We often see what appears like water on a dry road on sunny,
hot days. However, when we get to the
water-like area that produces the reflection, the road is perfectly dry. This is an optical effect called a
mirage. It appears not only on roads and
pavement, but also on deserts or any open area subject to heating by sunlight.
These mirages are caused not by any water on the surface, but
by warm air immediately above the pavement.
The sunlight beating on the pavement warms the pavement significantly
above the ambient air temperature. The
warm pavement in turn warms a layer of air immediately above the pavement. The warm air layer is about 5 cm deep. The simplest model to explain the mirage
considers the warm air to have a definite thickness and a well-defined boundary
with the cooler ambient air above it.
Because warm air is less dense than cool air, it has a lower
refractive index. Consider light originating in the cold air above the
boundary. When the light strikes the
boundary to traverse into the region of less refractive index it bends. If light strikes the boundary at a shallow
grazing angle, it is totally reflected by the boundary. This is called "Total Internal
Reflection". The cold air resembles
the material inside of glass - it is denser than the warm air. For glass, total internal reflection occurs
whenever the angle between the internal ray and the glass surface is less than
about 48 degrees.
The critical internal angle for total internal reflection for
glass is rather large due to the large relative refractive index for
glass. For the hot air mirage, however,
the critical angle very small because the hot air and cool air have very close
refractive indices.
The sharp boundary for a hot air mirage and total internal
reflection is an over simplification.
Instead of a sharp boundary, there is a temperature gradient over the
hot pavement and a corresponding smooth variation in the refractive index. As a result the light reflected in a mirage
follows a curved path rather than a straight path. The curved path model and the straight path
from a sudden change produce the same overall results.