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Why Send Spitzer into Space?
The amazing variety of objects in our Universe send us light all across the
electromagnetic spectrum. However, much of this light (or radiation) does
not reach us at ground level here on Earth. Why? Because we have an
atmosphere which blocks out certain types of radiation, while letting other
types through. Fortunately for life on Earth, our atmosphere blocks out
harmful high-energy radiation like x-rays, gamma rays and most of the
ultraviolet rays. The atmosphere also absorbs most of the infrared radiation which
reaches the Earth from space.
On the other hand, our atmosphere is transparent to visible
light, most radio waves, and small windows within the infrared region.
Most of the infrared light coming to us from the Universe is absorbed by
water vapor and carbon dioxide in the Earth's atmosphere. Only in a
few narrow wavelength
ranges, can infrared light make it through
(at least partially) to a ground based infrared telescope.
The Earth's atmosphere causes another problem for infrared astronomers.
The atmosphere itself radiates strongly in the infrared, often putting
out more infrared light than the object in space being observed. This
atmospheric infrared emission peaks at a wavelength of about 10 microns
(micron is short for a micrometer or one millionth of a meter).
So the best view of the infrared universe from ground based telescopes
are at infrared wavelengths which can pass through the Earth's
atmosphere and at which the atmosphere is dim in the infrared.
Ground based infrared observatories are usually placed near the
summit of high, dry
mountains to get above as much of the atmosphere as possible.
Even so, most infrared wavelengths are completely absorbed by the
atmosphere and never make it to the ground. The only way to observe these
wavelengths is to get high above the atmosphere.
From the table below, you can see that only a few of the infrared
"windows" have both high sky transparency and low sky emission.
These infrared windows are mainly at infrared wavelengths below
4 microns.
Infrared Windows in the Atmosphere
Wavelength
Range
|
Band
|
Sky Transparency
|
Sky Brightness
|
|
1.1 - 1.4 microns
|
J
|
high
|
low at night
|
|
1.5 - 1.8 microns
|
H
|
high
|
very low
|
|
2.0 - 2.4 microns
|
K
|
high
|
very low
|
|
3.0 - 4.0 microns
|
L
|
3.0 - 3.5 microns: fair
3.5 - 4.0 microns: high
|
low
|
|
4.6 - 5.0 microns
|
M
|
low
|
high
|
|
7.5 - 14.5 microns
|
N
|
8 - 9 microns and 10 -12 microns: fair
others: low
|
very high
|
|
17 - 40 microns
|
17 - 25 microns: Q
28 - 40 microns: Z
|
very low
|
very high
|
|
330 - 370 microns
|
|
very low
|
low
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For the most part, everything we learn about the Universe comes from
studying the light (or electromagnetic radiation) emitted by objects in
space. To get a complete picture of any object in the Universe,
we need to examine it in all of its light, using the information sent to us
at all wavelengths.
This is why it is so important
to send observatories, like the Spitzer Space Telescope,
into space, to get above our atmosphere
which prevents so much of this valuable information from reaching us.
Spitzer's instruments will study radiation
between wavelengths of 3 and 180 microns. Most of this infrared radiation is
blocked by the Earth's atmosphere and cannot be observed from the ground.
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