Proxies for overshooting above a convection zone

Details Proxies for overshooting above a convection zone Proxies for overshooting above a convection zone

Oct 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008iaus..252...43c&link_type=abstract

The Art of Modeling Stars in the 21st Century, Proceedings of the International Astronomical Union, IAU Symposium, Volume 252, p

Astronomy and Astrophysics

Astronomy

1

Convection, Turbulence, Waves, Methods: Numerical

Scientific paper

Due to the up/down asymmetry caused by stratification, overshooting
above differs from overshooting below a convection zone. The flux of
kinetic energy, frequently used as a proxy of overshooting below a
convection zone, cannot be used for the upward problem.

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