Recent high resolution observations of the Call fine structure are discussed, An analytic method is applied to examine the effects of velocity fields on multi-component model atmospheres in which the central reversal in the bright components is due to self-absorption. It is shown that the inclusion
A three-component model for the formation of the chromospheric CaiiK line
โ Scribed by P. R. Wilson
- Publisher
- Springer
- Year
- 1970
- Tongue
- English
- Weight
- 481 KB
- Volume
- 15
- Category
- Article
- ISSN
- 0038-0938
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โฆ Synopsis
A recent two-component model for the formation of the Ca II K line in the solar chromosphere put forward by Beebe and Johnson is discussed. Although this model is a great advance on existing one-component models, it is pointed out that observations require a minimum of three components in order to understand the formation of the K2 peaks.
In order to make some progress in the study of multicomponent models an adaptation of the empirical (or analytic) approach is suggested. This relates the line source function directly to observations and places a secondary importance (at this stage) on the synthetic approach to the problem. A model is obtained which is in adequate agreement with observed mean profiles and its features are briefly discussed.
๐ SIMILAR VOLUMES
We discuss a model for the formation of the chromospheric Ca n K line which does not make the usual assumption of complete redistribution. Using a physically reasonable scattering model, we find significant departures due to the frequency dependence of the line source function, particularly in the r
The emission of the CaII K line from a spinning cylindrical spicule model is considered. In order to reproduce the observed spicule K line profiles, the model must have both radial and axial gradients in Ne and Te. The rotating spicule model is optically thin at all heights and is hotter and more de
The formation of the solar Call K-line core is studied under the assumption of a two component chromosphere for many atmosphere models, which are tested by comparing observed and calculated average intensity profiles at several places on the solar disk. Non-LTE-line profile calculations are made usi