Traditionally the infrared region of the spectrum was considered to be
wavelengths just longer than the reddest colours visible to the human
eye, typically about 7000Å or (0.7
m). However, in modern
astronomical usage wavelengths up to about 10,000Å (or 1
m) tend
to be described as `optical' and longer wavelengths as `infrared'. This
terminology reflects both a change in the type of detector used and the
behaviour of the terrestrial atmosphere at about 10,000Å. It is
cumbersome to quote infrared wavelengths in Ångström and they are
usually given in micron. The infrared region stretches to about 350
m;
longer wavelengths are referred to as the sub-millimetre part of the
spectrum.
The terrestrial atmosphere is largely opaque at most infrared wavelengths
longer than 1
m, largely due to absorption by water vapour and
carbon dioxide. However, there are a series of wavelength ranges or
windows where the atmosphere is mostly transparent (see
Figure
). Ground-based infrared observations must be
made in these windows. Each window corresponds to a band in the
system (see Section
) and the corresponding band and window
have the same name.
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The width, maximum transmission and, to an extent, central wavelength
of the windows vary with geographical location and in particular with
altitude. They also vary with the current meteorological conditions.
The windows are particularly sensitive to the amount of water
vapour, which is why infrared observatories tend to be at high, dry sites.
The variation in the infrared windows at different locations is the
underlying reason for different versions of the
system being
used at different observatories, as mentioned in Section
.
The CCD Photometric Calibration Cookbook