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Topology of convection beneath the solar surface

Stein, R. F., Nordlund, A.·1989·The Astrophysical Journal

Abstract

It is shown that the topology of convection beneath the solar surface is dominated by effects of stratification. Convection in a strongly stratified medium has: (1) gentle expanding structureless warm upflows and (2) strong converging filamentary cool downdrafts. The horizontal flow topology is cellular, with a hierarchy of cell sizes. The small density scale height in the surface layers forces the formation of the solar granulation, which is a shallow surface phenomenon. Deeper layers support successively larger cells. The downflows of small cells close to the surface merge into filamentary downdrafts of larger cells at greater depths, and this process is likely to continue through most of the convection zone. Radiative cooling at the surface provides the entropy-deficient material which drives the circulation.

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Metadata

Authors
Stein, R. F., & Nordlund, A.
Venue
The Astrophysical Journal
Published
1989-07
Volume
342
Pages
L95
ISSN
  • 0004-637X (ISSN-L)
  • 1538-4357
OpenAlex
W2073847196
Cited by
301
References
0
FWCI
21.96
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Topology of convection beneath the solar surface. https://app.cochat.ai/papers/10.1086/185493
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Stein, R. F., & Nordlund, A. (1989). Topology of convection beneath the solar surface. The Astrophysical Journal. https://doi.org/10.1086/185493

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