and compared these to the known angular size of the sun. We started by covering a pocket mirror with black paper that had a small hole (~ 3 mm diameter) poked into it with a pencil. We secured the mirror to an adjustable stand for stability and placed the stand on the floor in the hallway facing towards the sun. To measure the image diameters, we created a measuring template in xfig with six concentric circles ranging from 5 to 30 mm in diameter. (Here's the xfig code for it.) When the template was printed, we noticed that each diameter was off by the same factor and took this into account when we plotted the data. For example, the 30 mm circle is actually about 28.7 mm. To make the measurements, I held the measuring template in the path of the reflected sunlight. I moved the template until the image matched the diameter of one of the circles and held this position whileDr. Noé measured the image distance with a tape measure. We repeated this for each circle.



     


To analyze our results, we created a plot of image diameter (d) versus image distance (D) in Excel. The six measured points are shown in red in the graph below. The black line is a prediction based on the known angular size of the sun at this time of year, α = 0.00928 radians. (Changing the size of the hole lets us shift the prediction curve. Parameters of a 2.5 mm hole coincide with an α of 9.36 mR, thus giving the best fit for the ideal α of 9.325 mR.) At D = 0 the diameter of the image (d) and the hole (d0) is the same, so we assumed the prediction could be represented by a hyperbolic function:





The seasonal variation of α due to the earth's elliptical orbit is shown below. Our measurement was made on March 12th.





Partial and Total Shadows

As Dr. Noé and I explored the geometry of shadows, we naturally got into a discussion about partial and total eclipses. A total solar eclipse can happen because the moon shares the same angular size as the sun, therefore allowing it to "cover" the sun. A total eclipse also depends on the position of the observer and time of the year. There are distinct parts of a shadow called the umbra and the penumbra. The umbra is where an observer must be positioned to see a total eclipse/shadow and the penumbra is where an observer can only see a partial eclipse/shadow. There is also another section called the antumbra where an observer sees the moon/object with a ring of light around it ( an annular eclipse ). Both Dr. Noé and I were curious if there was a distinct dividing line between the umbra and antumbra, and as a result we attempted an experiment that simulated a solar eclipse. We held a coin in the sunlight and its shadow was casted onto a piece of paper. I proceeded to move the paper further away from the coin and we looked carefully for the transition from the penumbra and antumbra. At this specific division we expected to see a lighter area within the shadow, but unfortunately this was too difficult to observe. The experiment was still a great introduction to total and partial shadows.




http://apod.nasa.gov/apod/ap100122.html




Demonstrating Diffraction

In this project we have shown that the spreading of sunlight is not due to diffraction. Diffraction requires a coherent light source, such as a laser. To demonstrate diffraction we aimed a red HeNe laser beam through a pinhole 0.2 mm (200 μm) in diameter. On a screen 3 meters away from the pinhole, we observed an enlarged spot of light about 1.5 centimeters in diameter surrounded by faint concentric circles. From the small angle approximation the angular size of the central spot is therefore about 1.5/300, or 5 milli-radians. The angles involved in diffraction effects are approximately given by λ/d, wavelength over aperture size. This predicts a diffraction angle of 0.633/200 or about 3 milli-radians, in rough agreement with the observation.


Conclusion

The behavior of sunlight when it passes through an aperture can be explained through simple geometry relating to the angular size of the sun. Although we used a simple method of measurement, its sensitivity allowed us to observe the seasonal variation of α and record measurements in very good agreement with our prediction. We used another effective method to observe the sun's movement across the sky that further related with the sun's angular size.


Acknowledgements

I have a found out that a simple topic such as the geometry of sunlight can become an extensive project where one can learn the basics of doing research.I would like to thank Dr. Noé for investing a large amount of his time to helping me. Without him as a mentor I would have little guidance and resources to perform our experiments and perfect the outcome of this report. Most importantly, he encouraged critical thinking and never just simply handed me the answers to my questions. I look forward to working with Dr.Noé on future projects, and I am enthusiastic about what we will come up with together.