A dynamical, homogeneous model of the chromosphere-corona transition region and of the lower corona is presented, based on the hydrodynamical equations and on a semi-empirical relation deduced from radio observations. The model is shown to be in agreement with radio and UV observations and with the
A dynamical model of the corona
β Scribed by Stephen L. Browne; Robert J. Bessey
- Publisher
- Springer
- Year
- 1973
- Tongue
- English
- Weight
- 926 KB
- Volume
- 31
- Category
- Article
- ISSN
- 0038-0938
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β¦ Synopsis
The hydrodynamic equations for art ideal, inviscid, fully ionized hydrogen gas in a gravitational, but not magnetic, field are solved by an explicit Lax-Wendroff two-step technique using a one-dimensional slab symmetry. Radiation and thermal conductivity are included. The model spans 100000 km starting from the chromosphere-corona transition region. An initially isothermal gas is seen to evolve coronal properties in 4000 s, by which time it settles into dynamic equilibrium characterized by a 2000 km transition region, a temperature maximum of 1.6 β’ 106 K at a height of 60000 kin, and a solar wind mass flux of 10 -9 gcm -~ s -1.
π SIMILAR VOLUMES
A simple model of the lower corona which allows for a possible difference in the electron and proton temperatures is analyzed. With the introduction of a phenomenological heating term, temperature and density profiles are calculated for several different cases. It is found that, under certain circum