A preliminary analysis of recent measurements of the brightness ratio spot-photosphere of various authors leads to the result, that the limb-darkening of the umbra is considerably less than that of the photosphere. The small value of the center-to-limb variation implies a very small temperature grad
Observations of the center-to-limb variation of the solar brightness in the far infrared (10 to 25 microns)
✍ Scribed by Pierre J. Léna
- Publisher
- Springer
- Year
- 1968
- Tongue
- English
- Weight
- 405 KB
- Volume
- 3
- Category
- Article
- ISSN
- 0038-0938
No coin nor oath required. For personal study only.
✦ Synopsis
Existing models of the solar atmosphere predict a limb brightening in the far infrared wavelengths. At shorter wavelengths this effect is confined to the extreme limb but at 25 a it extends inward from the limb to cos 0 = 0.3. Observations of I(a)/I(1.0) were made with the McMath Solar Telescope through atmospheric windows at 10.4, 17.9, 20.4, and 24.2 microns, respectively. The measurements, after having been smoothed, are compared with the theoretical predictions taking into account the diffraction pattern of the telescope. The expected brightening does not appear.
📜 SIMILAR VOLUMES
Brightness fluctuations at 1.65/x have been recorded by means of a 64-element array. Infrared photographs clearly show sunspots and granulation with a resolution better than 1". Quantitative analysis of the digitized data is used to compute autocorrelation and power spectrum. Half-width of autocorre
The center-to-limb variation (CLV) of several infrared carbon lines and the infrared continuum intensity around 1.75/zm were measured. The results were compared with theoretical predictions using four different photospheric models. It was found that the model by Holweger and Mi.iller (1974) describe
The model is that of . This model is in MHSE and includes tension forces. Results are presented in the form of contour maps, cross-sections of the contrast on axis, and integrated contrast as a function of viewing angle. Results are generally consistent with those of , but not with observations of .
We study the center-limb (CL) variation of the average profiles of four Cal lines near 26500 and compare these observations with synthetic data obtained from several line formation models having different thermal structures, line parameters, LTE and non-LTE conditions, and micro and macroturbulence