A rainbow is a meteorological phenomenon that is caused by reflection, refraction, and dispersion of light in water droplets, resulting in a spectrum of light appearing in the sky. It takes the form of a multicolored circular arc. Rainbows caused by sunlight always appear in the section of sky directly opposite the sun.
When sunlight enters a raindrop, it is refracted, or bent, and then reflected off the inside surface of the drop. The light is then refracted again as it exits the drop, creating a spectrum of colors. This spectrum forms the familiar arc of colors that we see as a rainbow.
Understanding the formation of rainbows can help us appreciate the beauty of this natural phenomenon and the science behind it. It also provides insights into the behavior of light and the properties of water droplets.