Astron. Astrophys. 336, 1029-1038 (1998)
2. Method
2.1. Magnetohydrodynamic equations
We consider a thin, vertically oriented magnetic flux tube in the
solar atmosphere which is embedded in a non-magnetic external medium.
Following Defouw (1976), Roberts & Webb (1979) as well as Herbold
et al. (1985) the magnetohydrodynamic equations in the thin flux tube
approximation can be written
![[EQUATION]](img3.gif)
![[EQUATION]](img4.gif)
![[EQUATION]](img5.gif)
![[EQUATION]](img6.gif)
In our present adiabatic calculations we set ,
while in subsequent work we will consider radiation damping
. In the thin tube approximation the tube is seen
as a slender string of mass elements where the variations of the
physical quantities across the tube are assumed to be small. Hence,
the state of each mass element can be given by the single values
, p, S, u and B at
the tube axis. Here is the density, p the
gas pressure, S the entropy, u the gas velocity, and
B the magnetic field strength. All these variables are
functions of height z and time t. Any wave disturbance
traveling along the tube is assumed not to perturb the outside
atmosphere. Therefore, the gas pressure outside the tube
is assumed to be a function of z only.
At this point we must stress that the thin tube approximation
assumption must be further tested by detailed 2-D and 3-D MHD
computations. Theoretical work by Huang (1996) on 2-D slabs akin to
solar flux tubes indicates that for longitudinal tube waves the energy
leakage is relatively small and thus the thin tube approximation is
acceptable.
The four Eqs. (1) to (4) are sufficient to compute the five
quantities , p, S, u and
B, because only two of the three thermodynamic variables are
independent. We now eliminate B from the system by using Eqs.
(1) and (3). From (1) we get
![[EQUATION]](img11.gif)
while from (3) we have
![[EQUATION]](img12.gif)
![[EQUATION]](img13.gif)
where
![[EQUATION]](img14.gif)
is the Alfvén speed. With (6) and (7), the B
derivatives in (5) can be replaced and one obtains
![[EQUATION]](img15.gif)
The system (1) to (4) is now reduced to the three differential
equations (2), (4) and (9) for the unknowns ,
p, S and u. We also must compute the
thermodynamic variables temperature T and adiabatic sound speed
. Only two of the thermodynamic variables are
independent. We thus express all thermodynamic variables by the
variables and S. The relationship
between the thermodynamic variables is given by the ideal gas law
![[EQUATION]](img17.gif)
and
![[EQUATION]](img18.gif)
where is the ratio of specific heats,
µ the molecular weight, and the
gas constant. Combining the first and second law of thermodynamics
yields
![[EQUATION]](img21.gif)
![[EQUATION]](img22.gif)
Using the above relations, Eqs. (2), (4) and (9) can now be written
as a system of three partial differential equations for the three
unknowns , S and u. To employ the
method of characteristics we transform this system of three partial
differential equations into a system of six ordinary differential
equations defined along the characteristic lines. We obtain the two
compatibility relations
![[EQUATION]](img23.gif)
![[EQUATION]](img24.gif)
along the and
characteristics given by
![[EQUATION]](img27.gif)
where the upper (lower) sign corresponds to the
( ) characteristic. The
tube speed is given by
![[EQUATION]](img29.gif)
Eqs. (14) and (15) are four ordinary differential equations. The
two remaining ordinary differential equations are obtained from (4)
written in characteristic form
![[EQUATION]](img30.gif)
along the (fluid path) C0 characteristic
![[EQUATION]](img31.gif)
2.2. Shocks
During propagation longitudinal tube waves form shocks due to the
density gradient. At the shocks we have the variables
, ,
, ,
, ,
in front of the shock and corresponding variables with index 2 behind
the shock. Here is the enthalpy and
the tube cross-section. The Rankine-Hugoniot
relations for longitudinal tube waves can be written (Herbold et al.
1985)
![[EQUATION]](img40.gif)
![[EQUATION]](img41.gif)
![[EQUATION]](img42.gif)
where , are the gas
velocities in the shock frame. The transformation of the gas velocity
from the laboratory (Euler) frame into the shock frame is accomplished
by
![[EQUATION]](img45.gif)
where is the shock velocity in the
laboratory frame. The Rankine-Hugoniot relations are solved by
assuming that the front shock state is known and by specifying a
post-shock velocity . The front shock state is
updated through the iteration process for the respective hydrodynamic
time-step. With and known quantities in front
of the shock the cubic equation
![[EQUATION]](img49.gif)
with
![[EQUATION]](img50.gif)
![[EQUATION]](img51.gif)
![[EQUATION]](img52.gif)
![[EQUATION]](img53.gif)
is solved for by using a Newton-Raphson
iteration scheme. Here is the magnetic flux.
The other post-shock quantities are then computed using
![[EQUATION]](img56.gif)
![[EQUATION]](img57.gif)
![[EQUATION]](img58.gif)
![[EQUATION]](img59.gif)
![[EQUATION]](img60.gif)
and
![[EQUATION]](img61.gif)
2.3. Flux tube models
In our investigation we consider three different magnetic flux tube
models. We start by constructing a non-grey radiative and hydrostatic
equilibrium solar atmosphere model with an effective temperature
K and gravity
cm s-2 using the temperature and flux correction
procedure of Cuntz et al. (1994). In this model, NLTE H-
continuum and Mg II k line cooling have been assumed. The
atmosphere has a temperature which continuously decreases in outward
direction and there is no mechanical heating. Magnetic flux tubes are
subsequently embedded in this atmosphere. At height
, where in the external atmosphere the optical
depth is , the tubes have a specified radius
km and a magnetic field strength
. The tubes are allowed to spread with height in
pressure balance with the surrounding gas pressure (cf. Eq. 3) up to a
height . The spreading rate from height
to the maximum height km
is chosen differently for the different tube models.
The case with is called exponential
tube . For the so-called wine-glass tube model we have
. Here for the heights we
fit a radius function , which ensures that the
slope at is continuous
and that the tube approaches a specified radius
at great height. is the radius at
and L is determined by the slope at
. To ensure that the tube has this specified
radius, an additional time-independent external pressure is assumed,
which is supposed to originate from magnetic interaction with
neighboring tubes. The gas pressure in the tube is computed in
hydrostatic equilibrium and the temperature is determined by radiative
equilibrium using the above-mentioned temperature correction
procedures. Choosing and
leads to our third tube model, the constant cross-section tube
. For the wine-glass tube, we take km and
km. The three types of tubes obtained are
displayed in Fig. 1.
![[FIGURE]](img81.gif) |
Fig. 1. Shape of the exponential (E), constant cross-section (C), and wine-glass (W) magnetic flux tubes as used in the present work. The radii of the tubes are shown as function of height.
|
The exponential tube with its unobstructed spreading may be typical
for tubes in the interior of supergranulation cells or in areas just
outside the network region, while the constant cross-section tube may
be representative for the inner part of a very crowded network region.
The wine-glass tube with a filling factor thus
corresponds to the situation at the outer parts of a normal network
region (Solanki 1997, private communication).
2.4. Wave computations
Using a time-dependent magnetohydrodynamic wave code (Herbold et
al. 1985; Zhugzhda et al. 1995) various monochromatic waves with
periods P and wave energy fluxes were
introduced at height at the bottom of the tube
by means of a piston. The values of P and
have been varied to present a set of case
studies. The piston velocity u is prescribed by
![[EQUATION]](img86.gif)
where is the velocity amplitude. Here
and are the density in
the tube and the tube speed at height . During
the propagation, shocks form, which are treated as discontinuities and
permitted to grow to arbitrary strength and to merge. The positions of
shock formation are found by monitoring intersection points of
adjacent characteristics.
© European Southern Observatory (ESO) 1998
Online publication: July 27, 1998
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