Abstract
In order to obtain a better agreement between observed and computed values of the solar intensity, an improved temperature distribution is deduced for the range 0.02 < τ0 < 10. The intensity observations here considered refer to the wavelength region between λ 1980 and λ 129 500, and the center-limb variations generally go down to cosθ = 0.11a1. The improved model, given in Figure 4 and Table II, differs rather little from the Utrecht 1964 model, used here as a reference.
It appears necessary to introduce an empirical correction function to be applied to the continuous absorption coefficient. This function was derived for the spectral region between 2000 and 130000 Å; it is shown in Figure 5.
Furthermore, an extension of the model (1.10−7 < τ0 < 2.10−2) is deduced (see Table III and Figure 8), which reasonably well represents the observations of the ultraviolet solar flux (λλ 900–1700 Å).
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Sauval, A. (1968). The Solar Continuum from 900 to 130000 Å and the Photospheric Temperature Model. In: de Jager, C. (eds) The Structure of the Quiet Photosphere and the Low Chromosphere. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-3470-8_9
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