Hostname: page-component-7bb8b95d7b-qxsvm Total loading time: 0 Render date: 2024-10-04T09:22:44.830Z Has data issue: false hasContentIssue false

Convective overshoot and upper boundary conditions

Published online by Cambridge University Press:  03 August 2017

A. Nesis*
Affiliation:
Kiepenheuer-Institut für Sonnenphysik, Schöneckstr. 6, West-Germany

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Calculations of the frequency of solar oscillation are sensitive to the upper boundary conditions of the model. Our investigations of the velocity fields of the overshoot layers (photosphere) have shown that there is a minimum of velocity at about 200 km above τ = 1: We suggest that this minimum provides a natural upper boundary condition for the calculations of solar oscillation. The propagation of sound in these layers has to be regarded as a propagation in a turbulent medium.

Type
Chapter 7: Oscillations in the Solar Atmosphere
Copyright
Copyright © Reidel 1988 

References

Gough, D.O.: 1984, Phil. Trans. R. Soc. Lond. A313, 27 Google Scholar
Kneer, F.: 1984, in Small-Scale Dynamical Processes in Quiet Atmospheres ed. Keil, S.L., (National Solar Observatory), p. 110 Google Scholar
Nesis, A., Durrant, C.J., Mattig, W.: 1984, in Small-Scale Dynamical Processes in Quiet Atmospheres, ed. Keil, S.L., (National Solar Observatory), p. 243 Google Scholar
Nesis, A.: 1984, The Hydromagnetics of the Sun, ESA SP-220, p. 203 Google Scholar
Stix, M.: 1986, private communication Google Scholar
Ulrich, R.K., Rhodes, E.J.: 1983, Astrophys. J. 265, 551 Google Scholar