Figure 66. Idealized structure
of the sun. Idealized structure of the sun (not to scale). There
is a complex interplay among the different regions of the sun.
Edward G. Gibson, The Quiet Sun
, NASA SP-303 (1973), p.11,
fig.2-3.
[366].....of the
photosphere to around 4300 at the base of the chromosphere, and
then rising through the chromosphere, at first slowly but then
very steeply to between 500000 and 1000000 K at the top. This
temperature curve posed a problem, for it was assumed that the
corona derived its heat from the chromosphere, yet that would
imply that heat was flowing from a colder region to a hotter one,
contrary to the laws of thermodynamics. As late as 1972 Leo
Goldberg, director of Kitt Peak National Observatory, pointed to
this phenomenon as "the most important unsolved mystery
surrounding the quiet sun."62
Above the chromosphere lies the corona,
the sun's exosphere. Here 1000000 K temperatures prevail, and an
important problem facing the solar physicist was to explain how
the corona gets its energy. Although the corona is extremely hot
and very active, its density is so very low that it is not
normally visible from the ground, where it is completely obscured
by scattered sunlight in the earth's atmosphere. Only during solar
eclipses, with the moon blocking out the sun's disk, could the
astronomer get a good look at the entire corona. One of the
benefits of rockets and satellites was to permit carrying
coronagraphs above the light-scattering atmosphere where the
corona could be seen even in the absence of a solar
eclipse.
Much of solar physics concerns the
interplay among the different regions of the sun. This interplay,
however, can be followed only in terms of its effect upon the
radiations emitted from those regions. For this reason, one of the
first tasks of the astronomer was to obtain good spectra of the
sun and their variation with time. Regions from which radiations
of highly ionized atoms came would be hot regions, and
temperatures could be estimated. The magnetic field intensities,
for example in sunspots, could be estimated from the splitting of
lines emitted within the field. If a cooler gas overlay a hotter,
similar gas, the cooler gas would absorb some of the light emitted
by the hotter one. This would produce reversals in the emission
lines of the hotter gas, generating the famous Fraunhofer lines of
the solar spectrum discovered in the 19th century. By piecing
together information of this kind, the locations of different
gases relative to each other and their temperatures could be
determined. Changes in magnetic field that occurred in association
with solar activity, such as the appearance of solar flares, could
be followed. Changes were important, since there were strong
indications that magnetic fields were the source of much of the
energy in solar flares.
These techniques were, of course,
applicable in the visible wavelengths and were employed to the
fullest by the ground-based astronomer. The space astronomer
simply provided an additional handle on things by furnishing
spectral data in the ultraviolet and x-ray wavelengths. And these
data began to accumulate from the very earliest sounding rocket
flights. Year by year, flight by flight, they were added to until
by the end of the [367] decade the
solar spectrum was known in great detail from visible through the
ultraviolet wavelengths and into the x-rays.63