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Sorry I still don't think I understand. My book says about Kirchoff's laws,
Emission Lines: "A low density hot gas emits light whose spectrum consists of a series of bright emission lines." Absorption Lines: "A cool thin gas absorbs certain wavelengths from a continuous spectrum, leaving dark absorption lines in their place supermimposed on the continuous spectrum." But why the difference in the photosphere and corona? |
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Think about "hot" and "cool". With respect to what? Photospheric gas, if you saw a box of it glowing by itself, would be a source of emission lines. However, in front of the solar interior, which is much hotter, it gives off many fewer photons in an emission-line wavelength than it absorbs from the background, so the net effect is still an absorption line. Similarly, the very hot component of the interstellar medium that forms O(5+) is occasionally seen as a source of emission lines near 1030 A in the far-UV, but it's much easier to see in absorption when there is a bright background source. (Just to complicate things, "hotter" and "cooler" need not refer to thermodynamic temperature, but more nearly to brightness temperature - the temperature of the blackbody which gives the same surface brightness at the relevant wavelength. Nonthermal processes can work just as well, as in the continuum light of the Crab Nebula). |
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Indeed and Nebula can show strong Emission
http://praxis.pha.jhu.edu/pictures/pneb_spec.gif this site explains things on spectra a little bit http://astrwww.astr.cwru.edu/reference/spectra.html |
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It is merely a question of brightness contrast. If you observe a light source against an even brighter background it will appear relatively darker (i.e. in 'absorption').
So if the continuum background of the lower solar atmosphere is brighter than the emission lines of the upper layers, the latter appear to be in 'absorption'. The continuum of the solar corona is very weak, so the coronal lines appear to be in emission relative to this, but against the bright continuum of the solar disk they would appear in absorption. On the other hand, if you could view the gas that produces the light in the absorption lines against the dark sky instead of the bright continuum of the photosphere, you would see them as emission lines. It also depends on the wavelength region you are considering: the solar Balmer series lines in the visible region for instance appear in absorption, but the Lyman series lines in the ultraviolet appear in emission, not primarily because they are stronger, but because the continuum in the ultraviolet is much weaker. By the way, the expression 'absorption' lines is somewhat misleading: there is actually no light being absorbed in the corresponding gas volumes but it is merely being scattered back into the lower layers. Spectral lines therefore merely tend to block the radiation that is emitted from the lower layers. True absorption would be due to photoionization and this would affect lines and continuum to the same degree and hence not change their relative intensity. |
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A not-too-inaccurate way of thinking of it is that a beam of light has a temperature associated with it (same as the temperature of the body that produced it, assuming that body is big/opaque enough). The longer that beam spends passing through a gas, the closer its temperature becomes to that gas. And, of course, hotter light is brighter. |