PHYSICAL ILLUSIONS

These are examples of physical illusions, where what we see is not really there, but where the cause of the illusion in the behavior of light before it reaches the eye.

Mirage Phenomena

A mirage is a natural illusion that is an optical phenomenon. It is produced by the reflection of light when it passes into a layer of hot air lying close to a heated ground surface (known as a temperature inversion). In deserts, mirage may create the illusion of a lake in the distance (which is actually an image of the sky reflected by the hot air (temperature inversion layer).

The most commonly observed mirage is the inferior mirage, which is usually seen as a shiny patch on a hot surface that is the reflection of the sky. Summer sunlight may raise the temperature of an exposed surface as much as 80°C or more than the air not far above it. A strong temperature gradient is established just above the surface, and with it a relatively thin layer of reduced density.

Inferior Mirage

Formation of inferior image

The air is normal except for a thin heated layer, so the rays are mostly straight lines, but strongly curved upwards in the heated layer. An object AB appears to the observer at O reflected at A'B', inverted and below the horizon, in front of the shining pool that is the reflection of the sky. Except for inversion, the object is not distorted. Note that the rays to the top and bottom of the object are crossed. This crossing is necessary to produce the reflection. The object AB is also visible by direct rays in the normal way. It is not very unusual to see such inverted images, but in many cases there is nothing to be imaged, so just the shining pool of the sky is seen. The inferior mirage with this geometry is frequently seen while driving in the summer, and cars ahead may be seen reflected in it.

A superior mirage occurs when the air below the line of sight is colder than that above. This is called a temperature inversion, since it does not represent the normal equilibrium temperature gradient of the atmosphere. Since in this case the light rays are bent down, the image appears above the true object, hence the name superior. They are in general less common than inferior mirages, but when they do occur they tend to be more stable, as cold air has no tendency to move up and warm air no tendency to move down.

Superior mirage - photo by Carlos Santos
Carlos photographed this horizon line at 19:39 pm on
the Semptember 5th, 2007 on the beach of Furadouro in Ovar, Portugal.

Superior mirage detail - photo by Carlos Santos

Formation of superior mirage (source: Sechrist et al. 1989)

Superior images can be straight up or upside down, depending on the distance of the true object and the temperature gradient. Often the image appears as a distorted mixture of up and down parts.

The fata morgana is a complex mirage in which distant objects are distorted as well as elongated vertically. For example, a relatively flat shoreline may appear to have tall cliffs, columns, and pedestals. The phenomenon occurs under much the same meteorological conditions as the superior mirage with inversion, and contains features of both towering and inversion.

Learn more about mirage phenomena: http://www.du.edu/~jcalvert/astro/mirage.htm#Mira

Antisolar Rays

Antisolar rays are sometimes seen in the direction opposite the sun, converging to the antisolar point (towards the shadow of your head). They are caused by sunlight being scattered from aerosols like dust particles and water vapor. Clouds or terrain may block the sun in some places, which causes rays of light to become visible. The sun's rays are all parallel to each other, because the sun is very far away. However, perspective causes the rays seemingly to diverge from the sun's position, or, in the case of antisolar rays, converge to the point opposite the sun (antisolar point).

© World-Mysteries.com
The sun's rays are actually parallel.
They look as if they converge only due to perspective effect
(just like road lines appear to converge in the distance).

Rainbow

There is no definitive location for a rainbow. Its location is determined only by observer's position relative to the sun and rain.

Flattening of the Sun and Moon

The temperature (and pressure) gradient in the atmosphere causes bending of light rays. This is called atmospheric refraction. Light rays from the low sun or moon will refract more closer to the horizon. This is why the setting or rising sun (and moon) appears flattened: the light rays from the lower part of the sun's disk refract more than the rays emerging from the top, and the vertical angle over which you see the sun is decreased - it is flattened.

Green Flash

Green flashes and green rays are rare optical phenomena that occur shortly after sunset or before sunrise, when a green spot is visible for a short period of time above the sun, or a green ray shoots up from the sunset point. It is usually observed from a low altitude where there is an unobstructed view of the horizon, such as on the ocean.

Its explanation lies in refraction of light (as in a prism) in the atmosphere and is enhanced by atmospheric layering. Whilst we would expect to see a blue light, the blue is dispersed (this is why the sky is blue) and only the green light remains visible.

With slight magnification, a green rim on the top limb of the solar disk can be seen on most clear-day sunsets. However the flash or ray effects require a stronger layering of the atmosphere and a mirage which serves to magnify the green for a fraction of a second to a couple of seconds.