Issue 
A&A
Volume 551, March 2013



Article Number  A124  
Number of page(s)  11  
Section  Stellar structure and evolution  
DOI  https://doi.org/10.1051/00046361/201220023  
Published online  05 March 2013 
Prompt thermal emission in gammaray bursts
^{1}
UPMCCNRS, UMR 7095, Institut d’Astrophysique de Paris,
75014
Paris,
France
email: hascoetiap.fr; daigneiap.fr; mochko@iap.fr
^{2}
Physics Department and Astronomy Department, Columbia
University, 538 West 120th
Street, New York,
NY
10027,
USA
^{3} Institut Universitaire de France
Received:
16
July
2012
Accepted:
22
January
2013
Context. Gammaray burst (GRB) spectra globally appear nonthermal, but recent observations of a few bursts with Fermi GBM have confirmed previous indications from BATSE of the presence of an underlying thermal component. Photospheric emission is indeed expected when the relativistic outflow emerging from the central engine becomes transparent to its own radiation, with a quasiblackbody spectrum in absence of additional subphotospheric dissipation. However, its intensity strongly depends on the acceleration mechanism – thermal or magnetic – of the flow.
Aims. We aim to compute the thermal and nonthermal emissions (light curves and spectra) produced by an outflow with a variable Lorentz factor, where the power Ė_{iso} injected at the origin is partially thermal (fraction ϵ_{th} ≤ 1) and partially magnetic (fraction 1−ϵ_{th}). The thermal emission is produced at the photosphere, and the nonthermal emission in the optically thin regime. Apart from the value of ϵ_{th}, we want to test how the other model parameters affect the observed ratio of the thermal to nonthermal emission.
Methods. We followed the adiabatic cooling of the flow from the origin to the photosphere and computed the emitted radiation, which is a sum of modified black bodies at different temperatures (as the temperature strongly depends on the Lorentz factor of each shell at transparency). If the nonthermal emission comes from internal shocks, it is obtained from a multishell model where a fraction of the energy dissipated in shell collision is transferred to electrons and radiated via the synchrotron mechanism. If, conversely, the nonthermal emission originates in magnetic reconnection, the lack of any detailed theory for this process forced us to use a very simple parametrisation to estimate the emitted spectrum.
Results. If the nonthermal emission is made by internal shocks, we selfconsistently obtained the light curves and spectra of the thermal and nonthermal components for any distribution of the Lorentz factor in the flow. If the nonthermal emission results from magnetic reconnection we were unable to produce a light curve and could only compare the respective nonthermal and thermal spectra. In the different considered cases, we varied the model parameters to see when the thermal component in the light curve and/or spectrum is likely to show up or, on the contrary, to be hidden. We finally compared our results to the proposed evidence for the presence of a thermal component in GRB spectra. Focussing on GRB 090902B and GRB 10072B, we showed how these observations can be used to constrain the nature and acceleration mechanism of GRB outflows.
Key words: gammaray burst: general / radiation mechanisms: thermal / radiation mechanisms: nonthermal / shock waves / magnetic reconnection
© ESO, 2013
1. Introduction
The first gammaray burst (GRB) spectra were obtained by the gamma and Xray spectrometers on board the IMP6 satellite and the Apollo 16 spacecraft (Cline et al. 1973; Metzger et al. 1974). These early observations were complemented by the large sample of 143 spectra collected by the Konus experiments on the Venera probes from 1978 to 1980 (Mazets et al. 1981). It was shown that these spectra could be fitted by a power law with an exponential cutoff or a broken power law (Cline & Desai 1975), and various physical processes were invoked to explain this shape, such as opticallythin thermal bremsstrahlung (Gilman et al. 1980), Compton scattering of soft photons by nonthermal electrons (Zdziarski & Lamb 1986) or synchrotron emission by thermal or nonthermal electrons (Brainerd & Lamb 1987). Following the launch of the Compton GammaRay Observatory, the Burst and Transient Source Experiment (BATSE) provided the first solid indications that GRBs were located at cosmological distances and confirmed the broken power law shape of the spectra that was represented by the phenomenological Band function (Band et al. 1993). Possible cyclotron or annihilation lines found by previous experiments were not seen by BATSE.
In the context of the cosmological models that were developed hereafter, the spectra were generally interpreted in terms of synchrotron emission from shock accelerated electrons (see e.g. Piran 1999) and therefore believed to be mostly nonthermal. The possibility that a thermal contribution could also be present was, however, considered by Mészáros et al. (2002), and was supported by several observational indications. The first one came from the very hard lowenergy spectral slopes that are found in some BATSE bursts during at least part of the evolution (Preece et al. 1998; Ghirlanda et al. 2003). While the commonly observed value of the lowenergy spectral index is α ~ −1, it reaches 0.5 to 1 in these events, suggesting the presence of a RayleighJeans contribution. Then Ryde (2004, 2005) proposed to fit all GRB spectra in the BATSE range with the combination of a thermal and a power law component. Using a time resolved analysis, he showed that during a pulse the temperature first stays approximately constant before decaying as a power law of temporal index close to −2/3.
In the previous examples the identified thermal component represented a major contribution responsible for the peak of the E^{2}N(E) spectrum. A different result was obtained by Guiriec et al. (2011) who found a subdominant thermal component in the FermiGammaray Burst Monitor (GBM) spectrum of GRB 100724B, accounting for a few percents of the energy released by the burst. The evolution of the temperature was not correlated to the peak energy of the nonthermal component, fitted by a Band function. Similar results have been found in other bright GBM bursts, such as GRB 110721A (Ryde et al. 2012), GRB 081207, and GRB 110920 (McGlynn et al. 2012). This improved characterisation of thermal components in the prompt emission of GRBs is allowed by the larger spectral coverage of GBM (8 keV–40 MeV) compared to BATSE (20 keV–2 MeV), leading to a better quality of the spectral fits.
On the theoretical side, a thermal emission originating from the photosphere is a natural prediction of most models based on the generic fireball scenario (Paczynski 1986; Goodman 1986; Shemi & Piran 1990; Mészáros et al. 1993). Moreover, if the acceleration of the outflow has a thermal origin (as would be the case if it was powered at its basis by neutrinoantineutrino annihilation), this photospheric emission would be very bright, outshining the nonthermal emission produced by internal shocks in the 100 keV–1 MeV spectral range (Daigne & Mochkovitch 2002). One is therefore faced with the following alternative: either most of the emission we observe is indeed this thermal component, but it has been Comptonised to produce a power law tail in the spectrum at high energy (see e.g. Thompson 1994; Rees & Mészáros 2005; Giannios & Spruit 2007; Beloborodov 2010) and complemented at low energy by additional processes (e.g. Pe’er et al. 2006; Vurm et al. 2011), or the acceleration has a magnetic origin (see e.g. Begelman & Li 1994; Daigne & Drenkhahn 2002; Vlahakis & Königl 2003; Komissarov et al. 2009; Tchekhovskoy et al. 2010; Komissarov et al. 2010; Granot et al. 2011) and the fraction ϵ_{th} of thermal energy in the flow is much smaller than unity.
In this work we explore the consequences of this second possibility. We selfconsistently compute the photospheric thermal emission and the nonthermal emission from internal shocks. If the internal dissipation is dominated by magnetic reconnection rather than internal shocks, we get the nonthermal spectrum in a very simple parametrised way. We discuss the conditions for the thermal emission to show up or, on the contrary, to be hidden. The paper is organised as follows: in Sect. 2 we describe the geometry and thermodynamics of the flow and explain our method to compute the photospheric and nonthermal emissions; our results are presented in Sect. 3 and discussed in Sect. 4. Finally, Sect. 5 is the conclusion.
2. Model description
2.1. Geometry and thermodynamics of the flow
We consider a schematic model where the flow that emerges from the central engine is accelerated by the conversion of thermal and/or magnetic energy to kinetic energy. We do not specify the initial geometry of the flow (which can be largely governed by magnetic forces), but we assume that beyond a radius R_{sph} it becomes spherically symmetric within a cone of half opening angle θ. We also define the radius R_{sat}, where the acceleration is essentially complete and suppose that R_{sph} < R_{sat}. The total injected power in the flow is Ė, with a fraction ϵ_{th} in thermal form. The temperature T_{0} at the origin of the flow can then be obtained from (1)where Ė_{iso} and S_{0} = πℓ^{2} are, respectively, the isotropic injected power and the section of the flow at the origin (see Fig. 1). The fraction of solid angle is (we count only one jet to be consistent with the definition of S_{0}) and a is the radiation constant. We finally get (2)with the opening angle, injected power, and radius of the jet in units of 0.1 rad, 10^{53} erg s^{1}, and 10^{7} cm, respectively.
We obtain the flow equations assuming that no dissipation takes place below the photosphere (so that the emerging spectrum at transparency will be thermal only). Mass and entropy conservation then lead to where ρ is the comoving density, S the surface perpendicular to the flow, β = v/c, and Γ = (1 − β^{2})^{−1/2}. From Eqs. (3), (4) we get (5)Using Eq. (5) we can obtain the temperature at any radius R > R_{sph} even if we ignore the details of the geometry from the basis of the flow up to R_{sph}. With S(R) = π θ^{2} R^{2} and assuming that β ~ 1 already close to the origin we have (6)so that, in the observer frame (7)where z is the burst redshift.
Fig. 1 Schematic view of the problem geometry. The flow emerges from the central engine through a “circular opening” of radius ℓ. Beyond a radius R_{sph} it expands radially within a cone of half opening θ. The acceleration is completed at R_{sat}. The photosphere is located at R_{ph} and dissipation of kinetic and/or magnetic energy takes place at R_{diss}. 

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At the photospheric radius R_{ph} (supposed to lie beyond R_{sph}) the thermal luminosity is given by (8)Equations (7) and (8) correspond to the usual scaling of the fireball scenario (Mészáros & Rees 2000; Mészáros et al. 2002; Daigne & Mochkovitch 2002) with, however, a modified normalisation that takes into account both the geometry and the mixed energy content of the outflow. Conversely, including subphotospheric dissipation as in Giannios (2012) would change the scaling.
To estimate the photospheric radius we assume that most of the acceleration is completed at R_{ph}^{1}. This is, for example, the case in the simulations made by Tchekhovskoy et al. (2010), where the Lorentz factor sharply increases beyond the stellar radius, when the flow suddenly becomes unconfined. Then, in a first approximation, the photospheric radius of a given shell writes (e.g. Piran 1999; Mészáros & Rees 2000; Daigne & Mochkovitch 2002) (9)where κ (κ_{0.2} in units of 0.2 cm^{2} g^{1}) is the material opacity and Γ (Γ_{2} in units of 100) the Lorentz factor of the shell. The flow keeps a magnetisation σ at the end of acceleration so that Ė/(1 + σ) is the injected kinetic power Ė_{K}. In the case of a passive magnetic field that is carried by the outflow without contributing to its acceleration (Spruit et al. 2001), the magnetisation σ equals (10)corresponding to a pure and complete thermal acceleration. Efficient magnetic acceleration leads to σ < σ_{passive}, whereas σ > σ_{passive} corresponds to an inefficient magnetic acceleration, for instance with no conversion of magnetic into kinetic energy and some conversion of thermal into magnetic energy.
When the shell reaches the photospheric radius, it releases its thermal energy content while a fraction of the remaining energy (kinetic or magnetic) can be dissipated farther away at a radius R_{diss} by internal shocks for σ ≲ 0.1−1, or reconnection for higher magnetisation, contributing to the nonthermal emission of the burst. It is therefore expected, on theoretical grounds, that thermal and nonthermal components both contribute to the observed emission (Mészáros et al. 2002; Daigne & Mochkovitch 2002). As mentioned in the introduction, this was already supported by BATSE results, with new evidence now coming from Fermi (Guiriec et al. 2011; Zhang et al. 2011). In Sect. 3 we present synthetic bursts showing both contributions. We explain below our method to compute the thermal and nonthermal emission.
2.2. Thermal emission
The thermal emission can be computed from Eqs. (1), (2), (7), (8), and (9), for a given set of central engine parameters ϵ_{th}, σ, ℓ, θ, Ė_{iso}, and a distribution of the Lorentz factor in the flow. Both the thermal luminosity and observed temperature are related to the injected power and temperature at the origin of the flow via the same factor (11)If a constant Ė_{iso} is assumed, the luminosity and temperature directly trace the distribution of the Lorentz factor Γ(s), where the Lagrangian coordinate s is the distance to the front of the flow at the end of the acceleration stage (s/c is the ejection time of the shell). The expanding flow becomes progressively transparent (starting from the front) and the contribution of a shell located at s is approximately received at an observer time t_{obs} = (1 + z)s/c (Daigne & Mochkovitch 2002). However, since the different parts of the flow do not become transparent at the same radius (because R_{ph} ∝ Γ^{3}), additional differences in arrival time of the order of (12)should be included. They are, however, negligible as long as Δt_{obs} < t_{var}, the typical variability time scale of the Lorentz factor.
The value of Δt_{obs} also gives the time scale of the luminosity decline after the last shell of the flow (emitted by the source at a time τ) has reached the transparency radius (highlatitude emission). Unless the Lorentz factor of this shell is small or the burst has a very short duration, the drop in luminosity for t_{obs} > (1 + z)τ is very steep, having initially a temporal decay index (see e.g. Sect. 6 in Beloborodov 2011) (13)This shows that in models where the prompt emission comes from a Comptonised photosphere, the early decay of index α ~ 3−5 observed in Xrays cannot be explained by the high latitude emission and should instead be related to an effective decline of the central engine (Hascoët et al. 2012).
The expected count rate in a given spectral range and the resulting spectrum are obtained from the luminosity and temperature evolution (Eqs. (7) and (8)). However, we do not use a true Planck function for the elementary spectrum corresponding to a given temperature. As discussed in Goodman (1986) and Beloborodov (2010), geometrical effects at the photosphere lead to a lowenergy spectral index close to α = +0.4 instead of α = +1 for a RaleighJeans spectrum (see also Pe’er 2008). We therefore adopt a “modified Planck function” having the modified spectral slope at low energy, an exponential cutoff at high energy, peaking at ≃3.9 × kT as a Planck function in νF_{ν}, and carrying the same total energy.
2.3. Nonthermal emission
We first estimate the nonthermal emission assuming that it comes from internal shocks (Rees & Meszaros 1994). For a given distribution of the Lorentz factor, we obtain light curves and spectra using the simplified model of Daigne & Mochkovitch (1998), where the outflow is represented by a large number of shells that interact by direct collisions only (see also Kobayashi et al. 1997). The elementary spectrum for each collision is a broken power law with the break at the synchrotron energy. The adopted values for the two spectral indices at low and high energy respectively are α = −1 and β = −2.25. The expected value for α in the fast cooling regime should normally be −1.5 (see e.g. Sari et al. 1998; Ghisellini et al. 2000), but detailed radiative models including inverse Compton scattering in KleinNishina regime tend to produce harder α slopes (Derishev et al. 2001; Bošnjak et al. 2009; Nakar et al. 2009; Daigne et al. 2011), close to the typical observed value α ≃ −1 (Preece et al. 2000; Kaneko et al. 2006; Nava et al. 2011; Goldstein et al. 2012). The global efficiency of internal shocks is given by the product (14)where f_{diss} is the efficiency for the dissipation of energy in shocks and ϵ_{e} the fraction of the dissipated energy transferred to electrons and eventually radiated. Typical values of f_{IS} do not exceed a few percents. We used this approach to compute nonthermal light curves and spectra in Sect. 3.1 for the case of a low magnetisation σ ≲ 0.1−1.
The presence of magnetic fields reduces shock efficiency and may even prevent shock formation for σ ≳ 1 (Mimica & Aloy 2010; Narayan et al. 2011). Then for σ ≳ 1, the magnetic field cannot be ignored, and energy must be extracted by magnetic reconnection (e.g. Thompson 1994; Spruit et al. 2001), possibly triggered by internal shocks (Zhang & Yan 2011). Our limited understanding of the relevant processes does not allow a reliable description of the resulting emission. Considering these difficulties, we have adopted in Sect. 3.2 a very basic and simple point of view. We do not try to predict the burst profile and obtain the spectrum in the following way: we suppose that a fraction f_{ Nth} of the total injected energy eventually goes into nonthermal emission with a spectrum represented by a Band function with low and highenergy spectral indices α = −1 and β = −2.25, and a peak energy obtained from the Amati relation (Amati et al. 2002) (15)where the exponent and normalisation values are taken from Nava et al. (2012). The validity of the Amati relation is strongly debated (see e.g. Nakar & Piran 2005; Band & Preece 2005; Kocevski 2012; Collazzi et al. 2012; Ghirlanda et al. 2012). It is not clear if it corresponds to an intrinsic property of GRBs or if the relation results from a complex chain of selection effects (threshold for burst detection, and various conditions for the measure of the redshift and peak energy). For the purpose of the present study we do not address this issue and use Eq. (15) simply because it is approximately satisfied by the sample of long bursts for which the peak energy and isotropic radiated energy have been measured.
Fig. 2 Thermal and nonthermal emission from a variable outflow – internal shock framework. Top left: initial distribution of the Lorentz factor in the flow. Top right: thermal (red), nonthermal (blue), and total (black) photon flux in the 8 keV–40 MeV spectral range. Bottom left: thermal (red), nonthermal (blue), and total (black) timeintegrated spectra. Bottom right: instant temperature (red) of the photospheric emission and instant peak energy (blue) of the internal shock emission. The dotted and dashed lines correspond to the temperature and peak energy averaged over time intervals of 2 and 4 s, respectively. The adopted flow parameters are Ė_{iso} = 10^{53} erg s^{1}, ϵ_{th} = 0.03, σ = 0.1, ℓ = 3 × 10^{6} cm, and θ = 0.1 rad; a redshift z = 1 is assumed. 

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Fig. 3 Thermal and nonthermal emission from a variable outflow – internal shock framework: impact of the outflow parameters. Starting from the reference case shown in Fig. 2 (with a redshift z = 1) we first change the thermal fraction ϵ_{th} to 0.3 (top left panel) and 0.003 (bottom left); then the isotropic power Ė_{iso} to 10^{54} erg s^{1} (top middle) and 10^{52} erg s^{1} (bottom middle); and finally the Lorentz factor is multiplied (top right) and divided (bottom right) by a factor of 2. Each time we vary a parameter, all the others keep the value corresponding to the reference case. 

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3. Results
3.1. Nonthermal emission from internal shocks
To study the relative intensities of the thermal and nonthermal emission components we have considered as an example a flow ejected by a central source active for a duration s_{tot}/c = 10 s, where the Lorentz factor takes the form (16)This distribution is arbitrary (see other possible examples in Daigne & Mochkovitch 1998) and was adopted simply to produce a burst made of three pulses, i.e. not too simple and not too complex. It is is shown in Fig. 2 (top left panel) together with the nonthermal light curve (between 8 keV and 40 MeV; top right panel) resulting from internal shocks. The related photospheric emission is shown in the same energy range for ϵ_{th} = 0.03. We adopt a constant Ė_{iso} = 10^{53} erg s^{1}, σ = 0.1, ℓ = 3 × 10^{6} cm and θ = 0.1 rad (i.e. l/θ = 300 km). We also represent in the bottom left and bottom right panels the spectrum (thermal, nonthermal, and global) and the temporal evolution of the instantaneous peak energy and temperature of the nonthermal and thermal emissions. As the thermal spectrum is a superposition of elementary modified Planck functions at different temperatures, its average spectral slope α (with N(E) ∝ E^{α}) below the peak is close to −1. The asymptotic value α = +0.4 is recovered only below a few keV, which corresponds to the photospheric contribution with the lowest temperature.
It can be seen in Fig. 2 (top right panel) that the emission is initially only thermal as it takes a time (17)for the first signal from internal shocks to arrive at the observer. In Eq. (17) the subscript “0” refers to the radius and Lorentz factor of the first shocked shell that contributes to the nonthermal emission. At late times the situation is just the opposite: the photospheric emission abruptly stops at t_{obs} = 20 s, while the emission from late internal shocks (both on and offaxis) still contribute for about 10 s (observer frame). The spectrum (Fig. 2, bottom left) is the sum of the thermal and nonthermal contributions. They peak at 200/(1 + z) and 1000/(1 + z) keV, respectively. Finally the plot of the temperature and of the peak energy of the nonthermal spectrum as a function of observer time shows (Fig. 2, bottom right panel) that the former is more sensitive than the latter to the fluctuations of the Lorentz factor (since T_{obs} ∝ Γ^{8/3}).
We now check how these results change when we vary the model parameters. We divide these parameters into three groups describing respectively the geometry (θ, l); the energetics and flowacceleration mechanism (Ė_{iso}ϵ_{th}, σ); and the ejecta structure (s_{tot}, , ), where and are the contrast () and average of the Lorentz factor distribution.
The geometry only affects the thermal emission (for a fixed Ė_{iso}). The dependence of T_{obs} and L_{th, iso} on θ and ℓ is weak. From Eqs. (2), (7), and (8) we get T_{obs} ∝ θ^{−1/6}ℓ^{1/6} and L_{th, iso} ∝ θ^{−2/3}ℓ^{2/3}. Similarly, changing the magnetisation has a moderate effect on the previous results, as long as σ < 1. As explained above, for σ ≳ 1 the whole theoretical framework adopted to compute the nonthermal emission probably becomes invalid.
The consequence of increasing or decreasing the thermal fraction ϵ_{th} is illustrated in Fig. 3 (left panels). With ϵ_{th} = 0.3 the thermal spectrum overtakes the nonthermal spectrum between 20/(1 + z) and 500/(1 + z) keV, and the thermal component represents about one third of the total in the light curve. Conversely, with ϵ_{th} = 0.003 the contribution of the thermal component to the global spectrum and the light curve is barely visible.
The dependence of the temperature and thermal luminosity on the injected isotropic power Ė_{iso} and average Lorentz factor can be also obtained from Eqs. (2), (7), and (8) yielding For the nonthermal component, the relation of the peak energy and luminosity to the model parameters can be found using the simplest possible description of internal shocks that only considers the interaction of two shells of equal mass (Barraud et al. 2005). One gets where t_{var} is of the order of one pulse duration, depends on only, and f_{IS}, defined by Eq. (14), is given by (22)It can be seen that the thermal and nonthermal components behave quite differently when the injected power and average Lorentz factor are changed. This is illustrated in Fig. 3 where we increase or decrease Ė_{iso} and by respective factors of 10 and 2, compared to the reference case shown in Fig. 2.
It appears that for a given value of ϵ_{th} (ϵ_{th} = 0.03 in Fig. 3, middle and right panels) the thermal component becomes more visible when Ė_{iso} is decreased and increased. This is a direct consequence of Eqs. (18) and (19) above, which can be made even more explicit by defining the global thermal efficiency (assuming κ = 0.2 cm^{2} g^{1}) (23)to be compared to the nonthermal efficiency f_{Nth} = f_{IS} approximated by Eq. (22). While changing Ė_{iso} and affects only the thermal efficiency, the opposite is true for the contrast in Lorentz factor . Reducing makes internal shocks much less efficient and considerably softens the emitted nonthermal spectrum. In the limit where (and moreover if the Lorentz factor is increasing outwards in the ejecta) there will be no internal shocks and the emission will only be thermal in the absence of an alternative dissipation process.
3.2. Nonthermal emission from magnetic dissipation
If the nonthermal emission is produced by reconnection in a magnetised outflow, the problem becomes very difficult, with no simple way to accurately follow the process in time and compute a light curve (see e.g. Spruit et al. 2001; Lyutikov & Blandford 2003; Giannios 2008; Zhang & Yan 2011; McKinney & Uzdensky 2012). As explained in Sect. 2.3 above, we adopted a very simple assumption to obtain the nonthermal spectrum: a Band function carrying a fraction f_{Nth} of the injected energy with the peak of E^{2}N(E) obtained from the Amati relation. Several examples of the thermal and nonthermal spectra are represented in the left panel of Fig. 4, with the thermal component still being computed with the distribution of Lorentz factor given by Eq. (16). The results are shown for several values of ϵ_{th} and σ, and a fixed value of the isotropic magnetic power at the photosphere σĖ/(1 + σ) = 10^{53} erg s^{1}. As expected, the detection of the photospheric component in the spectrum is favored by a high ϵ_{th}, a low f_{Nth}, and a high Γ. The specific dependency on the magnetisation is discussed in the next section.
Fig. 4 Thermal and nonthermal emission from a variable outflow – magnetic reconnection framework. In each panel we show a sequence of thermal (red) and nonthermal (blue), spectra (the source redshift is z = 1). The Lorentz factor distribution adopted for the calculation of the thermal emission is the same as in Fig. 2 (left panel) or the same but with Γ divided by 2 (right panel). The thermal emission is computed using the formalism developed in Sect. 2.2, using five values of ϵ_{th}: 0.01, 0.03, 0.10, 0.30, and 0.5. The nonthermal spectrum is simply parametrised by a Band function, with the peak energy being given by the Amati relation (see text) and using five values of the efficiency of the magnetic reconnection, f_{rec} = f_{Nth}(1 + σ)/σ: 0.01, 0.03, 0.10, 0.30, and 0.5. In all cases, the isotropic magnetic power at the photosphere is fixed to σĖ_{iso}/(1 + σ) = 10^{53} erg s^{1}. Finally, the magnetisation σ at large distance is either σ = 1 (solid lines) or 10 (dashed lines). 

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4. Discussion
4.1. Relative intensity of the thermal component in GRBs
Depending on the mechanism responsible for the acceleration of the outflow in GRBs, the consequences regarding the photospheric emission are very different. In a pure fireball (ϵ_{th} = 1) powered by neutrinoantineutrino annihilation (see e.g. Popham et al. 1999; Zalamea & Beloborodov 2011), the predicted thermal emission is very bright (Daigne & Mochkovitch 2002). To agree with the current data, the spectrum should then be Comptonised at high energy (as a result of some dissipative process below the photosphere, e.g. Rees & Mészáros 2005; Pe’er et al. 2006; Giannios 2008; Beloborodov 2010; Lazzati & Begelman 2010) to produce a power law tail and softened at low energy to decrease the spectral index α from a positive value to a negative one (possibly by the presence of an additional nonthermal component, e.g. Pe’er et al. 2006; Vurm et al. 2011). An alternative is to suppose that the flow is initially magnetically dominated (ϵ_{th} ≲ 0.1). A thermal component is still expected to be released at the photosphere, but it will now be subdominant compared to nonthermal processes such as internal shocks or magnetic reconnection.
We have explored this second possibility in the present paper, making the following assumptions: (i) we supposed that the flow evolves adiabatically from the origin to the photosphere, i.e. we did not include possible sources of heating below R_{ph}; (ii) if the remaining magnetisation σ at the end of acceleration is weak and does not prevent the formation of internal shocks, we computed their contribution to the emitted radiation as if σ = 0; (iii) when σ > 1 we limited ourselves to a very simple parametrised study where we assumed that a fraction f_{Nth} of the injected power goes into the nonthermal component.
Regarding the light curve and spectrum of the thermal emission we obtained the following results:

Both the photosphere luminosity and temperature depend on thesame factor Φ given by Eq. (11), which directly traces the evolution of the Lorentz factor if the injected power stays constant.

The duration of the photospheric emission corresponds to the duration τ of production of the relativistic wind. For t > τ the luminosity drops rapidly on a time scale a few ms for typical values of the burst parameters.

The global spectrum of the thermal emission is a composite of many elementary contributions at different temperatures. Before asymptotically reaching a slope α = +0.4 at low energy it can be much softer below the peak as shown in Fig. 2. A time resolved spectrum will resemble more closely the “modified Planck function” adopted for each elementary collision.
If the nonthermal emission comes from internal shocks, its light curve and spectrum have been computed using the simplified approach described in Sect. 2.3. We have varied several of the model parameters: fraction ϵ_{th} of thermal energy at the origin of the flow, isotropic injected power Ė_{iso}, and average to see under which conditions the thermal component would appear in the observed spectrum, in the internal shock scenario for σ ≲ 0.1−1 (Fig. 3) or in the magnetic reconnection scenario for σ ≳ 1 (Fig. 4). In the internal shock framework, assuming κ = 0.2 cm^{2} g^{1}, the ratio Q of the thermal to nonthermal efficiency is given by (24)As illustrated by this formula and in Fig. 3, increasing ϵ_{th}, but also increasing or reducing Ė_{iso} or will make the thermal component more visible. The magnetisation σ has a low impact as 1 + σ ≃ 1 in this scenario. In the examples shown in Fig. 3, the model parameters are taken from the reference case used in Fig. 2 and equal l_{7} = 0.3, θ_{1} = 1, ϵ_{e} = 1/3, and σ = 0.1. The effective constrast corresponding to the initial distribution of the Lorentz factor plotted in the upper left panel of Fig. 2 is . Then Eq. (24) leads to , in reasonable agreement with Fig. 3: for instance, the upper left panel corresponds to ϵ_{th} = 0.3, Ė_{iso,53} = 1, , and Q ≃ 0.4, and the bottom right panel corresponds to ϵ_{th} = 0.03, Ė_{iso,53} = 1, , and Q ≃ 0.006. Note that in the E^{2}N(E) spectrum, the ratio of the maxima of the two components is expected to be slightly higher than Q because the photospheric component has a narrower spectrum than the nonthermal one.
In the case of magnetic reconnection, the nonthermal emission is simply parametrised by its global efficiency f_{Nth}, and we have (25)in good agreement with Fig. 4 (f_{Nth, −2} being the nonthermal efficiency in %). Especially, Eq. (25) shows that the ratio Q increases with the magnetisation σ, which seems counterintuitive. For a fixed value of Ė, increasing σ reduces Ė_{K}, and therefore decreases the photospheric radius R_{ph} (see Eq. (9)). Therefore, for a given value of ϵ_{th}, the luminosity and temperature of the photosphere increase. However, for a given acceleration mechanism, one would expect an increase of σ to be associated with a decrease of ϵ_{th}, which may affect the dependency of the ratio Q on the magnetisation σ. For instance, in the case of a passive magnetic field, including σ = σ_{passive} in Eq. (25) leads to , i.e. a decreasing ratio for an increasing magnetisation. Since increasing the final magnetisation σ tends to decrease the photospheric radius, it should also be noted that the acceleration of the flow may well be incomplete at the photosphere in high σ scenarios. As discussed in Appendix A, this will also reduce the photospheric emission.
4.2. Comparison to observations
We now check how these results compare to the various observational indications of the presence of a thermal component in GRB spectra.
One first indirect indication comes from the very hard spectral slopes α > 0 that are sometimes observed during burst evolution (e.g. Ghirlanda et al. 2003; Bosnjak et al. 2006; Abdo et al. 2009). Indeed, our results allow the thermal over nonthermal ratio (Eq. (24)) to vary with time. A locally large will boost the thermal component while a low contrast will reduce the nonthermal component (under the condition that the nonthermal emission comes from internal shocks). This can explain an erratic behaviour of the α slope, but observations often show a regular shift of α from positive to negative values during a single pulse. As explained in Sect. 3.1 a thermal start and a nonthermal ending are predicted by our models, but the fraction of time during which the emission is thermal is generally smaller than observed in the few bursts where the measured α slope is positive. It remains possible to adopt a distribution of the Lorentz factor that would extend the duration of the thermal emission but smoothly connecting the thermal and nonthermal components may not be easy.
Fig. 5 Constraints on the thermal and nonthermal emission in GRB 090902B and GRB 100724B. Top: for a given thermal fraction ϵ_{th} = 10^{2}, 10^{1.5}, 10^{1}, 10^{0.5}, and 1, the radius R_{0} = ℓ/θ at the base of the flow is plotted as a function of the nonthermal efficiency f_{Nth}. The corresponding thermal efficiency f_{th} is also shown (top xaxis). Bottom: for a given magnetisation σ = 10^{1}, 10^{0.5}, 1, 10^{0.5}, 10^{1}, 10^{1.5}, and 10^{2} at the end of acceleration phase, the Lorentz factor of the flow is plotted as a function of f_{Nth} (the unmagnetised case σ = 0 cannot be distinguished from the case σ = 0.1). Sets of parameters representative of the different classes of scenarios discussed in the paper are indicated: F (ϵ_{th} = 1, σ = 0) (standard fireball), M,is_{1} (log ϵ_{th} = −0.5, σ = 0,) and M,is_{2} (log ϵ_{th} = −1.5, σ = 0) (efficient magnetic acceleration: magnetisation is low above the photosphere and the dominant nonthermal mechanism is internal shocks), M,rec_{1} (log ϵ_{th} = −0.5, σ = 10), and M,rec_{2} (log ϵ_{th} = −1.5, σ = 10) (magnetised flow at large distance, the dominant nonthermal mechanism is magnetic reconnection). The initial radius is fixed to R_{0} = 300 km, a typical value for long GRBs. The observational data (thermal flux, temperature, ratio of the thermal over the total flux) used for the calculation (see text) are taken from Abdo et al. (2009); Pe’er et al. (2012) for GRB 090902B (left column), and from Guiriec et al. (2011) for GRB 100724B (right column). 

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A second indication comes from the recent detection of possible thermal components in a few Fermi GRBs. GRB 090902B is a very peculiar case of a burst showing a spectrum best fitted by a Band function with a hard lowenergy photon index, or a multicolour black body, together with an additional subdominant power law (Abdo et al. 2009; Ryde et al. 2010). A first possibility is to interpret this burst as photospheric emission with additional dissipative processes affecting the spectrum by Comptonisation and possibly other nonthermal processes. Conversely, using the formalism presented here, we can also derive constraints on the burst parameters for alternative scenarios where the Band component is interpreted as the thermal emission produced at the photosphere without subphotospheric dissipation, and the power law as nonthermal emission produced above the photosphere in the optically thin regime. From the analysis made by Abdo et al. (2009) and Pe’er et al. (2012), the implied thermal luminosity and temperature are large, L_{th} ≃ 4.6 × 10^{53} erg s^{1} and T_{obs} ≃ 168 keV. The thermal luminosity represents 53% of the total luminosity. Then, for a given ϵ_{th}, σ, and f_{Nth}, one can deduce from Eqs. (7)–(9) the isotropic power Ė_{iso}, the size R_{0} = ℓ/θ of the region at the base of the outflow (see Fig. 5, topleft panel), and the Lorentz factor Γ (see Fig. 5, bottomleft panel). This is a similar approach to the one proposed by Pe’er et al. (2007), but within the more general framework defined in this paper, which allows us to consider several scenarios for the acceleration of the outflow. As GRB 090902B is very bright, this leads to huge values of Ė_{iso}, the minimum being obtained for ϵ_{th} ≃ 1, which would make GRB 090902B a peculiar burst associated to a situation close to a pure fireball. For instance, for ϵ_{th} = 1, l_{7} = 0.3, θ_{1} = 1 (i.e. R_{0} = 300 km), and σ ≪ 1 we get an isotropic power Ė_{iso} ~ 2.6 × 10^{54} erg s^{1} and a Lorentz factor Γ ~ 1160. The efficiency of the photospheric emission in this case is f_{th} ≃ 0.18 and the efficiency of the nonthermal emission above the photosphere is f_{Nth} ≃ 0.16, marginally compatible with internal shocks. This case is labelled as F in Fig. 5 (left column) and is in good agreement with the analysis made by Pe’er et al. (2012).
As most GRBs do not show such a bright thermal component, they usually require much lower values of ϵ_{th}, as illustrated below with GRB 100724B. Then, it is worth studying the possibility to model GRB 090902B with ϵ_{th} < 1, which would correspond to an initially magnetised outflow. Reducing ϵ_{th} in this burst has several consequences. As illustrated in Fig. 5 (left column), it implies a general decrease of the efficiency, except if the initial size R_{0} = ℓ/θ is very large (R_{0} ≫ 3000 km), which is not expected for most models of the central engine of long GRBs, because of their short timescale (~1–10 ms) variability. For instance, for ϵ_{th} = 10^{0.5} (case labelled as M,is_{1}, where we keep R_{0} = 300 km and σ ≪ 1), the thermal and nonthermal efficiencies are reduced to f_{th} = 0.06 and f_{Nth} = 0.05, leading to an isotropic equivalent power Ė_{iso} = 9.4 × 10^{54} erg s^{1}. It also leads to an increase of the Lorentz factor, which was already quite high for the pure fireball scenario (see Fig. 5, bottomleft panel). Therefore, ϵ_{th} ≃ 0.3−0.5 seems a reasonable lower limit for GRB 090902B. Note that a decrease of ϵ_{th} compared to the standard fireball leads in this case to a reduced nonthermal efficiency f_{th} in good agreement with the expected value for internal shocks. For higher values of ϵ_{th}, magnetic reconnection, which is supposed to have a higher efficiency, is a better candidate, as illustrated in Fig. 5 (left column). In addition, for a fixed value of ϵ_{th}, increasing the magnetisation σ at the end of acceleration always reduces the constraint on the Lorentz factor (bottom left panel). A more detailed modelling of GRB 090902B would be necessary to distinguish between these different possibilities.
Conversely, the results of Guiriec et al. (2011) indicating the presence of a subdominant thermal component in GRB 100724B, representing about 4% of the total flux, point towards low values of ϵ_{th} and, therefore, a magnetic acceleration. As shown in Fig. 5, it is difficult to interpret GRB 100724B within the standard fireball scenario (thermal acceleration) that would imply either f_{Nth} > 1 or R_{0} < 120 km (and even R_{0} < 40 km if f_{Nth} < 0.5 is required). This is obtained assuming a redshift z = 1, but we checked that our conclusions are unchanged for larger redshifts. Then a low thermal fraction ϵ_{th} ≲ 0.01−0.1 is required in GRB 100724B, whose spectral properties are much more representative of the bulk GRB population than in the unusual case of GRB 090902B. A similar conclusion was obtained by Zhang & Pe’er (2009) in the case of the very energetic burst GRB 080916C where no bright thermal component was detected. Assuming a passive magnetic field below the photosphere, they obtain the constraint σ_{passive} ≳ 15−20, which leads to the more general condition ϵ_{th} ≲ 0.05, from Eq. (10).
If magnetic acceleration is common in GRBs, several scenarios can be discussed. In scenarios where magnetic acceleration is efficient, implying a low magnetisation at large radius and a dominant role of internal shocks, the thermal fraction should not be much larger than a few percents to avoid an unrealistic efficiency f_{Nth}. For instance in the case of GRB 100724B, for z = 1, ϵ_{th} = 10^{1.5}, ℓ_{7} = 0.3, θ_{1} = 1 (i.e. R_{0} = 300 km), and σ ≪ 1 (case labelled as M,is_{2} in Fig. 5 right column), we get a nonthermal efficiency f_{Nth} ≃ 0.06 and a thermal efficiency f_{th} ≃ 2 × 10^{3}. The isotropic kinetic power and the Lorentz factor in this case are Ė_{iso} ≃ 5.6 × 10^{53} erg s^{1} and Γ ≃ 660. Alternative scenarios – where the flow is still magnetised at large radius and magnetic reconnection is the dominant mechanism to produce nonthermal emission – are less constrained, because of the uncertainties in the underlying physics. As illustrated in Fig. 5, for a fixed ϵ_{th}, increasing σ tends to reduce Γ, which is already in the typical range of a few hundreds for σ = 0. High values of the nonthermal efficiency f_{Nth} ≳ 0.1−0.5 (as usually expected for magnetic reconnection, see e.g. Zhang & Yan 2011; McKinney & Uzdensky 2012) also require high values of the thermal fraction ϵ_{th} ≳ 0.1−0.3, which does not seem natural in such scenarios of highly magnetised outflows.
As illustrated in Sect. 3, spectra with nonthermal and thermal components resembling those found by Guiriec et al. (2011) are easily obtained with our model, either for a photospheric + internal shocks scenario in a case of efficient magnetic acceleration, or for a photospheric + reconnection scenario if the magnetisation at large distance is still large. A potential issue for the internal shock scenario is the moderate variation of the temperature (within a factor of 2) found in the timeresolved analysis. To be efficient, internal shocks require large fluctuations of the Lorentz factors that are even amplified in the observed temperature (T_{obs} ∝ Γ^{8/3}, see Fig. 2). This may suggest that the nonthermal emission in GRB 100724B comes from magnetic reconnection. This is unfortunately difficult to test in absence of theoretical predictions for the spectral evolution in this case. It should however be noted that when the temperature drops, the luminosity also drops so that, in practice, the temperature can be determined only when it is high enough. Depending on the time scale for the Lorentz factor fluctuations and the temporal resolution of the analysis, this may artificially reduce the amplitude of the measured variations of temperature. This is illustrated in Fig. 2 where dotted and dashed lines show the temperature (and peak energy of the nonthermal spectrum) averaged over intervals of 2 and 4 s, respectively. It remains to be tested if this smoothing effect can account for GRB 100724B evolution in the photospheric + internal shocks scenario.
5. Conclusion
We have explored in detail GRB scenarios with two episodes of emission: thermal emission from the photosphere without subphotospheric dissipation, and nonthermal emission from internal dissipation above the photosphere. Our results can be used to interpret the data and obtain constraints on the burst parameters or acceleration mechanism. But one faces the difficulty arising from the diversity of the proposed evidence for the presence of a thermal component in GRB spectra. In some cases this thermal component represents a major contribution to the global spectrum (with additional nonthermal contributions) while in others it is always subdominant, most of the emission having a nonthermal origin. These different situations seem to imply quite different magnetic over thermal energy ratios at the origin of the flow. However the lack of bright thermal components in most GRBs clearly points towards magnetic acceleration, with ϵ_{th} ≲ 0.01 in most cases, and ϵ_{th} ≃ 0.01−0.1 in less frequent cases such as GRB 100724B. GRB 090902B with ϵ_{th} ≃ 0.3−1 remains an exception^{2}.
More generally, one may wonder what would be the best conditions for the thermal emission to show up. Apart from the obvious requirement that ϵ_{th} should be as large as possible, Eq. (24) may suggest looking for events with a low Ė_{iso} and/or a large average Lorentz factor. This, however, supposes that these two quantities are independent. Having and q > 1/4 would favor both a large Ė_{iso} and Γ while the opposite is true for q < 1/4. Finally, if the nonthermal emission comes from internal shocks, a pure thermal spectrum can be possible even if the distribution of the Lorentz factor has a low contrast or if Γ is increasing outwards.
The observation of a burst with an unambiguous photospheric signature in its spectrum would greatly help to clarify several issues in GRB physics: (i) estimating the value of ϵ_{th} would provide insight on the acceleration mechanism of the flow; (ii) obtaining the temperature and thermal luminosity evolution would constrain the distribution of Lorentz factor and injected power; and (iii) measuring the level of temperature fluctuations with a high temporal resolution would help to discriminate between internal shocks and magnetic reconnection for the nonthermal emission. Isolating the photospheric component in the available data is, however, not an easy task: it is generally one among other spectral components and possibly subdominant, and does not have a simple blackbody spectrum.
An intermediate case between GRB 100724B and 090902B has been recently found in the short GRB 120323A (Guiriec et al. 2012).
Acknowledgments
The authors thank the referee for constructive comments helping us to clarify the formulation of the paper. This work is partially supported by a grant from the French Space Agency (CNES). R.H.’s PhD work is funded by a Fondation CFMJP Aguilar grant.
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Appendix A: incomplete acceleration at the photosphere
In the case where the flow is still accelerating at the photosphere, the expressions for the photospheric radius, observed temperature, and thermal luminosity will depend both on the Lorentz factor at the photosphere and on its value at the end of acceleration Γ_{∞}. To obtain the new expressions for R_{ph}, T_{obs}, and L_{th} we write that the optical depth seen by a photon produced at R_{ph} and leaving the flow at R_{out} is equal to unity (A.1)For simplicity we suppose in this Appendix that the flow is stationary, i.e. that Ṁ is constant and that Γ_{∞} is identical for all the shells. Then, adopting a simple parametrisation for the Lorentz factor (A.2)and with Ṁ = Ė_{K}/Γ_{∞} c^{2} we get (neglecting terms of the order of (R_{ph}/R_{sat})^{2α + 1}) (A.3)This finally leads to (A.4)and (A.5)where the index c refers to the case where the acceleration is essentially complete at the photosphere. It can be seen that an incomplete acceleration can substantially reduce the thermal contribution.
All Figures
Fig. 1 Schematic view of the problem geometry. The flow emerges from the central engine through a “circular opening” of radius ℓ. Beyond a radius R_{sph} it expands radially within a cone of half opening θ. The acceleration is completed at R_{sat}. The photosphere is located at R_{ph} and dissipation of kinetic and/or magnetic energy takes place at R_{diss}. 

Open with DEXTER  
In the text 
Fig. 2 Thermal and nonthermal emission from a variable outflow – internal shock framework. Top left: initial distribution of the Lorentz factor in the flow. Top right: thermal (red), nonthermal (blue), and total (black) photon flux in the 8 keV–40 MeV spectral range. Bottom left: thermal (red), nonthermal (blue), and total (black) timeintegrated spectra. Bottom right: instant temperature (red) of the photospheric emission and instant peak energy (blue) of the internal shock emission. The dotted and dashed lines correspond to the temperature and peak energy averaged over time intervals of 2 and 4 s, respectively. The adopted flow parameters are Ė_{iso} = 10^{53} erg s^{1}, ϵ_{th} = 0.03, σ = 0.1, ℓ = 3 × 10^{6} cm, and θ = 0.1 rad; a redshift z = 1 is assumed. 

Open with DEXTER  
In the text 
Fig. 3 Thermal and nonthermal emission from a variable outflow – internal shock framework: impact of the outflow parameters. Starting from the reference case shown in Fig. 2 (with a redshift z = 1) we first change the thermal fraction ϵ_{th} to 0.3 (top left panel) and 0.003 (bottom left); then the isotropic power Ė_{iso} to 10^{54} erg s^{1} (top middle) and 10^{52} erg s^{1} (bottom middle); and finally the Lorentz factor is multiplied (top right) and divided (bottom right) by a factor of 2. Each time we vary a parameter, all the others keep the value corresponding to the reference case. 

Open with DEXTER  
In the text 
Fig. 4 Thermal and nonthermal emission from a variable outflow – magnetic reconnection framework. In each panel we show a sequence of thermal (red) and nonthermal (blue), spectra (the source redshift is z = 1). The Lorentz factor distribution adopted for the calculation of the thermal emission is the same as in Fig. 2 (left panel) or the same but with Γ divided by 2 (right panel). The thermal emission is computed using the formalism developed in Sect. 2.2, using five values of ϵ_{th}: 0.01, 0.03, 0.10, 0.30, and 0.5. The nonthermal spectrum is simply parametrised by a Band function, with the peak energy being given by the Amati relation (see text) and using five values of the efficiency of the magnetic reconnection, f_{rec} = f_{Nth}(1 + σ)/σ: 0.01, 0.03, 0.10, 0.30, and 0.5. In all cases, the isotropic magnetic power at the photosphere is fixed to σĖ_{iso}/(1 + σ) = 10^{53} erg s^{1}. Finally, the magnetisation σ at large distance is either σ = 1 (solid lines) or 10 (dashed lines). 

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In the text 
Fig. 5 Constraints on the thermal and nonthermal emission in GRB 090902B and GRB 100724B. Top: for a given thermal fraction ϵ_{th} = 10^{2}, 10^{1.5}, 10^{1}, 10^{0.5}, and 1, the radius R_{0} = ℓ/θ at the base of the flow is plotted as a function of the nonthermal efficiency f_{Nth}. The corresponding thermal efficiency f_{th} is also shown (top xaxis). Bottom: for a given magnetisation σ = 10^{1}, 10^{0.5}, 1, 10^{0.5}, 10^{1}, 10^{1.5}, and 10^{2} at the end of acceleration phase, the Lorentz factor of the flow is plotted as a function of f_{Nth} (the unmagnetised case σ = 0 cannot be distinguished from the case σ = 0.1). Sets of parameters representative of the different classes of scenarios discussed in the paper are indicated: F (ϵ_{th} = 1, σ = 0) (standard fireball), M,is_{1} (log ϵ_{th} = −0.5, σ = 0,) and M,is_{2} (log ϵ_{th} = −1.5, σ = 0) (efficient magnetic acceleration: magnetisation is low above the photosphere and the dominant nonthermal mechanism is internal shocks), M,rec_{1} (log ϵ_{th} = −0.5, σ = 10), and M,rec_{2} (log ϵ_{th} = −1.5, σ = 10) (magnetised flow at large distance, the dominant nonthermal mechanism is magnetic reconnection). The initial radius is fixed to R_{0} = 300 km, a typical value for long GRBs. The observational data (thermal flux, temperature, ratio of the thermal over the total flux) used for the calculation (see text) are taken from Abdo et al. (2009); Pe’er et al. (2012) for GRB 090902B (left column), and from Guiriec et al. (2011) for GRB 100724B (right column). 

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In the text 
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