Primary Rainbows - WIP

Relationship to the Viewer

A rainbow is not in a static position, rather it depends on the viewers angle with the sun (or other light source). The sun, the viewer, and the antisolar point lie on the same line, with the viewer in the middle. A primary rainbow will always oppose the sun.

diagram showing the sun, an observer, and the center of the rainbow in a straight line. The observer is in the middle, with the sun and rainbow opposing each other. a cone shape forms from the observer with the rainbow along the surface. The red part of the rainbow is 42.4 degrees from the viewer, and the purple is 40.7 degrees.

my diagram

In this diagram, the center of the rainbow is the "antisolar point," which is also the same place the head of the viewers shadow would be. Essentially an infinite cone is formed with the viewer at the point and the rainbow as the surface of the cone. The small diagram shows that the cone on its side, illustrating how the outer surface of the cone makes a 42.4 degree angle with the central axis. This 42.4 degrees is on the very outside edge of the rainbow, the red band; violet is at 40.7 degrees.

A rainbow is also not a specific distance away from the viewer, as long as there are water droplets on the cone's surface, a rainbow can be formed whether the droplets are feet or miles away. Their distance does not impact the appearance of the rainbow.

Considering the observer is a key component to the rainbow, each person will see a rainbow made by different water droplets (as the observers each make a different cone). The further away the droplets are, the less obvious this is however.

simple diagram showing the sun, viewer, and rainbow in five different senarios. 1: the sun and observer are at the horizon, showing half of a full rainbow. 2: the ground slopes upwards from the viewer, obscuring more than half the rainbow. 3: the viewer ontop a mountain, allowing more than half the rainbow to be seen. 4: the sun higher in the sky and the viewer on flat land, with less than half the rainbow visable. 5: The viewer in an airplane, allowing the full rainbow to be seen

The full rainbow circle is rarely seen due to the relationship between the sun and viewer, causing the rest of the rainbow to be hidden by the ground (more accurately, there are no raindrops between the viewer and the visible ground). However, the amount of rainbow visible can increase if the sun is lower to the horizon and/or the viewer is higher (a full circle can be seen from a plane). The reverse is also true, the higher the sun and/or the lower the viewer, the less the circle can be seen. Check out my rainbow gallery for full circle rainbow photos!

Here is a much better diagram by Lourdes B. Avilés in Invisible Rainbows, showing how at a high vantage point, a viewer can see an entire rainbow.

Here is a real life view of what a rainbow from a mountain top looks like (from Alexander Haussmann)! Part of the mountain is covering the raindrops, but a lot is visible!

Caustics - WIP

notice how the light passes through the prism, but reflects on the inside surface of the water drop

Light does infact pass stright through a water drop light like it does through a prism (still bent of course) but the shape of the drop does not allow the dispersed light to form a rainbow, despite the droplet acting as a prism. These rays of light wash each other out, creating extra brightness around the sun (zeroth order glow).

diagram by Les Crowley of Atmospheric Optics. He also describes rainbow caustics

Light rays passing through the drop can enter from any point of the drop facing the sun, and will exit so that they all flare outwards from each other without hitting any bouyndaries. Light that is reflected by the inside surface of the drop reflects back and they start to flare from each other on exit, until they hit a hard line, and start to cross over each other.

A reflection within the drop is important to create a caustic. A caustic is a physics phenonema describing distinct areas or lines where light rays are densely packed. Caustics are frequently observed in clear water on a sunny day, where light collects into thin shimmery lattices on the bottom of the pool.

diagram from Like a Bridge over Colored Water

Here we can see the hard line where the reflected rays will not cross, where light collects in a caustic. This is also called the minimum angle of deviation.

Each wavelenghth of light creates a caustic at a slightly different angle from the incident light, allowing the larger angles (red) to be seen outside of the smaller angles (violet). These caustics result in a 3D cone for each color.