会议专题

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)