Abstract
Steady stellar winds are generally divided into two classes: (i) the winds proper, for which the energy flux per unit solid angle, E
∞
, is non-zero, and (ii) the breezes, for which E
oo
= 0. The breezes may be distinguished from one another by the value of the ratio,
g
, of kinetic to thermal energy of the particles in the limit of large distance,
r
, from the stellar centre, or more precisely by g=lim mv
2
r->∞ —
kT
' where
v
(
r
) is breeze velocity,
T
(
r
) is temperature,
m
is mean particle mass, and
k
is the Boltzmann constant. Solutions have previously been obtained for values of
g
in the range 0 <
g
< 1, in which the breezes are subsonic everywhere with respect to the isothermal speed of sound. It is demonstrated here that two distinct solutions exist as g -> 5/3, namely (in an obvious notation) the
g
= 5/3 — and the
g
= 5/3 + possibilities. It is shown that, if
g
> 5/3 (
g
< 5/3) the solutions are everywhere supersonic (subsonic) with respect to the adiabatic speed of sound. If 1 <
g
< 5/3, they possess a critical point, at which the isothermal speed of sound and the flow speed coincide. The winds are examined in the limit
E
∞ -> 0, and the relation with the breezes is studied. In particular, it is shown that, for r <
0
(
E
∞
-2/5
), the winds satisfy the stellar breeze equations to leading order, and possess a critical point at
r
=
0
(1). For r >
0
(
E
∞
-2/5
), the solutions do not obey the breeze equations. They ultimately follow the Durney asymptotic law [T =
0
(
r
-4/3
), for
r
-> ∞] for the winds. This demonstration of how the winds merge continuously into the breezes as
E
∞
-> 0 is new. The question of how the particle density (
N
0
) and temperature (
T
0
) at the base of the stellar corona determine the type of solution realized outside the star is examined. Even when the flow speed,
v
0
, at the base of the corona is subsonic, non-uniqueness can occur. In one domain of the (
N
0
,
T
0
) plane, two distinct types of breeze are possible; in another these, together with a wind (E∞ =f= 0), are permissible. Elsewhere (large
N
0
, moderate
T
0
) only a unique breeze exists or (small
N
0
and/or
T
0
) a unique wind. In some domains (large
T
0
) no steady solution exists, unless the requirement that the corona is subsonic is relaxed. In this case, however, the problems of non-uniqueness are severely aggravated.
Cited by
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