When it comes to rainbows, most people think they’ve seen all
there is to see. Certainly, we’ve all seen the simple rainbow – and even
the most ordinary can be a stunning sight. But rainbows come in more
than just one color: there are plenty of less common types of rainbows
which can be even more beautiful than the usual kind. Check them out:
This is the rainbow we are all most familiar with. The primary rainbow is the single multi-colored arc that usually appears after a rainstorm. Primary rainbows are formed when refracted light is reflected through a water droplet. The intensity of the rainbow’s colors depends on how large the water droplets are.
If you have seen a primary rainbow, then chances are you have also seen a secondary rainbow. They are also known as double rainbows. A secondary rainbow forms behind the primary rainbow when the light in the water droplet is reflected twice instead of once. The secondary is about twice as wide as the primary rainbow, but is only one-tenth as intense. Its colors are also reversed.
Alexander’s Band is technically not a rainbow, but it is associated with the primary and secondary rainbows. An Alexander’s band is the area of sky between the primary and secondary rainbow and it is noticeably darker than the rest of the sky. The single reflected light of the primary brightens the sky inside and the double reflected light of the secondary brightens the sky outside of it. To our eyes, it appears that the sky is darker between the primary and secondary rainbows.
Supernumerary rainbows are also known as stacker rainbows, and occur rather infrequently. They consist of several faint rainbows on the inner side of the primary – and more rarely, they appear outside of the secondary. They are formed by small but similarly sized raindrops, and by the interference of light which reflects once, but travels along a different path inside the raindrop.
Red rainbows – also called monochrome rainbows – are formed after rainfall during sunrise or sunset. The shorter wavelengths of the spectrum, such as blue and green, are scattered by dust and air molecules. This leaves the remaining light to display the colors with the longest wavelengths, red and yellow, to finally form the red rainbow.
Cloud rainbows form from small water droplets in clouds and damp air, rather than from raindrops. They appear white because the water drops are very small in size (bigger water drops are more able to reflect the spectrum colours). Cloud rainbows are much broader than normal rainbows, and are most likely to form over water. They can also form over land, so long as the fog is thin enough for the sun’s rays to shrine through.
Twinned rainbows are not the same as the double rainbow – they’re actually very rare. They’re made up of two rainbow arcs that stem from a single base point, and they’re caused when a combination of small and large water droplets fall from the sky. The large drops are forced to flatten by air resistance, while the smaller drops are kept in shape by its surface tension. The water droplets then form their own rainbow, which may come together to form twinned rainbows.
Reflected and reflection rainbows – which are not the same thing, despite their similar names – only form over water. A reflected rainbow is the most commonly seen: it appears when light is deflected off the water droplets and then reflected off the water before we have time to process the light with our eyes.
A reflection rainbow is what appears when light reflects off the water before it is deflected off the water droplets. Reflection rainbows are not nearly as visible as a reflected rainbow, because of the specific conditions they require.
Lunar rainbows are rainbows that are formed at night by moonlight. However, moonlight is very weak and lunar rainbows are very rarely seen. The best time to see them, logically, is on the night of a full moon while it’s raining. The sky must also be very dark, which means that lunar rainbows appear very dull or white because the colour of the night is not bright enough to activate the cone cells (colour receptors) in our eyes.
10 Primary Rainbows
This is the rainbow we are all most familiar with. The primary rainbow is the single multi-colored arc that usually appears after a rainstorm. Primary rainbows are formed when refracted light is reflected through a water droplet. The intensity of the rainbow’s colors depends on how large the water droplets are.
9
Secondary Rainbows
If you have seen a primary rainbow, then chances are you have also seen a secondary rainbow. They are also known as double rainbows. A secondary rainbow forms behind the primary rainbow when the light in the water droplet is reflected twice instead of once. The secondary is about twice as wide as the primary rainbow, but is only one-tenth as intense. Its colors are also reversed.
8
Alexander’s Dark Band
Alexander’s Band is technically not a rainbow, but it is associated with the primary and secondary rainbows. An Alexander’s band is the area of sky between the primary and secondary rainbow and it is noticeably darker than the rest of the sky. The single reflected light of the primary brightens the sky inside and the double reflected light of the secondary brightens the sky outside of it. To our eyes, it appears that the sky is darker between the primary and secondary rainbows.
7
Supernumerary Rainbows
Supernumerary rainbows are also known as stacker rainbows, and occur rather infrequently. They consist of several faint rainbows on the inner side of the primary – and more rarely, they appear outside of the secondary. They are formed by small but similarly sized raindrops, and by the interference of light which reflects once, but travels along a different path inside the raindrop.
6
Red Rainbows
Red rainbows – also called monochrome rainbows – are formed after rainfall during sunrise or sunset. The shorter wavelengths of the spectrum, such as blue and green, are scattered by dust and air molecules. This leaves the remaining light to display the colors with the longest wavelengths, red and yellow, to finally form the red rainbow.
5
Cloud Rainbows
Cloud rainbows form from small water droplets in clouds and damp air, rather than from raindrops. They appear white because the water drops are very small in size (bigger water drops are more able to reflect the spectrum colours). Cloud rainbows are much broader than normal rainbows, and are most likely to form over water. They can also form over land, so long as the fog is thin enough for the sun’s rays to shrine through.
4
Twinned Rainbows
Twinned rainbows are not the same as the double rainbow – they’re actually very rare. They’re made up of two rainbow arcs that stem from a single base point, and they’re caused when a combination of small and large water droplets fall from the sky. The large drops are forced to flatten by air resistance, while the smaller drops are kept in shape by its surface tension. The water droplets then form their own rainbow, which may come together to form twinned rainbows.
3
Reflected and Reflection Rainbows
Reflected and reflection rainbows – which are not the same thing, despite their similar names – only form over water. A reflected rainbow is the most commonly seen: it appears when light is deflected off the water droplets and then reflected off the water before we have time to process the light with our eyes.
A reflection rainbow is what appears when light reflects off the water before it is deflected off the water droplets. Reflection rainbows are not nearly as visible as a reflected rainbow, because of the specific conditions they require.
2
Rainbow
wheels are formed when dark clouds or dense rain showers prevent the
light from reaching your eye. The shadowed raindrops do not allow you
to see the colours of the rainbow. The result is a rainbow that can
resemble a wagon wheel, with large spokes centered towards a specific
point. If the clouds are moving quickly across the sky, then the rainbow
wheel can appear to rotate.
Rainbow Wheels
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Lunar Rainbows
Lunar rainbows are rainbows that are formed at night by moonlight. However, moonlight is very weak and lunar rainbows are very rarely seen. The best time to see them, logically, is on the night of a full moon while it’s raining. The sky must also be very dark, which means that lunar rainbows appear very dull or white because the colour of the night is not bright enough to activate the cone cells (colour receptors) in our eyes.
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