The world viewed in near IR light.
The world would not look the same if we were able to see near
IR light instead of visible light.
visible light
reflected by the tree
and photographed with normal
film
near IR light
reflected by the tree
and photographed using near
IR film
The picture at left
was taken using normal film, film that is sensitive to
visible light. The picture at right used near
infrared film. In both pictures we are looking
at sunlight that strikes the tree or the ground and is
reflected toward the camera where it can
be photographed (i.e. these aren't photographs of
visible light being emitted by the tree or the
ground).
Some things change, some things stay the same.
The tree and the grass at left are green and
relatively dark (they reflect green light but absorb
the other colors of visible light). The tree and
grass at right are white, almost like they were
covered with snow. The tree and grass are very
good reflectors of near infrared light. Clouds
are also good reflectors of near IR light, they appear
white in both images. Here are many
more images taken with infrared film.
Photographs of the ground taken from an air plane using
ordinary film at left (responds to visible light) and near
infrared film at right. Notice how much clearer the river is
in the picture at right. The IR photograph is able to "see
through" the haze. The haze is light being scattered
predominantly by air molecules. You may remember from the
1S1P topic on scattering that air molecules scatter shorter
wavelengths in much greater amounts that longer wavelengths.
Near IR light is not scattered nearly as much as visible light.
You wouldn't have seen the tree or the river if the photos above
had been taken at night. That is because they are
photographs of reflected sunlight.
This is a picture of the far IR light
that is emitted by a house (source
of this image). You'd see this during
the day or night, sunlight doesn't need to be present.
Remember that the amount of energy
emitted by an object depends strongly on temperature (temperature
to the 4th power in the Stefan-Boltzmann law). Thus it is
possible to see hot spots that emit a lot of energy and appear
"bright" and cold spots. Photographs like these are often
used to perform an "energy audit" on a home, i.e. to find spots
where energy is being lost. Once you locate one of these hot
spots you can add insulation and reduce the energy loss.
This photograph has been color coded. Reds and orange mean
more intense emission of IR radiation (warmer temperature) than
the blues and greens. The reds show you were energy is being
lost, escaping from the warm interior of the house (often through
poorly insulating windows). Many of the roof tops are blue,
they are cool. There is probably a lot of insulation in the
attic and little energy is being lost out the roof.
Later in the semester we will looking at satellite
photographs of clouds. Satellites take pictures of both
the visible light reflected by clouds and also the IR
radiation emitted by clouds.