In the vicinity of the Earth, (i.e., at about 1 AU from the
Sun) the solar wind velocity typically
ranges between 300 and 1400
. The average value
is approximately
, which corresponds to about a
4 day time of flight from the Sun. Note that the solar wind is
both super-sonic and super-Alfvénic.
The solar wind is predominately composed of protons and electrons.
Amazingly enough, the solar wind was predicted
theoretically by Eugine Parker
a number of years before its
existence
was confirmed using satellite data.
Parker's prediction of a super-sonic
outflow of gas from the Sun is a
fascinating scientific detective story, as well as a wonderful application
of plasma physics.
The solar wind originates from the solar corona. The solar corona
is a hot, tenuous plasma surrounding the Sun, with characteristic temperatures and
particle densities of about
K and
,
respectively. Note that the corona is far hotter than the solar
atmosphere, or photosphere. In fact, the
temperature of the photosphere is only about
K. It is
thought that the corona is heated by Alfvén waves emanating from the
photosphere. The solar corona is most easily observed during a total
solar eclipse, when it is visible as a white filamentary region
immediately surrounding the Sun.
Let us start, following Chapman,
by attempting
to construct a model for a static solar corona. The equation
of hydrostatic equilibrium for the corona takes the form
The thermal conductivity of the corona is dominated by the electron thermal
conductivity, and takes the form [see Eqs. (260) and (280)]
| (734) |
| (735) |
| (736) |
![]() |
(737) |
Equations (731), (732), (733), and (738) can be combined and
integrated to give
![]() |
(739) |
![]() |
(740) |
Since we have just demonstrated that a static model of the solar corona is unsatisfactory, let us now attempt to construct a dynamic model in which material flows outward from the Sun.