Issue |
A&A
Volume 396, Number 1, December II 2002
|
|
---|---|---|
Page(s) | 243 - 253 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361:20021358 | |
Published online | 22 November 2002 |
Detectability of large-scale flows in global helioseismic data – A numerical experiment
1
Kiepenheuer-Institut für Sonnenphysik, 79104 Freiburg, Germany
2
National Solar Observatory (Operated by the Association of Universities for Research in Astronomy, Inc. under cooperative agreement with the National Science Foundation.) , 950 N. Cherry Ave., Tucson, AZ 85719, USA
Corresponding author: M. Roth, mroth@kis.uni-freiburg.de
Received:
5
November
2001
Accepted:
18
September
2002
Convective motions affect the solar p-modes by shifting
their frequencies. In comparison to the frequency splitting caused by
the differential rotation, this is only a small additional effect. As
the spatial resolution of the inversions for the differential rotation
becomes better, it is important to know how these additional frequency
shifts modify the splitting coefficients and how these two effects
might be disentangled. Therefore we carry out a numerical
experiment. We use quasi-degenerate perturbation theory to create
frequencies of p-modes that are affected by differential rotation and
by large-scale flows. The simulated frequency sets are analyzed and
inverted for differential rotation. We use changes in the
coverage, the multiplets, and the inversion results as diagnostics to
draw conclusions about the detectability of large-scale flows in
global helioseismic data. The result is a detectability limit of the
order of 10 m s-1 for large-scale flows in the convection
zone. A sectoral poloidal flow with greater amplitude will lead to a
noticeable distortion of the rotation rate, while a zonal poloidal
flow with greater amplitude will lead to distorted even-a
coefficients and disrupted multiplets.
Key words: convection / Sun: rotation / Sun: oscillations
© ESO, 2002
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