Issue 
A&A
Volume 617, September 2018



Article Number  L6  
Number of page(s)  5  
Section  Letters to the Editor  
DOI  https://doi.org/10.1051/00046361/201833848  
Published online  25 September 2018 
Letter to the Editor
Spectral gradient of the thermal millimetre continuum as a diagnostic for optical thickness in the solar atmosphere
SUPA School of Physics and Astronomy, University of Glasgow, Glasgow, G12 8QQ UK
email: a.rodger.1@research.gla.ac.uk
Received:
13
July
2018
Accepted:
21
August
2018
Aims. In this Letter we aim to show how the gradient of the thermal millimetre continuum spectrum, as emitted from the quiet solar atmosphere, may be used as a diagnostic for the optical thickness regime at the centre of the observing frequency band.
Methods. We show the theoretical derivation of the gradient of the millimetre continuum for both logarithmic and linearscale spectra. We compare this expression with the empirical relationship between the slope of the millimetre continuum spectrum and the plasma optical thickness computed from both isothermal and multithermal twodimensional cylindrical radiative transfer models.
Results. It is found that the logarithmicscale spectral gradient provides a clear diagnostic for the optical thickness regime for both isothermal and multithermal plasmas, provided that a suitable correction is made for a nonconstant gaunt factor over the frequency band. For the use of observers we present values for this correction at all ALMA bands and at a wide range of electron temperatures.
Conclusions. We find that the spectral gradient can be used to find (a) whether the source is fully optically thin, (b) the optical thickness of the source if it lies within the transitional regime between optically thin and thick plasma (τ ≈ 10^{−1}−10^{1}), or (c) whether the source is fully optically thick for an isothermal plasma. A multithermal plasma will act the same as an isothermal plasma for case (a), however, the transitional regime will only extend from τ ≈ 10^{−1} to τ ≈ 10^{0}. Above τ = 1 the slope of the continuum will depend increasingly on the temperature gradient, as well as the optical thickness, reducing the reliability of the diagnostic.
Key words: radiation mechanisms: thermal / Sun: atmosphere / Sun: filaments, prominences
© ESO 2018
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
1. Introduction
Millimetre continuum emission has frequently been presented as a powerful, direct temperature diagnostic for the plasma of the quiet solar atmosphere. Within the Rayleigh–Jeans limit, a predominantly collisional emission mechanism results in a direct relationship between plasma electron temperature and millimetrewavelength brightness temperature for a particular formation region within a lineofsight (LOS) through an optically thick medium. Observations using the millimetre regime have long been hampered by low resolutions. However, with the advent of the Atacama Large Millimeter/submillimeter Array (ALMA) solar physicists have the ability to observe the solar atmosphere in the millimetre regime at unprecedented spatial resolutions. Solar science with ALMA has been discussed in several articles, for example, Heinzel et al. (2015), Wedemeyer et al. (2016), White et al. (2017), Shimojo et al. (2017), and Rodger & Labrosse (2017).
The limitations of the millimetre brightness temperature as a plasma diagnostic occur when the optical thickness of the source in consideration is unknown. In this Letter we aim to show how the gradient or slope of the millimetre continuum spectrum, across the observing band, may be used to estimate the optical thickness regime at the band centre. With knowledge of the optical thickness regime at the band centre it becomes possible to judge which plasma diagnostic is available from the brightness temperature: if it is clear that the plasma is optically thick, the brightness temperature may be used as the direct diagnostic for the local electron temperature of the forming region.
We show the derivation of the relationship between the gradient of the spectrum and the optical thickness of the emitting material for both a linear and a logarithmicscale spectrum discussing the merits of both as plasma diagnostics. The relationship between the gradient and optical thickness is tested using results from the twodimensional (2D), cylindrical crosssection, nonlocal thermodynamic equilibrium numerical radiative transfer models of Gouttebroze & Labrosse (2009).
In Sect. 2 we present the theoretical derivation of the spectral gradient expressions used in this Letter. Section 3 compares the results from both isothermal and multithermal numerical models to the derived expressions. The conclusions from this study are presented in Sect. 4.
2. Theory
The millimetre spectrum in the quiet solar atmosphere is dominated by freefree collisional processes. The dominant emission mechanism across the millimetre regime is thermal bremsstrahlung, and therefore we assume a purely thermal bremsstrahlung emission mechanism for the optical thickness diagnostic discussed in this Letter. The statement that thermal bremsstrahlung is dominant, however, becomes untrue at low temperatures below 5000 K, and at high densities where neutral hydrogen absorption becomes significant (Rutten 2017), and therefore due care should still be taken when using these diagnostics. The frequencydependent absorption coefficient, κ _{ ν }, for thermal bremsstrahlung is described by (Dulk 1985; Wedemeyer et al. 2016):(1)
in cgs units, where n_{e} is the electron density, T is the electron temperature, g_{ff} is the thermal gaunt factor, and Z_{i} and n_{i} are the charge and density for the ion species i. The optical thickness of an homogeneous LOS of length L can be approximated as τ_{ν} = κ_{ν}L, such that the optical thickness, when assuming purely thermal bremsstrahlung absorption, will vary with frequency as τ_{ν} ∝ g_{ff}ν^{−2}, where g_{ff} is slowly varying with frequency and temperature.
The advantage of observing the solar atmosphere in the millimetre regime is the strong potential for temperature diagnostics. This statement arises from the emission mechanism being dominated by thermal mechanisms such that the source function of the emission can be described by the Planck function, whilst the millimetre regime also lies within the Rayleigh–Jeans limit. Combining these two aspects of solar millimetre emission, the brightness temperature can be described as:(2)
where the integration is performed over a LOS of length s with a path element of ds. For a sufficiently optically thick source the brightness temperature will tend towards saturation at the electron temperature of the plasma. For this diagnostic to be used successfully, however, knowledge of the source’s optical thickness at the observing wavelength is required, as optically thin or notsufficiently optically thick material will provide brightness temperatures nonrepresentative of the electron temperature.
In this section we discuss how the gradient of the logarithmic brightness temperature spectrum may be used as a diagnostic for the optical thickness at the centre of the observing band. By differentiating the logarithm of Eq. (2) with respect to the logarithm of the frequency, the gradient of the logarithmic spectrum is found to be:(3)
where is the rate of change of the thermal gaunt factor with frequency.
If it can be assumed that the LOS is isothermal and Eq. (3) can be simplified to:(4)
such that the gradient of the logarithmic spectrum is solely dependent on the optical thickness of the source material. In the highopticalthickness limit, τ_{ν} ≫ 1, Eq. (4) reduces to 0, whilst in the lowopticalthickness limit, τ_{ν} ≪ 1 it reduces to −2. Therefore, by measuring the gradient of a smallenough frequency band the optical thickness regime at the band centre may be estimated.
In the earlier part of this section we described how the gradient of the logarithmic brightness temperature spectrum may be used as a diagnostic for the optical thickness at the centre of the observing band. For completeness, here we shall discuss the gradient of the linear expression for T_{B}(ν). Similar to Eq. (3) the general form for the brightness temperature spectral gradient is given by:(5)
For an isothermal LOS and a thermal gaunt factor approximately constant with frequency, Eq. (5) simplifies to:(6)
In the extreme optical thickness limits Eq. (6) reduces to 0 for τ_{ν} ≫ 1 and to for τ_{ν} ≪ 1. Hence for an optically thin source the linearscale spectral gradient will vary with both frequency and temperature as well as optical thickness, such that the value of the gradient is nonunique for a given optical thickness. Due to the relative simplicity of the two diagnostics we conclude that the gradient of the logarithmic brightness temperature spectrum is a stronger optical thickness diagnostic than the gradient of the linearscale brightness temperature spectrum.
3. Modelling
To test the theory presented in Sect. 2 we use a set of numerical radiative transfer models. The models we use are the twodimensional, cylindrical crosssection, nonlocal thermodynamic equilibrium (nonLTE) radiative transfer prominence models of Gouttebroze & Labrosse (2009). Each cylinder crosssection considers a mixture of hydrogen and helium at a range of isobaric pressures with either isothermal or multithermal radial temperature distributions. The code considers a 34level He atom, which includes 4 levels for He II and 1 level for He III, as well as a 5levelplus continuum H atom. By calculating the full nonLTE radiative transfer for each model we find the energy level populations and thus ionization densities for both atomic species. The cylinder is orientated such that its axis is parallel to the solar surface. We then calculate the brightness temperature for a set of horizontal linesofsight through the prominence cylinder. We follow the same methods for brightness temperature calculation as outlined in Rodger & Labrosse (2017) with one notable change in the calculation of the thermal gaunt factor. In this study we no longer estimate the thermal gaunt factor through the assumption given in Dulk (1985) for plasma of temperature < 2 × 10^{5} K, but instead take our values by interpolating the table of calculated thermal gaunt factors of van Hoof et al. (2014), as described in Gayet (1970) and Simões et al. (2017). Whilst the optical thickness diagnostic discussed in this study assumes purely thermal bremsstrahlung absorption, the results from these numerical models are calculated using both thermal bremsstrahlung and neutral hydrogen absorption. For this analysis we first consider a set of isothermal prominence models to see how well they agree with Eq. (4) and see how this changes when considering a multithermal plasma instead.
Whilst nominally the models used here describe solar prominences, the results are applicable to any offlimb solar atmospheric structure. For ondisc structures, the spectral gradient will follow a similar relation to Eq. (4) with an additional term corresponding to the contribution of the background solar continuum spectrum. Ondisc structures would therefore require knowledge of the brightness temperature of the structure and the background emission illuminating it from the solar disc. This will likely be problematic unless the structure in observation is formed above the chromosphere, the forming region for most millimetre radiation, or where the structure is transient in nature such that measurements of both the background and enhanced brightness temperature phases are obtainable.
3.1. Isothermal models
The set of isothermal models we use here are the same as the “t” models as described in Gouttebroze & Labrosse (2009). They each consider a prominence cylindrical crosssection of radius 0.5 Mm at an altitude of 10 Mm. The isobaric pressure is 0.1 dyn cm^{−2}, the helium abundance is 0.1 and the microturbulent velocity is 5 km s^{−1} in all models. The set of temperatures considered is {6000, 8000, 10 000, 15 000, 20 000, 30 000, 40 000, 50 000, 65 000, 80 000, 100 000} K.
From Fig. 1 it can be seen that whilst the relationship between the modelled spectral gradient and the optical thickness follows a similar trend to that expected by Eq. (4) the values are slightly lower. This discrepancy is caused by the assumption that the gaunt factor is approximately constant over the frequency band. In fact, recomputing the brightness temperatures with a constant gaunt factor removed this discrepancy entirely.
Fig. 1.
Relationship between optical thickness and logarithmic spectral gradient for a set of isothermal prominence models. The solid red line shows the simple relationship as defined by Eq. (4). The dashedblue line shows τ = 1. 

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If the thermal gaunt factor variation across the observing band is to be significant enough to affect this relationship, a method to account for it must be found. From Eq. (3) it can be found for an isothermal plasma that(7)
where α is the offset factor described by(8)
We evaluated α at the known isothermal temperatures of each prominence model and at the frequency of ALMA Band 3 centre (100 GHz). By dividing the modelled spectral gradient versus optical thickness relationship by this correcting factor we find results as shown in Fig. 2. It can be seen that as long as the nonzero rate of change of thermal gaunt factor with frequency is corrected for, isothermal models provide the expected relationship between optical thickness and logarithmic spectral gradient as described in Eq. (4).
Fig. 2.
As in Fig. 1, except that the spectral gradient has been corrected using the known temperature of the isothermal models for the nonzero through Eqs. (7) and (8). 

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3.2. Multithermal models
In this section we replicate the previous tests using multithermal prominence models. The prominence models that we use are the same as the “p” models as described in Gouttebroze & Labrosse (2009). The radius of these models is larger than that of the t models at a value of 1 Mm. The nonisothermal temperature distribution is adhoc and defined by Eq. (1) of Gouttebroze (2006). Each model has a different isobaric pressure from the set of pressures: {0.02, 0.03, 0.05, 0.10, 0.20, 0.30, 0.50} dyn cm^{−2}. The altitude, helium abundance, and microturbulent velocity for all models are the same as described for the isothermal models.
The same process as for the isothermal models was followed whereby the brightness temperature spectrum was calculated and the gradient was found for each of the subband wavelengths of ALMA Band 3. The relationship between logarithmic spectral gradient and optical thickness at the centre of Band 3 for this set of multithermal models can be seen in Fig. 3.
Fig. 3.
As in Fig. 1 but for a set of multithermal isobaric prominence models at various pressures. 

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It can be seen again in Fig. 3 that the relationship found in the simulated data is below the simple relationship in Eq. (4) during the optically thin regime, as expected due to the same issues with nonzero rate of change of gaunt factor with frequency. However, when considering a set of multithermal LOSs, or generally a structure of unknown temperature, it is less simple to correct for α through Eqs. (7) and (8) due to the lack of a single representative temperature value. To attempt to find a solution to this, we have calculated α at all ALMA Bands and at a wide range of temperatures between 10^{3} and 10^{6} K.
Due to the very small magnitude of the rate of change of the gaunt factor with frequency (), the α variation with temperature displayed a jagged, oscillationlike pattern at low temperatures. This numerical artifact was removed by fitting with the function(9)
and calculating α using the fitted values for . The factors a(ν), b(ν), c(ν) and d(ν) are constants dependent on the frequency band. The resulting smoothed variation of α for each ALMA Band with temperature is shown in Fig. 4. The temperature values in Fig. 4 extend below the temperature range (∼5000 K) where this method may be applied, as neutral hydrogen will become a more significant emission mechanism. Applying the maximum and minimum values for α(100 GHz) to Eq. (7) we compare the corrected relationship to the results from the multithermal models. The results from this method are shown in Fig. 5.
Fig. 4.
Smoothed variation of α correction, evaluated at all ALMA bands over a wide range of temperatures. 

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Fig. 5.
Relationship between optical thickness and spectral gradient for all multithermal numerical models is shown in black. The simple, isothermal expression from Eq. (4), without the correction for α factor is shown in red. The orange region shows the corrected relationship from Eq. (7), where α is evaluated for ALMA Band 3 at temperatures between 10^{3} and 10^{6} K. The dashedblue line shows τ = 1. 

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For each isothermal model listed above we calculated the brightness temperature at the four spectral subbands of ALMA Band 3, that is, 93, 95, 105 and 107 GHz (White et al. 2017). From these brightness temperature values we fit a straight line to the logarithmic spectra of the millimetre continuum. The plot showing the optical thickness of the LOS versus the logarithmic spectral gradient for all isothermal models is shown in Fig. 1 alongside the simple derived expression from Eq. (4).
Figure 5 shows that the α(100 GHz) correction can lead to a relatively close agreement to the values found from the multithermal numerical models, although the relationship notably differs at higher optical thickness. This is primarily due to the breakdown in the assumption that the LOS is isothermal as the spectral gradient becomes dependent on the temperature gradient of the LOS in addition to the optical thickness. Using the nonzero corrected logarithmic spectral gradient may, however, be used to discern (a) whether the emission is optically thin, (b) the optical thickness of the material if it is in the range τ ≈ 10^{−1} − 1, or (c) whether it is optically thick and the gradient is defined by the temperature gradient of the plasma.
3.3. Minimum required uncertainty in brightness temperature measurement
Estimating the optical thickness regime using the logarithmic spectral gradient of the millimetre continuum requires suitably precise measurements of the brightness temperature across the ALMA subband. Ideally for the gradient of the logarithmic spectrum to be calculated the uncertainty in the brightness temperature should be significantly less than the brightness temperature difference across the subband spectrum. Higher precision will therefore be necessary when the brightness temperature is very low, or when the spectral gradient tends towards zero for fully optically thick material. In Fig. 6 we show the brightness temperature difference across ALMA Band 3 for both the sets of isothermal and multithermal models used in this study. As may be expected, verylowopticalthickness, and therefore verylowbrightnesstemperature models, require significantly better precision in the brightness temperature measurements than models with higher brightness temperatures.
Fig. 6.
Brightness temperature difference across the ALMA Band 3 subband spectra created by the set of isothermal models (left panel) and multithermal models (right panel). To give an estimate of the spectral gradient the uncertainty of the brightness temperature must be less than the brightness temperature difference across the spectrum. 

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4. Conclusions
In this study we have discussed how the spectral gradient of the millimetre continuum spectrum may be used as a diagnostic of the optical thickness regime at the centre of the observing band when a thermal bremsstrahlung emission mechanism is assumed. We show the derived expressions for both a logarithmic and linearscale spectral gradient, where we find that through the simplicity of the relationship between spectral gradient and the optical thickness that the logarithmic scale provides a better, simpler diagnostic. Through testing the theoretical expression with both isothermal and multithermal numerical prominence simulations we find that the spectral gradient can be used to estimate the optical thickness regime at band centre provided that a suitable correction is made to account for a nonconstant gaunt factor over the frequency band.
The results presented here for prominence models are however more generally applicable to any offlimb solar structure. Enhancement from ondisc structures will follow a similar relationship with the addition of a term dependent on the gradient of the background continuum spectrum. For ondisc structures, the method will therefore require knowledge of both the structure’s brightness temperature spectrum and the background brightness temperature spectrum illuminating it from the solar disc. This may be problematic unless the structure is clearly observed to be above the formation region of the millimetre regime, or where the observed structure is transient in nature.
We find that for an isothermal plasma, if the optical thickness of the emitting material lies within the range τ ≈ 10^{−1} − 10^{1}, our method may be used to estimate the optical thickness of the material, and that this relationship should always hold. However, for a multithermal plasma, the relationship will become less able to estimate directly the optical thickness for τ > 1 as the spectral gradient will become increasingly defined by the temperature distribution of the emitting plasma.
Acknowledgments
AR acknowledges support from a STFC studentship ST/N504075/1. NL acknowledges support from STFC grant ST/P000533/1. The authors would like to acknowledge the members of ISSI team number 374 “Solving the Prominence Paradox” led by NL for helpful discussion around the results and applications presented in this study. The authors would also like to thank the anonymous referee for their constructive questions and feedback.
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All Figures
Fig. 1.
Relationship between optical thickness and logarithmic spectral gradient for a set of isothermal prominence models. The solid red line shows the simple relationship as defined by Eq. (4). The dashedblue line shows τ = 1. 

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In the text 
Fig. 2.
As in Fig. 1, except that the spectral gradient has been corrected using the known temperature of the isothermal models for the nonzero through Eqs. (7) and (8). 

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In the text 
Fig. 3.
As in Fig. 1 but for a set of multithermal isobaric prominence models at various pressures. 

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In the text 
Fig. 4.
Smoothed variation of α correction, evaluated at all ALMA bands over a wide range of temperatures. 

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In the text 
Fig. 5.
Relationship between optical thickness and spectral gradient for all multithermal numerical models is shown in black. The simple, isothermal expression from Eq. (4), without the correction for α factor is shown in red. The orange region shows the corrected relationship from Eq. (7), where α is evaluated for ALMA Band 3 at temperatures between 10^{3} and 10^{6} K. The dashedblue line shows τ = 1. 

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In the text 
Fig. 6.
Brightness temperature difference across the ALMA Band 3 subband spectra created by the set of isothermal models (left panel) and multithermal models (right panel). To give an estimate of the spectral gradient the uncertainty of the brightness temperature must be less than the brightness temperature difference across the spectrum. 

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In the text 
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