191
of these kinds of radiation. The
waves are absorbed by the air’s
molecules, reflected back into
space, or scattered in all directions
into a meaningless hodgepodge.
As a result, it is almost impossible
to garner information about most
kinds of non-visible radiation
from terrestrial observatories.
Spitzer’s 1946 paper, entitled
Astronomical Advantages of
an Extra-terrestrial Observatory,
highlighted the problem of detecting
non-visible radiation. His solution
was to put a telescope into space.
But Spitzer also highlighted the
obstacles to such a proposal: first,
the technological challenge of
inventing space travel, and second,
that of designing an instrument
capable of operating in space by
remote control from the ground.
Twinkle, twinkle little star
The rest of Spitzer’s paper was
focused on solving a problem that
had frustrated astronomers for
centuries—the sky itself. Viewed
from Earth, the stars appear to
twinkle. This effect is caused by the
star’s light shifting back and forth,
and rising and falling in brightness.
This is not a property of starlight,
but is caused by Earth’s thick
atmosphere. The twinkle becomes
more marked as magnification
increases, making the objects
appear shaky and fuzzy in the
eyepiece of a telescope or as diffuse
smears of light in photographs.
The scientific term for twinkling is
scintillation. It is caused when light
passes through layer upon layer
of turbulent air in the atmosphere.
The turbulence itself has no effect
on the light, but the density and
temperature differences that are
making the air churn and swirl
do have an effect. As the starlight
passes through one pocket of air
to another of a different density,
it refracts slightly, with some ❯❯
See also: Beyond the Milky Way 172–77 ■ Radio astronomy 179 ■ Studying distant stars 304–05 ■
Gravitational waves 328–31
ATOMS, STARS, AND GALAXIES
The level of the orange curve in this graph represents how
opaque the atmosphere is at the given wavelength of radiation.
The major windows are around visible wavelengths (marked by
the rainbow) and radio wavelengths from about 1 mm to 10 m.
The solution to both problems
is to put telescopes in space.
Earth’s atmosphere
causes astronomical
objects to twinkle, so they
cannot be captured with
sharp definition.
Many kinds of
electromagnetic radiation
cannot pass through
the atmosphere.
ATMOSPHERIC OPACITY (%)
100
150
50
0
WAVELENGTH
0.1nm 1 nm 10nm 100nm 1 μm 10pm 100pm 1 mm 1 cm 10cm 1 m 1 0m 1 00m 1 km