Shocks and dust formation in Nova V809 Cep
Abstract
The discovery that many classical novae produce detectable GeV -ray emission has raised the question of the role of shocks in nova eruptions. Here we use radio observations of nova V809 Cep (Nova Cep 2013) with the Jansky Very Large Array to show that it produced non-thermal emission indicative of particle acceleration in strong shocks for more than a month starting about six weeks into the eruption, quasi-simultaneous with the production of dust. Broadly speaking, the radio emission at late times – more than a six months or so into the eruption – is consistent with thermal emission from of freely expanding, K ejecta. At 4.6 and 7.4 GHz, however, the radio light-curves display an initial early-time peak 76 days after the discovery of the eruption in the optical (). The brightness temperature at 4.6 GHz on day 76 was greater than , an order of magnitude above what is expected for thermal emission. We argue that the brightness temperature is the result of synchrotron emission due to internal shocks within the ejecta. The evolution of the radio spectrum was consistent with synchrotron emission that peaked at high frequencies before low frequencies, suggesting that the synchrotron from the shock was initially subject to free-free absorption by optically thick ionized material in front of the shock. Dust formation began around day 37, and we suggest that internal shocks in the ejecta were established prior to dust formation and caused the nucleation of dust.
1 Introduction
A classical nova is an eruption that occurs in an interacting stellar binary system in which one star is a white dwarf and the other is typically a main sequence star (Chomiuk et al., 2020a; Della Valle & Izzo, 2020). Hydrogen-rich material from the donor star accretes onto the white dwarf and is compressed, causing the temperature to rise. The soaring temperatures trigger a thermonuclear runaway and a subsequent ejection of matter from the white dwarf (Starrfield et al., 2016). As material is ejected from the white dwarf, the system brightens across much of the electromagnetic spectrum, allowing for the discovery of such phenomenon.
Between its launch in 2008 June and 2021 April, the Large Area Telescope (LAT; Atwood et al. 2009) of the Fermi Gamma Ray Space Telescope detected GeV gamma-rays from 17 novae (see the list in Chomiuk et al. 2020b; Franckowiak et al. 2018, plus the recurrent nova V3890 Sgr; Buson et al. 2019), typically within a few days of their optical peak (e.g., Ackermann et al., 2014; Chomiuk et al., 2020a, b) The presence of GeV gamma-rays implies that these eruptions have generated a population of relativistic particles. These particles are likely produced via the diffusive shock acceleration mechanism as a result of internal shocks within the ejecta (e.g., Blandford, 1994; Metzger et al., 2016). The high-energy particles may produce gamma-rays via a number of processes including pion decay, inverse Compton scattering of ambient optical photons and relativistic bremsstrahlung (Metzger et al., 2015; Martin et al., 2018). High-energy particles may also produce synchrotron radiation in the radio band (Vlasov et al., 2016). Radio imaging of nova V959 Mon revealed regions of synchrotron emission, further confirming the presence of shocks and providing a localization within the ejecta. From the images, Chomiuk et al. (2014a) postulated that the shocks are the result of collisions between two outflows from the white dwarf: the first, more slowly moving outflow having a toroidal geometry, and the second, faster flow having a more spherical geometry. The shocks were located near the equatorial plane, where the two outflows collided. Based on the optical spectral evolution of a large sample of novae, Aydi et al. (2020b) found consistent evidence for this colliding outflows scenario Finally, observations of correlated variations in GeV and optical brightness suggest that shocks may transport a significant fraction of the nova eruption energy (Li et al., 2017; Aydi et al., 2020a) and power a substantial fraction of the bolometric luminosity during the early weeks of a nova eruption.
In nova-producing binaries that are too distant for -ray detections, radio observations provide a unique opportunity to study developing shocks. Radio lightcurves sometimes contain local maxima, which we refer to as early-time flares, within months of the initial optical peak (Taylor et al., 1987; Finzell et al., 2018; Weston et al., 2016a). These early-time flares correspond to radio surface brightnesses (parameterized as brightness temperatures) that are at least an order of magnitude higher than expected from thermally emitting, K ionized gas that is expanding freely with speeds inferred from optical spectral lines (Cunningham et al., 2015). Because the brightness temperature represents a lower limit on the temperature of thermally emitting material, brightness temperatures in excess of K indicate that either the the ejecta contain enough T K gas for that gas to be optically thick to free-free emission at radio wavelengths or the radio emission is non-thermal emission from electrons accelerated via shocks. In at least one case (V1723 Aql), Weston et al. (2016a) argued that the mass of K gas required for the ejecta to generate the observed radio emission through thermal processes was unfeasible, and that the high brightness temperature was more likely to be the result of synchrotron emission produced near the internal shocks in the ejecta (Vlasov et al., 2016).
Optical and Infared (IR) light curves of classical novae sometimes display characteristics of dust formation days to months after the initial eruption (e.g., Evans, 2001; Shore et al., 2018). Sudden decreases in the optical flux are seen in about 20 percent of novae within 100 days of the optical peak (Strope et al., 2010). These decreases occur earlier than what would be expected due to the natural fading in nova luminosity over time, and – along with the subsequent optical rebrightenings – are referred to as “dust dips”. They result from the obscuring of some optical light from the nova due to the formation of dust and also often appear along with brightening at infrared wavelengths, a typical signature of dust emission (Gehrz, 2008).
Dust production requires cool (T K) gas for the condensation of dust grains, and regions of dust condensation must be shielded from the ionizing radiation emanating from the white dwarf. Derdzinski et al. (2017); Gallagher (1977) reconciles the presence of harsh radiation with the onset of dust formation. Their model, which we refer to as the Shock-Dust Model, postulates that dense radiative shocks, such as the ones thought to give rise to the -rays and early-time radio peaks, provide the optimal conditions for dust condensation. As both the forward and reverse shocks progress, the gas density behind the shocks increases rapidly, producing a thin shell of dense gas between the forward and reverse shocks (Steinberg & Metzger, 2018; Vlasov et al., 2016). This shell is dense enough to be protected from radiation, and as the gas cools, molecules can begin to nucleate into dust particles. Because radio imaging shows that shocks are produced at the interface between the slow-moving toroidal outflow and the fast-moving spherical outflow, the dense shells (and dust formation) might be localized in the equatorial plane.

V809 Cep was first discovered in a nova eruption on 2013 February 2 by K. Nishiyama and F. Kabashima (CBET 3397), and we take this date to be the start of the eruption, . V809 Cep reached peak optical brightness one day later (Munari et al., 2014). Emission line profiles on day 220 and 352 for [OIII] 5007 and [NII] 6548, 6584 + H had a double peak with a separation of 1160 km/s corresponding to a bulk velocity of 600 km/s (Munari et al., 2014). Using the Echelle spectra and comparing with Brand & Blitz (1993), Munari et al. (2014) found the lower limit on the distance to be 6 kpc associated with the crossing of the Perseus or Outer arm. Additionally, using methods from Downes & Duerbeck (2000) and MMRD techniques, they refined their distance estimate to 6.5 kpc. We thus take the distance to be D=6.5 kpc.
In this paper, we use radio observations to show that nova V809 Cep produced non-thermal emission quasi-simultaneously with dust production. We postulate that the non-thermal emission occurred prior to the dust formation, but was initially absorbed by photo-ionized gas ahead of the shock. In Section 2, we describe the technical details of the observations and data reduction. In Section 3, we present our results, and in Section 4 we discuss the implications of our findings in validating the shock-dust model.
2 Observations
We monitored V809 Cep using the Karl G. Jansky Very Large Array Telescope (VLA) between 2013 February 14 and 2016 January 28 under programs 13A-455, 13B-057, and 15B-343. Between 2013 February and 2016 January, the VLA cycled through all configurations, and observed V809 Cep at C band (4 – 8 GHz), Ku band (12 – 18 GHz), and Ka band (26 – 40 GHz). All the observations from 2013 February to 2015 April were performed in the 8-bit observing mode with 2-GHz bandwidth at all bands. The observations in 2015 September and 2016 January were performed in the 3-bit mode with 4-GHz bandwidth at C band, 6-GHz bandwidth at Ku band, and 8-GHz bandwidth at Ka band. Table 1 lists details for each observation.
For observations carried out prior to 2013 May, we reduced the data using AIPS (Greisen, 2003). For observations carried out between 2013 May and 2016 May, we reduced the data using standard routines in CASA (McMullin et al., 2007).To obtain radio flux densities, we fit an elliptical Gaussian to the source image using JMFIT in AIPS and gaussfit in CASA. We estimated uncertainties in the flux density by adding in quadrature the uncertainty from the fit with a systematic uncertainty from absolute flux calibration. At frequencies above 10 GHz, we took the absolute flux density uncertainty to be 10, and at frequencies below 10 GHz, we took the uncertainty introduced by the calibration to be 5. During each observation of V809 Cep, we also observed the source J2339+6010 and source 3C48. Source J2339+6010 was used for complex gain calibration and source 3C48 was used for absolute flux calibration.
[t] Date 1 MJD Epoch Configuration Bands Observed Time (min)2 02/14/2013 12 56337.0 1 D C,Ka 47.9 03/22/2013 48 56373.5 2 D C,Ka 47.9 04/04/2013 61 56386.9 3 D C,Ka 47.9 04/19/2013 76 56401.6 4 D C,Ka 29.9 05/23/2013 110 56435.4 5 C C,U,Ka 29.9 06/10/2013 128 56453.5 6 C C,U,Ka 29.9 06/16/2013 134 56459.3 7 C C,U,Ka 29.9 07/05/2013 153 56478.3 8 C C,U,Ka 29.9 08/27/2013 206 56531.2 9 C C,U,Ka 29.9 09/27/2013 237 56562.2 10 B C,U,Ka 29.2 11/22/2013 293 56618.0 11 B C,U,Ka 29.9 11/30/2013 301 56626.8 12 B C,U,Ka 29.9 12/16/2013 317 56642.8 13 B C,U,Ka 29.9 03/14/2014 405 56719.7 14 A C,U,Ka 29.9 04/29/2014 451 56776.5 15 A C,U,Ka 30.2 05/28/2014 480 56805.6 16 A C,U,Ka 30.2 07/08/2014 521 56846.3 17 D C,U,Ka 29.9 09/06/2014 581 56906.2 18 D C,U,Ka 29.9 11/07/2014 642 56968.0 19 C C,U,Ka 29.9 01/29/2015 726 57051.1 20 B C,U,Ka 27.4 04/21/2015 808 57133.5 21 B C,U,Ka 29.9 09/06/2015 946 57271.4 22 A Ka,U,S,C 31.4 01/28/2016 1090 57415.0 23 C Ka,U,S,C 38.6
-
1
We take the start time of the eruption, , to be 2013 Feb 2.
-
2
Total time on source
3 Results
[t] Epoch 4.6 GHz 7.4 GHz 13.5 GHz 17.4 GHz 28.2 GHz 36.5 GHz 1 0.0511 0.0181 – – 0.0311 0.039 1 2 0.052 0.016 2 0.189 0.020 – – 0.696 0.040 0.718 0.051 3 0.229 0.027 0.503 0.032 – – 1.00 0.028 0.926 0.037 4 0.410 0.061 0.627 0.016 0.789 0.015 0.942 0.017 1.521 0.031 2.143 0.057 5 0.054 1 0.334 0.029 0.814 0.025 1.150 0.022 2.639 0.065 3.809 0.097 6 0.240 0.027 0.434 0.014 1.08 0.015 1.56 0.015 3.25 0.039 4.69 0.058 7 0.260 0.033 0.542 0.021 1.05 0.017 1.48 0.021 3.39 0.0608 4.40 0.082 8 0.252 0.039 0.501 0.015 1.366 0.021 1.992 0.024 4.228 0.077 6.05 0.12 9 0.287 0.025 0.650 0.024 1.583 0.024 2.419 0.035 3.33 0.01 4.51 0.03 10 0.292 0.019 0.515 0.030 1.494 0.037 1.797 0.089 3.40 0.13 3.37 0.12 11 0.448 0.018 0.820 0.013 1.98 0.02 2.55 0.02 3.79 0.05 3.87 0.07 12 0.417 0.023 0.831 0.015 1.88 0.02 2.28 0.02 3.19 0.04 3.03 0.05 13 0.380 0.023 0.902 0.016 2.04 0.02 2.66 0.02 3.72 0.06 3.47 0.08 14 0.492 0.017 0.916 0.012 1.697 0.013 1.907 0.017 2.314 0.040 2.187 0.065 15 0.513 0.027 0.896 0.014 1.34 0.01 1.48 0.02 1.55 0.02 5 1.44 0.03 16 0.495 0.017 0.854 0.011 1.22 0.02 1.22 0.02 1.26 0.03 5 1.16 0.03 17 0.458 0.037 0.903 0.029 1.09 0.02 1.20 0.03 1.20 0.05 1.26 0.08 18 0.526 0.033 0.765 0.024 0.904 0.020 0.952 0.025 0.980 0.062 0.887 0.072 19 0.492 0.024 0.667 0.014 0.713 0.015 0.688 0.017 0.697 0.043 0.620 0.051 20 0.437 0.034 0.503 0.022 0.515 0.022 0.523 0.022 0.456 0.044 0.351 0.062 21 0.413 0.020 0.432 0.015 0.402 0.015 0.382 0.018 0.458 0.042 0.549 0.057 22 0.265 0.013 3 0.243 0.012 4 0.288 0.022 0.311 0.032 6 0.234 0.079 5 0.124 0.071 7 23 0.305 0.024 3 0.203 0.014 4 0.176 0.015 0.165 0.011 6 0.191 0.024 5 0.092 0.025 7
-
1
We take the threshold for detection to be a flux density of at least three times the uncertainty (). We list non-detections as . upper limits.
-
2
The flux density reported is measured at 4.7 GHz
-
3
The flux density reported is measured at 5.0 GHz
-
4
The flux density reported is measured at 7.0 GHz
-
5
The flux density reported is measured at 16.5 GHz
-
6
The flux density reported is measured at 29.5 GHz
-
7
The flux density reported is measured at 35.0 GHz
At radio frequencies above 13 GHz, roughly speaking, the flux density rose over the course of five to ten months, and then faded, but at frequencies below 7.4 GHz, V809 Cep brightened and faded twice (Fig. 1). On 2013 March 22 (day 48-Epoch 2), five weeks after a non-detection on 2013 February 14 (day 12-Epoch 1), the VLA detected V809 Cep at 7.4, 28.2, and 36.5 GHz. The source continued to brighten and was detected at all observed frequencies (4.6, 7.4, 28.2, and 36.5 GHz) on 2013 April 19. On day 76 (Epoch 4), the brightness at 4.6 GHz and 7.4 GHz reached local maxima, at flux densities of mJy and mJy, respectively (see Figure 1). We refer to this low frequency brightening two to three months after the initial outburst as the early-time flare. Even during the decay of the flare, the flux densities at high frequencies continued to rise and reached maxima between days 100 and 300 before beginning to decline (see Figure 1). Table 2 presents the flux densities and associated uncertainties. We take a measured flux density of between three and five times the total uncertainty to be a low-significance detection and a measured flux density of at least five times the total uncertainty to be a high-significance detection. Error bars correspond to 1 uncertainties. V809 Cep appeared as an unresolved point source at all epochs.
The radio spectrum evolved through four distinct stages: 1) a broken power law during the rise of the early-time flare; 2) a simple power law between epochs 5 and 8 (Day 110 - 153), with a spectral index that remained stable at around to 1.6 for more than a month as the radio emission brightened again (taking , where is the flux density at frequency ); 3) a broken power law again as the main decline started first at the highest and then lower frequencies; and 4) a simple, flat spectrum during the final decline. Over the full three-year time scale of the eruption – from 2013 March 22 (day 48) to 2016 January 28 (day 1090)– the radio spectrum evolved from one in which flux density increased with frequency, as expected for optically thick emitting material, to one in which flux density decreased slightly with frequency. We obtained the spectral index () for a given date and frequency range by performing a linear regression using SciPy’s least squares curve fitting method in log-log space, taking into account the uncertainties in the flux density measurements. We generally split the frequencies into low frequencies (4.6, 7.4 GHz), intermediate frequencies ( 13.5 GHz, 17.4 GHz), and high frequencies (28.2, 36.5 GHz). If the spectral indices at low, intermediate, and high frequencies were within 0.2 of each other, we fit them with a single powerlaw. If the spectral indices differed by more than 0.2, we fit the spectrum with a broken powerlaw.
Figure 2 shows the radio spectral energy distribution for selected epochs between 2013 March 22 and 2016 January 28. During Epochs 2, 3, and 4 (stage 1), the spectral index at low frequencies (4.6 GHz and 7.4 GHz) differed from that at high frequencies. At low frequencies, the spectral index evolved from in Epoch 2 to a much flatter in Epoch 4. In contrast, at high frequencies the spectral index evolved from being quite flat at Epoch 2 ( = 0.1 0.4) to rising with at Epoch 4. During stage 3 (Epochs 10-16), the spectrum flattened first at the highest frequencies (Epoch 10) and subsequently at lower frequencies, leading to stage 4 (Epochs 18-22), during which time the spectrum was flat ( = 0.1 0.1 at Epoch 22) across the full range of frequencies.

4 Discussion
4.1 Early Time Radio Flare
During the second and third month of the outburst, the nova produced a flare of low-frequency radio emission that brightened more quickly than expected for freely expanding thermal ejecta and reached a brightness that exceeded expectations for thermally emitting material expanding at the speed of the principal optical absorbing system, suggesting that the flare was non-thermal in origin. The first piece of evidence in support of non-thermal emission is the rapid brightening at low frequencies. Between Epochs 2 and 3, the 4.6-GHz emission increased roughly as , where here is the time since . Even if the material that generated the early-time flare was not ejected from the region of the white dwarf until four days after the start of the eruption (Munari et al., 2014), the 4.6-GHz flux density increased faster than . During the same interval, the 7.4-GHz brightness increased as . Between Epochs 3 and 4, the 4.6-GHz emission continued to increase faster than . For a freely expanding blackbody with constant temperature, the brightness of thermal radio emission can only increase as fast as , proportional to the increasing area of the source on the sky. Although it would be possible for the size of a thermally emitting source to increase faster than if an ionization front was rapidly propagating through the ejecta, or if the electron temperature of the emitting material was increasing, the high radio brightness during Epochs 3 and 4 (see discussion below and Fig. 3) disfavors either of these possibilities.
The second piece of evidence in support of non-thermal emission is the strength of the low-frequency radio emission during Epochs 3 and 4. We parameterize the radio flux density in terms of a brightness temperature, – the minimum electron temperature required for the observed radio emission to arise from thermal Bremsstrahlung. Brightness temperature is a measure of surface brightness. If a uniform temperature, Bremsstrahlung-emitting medium is optically thick over its full area on the sky, the brightness temperature corresponds to its physical temperature; however, if it is even partially optically thin, or if the radio emission emanates from a region that is smaller than the size of the putative spherical ejecta, then the brightness temperature only provides a lower limit for the physical temperature. Assuming a spherically expanding shell, is given by:
(1) |
where c is the speed of light, is the Boltzmann constant, is the time since , and is the maximum expansion velocity. Using a distance of D = 6.5 kpc and a maximum ejection velocity of 1200 km/s (corresponding roughly to the faster of the two principal absorption systems seen in optical spectroscopy; Munari et al., 2014), the brightness temperature at 4.6 GHz reached K (Epoch 4 (day 76); see Figure 3). For the early-time radio flare to have had a thermal origin would therefore require that on day 76 (Epoch 4), the ejecta included a shell of material with an electron temperature of at least K, that was at least as extended on the sky as the 1200 km/s flow, and that was dense enough to be optically thick at 4.6 GHz. If the radio emission emanated from knots, or a portion of the ejecta that subtended a smaller solid angle on the sky than the 1200 km/s flow, the required electron temperature for the early-time flare to have been thermal is even higher. We argue below that such a large, hot, dense ejecta on day 76 (Epoch 4) seems unlikely.
Crucially, given that K is the approximate equilibrium temperature for a plasma cooled by forbidden emission lines (Weston et al., 2016a), photoionized ejecta from novae are typically expected to have electron temperatures of around this value. In fact, Cunningham et al. (2015) found that for a wide range of white dwarf masses, ejecta masses, and ejecta speeds, the temperature of the photoionized ejecta generally does not exceed a few times K at any point. It is possible that the peak brightness of the early-time radio flare in V809 Cep could have been generated by the most spatially extended flow associated with the so-called diffuse enhanced optical spectroscopic system (which had speeds of up to 2000 km/s, Munari et al., 2014) if it had a temperature of K and was completely optically thick. However, the low-frequency spectral index on day 76 (Epoch 4) was , much lower than the expected for optically thick Bremsstrahlung, indicating that the radio-emitting ejecta were not optically thick at that time.
The expected temperature for photoionized ejecta and the spectral index thus both argue against a thermal origin for the early-time flare.

.
The high is also unlikely to be due to a shell of shock-heated, K gas between the forward and reverse shocks. Steinberg & Metzger (2018) explore the possibility of forward and reverse shocks in the ejecta producing a shell of cool (), dense gas bounded by a shell of K gas. We define as the mass of K gas that would be needed to make a shell of width optically thick at radio frequencies and as the mass of K gas theoretically expected to be present. Below, we compare and .
The expected geometrical thickness of the shell of hot gas can be approximated as the cooling length (; Steinberg & Metzger, 2018):
(2) |
Because it is not clear whether the early-time radio flare was the result of the forward or reverse shock, we take to be the velocity of the forward shock. The reverse shock was directed into the fast moving, low density ejecta and thus had a higher velocity than the forward shock which was directed into higher density ejecta. This lower forward-shock velocity ends up being a more conservative estimate for (see Fig. 4 for a comparison between and as a function of ). The maximum velocity of the principle absorption system seen in optical spectroscopy was 1200 km/s, and the lowest expansion velocity observed was 600 km/s (Munari et al., 2014); therefore, we assume a shock velocity between 600 km/s and 1200 km/s. As gas behind the shock cools radiatively, is given by (Steinberg & Metzger, 2018):
(3) |
where the mean molecular weight is for a typical composition of a fully ionized classical nova ejecta (Vlasov et al. 2016; Sokolovsky et al. 2020, , and . From Steinberg & Metzger (2018), we estimate the value of the cooling function () for K gas to be cm3/s. Assuming , the temperature of the shock, , is related to the shock velocity as (Steinberg & Metzger, 2018):
(4) |
Multiplying the mean molecular weight by the expected shell thickness and number density at the location of the shell on day 76 – for the appropriate range of shock velocities, a density profile (where is the distance from the white dwarf), a number density () at from the standard shock jump conditions (Steinberg & Metzger, 2018) , and a total ejecta mass determined from the late-time radio evolution – we find that likely fell between and (see Fig. 4).
For the early-time flare to have been due to thermal emission from gas enclosed within , that gas must either have been optically thick with a temperature in excess of K or had an even higher temperature. In fact, the mass of hot gas that would have been needed to make the hot shell optically thick, , is more than an order of magnitude greater than . To estimate , we assume the hot shell expanded with velocity . We derive the number density of electrons needed to make a K shell optically thick at 4.55 GHz by setting in the expression for the emission measure and taking a constant density profile within the hot shell. The emission measure is , where is the electron density. Following Bode & Evans (2008), we calculate the emission measure needed to make the hot shell optically thick () from:
(5) |
Figure. 4 shows both and enclosed in a shell of thickness as a function of of shock velocity.

For between 600 km/s to 1200km/s, exceeded by at least an order of magnitude. For of 900km/s, and . It is thus implausible for the high brightness temperature to have been the result of thermal emission from a shock-heated shell. This finding further supports our assertion that the high brightness temperature is most likely the result of non-thermal emission produced in a shock.
Non-thermal emission from novae is widely accepted to be the result of internal shocks in the ejecta (Chomiuk et al., 2020a; Vlasov et al., 2016; Finzell et al., 2018; Weston et al., 2016a; Franckowiak et al., 2018; O’Brien & Lloyd, 1994). The collision of the fast and slow flows results in shocks that are responsible for accelerating particles to relativistic speeds. Novae V1723 Aql (Weston et al., 2016a), V5589 Sgr (Weston et al., 2016b) and Nova 1324 Sco (Finzell et al., 2018) had brightness temperatures of greater than K, interpreted as evidence for radio synchrotron emission from shocks. We similarly propose that the bright radio emission that the VLA detected on April 19 2013 (Epoch 4) was the result of shocks in ejecta from V809 Cep. V809 Cep thus joins six other classical novae with radio evidence for shocks: V906 Car (Aydi et al., 2020a), V1324 Sco (Finzell et al., 2018), V1723 Aql (Weston et al., 2016a), 5589 Sgr (Weston et al., 2016b), V959 Mon (Chomiuk et al., 2014a) and QU Vul (Taylor et al., 1987). Non-thermal radio emission has also been found in the eruptions of closely related objects including the helium nova V445 Pup (Nyamai et al., 2021) and the symbiotic system V407 Cyg (Giroletti et al., 2020).
4.2 Spectral Evolution
The radio spectral evolution during the rise to maximum of the early-time flare in V809 Cep had some resemblance to theoretical predictions for synchrotron from internal shocks in novae by Vlasov et al. (2016). Those authors suggested that photo-ionized gas ahead of the shock initially absorbs radio synchrotron emission, causing the spectral index () to evolve from approximately 2.0, as expected for optically thick thermal emission, to 2.5 when the photo-ionized gas ahead of the shock becomes transparent and optically thick synchrotron emission begins to dominate the spectrum. Vlasov et al. (2016) predicted that the spectral index then gradually decreases toward the expected for optically thin synchrotron (the exact value depends on the energy spectrum of the emitting particles, e.g. Pacholczyk 1970). Later, the spectral index is expected to once again rise as the radio emission becomes dominated by optically thick thermal emission from the bulk of the expanding, photoionized ejecta. The peak of the early-time flare occurs as the synchrotron transitions from optically thick to optically thin (Vlasov et al., 2016).
At low frequencies (below 7.4 GHz), the radio emission during the early-time flare in V809 Cep was consistent with theoretical expectations – if the VLA began detecting the flare when photoionized gas ahead of the shock had already become partially transparent. During the flare, the low-frequency spectral index transitioned from a high value suggestive of optically thick synchrotron emission (2.8 0.7 in Epoch 2) to the more modest value of 0.5 0.1 at the peak of the flare (during Epoch 4). Though the error bars on the low frequency spectral index at Epoch 2 are large, in combination with the high brightness temperature, the high spectral index implies optically thick synchroton emission.
The flattening of the low-frequency spectral index at Epoch 4 suggests that the spectrum was indeed transitioning from one indicative of optically thick to optically thin synchrotron emission at that time, as predicted by Vlasov et al. (2016). At Epoch 5, the low-frequency spectral index increased again, to 1.58 0.05, as expected for optically thick thermal emission from the main, expanding ejecta beginning to dominate over the early-time synchrotron emission.
At high frequencies, the radio emission during the early-time flare can also be understood within the framework of Vlasov et al. (2016). Synchrotron emission from an expanding medium is expected to become optically thin, and the spectral index to decrease, at the highest frequencies first (29 GHz and above, in our case). The high-frequency spectral indices at Epochs 2 and 3 of 0.1 0.4 and -0.3 0.2, respectively, thus follow the spectral evolution modeled in Vlasov et al. (2016) if the synchrotron emission had already become fairly optically thin at those frequencies by Epochs 2 and 3. Moreover, because the high-frequency radio spectrum was already quite flat when the VLA first detected the source in Epoch 2, with the high-frequency flux densities well below an extrapolation of the low-frequency spectrum at that time, synchrotron emission at frequencies higher than 7.4 GHz likely peaked before it peaked at low frequencies, and even prior to the first radio detection. Further supporting the possibility that any synchrotron peaked at high frequencies before low frequencies, at 7.4 GHz, the brightness temperature peaked during Epoch 3, an epoch before the peak at 4.6 GHz. Brightness temperature represents a lower limit on the physical temperature of an optically thin gas; therefore, we expect the brightness temperature to peak at high frequencies prior to peaking at low frequencies as the high frequencies become optically thin first. Figure 3 displays a peak first a Epoch 3 (Day 61) at 7.4 GHz and later at Epoch 4 (Day 76) at 4.6 GHz. We thus posit that the early-time flare peaked at high frequencies prior to the first radio detection.
Absorption by photo-ionized gas ahead of the shock would initially obscure the non-thermal emission and produce a delay between the early-time radio maxima at progressively lower frequencies (Vlasov et al., 2016). As the photo-ionized gas ahead of the shock begins to diffuse and become optically thin at lower frequencies, the non-thermal emission from the shock becomes increasingly dominant first at higher frequencies and finally at lower frequencies. So, hints that the synchrotron flare peaked at higher frequencies first (rather than at all frequencies simultaneously) suggest that non-thermal emission from internal shocks in the V809 Cep ejecta was initially absorbed by photo-ionized gas ahead of the shock. However, even if any synchrotron emission was initially somewhat absorbed by photoionized gas, the high spectral index of during Epoch 2 (Day 48) would indicate that we caught the flare when the putative synchrotron emission was already peeking through at low frequencies.
The radio spectral evolution during Stage 2 (Epochs 5-9) further supports our assertion that the spectrum during stage 1 was attributable to an emission component that was physically distinct from the main photoionized ejecta. As the early emission component thinned, the radio spectrum became increasingly dominated by optically thick thermal emission. Indeed, during Epochs 4 (Day 76), the spectral index at high frequencies rose to 1.5 0.1, indicative of optically thick thermal emission. During Epoch 5 through 9 (Day 110 - 206) , the spectral index for all frequencies increased to 1.58 0.05 and remained around 1.5 as the ejecta expanded and the radio emission brightened for the remainder of stage 2. Although the stage 2 spectral indices were lower than the expected 2.0 for optically thick thermal emission from a medium with an infinitely sharp outer edge, values of 1.5 are typical for actual nova remnants. Therefore, the radio spectral evolution was consistent with emission from an increasingly optically thin synchrotron source and a gradually brightening optically thick thermal component. During stage 3 and 4, the radio spectrum was typical of a thermal source becoming increasingly optically thin, with the spectrum flattening at progressively lower frequencies as gas began to become optically thin first at high frequencies ( 29 GHz) and by Epoch 20 (Day 726) at all frequencies.
Event | Date | |
---|---|---|
Optical Detection | 2013 February 2 | 0 |
Optical Peak | 2013 February 3 | 1 |
Onset of dust production | 2013 March 11 | 37 |
Synchrotron detected | 2013 March 22 | 48 |
Peak of Low-Frequency synchrotron | 2013 April 19 | 76 |
4.3 Quasi-simultaneity of synchrotron flare and dust formation
Around the start of the early-time flare, dust production also commenced, providing evidence for a connection between shocks and dust formation. In the shock-dust model (Derdzinski et al., 2017), internal shocks in the ejecta lead to dust condensation. We would naively expect, therefore, to see evidence for the shocks prior to the onset of dust formation, which began around 2013 March 11 (day 37; Munari et al. 2014). The VLA did not observe V809 Cep between day 12 (Epoch 1) and day 48 (Epoch 2) of the eruption, so we cannot pinpoint the exact time at which synchrotron emission appeared (or peaked at high frequencies). But on day 48 (Epoch 2), 11 days past the onset of dust formation, we detected radio emission almost certainly associated with shocks within the ejecta. Therefore, both signatures of shocks and dust appeared during the one month gap between Epoch 1 (Day 12) and Epoch 2 (Day 48). Given the evidence that the early-time flare did not peak at the same time at all frequencies and therefore that any synchrotron was initially obscured, the radio observations are consistent with the shocks arising either slightly before or around the same time as the onset of dust production.
4.4 Properties of the Thermal Ejecta
Starting about nine months into the eruption, the radio emission was reasonably consistent with Bremsstrahlung (free-free emission) from freely expanding, photoionized ejecta. We modeled the main ejecta as a Hubble-flow (Gehrz, 2008; Finzell et al., 2018; Weston et al., 2016a; Seaquist & Palimaka, 1977; Hjellming et al., 1979), in which the ejecta consists of a homologously expanding isothermal spherical shell of gas bound between inner and outer radii and , with a density profile (where is the distance from the white dwarf), and a volume filling factor, . The filling factor is a measure of inhomogeneities in the ejecta, such as clumps (e.g., Weston et al., 2016a; Hjellming, 1996). We assume no inhomogeneities (). If the ejecta were actually clumpy, that would reduce the ejecta mass needed to generate the observed radio emission (Weston et al., 2016a; Hjellming, 1996; Abbott et al., 1981; Leitherer & Robert, 1991; Chomiuk et al., 2014b).
At low frequencies ( 7.4 GHz) during the first six or so months of the outburst, the model fit the observed flux densities poorly, and as expected, was unable to account for the early-time flare. At 13.5 and 17.0 GHz, the discrepancy between the model and the observed flux densities during the first few months of the eruption supports our contention (in Sec. 4.2) that the flare at these frequencies could have peaked before Epoch 4 (Day 76). At these frequencies, the Hubble-Flow model matched the observed flux densities well after Epoch 4 (Day 76). At Epoch 4 (Day 76), however, the observed flux density at 17.4 GHz was mJy, 0.61 mJy in excess of the the model flux density of 0.33 mJy. At 13.5 GHz, the observed flux density was , 0.58 mJy in excess of the model flux density. That the observed 13.5- and 17.4-GHz flux densities were far in excess of the model during Epoch 4 (Day 76) indicates that any synchrotron emission was still dominant at those frequencies at that time and could therefore have peaked even earlier (the VLA did not collect data at these frequencies during Epochs 2 and 3 (Day 48 and Day 61)).
At 28.8 and 36.5 GHz, and after approximately days 200-300 (¿Epoch 9) at all frequencies, however, the model reproduces the observed flux densities moderately well. Using kpc, km s-1, and km s-1, we determined the best-fit ejecta mass and temperature by employing the Markov Chain Monte Carlo program pymc. We found and when the hubble flow model was fit to the reduced flux densities starting from Epoch 2 (Day 48) (first detection). Figure 5 displays the observed flux densities as well as the modeled free-free emission for kpc, and K.

5 Conclusions
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•
The radio light-curves at 4.6 GHz and 7.4 GHz display an early-time flare that peaks at Epoch 4 (day 76). At 4.6 GHz, the brightness temperature at that time was at least 1.5 .
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•
At low frequencies ( 7.4 GHz) the rise of the early-time flare began at Epoch 2 (Day 48, 2013 March 22). The spectral index at low frequencies at Epoch 2 (Day 48) was 2.82 0.71.
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•
The high brightness temperature at the peak of the early-time flare at Epoch 4 (Day 76) combined with the high spectral index at Epoch 2 (Day 48) suggests the presence of non-thermal emission due to internal shocks in the nova ejecta. This is the first report showing evidence for shocks in V809 Cep.
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•
The discovery of non-thermal radio emission early in the evolution of the eruption puts V809 Cep in the same category as six other novae known to show radio evidence for shocks: V906 Car (Aydi et al., 2020a), V1324 Sco (Finzell et al., 2018), V1723 Aql (Weston et al., 2016a), V5589 Sgr (Weston et al., 2016b), V959 Mon (Chomiuk et al., 2014a),and QU Vul (Taylor et al., 1987).
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•
At late times (after Epoch 4 (Day 76)), the radio emission was consistent with thermal emission from freely expanding ejecta with a maximum ejecta speed of 1200km/s, = 600km/s, D =6.5 kpc, , and a .
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•
Our finding that a radio synchrotron flare associated with internal shocks in the ejecta began during a roughly month-long period of time during which dust formation also commenced supports the idea that shocks could form ideal environments for dust formation around novae.
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•
If shocks in the nova ejecta lead to dust formation, the 11 day delay between the onset of dust and the rise of the early-time flare suggests that the radio emission was absorbed by photo-ionized gas ahead of the shock.
Data availability
The data underlying this article will be shared on reasonable request to the corresponding author. The uncalibrated radio observations are publicly available from the NRAO Data Archive (archive.nrao.edu or data.nrao.edu)
Acknowledgements
The National Radio Astronomy Observatory is a facility of the National Science Foundation operated under cooperative agreement by Associated Universities, Inc. A. B. and J. L. S. acknowledge support from NSF grant AST-1816100 and Heising-Simons Foundation grant 2017-246, as well as NRAO 362918. Laura Chomiuk, Adam Kawash, Elias Aydi, and Kirill V. Sokolovsky were supported by NSF grant AST-1751874 and a Cottrell fellowship of the Research Corporation.
References
- Abbott et al. (1981) Abbott D. C., Bieging J. H., Churchwell E., 1981, ApJ, 250, 645
- Ackermann et al. (2014) Ackermann M., et al., 2014, Science, 345, 554
- Atwood et al. (2009) Atwood W. B., et al., 2009, ApJ, 697, 1071
- Aydi et al. (2020a) Aydi E., et al., 2020a, Nature Astronomy, 4, 776
- Aydi et al. (2020b) Aydi E., et al., 2020b, ApJ, 905, 62
- Blandford (1994) Blandford R. D., 1994, ApJS, 90, 515
- Bode & Evans (2008) Bode M. F., Evans A., 2008, Classical Novae
- Brand & Blitz (1993) Brand J., Blitz L., 1993, A&A, 275, 67
- Buson et al. (2019) Buson S., Jean P., Cheung C. C., 2019, The Astronomer’s Telegram, 13114, 1
- Chomiuk et al. (2014a) Chomiuk L., et al., 2014a, Nature, 514, 339
- Chomiuk et al. (2014b) Chomiuk L., et al., 2014b, ApJ, 788, 130
- Chomiuk et al. (2020a) Chomiuk L., Metzger B. D., Shen K. J., 2020a, arXiv e-prints, p. arXiv:2011.08751
- Chomiuk et al. (2020b) Chomiuk L., Metzger B. D., Shen K. J., 2020b, arXiv e-prints, p. arXiv:2011.08751
- Cunningham et al. (2015) Cunningham T., Wolf W. M., Bildsten L., 2015, ApJ, 803, 76
- Della Valle & Izzo (2020) Della Valle M., Izzo L., 2020, A&ARv, 28, 3
- Derdzinski et al. (2017) Derdzinski A. M., Metzger B. D., Lazzati D., 2017, MNRAS, 469, 1314
- Downes & Duerbeck (2000) Downes R. A., Duerbeck H. W., 2000, AJ, 120, 2007
- Evans (2001) Evans A., 2001, Ap&SS, 275, 131
- Finzell et al. (2018) Finzell T., et al., 2018, ApJ, 852, 108
- Franckowiak et al. (2018) Franckowiak A., Jean P., Wood M., Cheung C. C., Buson S., 2018, A&A, 609, A120
- Gallagher (1977) Gallagher J. S., 1977, AJ, 82, 209
- Gehrz (2008) Gehrz R. D., 2008, Infrared studies of classical novae, 2 edn. Cambridge University Press, p. 167–193, doi:10.1017/CBO9780511536168.010
- Giroletti et al. (2020) Giroletti M., et al., 2020, A&A, 638, A130
- Greisen (2003) Greisen E. W., 2003, AIPS, the VLA, and the VLBA. p. 109, doi:10.1007/0-306-48080-8˙7
- Hjellming (1996) Hjellming R. M., 1996, in Taylor A. R., Paredes J. M., eds, Astronomical Society of the Pacific Conference Series Vol. 93, Radio Emission from the Stars and the Sun. p. 174
- Hjellming et al. (1979) Hjellming R. M., Wade C. M., Vandenberg N. R., Newell R. T., 1979, AJ, 84, 1619
- Leitherer & Robert (1991) Leitherer C., Robert C., 1991, ApJ, 377, 629
- Li et al. (2017) Li K.-L., et al., 2017, Nature Astronomy, 1, 697
- Martin et al. (2018) Martin P., Dubus G., Jean P., Tatischeff V., Dosne C., 2018, A&A, 612, A38
- McMullin et al. (2007) McMullin J. P., Waters B., Schiebel D., Young W., Golap K., 2007, in Shaw R. A., Hill F., Bell D. J., eds, Astronomical Society of the Pacific Conference Series Vol. 376, Astronomical Data Analysis Software and Systems XVI. p. 127
- Metzger et al. (2015) Metzger B. D., Finzell T., Vurm I., Hascoët R., Beloborodov A. M., Chomiuk L., 2015, MNRAS, 450, 2739
- Metzger et al. (2016) Metzger B. D., Caprioli D., Vurm I., Beloborodov A. M., Bartos I., Vlasov A., 2016, MNRAS, 457, 1786
- Munari et al. (2014) Munari U., et al., 2014, MNRAS, 440, 3402
- Nyamai et al. (2021) Nyamai M. M., Chomiuk L., Ribeiro V. A. R. M., Woudt P. A., Strader J., Sokolovsky K. V., 2021, MNRAS, 501, 1394
- O’Brien & Lloyd (1994) O’Brien T. J., Lloyd H. M., 1994, Ap&SS, 216, 167
- Pacholczyk (1970) Pacholczyk A. G., 1970, Radio astrophysics. Nonthermal processes in galactic and extragalactic sources
- Seaquist & Palimaka (1977) Seaquist E. R., Palimaka J., 1977, ApJ, 217, 781
- Shore et al. (2018) Shore S. N., Kuin N. P., Mason E., De Gennaro Aquino I., 2018, A&A, 619, A104
- Sokolovsky et al. (2020) Sokolovsky K. V., et al., 2020, MNRAS, 497, 2569
- Starrfield et al. (2016) Starrfield S., Iliadis C., Hix W. R., 2016, PASP, 128, 051001
- Steinberg & Metzger (2018) Steinberg E., Metzger B. D., 2018, MNRAS, 479, 687
- Strope et al. (2010) Strope R. J., Schaefer B. E., Henden A. A., 2010, AJ, 140, 34
- Taylor et al. (1987) Taylor A. R., Seaquist E. R., Hollis J. M., Pottasch S. R., 1987, A&A, 183, 38
- Vlasov et al. (2016) Vlasov A., Vurm I., Metzger B. D., 2016, MNRAS, 463, 394
- Weston et al. (2016a) Weston J. H. S., et al., 2016a, MNRAS, 457, 887
- Weston et al. (2016b) Weston J. H. S., et al., 2016b, MNRAS, 460, 2687