Abstract
The energy generated in the solar core must be carried to the surface. In Chap. 2 radiation was treated as one possible way of energy transport. Another is convection, where internal energy, sometimes including latent heat, is carried along with the motion of matter. We know that convection is quite efficient in distributing heat in rooms, and we shall see in the present chapter that convection is also an efficient carrier of solar energy, at least in the outer 30% or so (by radius) of the Sun. The stratification of these outer layers will be found to be unstable, much like the stratification of the Earth’s troposphere which becomes unstable when the ground is heated.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1989 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Stix, M. (1989). Convection. In: The Sun. Astronomy and Astrophysics Library. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-97129-7_6
Download citation
DOI: https://doi.org/10.1007/978-3-642-97129-7_6
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-53796-0
Online ISBN: 978-3-642-97129-7
eBook Packages: Springer Book Archive