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
(Priest 1984). 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, and is predominately composed of protons and electrons.
The solar wind was predicted theoretically by Eugine Parker (Parker 1958) a number of years before its existence was confirmed by means of satellite data (Neugebauer and Snyder 1966). Parker's prediction of a super-sonic outflow of gas from the Sun is a fascinating application of plasma physics.
The solar wind originates from the solar corona, which
is a hot, tenuous plasma, surrounding the Sun, with characteristic temperatures and
particle densities of about K and
,
respectively (Priest 1984). The corona is actually 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 (Priest 1984). 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 (Chapman 1957), by attempting to construct a model for a static solar corona. The equation of hydrostatic equilibrium for the corona takes the form
whereThe thermal conductivity of the corona is dominated by the electron thermal conductivity, and takes the form [see Equations (4.70) and (4.89)]
![]() |
(8.54) |
![]() |
(8.55) |
![]() |
(8.56) |
![]() |
(8.57) |
Equations (8.51), (8.52), (8.53), and (8.58) can be combined and integrated to give
![]() |
(8.59) |
![]() |
(8.60) |
We have just demonstrated that a static model of the solar corona is unsatisfactory. Let us, instead, attempt to construct a dynamic model in which material flows outward from the Sun.