The existence of winds from cataclysmic variables (CVs)
has been known for some time, there are a variety of unresolved
questions surrounding this phenomenon. These include: the origin
of the apparent polar nature of the winds; the rate of mass loss
in the winds and the associated driving mechanism; the origin for
the characteristic shapes of the UV resonance line profiles,
particularly the absorption component; and the apparent association
between outburst state and the wind existence. Resolution of all
these issues depends on understanding the dynamics of the wind.
We have developed one and two dimensional hydrodynamical models for
these winds which explains many of the observed properties
Our procedures for treating the winds in one dimension are analagous to
those developed for radiation pressure driven winds from stars by, for example,
Castro Abbott and Klein (1978; CAK). However, the critical point conditions
in the disk case are more complicated owing to the fact that in the
disk wind problem the force of gravity per mass along the stream
lines increases. Also there is no spherical symmetry in the disk wind,
thus we introduce a geometric correction for the mass conservation equation
which reflects the fact that the wind streamlines are likely to start out
vertically relative to the disk plane, and end up more nearly radial
relative to the central star far from the disk. As a result, where CAK
obtained an analytic expression for the mass loss rate in the wind and
for the velocity law far from the critical point, we are forced to
solve our transcendental equation numerically, and cannot present
simple analytic expressions for the corresponding quantities.
We can, however, easily explore numerically a wide range of parameter
values. We obtain several wind solutions varying disk radius from
0.1 R_sun to 10 R_sun . The height of the critical point is
found to be approximately 2.5 times the photospheric height
throughout this range. We find that the terminal velocity decreases
with radius according to R^-0.85 approximately, and that
dot M_wind varies with radius according to R^+0.29
approximately. This can be compared with the variation of escape
velocity with radius ( sim R^-1/2 ). The most important physical
quantities which change with radius in these one dimensional models
and which may explain the radial dependencies are the gravity,
the photospheric height, and the radiation flux. We obtain a
ratio of wind terminal speed to escape speed which ranges from
28.15 to 5.76 over the disk radii varying from 0.1R_sun to
10R_sun . The wind velocity profile starts with a low
gradient near the surface of the disk, arrives at a large gradient
at a height of z approx 0.1 R_disk , and achieves a velocity of
the order of the terminal velocity at a height of
z approx 4 R_disk .
The highest value of optical depth is found at approximately
15 rm ;km ; sec^-1 . This is consistent since our winds
start at sound speed ( 10rm ;km ; sec^-1 in our models)
and at 1.5 times the sound speed the optical depth will receive
contributions from the start of the wind until twice the sound speed
at a maximum average of density, since density is found to decrease
along the streamline. Optical depths greater than 0.1 , which could
in principle generate absorption lines, are found approximately
between the velocities of 6rm ;km ; sec^-1 and
39rm ;km ; sec^-1 . In spite of these results, we do not
expect an absorption line to be observed at these relatively small
speeds since they will likely be superimposed on stronger emission
lines. On the other hand for velocities equal to or greater than
200rm ;km ; sec^-1 we obtain optical depths less
than 0.01; . Thus, from our one dimensional model, we would conclude
that due to the steep diminution in density, the optical depths are
too small to produce an observable P-Cygni absorption line.
Additional wind solutions are obtained by varying L_disk from
0.1 L_sun to 10 L_sun , for a value of R_disk=R_sun .
We find that the terminal speed is approximately independent
of luminosity. Early type stars with line driven winds also show
terminal speeds approximately independent of luminosity
(citecas75,abb78). We also found that mass loss rates depend on
the luminosity of the disk according to L_disk^+1.4288
approximately, again analogous to line driven winds of early type
stars which show a dependence of
L_star^1/ alpha (in our models
1 over alpha=1 over 0.7 approx +1.4286 ).
From our one dimensional models we are able to identify a criterion
for the existence of winds in terms of the logarithmic derivitive of the
radiation field with height above the disk. That is, if this quantity
does not increase with height faster than z^{1/2}, there can be no wind
solution. In other words,
a minimum of optical depth of the lines driving the wind is necessary
for a wind to exist. This contrasts with the case of early type stars
where a wind will always develop for the values of alpha between
zero and one. The minimum optical depth that we find
to be a requirement for the existence of disk winds may be physically
interpreted as the necessity of the wind to surpass the barrier of an
increasing gravity, which is a peculiarity of the disk wind case.
The most important feature of the 2D model results, the role of
rotational forces, is apparent in the figure. Gas leaving the disk is
accelerated upwards by the radiation pressure force. However,
at a height comparable to the disk radius the Keplerian balance,
which initially allows a stable flow in the direction normal to the
disk, is lost. The wind flows radially above this region. This effect
occurs at all radii, but the strength of the radial force is greater
at smaller radii. Thus the initially vertical streamlines are bent
most at small radius, with the result that they collide with more
nearly vertical streamlines of material originating at large radii.
This collision results in shocks and a large region of enhanced
density which runs diagonally in the z - r plane.
Figure 1a: Contours of constant density superimposed on velocity vectors
as a function of position from a simulation of a line driven disk wind.
Position is expressed in units of the fiducial radius, chosen to be one
solar radius.
Figure 1b Color contour plot of density for the same simulation shown in
figure 1a. Density scale is shown in the upper right.
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Accretion Disk Winds
Background
One Dimensional Models
Two Dimensional Models
The gas flow near a disk is inherently two
dimensional, and one dimensional models require severe approximations
which may limit their validity. Therefore, we have constructed a two
dimensional numerical model for line driven winds near CV disks.
The numerical method we adopt is based on the PPM (Piecewise
Parabolic Method) numerical scheme. The PPM method has been discussed
in detail by Colella and Woodward (1984) for a one dimensional spatial
grid with planar, cylindrical or spherical symmetries.
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