Solberg-Hoiland criterion sanjidâr-e Solberg-Høiland Fr.: critère de Solberg-Høiland A criterion for → convective stability in → massive stars. The Solberg-Høiland stability criterion corresponds to the inclusion of the effect of → rotation (variation of → centrifugal force) in the convective stability criterion. It is a combination of → Ledoux’s criterion (or possibly → Schwarzschild’s criterion) and → Rayleigh’s criterion. Both the dynamical shear and Solberg-Høiland instabilities occur in the case of a very large → angular velocity decrease outwards. Therefore, in a → rotating star the Ledoux or Schwarzschild criteria for convective instability should be replaced by the Solberg-Høiland criterion. More specifically, this criterion accounts for the difference of the centrifugal force for an adiabatically displaced fluid element. It is also known as the axisymmetric baroclinic instability. It arises when the net force (gravity + buoyancy + centrifugal force) applied to a fluid parcel in an adiabatical displacement has components only in the direction of the displacement (A. Maeder, Physics, Formation and Evolution of Rotating Stars, 2009, Springer). See also: E. Høiland, 1939, On the Interpretation and Application of the
Circulation Theorems of V. Bjerknes. Archiv for mathematik og
naturvidenskab. B. XLII. Nr. 5. Oslo. H. Solberg, 1936 (reprint), Le mouvement d’inertie de l’atmosphere
stable et son rôle dans la théorie des cyclones. H. Solberg, 1941, On the Stability of the Circular
Vortex. Avhandl. utg. av Det Norske Videnskaps-Akademi i
Oslo. I. Mat-Naturv. Klasse. No. 11. |