Proxies for overshooting above a convection zone
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.
Convection turbulence waves methods:numerical
Kwing L.Chan Harinder P.Singh
Department of Mathematics and Center for Space Science Research,Hong Kong University of Science and Department of Physics & Astrophysics,University of Delhi,Delhi,India
国际会议
The 252th Symposium of the International Astronomical Union(国际天文学联合会第252届研讨会)
海南三亚
英文
43-44
2008-04-06(万方平台首次上网日期,不代表论文的发表时间)