Dodd wrote:Here's a mediocre photo I took near Columbus, GA, October 27, 2010 of a strangely flattened rainbow. I never even considered that a rainbow could be any other arch/diameter than what is "normal." Trust me, they can. Please explain. Thanks. Dodd Clifton
The center of a rainbow is always at the anti-solar point (except when the sun is reflected off of lakes).
Céline Richard wrote:Does anyone know how a double rainbow can form: I mean, when a weak rainbow appears above a brighter one?
Reflection from smooth water sends parallel shafts of sunlight upwards. To falling raindrops this appears like a second sun shining upwards from below the horizon. The opposite point in the sky from the reflected sun is the anthelic point - the same distance above the horizon as the antisolar point is below it. Drops on the surface of a rainbow cone with an axis pointing to the anthelic point form a reflection rainbow.
The water mirror does not have to be behind the observer but when it is in front only the lower parts of the reflection bow will be seen
Céline Richard wrote:So a rainbow can reflect on the sea, water, or wet sand...
Chris Peterson wrote:Basically, all rainbows are double, because there are two paths light takes through water drops.
owlice wrote:I agree with Chris; Céline, your picture shows a primary and secondary rainbow. The second bow is concentric with the first and its colors are reversed. The spacing between the two bows looks right for the dimmer one being a secondary ("some 9º outside the primary bow").

Evan wrote:Here is a good puzzle. This was taken in my driveway last summer. The ground is dry even though it is raining heavily. There is a rainbow visible within 20 metres of the point of view. This is a 3D image intended for crossed eye viewing. If you study it in 3D you will notice that even individual raindrops have been captured in 3D.
The question is how? The images were taken from the same camera at slightly different times. Note that I do have what I consider a very good working hypothesis.
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