In article <0d5c0f1b-fce0-4aa0-8598-
d74dcf...@z19g2000vbe.googlegroups.com>,
chr...@nypost.dk says...
That's because the solar radiation in H-alpha originates from near the
temperature minimum in the solar atmosphere. White light originates
from a layer a few thousand kilometers below the temperature minimum.
It works like this: the Sun has no solid surface but is a "ball of gas"
which is mostly non-transparent (= opaque). When we look at the center
of the solar disk, we see somewhat deeper down in the "ball of gas" of
the Sun compared to when we look near the limb of the solar disk. This
is because of geometrical reasons combined with the fact that we can see
through a certain number of atoms (that number is wavelength dependent)
before the gas becomes too non-transparent for us to see any further
down.
Now, do we get limb darkening or limb brightening? That depends on how
the temperature changes with altitude at the region where most of the
light we see originates. At the photosphere, where the white light
originates, the temperature drops with altitude. Near the solar limb we
don't see as far down as at the center of the solar disk. That means
near the solar limb we see somewhat cooler gases. Cooler gases radiate
less, and therefore we see a limb darkening.
The light at H-alpha originates from a higher layer in the Sun, in the
chromosphere near the temperature minimum. Therefore, the temperature
rises above where H-alpha originates. Again, near the solar limb we
don't see as far down as at the center of the solar disk. But in this
case it means we see somewhat hotter gases near the solar limb in H-
alpha (as well as in the center of any dark spectral line in the Sun's
spectrum), i.e. we see a limb brightening.
This effect is even more pronounced in the Lyman-alpha spectral line in
the far ultraviolet: Lyman-alpha is even an emission (= bright) line in
the solar spectrum, as opposed to H-alpha which is an absorption (=
dark) line. That's because Lyman-alpha originates from an even higher
altitude in the solar atmosphere.
If you want to know more about how this works, read about Plank's Law
and Kirchoff's Laws -- Wikipedia is a good starting point. You could
also read about Radiative Transfer.