The best – albeit indirect – proof of the presence of magnetized winds is the spin-down of convective stars on the main sequence as such a wind carries away angular momentum from the star. I will discuss this in Section 5.2.
Direct measurement of ionized winds from solar-like stars has not yet succeeded; potential detection
methods include the measurement of thermal radio emission from the winds (Lim and White, 1996
; Gaidos
et al., 2000
), and signatures of charge exchange in X-ray spectra (Wargelin and Drake, 2001). Lim and
White (1996) and van den Oord and Doyle (1997) gave upper limits to the mass-loss rates of
for “solar-like” winds with T
1 MK emanating from M-type dwarfs. Gaidos
et al. (2000
) derived upper limits to
for three young solar analogs (
UMa,
Cet, and
Com), finding
.
The most promising approach to date is an indirect method making use of Ly
absorption in so-called
“astrospheres”; the latter are suggested to be a consequence of interactions between stellar winds and the
interstellar medium (ISM). This subject has been extensively reviewed in the Living Reviews in
Solar Physics article by Wood (2004
); I will therefore only briefly summarize the essential
results.
Solar/stellar winds collide with the interstellar medium, forming, with increasing distance from the star,
a termination shock (where the wind is shocked to subsonic speeds), a heliospause (separating the plasma
flows from the star and the ISM), and the bow shock (where the ISM is shocked to subsonic speeds). The
heliosphere is permeated by interstellar H i with T
(2–4)
104 K (Wood et al., 2002
). Much of
this gas is piled up between the heliospause and the bow shock, forming the so-called “hydrogen wall” that
can be detected as an absorption signature in the Ly
line. The excess absorption from the Sun’s own
hydrogen wall is, due to the deceleration of the ISM relative to the star, redshifted, while that of other
astrospheres is blueshifted.
The measurable absorption depths are compared with results from hydrodynamic model calculations
(Wood et al., 2002
, 2005
). The important point is that the amount of astrospheric absorption should scale
with the wind ram pressure,
, where
is the (unknown) wind velocity (Wood and
Linsky, 1998). The latter is usually assumed to be the same as the solar wind speed. From this,
is
derived.
The Sun’s hydrogen wall was detected in ultraviolet spectra by Linsky and Wood (1996), and an
equivalent astrosphere around
Cen A and B was interpreted by Gayley et al. (1997). Further
important wind mass loss measurements based on this method have been presented by Wood
et al. (2002
) (and references therein) and Wood et al. (2005
). A systematic study of all derived
mass-loss rates shows that
per unit stellar surface correlates with the stellar X-ray surface
flux,
(an equivalent relation therefore holds between
and LX); using the activity-age relation
(Section 5.5.1), one finds
(Wood et al., 2005
). These two laws indicate that stellar-wind mass loss is – in principle – a genuine
activity indicator, the mass-loss being higher in young, magnetically active stars. Extrapolating the above
law up to the X-ray saturation limit (FX
2
107 erg cm–2 s–1) would suggest
(or
)
of the youngest solar analogs to be about a thousand times higher than the present-day solar
mass loss (
; e.g., Feldman et al. 1977). However, this power-law
relation breaks down for the most active stars with FX
8
105 erg cm–2 s–1 (Wood
et al. 2005
, Figure 10
). Stars at this limit show
about 100 times the present solar value, while
drops toward higher activity levels to about 10 times the solar value. The reason for this
breakdown between X-ray activity and wind-mass loss may be related to the appearance of
high-latitude active regions (spots) in the most active stars (Section 4.1.2); if the magnetic field
becomes more akin to a global dipole, then wind escape may be inhibited in such stars (Wood
et al., 2005
).
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