Abstract

We present very-high-energy γ-ray observations of the BL Lac object 1ES 2344+514 taken by the Very Energetic Radiation Imaging Telescope Array System between 2007 and 2015. 1ES 2344+514 is detected with a statistical significance above the background of 20.8σ in 47.2 h (livetime) of observations, making this the most comprehensive very-high-energy study of 1ES 2344+514 to date. Using these observations, the temporal properties of 1ES 2344+514 are studied on short and long times-scales. We fit a constant-flux model to nightly and seasonally binned light curves and apply a fractional variability test to determine the stability of the source on different time-scales. We reject the constant-flux model for the 2007–2008 and 2014–2015 nightly binned light curves and for the long-term seasonally binned light curve at the >3σ level. The spectra of the time-averaged emission before and after correction for attenuation by the extragalactic background light are obtained. The observed time-averaged spectrum above 200 GeV is satisfactorily fitted (χ2/NDF = 7.89/6) by a power-law function with an index Γ = 2.46 ± 0.06stat ± 0.20sys and extends to at least 8 TeV. The extragalactic-background-light-deabsorbed spectrum is adequately fit (χ2/NDF = 6.73/6) by a power-law function with an index Γ = 2.15 ± 0.06stat ± 0.20sys while an F-test indicates that the power law with an exponential cut-off function provides a marginally better fit (χ2/NDF = 2.56/5) at the 2.1σ level. The source location is found to be consistent with the published radio location and its spatial extent is consistent with a point source.

1 INTRODUCTION

1ES 2344+514 (RA: 23h47΄04.837, Dec.: +51°42΄17.881 (J2000); Petrov et al. 2008) is a BL Lac object located at a redshift of z = 0.044 (Perlman et al. 1996). It was the third reported extragalactic source of very-high-energy (VHE, E ≳ 100 GeV) γ-rays (Catanese et al. 1998) after Markarian 421 and Markarian 501. To date, approximately 60 BL Lac objects have been detected as VHE sources.1 BL Lac objects, along with flat-spectrum radio quasars, constitute the blazar class of active galactic nuclei (AGNs), which are thought to consist of AGNs with relativistic jets that happen by chance to be oriented towards the Earth.

BL Lacs are highly variable and exhibit double-humped broad-band non-thermal spectra, with the first peak, located in the infrared to X-ray regimes, believed to be relativistically beamed incoherent synchrotron radiation. The location of the synchrotron peak is used to classify a BL Lac as a low- (LBL), intermediate- (IBL) or high-frequency-peaked BL Lac object (HBL) (Padovani & Giommi 1995). 1ES 2344+514 is classified in the HBL category, as are the majority (∼80 per cent) of the VHE-detected BL Lacs to date. The higher-energy peak, located in the γ-ray regime, is likely due to inverse-Compton scattering of either the synchrotron photons themselves (known as synchrotron self-Compton, SSC) or soft photons external to the jet (known as external inverse-Compton, EIC), or a combination of both, although other emission mechanisms such as from hadronic processes have not been ruled out (for an overview see e.g. Böttcher 2007). Measurements of the γ-ray variability and spectrum of a BL Lac object, when combined with multiwavelength measurements, may be used to constrain the size of the emission region, and to test theoretical models and constrain model parameters such as the magnetic field strength and electron energy distribution (e.g. Cerruti, Boisson & Zech 2013). It has been found that most HBLs are adequately described by pure single-zone SSC models while IBLs and LBLs require increasing EIC contributions to reproduce the observed spectra (see Böttcher 2007, and references therein). Spectral studies of VHE BL Lac objects tend to utilize bright states associated with flares due to the high photon statistics obtained. Long-term monitoring, as presented here for 1ES 2344+514, is needed to obtain statistically significant detections over a reasonable energy range to facilitate the study and spectral modelling of low-flux states. In addition, the long-term monitoring is important for characterizing the duty cycle of flaring blazars, which has an impact on the contributions of blazars to the extragalactic γ-ray background radiation fields (Giommi et al. 2006; Pittori et al. 2007).

VHE photon fluxes undergo energy-dependent attenuation when travelling cosmological distances due to pair production via interaction with low-energy optical/IR extragalactic background light (EBL) photons. Thus, the observed VHE spectrum of an object is the emitted spectrum modified by absorption due to EBL photons. EBL absorption ultimately limits the distance over which VHE γ-ray sources can be detected. Correcting for EBL absorption is necessary in order to uncover the intrinsic VHE spectrum of a BL Lac object. The intensity and spectrum of the EBL is also of cosmological interest as it contains a record of the star-formation history of the Universe, but direct measurement is difficult due to the foreground contamination by zodiacal light. However, constraints can be obtained from VHE spectral measurements of distant objects by finding the maximum allowed EBL such that the de-absorbed spectrum does not conflict with the hardest allowed spectrum from theoretical arguments or extrapolated spectra from lower energies where EBL absorption does not take place (for a review see e.g. Dwek & Krennrich 2013). The most comprehensive studies involve combining the constraints from multiple different objects at a variety of redshifts (Biteau & Williams 2015). In this work, we use a published EBL model to estimate the intrinsic VHE spectrum of 1ES 2344+514.

If BL Lac objects generate multi-TeV emission then the interactions with EBL photons may produce magnetically broadened cascades resulting in extended halo emission around these sources. Spatial profiles of such objects in VHE γ-rays may be used to place model-dependent constraints on intergalactic magnetic fields (e.g. Aharonian, Coppi & Voelk 1994; Archambault et al. 2017b). While 1ES 2344+514 is not an ideal candidate for magnetically broadened emission due to its proximity and relatively low flux (an estimate of the cascade fraction is below the VERITAS sensitivity), a search for spatially extended emission was carried out as part of this study to compare the location of the site of the VHE emission with that at other wavelengths.

1ES 2344+514 is an important target for VERITAS. The source is regularly monitored as part of the blazar science programme (Benbow et al. 2015) in order to obtain measurements of its long-term flux states. These observations can be used to build statistics for spectral determination at the highest energies, and to trigger intensive multiwavelength observations should exceptional flaring activity be observed. The spectral information obtained from these observations will be used as part of the VERITAS multi-object study to place constraints on the EBL. In this publication, we report on the analysis of the complete VERITAS data set taken on 1ES 2344+514 from 2008 October to 2015 January. The data from 2007–2008, previously published in Acciari et al. (2011), are also incorporated in order to provide updated spectra and light curves. These data provide important measurements of the highest energy component emission from 1ES 2344+514, which can be combined with multiwavelength observations to search for correlated variability and to construct the overall SED for model evaluation.

2 1ES 2344+514 VHE γ-RAY OBSERVATIONAL HISTORY

1ES 2344+514 was first detected as a VHE γ-ray source by the Whipple 10 m telescope during observations made between 1995 and 1996 (Catanese et al. 1998), with most of the signals coming from a flare on a single night. These and subsequent observations performed by several imaging atmospheric Cherenkov telescopes (IACTs) (e.g. Aharonian et al. 2004; Godambe et al. 2007; Albert et al. 2007; Acciari et al. 2011; Aleksić et al. 2013) have revealed the source to have variable flux states. The integral flux is typically less than 10 per cent that of the Crab nebula, but day-scale flares of 60 per cent and 50 per cent of the Crab nebula flux have been observed (Catanese et al. 1998; Acciari et al. 2011).

Current-generation IACTs have allowed variability and spectral studies of 1ES 2344+514 to be extended to lower flux states. The MAGIC collaboration observed 1ES 2344+514 in a particularly low state for ∼20 h spread across 14 nights (2008 October 20 to 2008 November 30) as part of a multiwavelength campaign; it was marginally detected at a level of 3.5 standard deviations above the background (σ) and determined to have a flux approximately 2.5 per cent that of the Crab nebula with a power-law energy spectrum of index 2.4 ± 0.4stat in the energy range from 0.17 to 2 TeV (Aleksić et al. 2013). VERITAS detected 1ES 2344+514 at the 20σ level in 18 h of observations spread across 37 nights in 2007/2008 (from 2007 October 4 to 2008 January 11) including a one-day flare of ∼50 per cent of the Crab nebula flux on 2007 December 7 (MJD 54441) (Acciari et al. 2011). Analysis of the data excluding the flare revealed a low-state flux of ∼7.6 per cent of the Crab nebula with a spectrum well fitted by a power-law index of 2.78 ± 0.09stat ± 0.15sys in the energy range from 0.39 to 8.3 TeV. The flare-state spectrum was well fitted by a power-law index of 2.43 ± 0.22stat ± 0.20sys, consistent with the spectral analysis of the previous large flare seen with the Whipple 10 m telescope on 1995 December 20 which showed a power-law index of 2.54 ± 0.17stat ± 0.07sys (Schroedter et al. 2005). MAGIC observations in 2005/2006 (27 nights in the interval 2005 August 3 to 2006 January 1) totalling 32 h provided an 11σ detection with an average flux of ∼10 per cent that of the Crab nebula, with a spectrum well fitted by a power-law index of 2.95 ± 0.12stat ± 0.2sys between 0.14 and 5 TeV (Albert et al. 2007). HBL objects tend to show a harder spectral index with an increased flux, with the MAGIC observations in 2008 being an unusual exception as discussed by Aleksić et al. (2013).

3 VERITAS OBSERVATIONS AND ANALYSIS

The Very Energetic Radiation Imaging Telescope Array System (VERITAS; Holder et al. 2006) is an array of four IACT telescopes, located at the Fred Lawrence Whipple Observatory in Southern Arizona. Each telescope is of 12 m diameter, with a 499-pixel photomultiplier-tube (PMT) camera located at the focal plane. Since commissioning in 2007, the array has undergone two major upgrades to improve the performance: in 2009 May, Telescope 1 was moved to improve the collection area of the array, which, along with the upgraded mirror alignment (McCann et al. 2010) and trigger systems (Zitzer et al. 2013), resulted in a 30 per cent improvement in sensitivity (Perkins et al. 2009). In the summer of 2012, the cameras were upgraded with higher-quantum-efficiency PMTs, which resulted in a significantly improved sensitivity below 100 GeV (Otte 2011). In its current configuration, VERITAS can detect a source with a flux of 1 per cent that of the Crab nebula at the 5σ level in ∼25 h, has a minimum individual photon angular resolution (68 per cent containment radius) of ∼0.1° at 1 TeV, an energy resolution of 15–25 per cent and an effective area for >1 TeV photons on the order of 105 m2. For a detailed discussion of the current performance of VERITAS, see Park et al. (2015).

In addition to normal dark-sky observations, VERITAS has been operated under moderate moonlight using reduced high voltage (RHV) to the PMTs, resulting in an increased observing time, but with a loss of sensitivity below ∼200 GeV (Archambault et al. 2017a). The extra observing time that RHV observations offer has already been beneficial with the detection of a flare from the blazar 1ES 1727+502 (Archambault et al. 2015).

The 47.2 h of data presented here include all three-telescope configurations, incorporate 11.6 h of RHV observations and include the data presented in Acciari et al. (2011). The flare (on MJD 54441) reported in Acciari et al. (2011) was observed under less-than-optimal weather conditions and is excluded from this analysis, but is shown in the light curves in order to put the long-term variability of the source in perspective.

Independent analyses were carried out using the collaboration's two main data analysis software packages and excellent agreement was found. Details of the analysis procedures used by VERITAS can be found in Acciari et al. (2008). The γ-ray selection criteria used were optimized for a source with 5 per cent Crab nebula flux and a power-law spectral index of 2.5. Background estimation was performed using the reflected-region method (Fomin et al. 1994) with eight reflected regions, and the significance of the γ-ray excess was calculated using equation (17) of Li & Ma (1983).

We define the nominal VERITAS observing season to be from September to June, with September to August being a full year. The breakdown of the observations by observing season is given in Table 1. To compare the measured fluxes to that of the Crab nebula, we use the differential spectrum derived in Hillas et al. (1998). Due to the varying energy thresholds of the observations caused by zenith angle differences, the inclusion of RHV data and different array configurations, we have quoted the detection significance and conducted the light-curve analysis above a common energy threshold of 0.35 TeV. It should be noted that this energy threshold cut is not applied to the spectral analysis.

Table 1.

Breakdown of observations by season including hours of data (livetime), detection significance, flux, the results of a χ2 test for constant emission and the results of the fractional variability (Fvar) test (see Section 4.3).

Data setLivetimeDetectionFluxaχ2/NDFFvar
(h)(σ)(>0.35 TeV)
2007–200817.116.213.2 ± 1.0192/370.78 ± 0.13
2008–20090.4−0.7<6.4N/AN/A
2010–20115.43.33.1 ± 1.026/150.56 ± 0.66
2011–20123.02.62.8 ± 1.223/91.58 ± 0.50
2012–20134.29.78.3 ± 1.219/8b
2013–20147.82.51.5 ± 0.616/12b
2014–20159.311.06.4 ± 0.752/100.52 ± 0.23
2007–201547.220.87.1 ± 0.4464/970.97 ± 0.10
Data setLivetimeDetectionFluxaχ2/NDFFvar
(h)(σ)(>0.35 TeV)
2007–200817.116.213.2 ± 1.0192/370.78 ± 0.13
2008–20090.4−0.7<6.4N/AN/A
2010–20115.43.33.1 ± 1.026/150.56 ± 0.66
2011–20123.02.62.8 ± 1.223/91.58 ± 0.50
2012–20134.29.78.3 ± 1.219/8b
2013–20147.82.51.5 ± 0.616/12b
2014–20159.311.06.4 ± 0.752/100.52 ± 0.23
2007–201547.220.87.1 ± 0.4464/970.97 ± 0.10

Notes.aUnits: ×10−12 cm−2 s−1.

bUndefined as variance determined to be smaller than the mean error (see Section 4.3).

Table 1.

Breakdown of observations by season including hours of data (livetime), detection significance, flux, the results of a χ2 test for constant emission and the results of the fractional variability (Fvar) test (see Section 4.3).

Data setLivetimeDetectionFluxaχ2/NDFFvar
(h)(σ)(>0.35 TeV)
2007–200817.116.213.2 ± 1.0192/370.78 ± 0.13
2008–20090.4−0.7<6.4N/AN/A
2010–20115.43.33.1 ± 1.026/150.56 ± 0.66
2011–20123.02.62.8 ± 1.223/91.58 ± 0.50
2012–20134.29.78.3 ± 1.219/8b
2013–20147.82.51.5 ± 0.616/12b
2014–20159.311.06.4 ± 0.752/100.52 ± 0.23
2007–201547.220.87.1 ± 0.4464/970.97 ± 0.10
Data setLivetimeDetectionFluxaχ2/NDFFvar
(h)(σ)(>0.35 TeV)
2007–200817.116.213.2 ± 1.0192/370.78 ± 0.13
2008–20090.4−0.7<6.4N/AN/A
2010–20115.43.33.1 ± 1.026/150.56 ± 0.66
2011–20123.02.62.8 ± 1.223/91.58 ± 0.50
2012–20134.29.78.3 ± 1.219/8b
2013–20147.82.51.5 ± 0.616/12b
2014–20159.311.06.4 ± 0.752/100.52 ± 0.23
2007–201547.220.87.1 ± 0.4464/970.97 ± 0.10

Notes.aUnits: ×10−12 cm−2 s−1.

bUndefined as variance determined to be smaller than the mean error (see Section 4.3).

4 RESULTS

4.1 Overall detection

The livetime of 47.2 h on 1ES 2344+514 results in a total number of ‘on’ and ‘off’ region counts of 1232 and 4826, respectively (using eight background regions and a common energy threshold of 0.35 TeV); hence, we report a detection significance of 20.8σ above background.

The time-averaged event rate for all nights is measured to be (0.20 ± 0.01) γ min−1 and the total time-averaged flux above 0.35 TeV is calculated to be F(E > 0.35 TeV) = (7.1 ± 0.4) × 10−12 cm−2 s−1 or 7 per cent that of the Crab nebula.

4.2 Source localization

A symmetric two-dimensional Gaussian function is fitted to the excess-count sky map using a χ2 method. The χ2 statistic is minimized at the coordinates (J2000):

 RA: (23h 47΄ 4) ± (0 h 0΄ 2 )stat,

 Dec.: (+51° 42΄ 49) ± (0° 0΄ 16 )stat.

The fitted extension is consistent with a point source convolved with the point-spread function of VERITAS. The systematic error on the VERITAS pointing accuracy is <25, which gives systematic errors on the right ascension of ±(0 h 0΄ 3) and on the declination of ±(0° 0΄ 25). As this is the first study of the source location with VERITAS, 1ES 2344+514 is allocated the VERITAS catalogue name VER J2347+517.

4.3 Variability analysis

We tested the stability of the season-to-season flux by applying a χ2 test for constant emission to the seasonally averaged fluxes. We also tested for variability within each season by binning the data by night and performing a χ2 test for constant emission. The results of the χ2 tests are summarized in Column 5 of Table 1 and the light curves are shown in Fig. 1. The flare on the night of MJD 54441 is excluded from this analysis, but included in Fig. 1 for comparison reasons. Due to having only ∼30 min of observations during the 2008–2009 season, we exclude that season from the seasonal variability test and calculate a 95 per cent upper limit on the flux. We reject the constant-flux hypothesis on seasonal time-scales due to the calculated χ2/NDF of 121/5. Within each season, the light curves were found to be inconsistent with the constant-flux model at a level >3σ for the 2007–2008 and 2014–2015 observing seasons.

Light curves for 1ES 2344+514. Panel (a) shows the average nightly flux. Observations taken during the 2008–2015 seasons are plotted as red squares and observations taken during the 2007–2008 season are plotted as blue circles. All points are plotted regardless of their significance. Panel (b) shows the average flux within each seasonal bin with an upper limit plotted for the 2008–2009 observation season. In calculating average fluxes, we consider all flux measurements regardless of their significance to obtain an unbiased measurement.
Figure 1.

Light curves for 1ES 2344+514. Panel (a) shows the average nightly flux. Observations taken during the 2008–2015 seasons are plotted as red squares and observations taken during the 2007–2008 season are plotted as blue circles. All points are plotted regardless of their significance. Panel (b) shows the average flux within each seasonal bin with an upper limit plotted for the 2008–2009 observation season. In calculating average fluxes, we consider all flux measurements regardless of their significance to obtain an unbiased measurement.

The fractional variability statistic (Fvar; Vaughan et al. 2003) given by
\begin{equation*} F_{\text{var}}= \sqrt{ \frac{ S^2 - \overline{\sigma _{\text{err}}^2}}{ \overline{x}^2 } }\pm \sqrt{ \left( \sqrt{\frac{1}{2N}} \frac{ \overline{\sigma _{\text{err}}^2} }{\overline{x}^2 F_{\text{var}}}\right)^2 + \left( \sqrt{ \frac{\overline{\sigma _{\text{err}}^2}}{N} }\frac{1}{\overline{x}}\right)^2 }, \end{equation*}
where S is the sample variance, |$\overline{\sigma _{\text{err}}^2}$| is the mean squared error on the flux of the sample, N is the sample size and |$\overline{x}$| is the average flux of the sample, is calculated for each season. The calculated Fvar indicates the fractional observed variance in excess of the known average statistical uncertainty. The results are summarized in Column 6 of Table 1. Variability in excess of the statistical uncertainty is observed in the 2007–2008, 2011–2012 and 2014–2015 observing seasons, while the 2010–2011, 2012–2013 and 2013–2014 seasons exhibit variability that is consistent with that expected from statistical uncertainties.

For consistency, both the already-published 2007–2008 and newly presented 2008–2015 data sets are analysed using the most recent version of the VERITAS analysis software. This allows for a comparison of the two data sets. The time-averaged flux for the low-state observations during the 2007–2008 season is measured to be F(E > 0.35 TeV) = (13.2 ± 1.0) × 10−12 cm−2 s−1, equivalent to 13 per cent that of the Crab nebula, while the 2008–2015 data set shows a considerably dimmer flux level of F(E > 0.35 TeV) = (4.4 ± 0.4) × 10−12 cm−2 s−1, equivalent to 4 per cent that of the Crab nebula. The significance of the decrease is calculated as |$(F_{2007-2008} - F_{2008-2015})/\sqrt{\delta F_{2007-2008}^2 + \delta F_{2008-2015}^2}$|⁠, where F and δF are the flux and flux error for the respective observation periods, and has the value 8.3σ.

4.4 Spectral analysis

To investigate any possible bias introduced by combining data with different energy thresholds, we compare the best-fit energy spectra before and after applying the common energy threshold of 350 GeV. The resulting best-fit spectra are found to be in excellent agreement, indicating no bias is present. The spectral analysis was thus conducted above the lower energy threshold of 200 GeV.

The observed and EBL-corrected differential spectra were fitted with power-law functions, and, in addition, the EBL-corrected spectrum was fitted with a power law with an exponential cut-off function to test the intrinsic spectral curvature.

The power-law function fitted is of the form
\begin{equation*} \frac{{\rm d}N}{{\rm d}E} = N_0 \left(\frac{E}{E_0}\right)^{-\Gamma }, \end{equation*}
where E0 is the decorrelation energy (i.e. the energy at which the correlation between the normalization flux (N0) and the spectral index (Γ) is a minimum). The fit is applied to the original low-state data set published in Acciari et al. (2011), the new data taken since that publication and the combined data set, with the results presented in Table 2.
Table 2.

Spectral analysis of 1ES 2344+514 broken down into observation periods. The systematic errors on N0 and Γ are estimated to be 20 per cent and 0.20, respectively.

Power-law fit
Data setN0E0Γχ2/NDF
(×10−12 cm−2 s−1)(TeV)
2007–20083.19 ± 0.23stat1.112.43 ± 0.09stat4.03/5
2008–20153.42 ± 0.29stat0.692.63 ± 0.14stat3.39/4
2007–20152.65 ± 0.14stat0.912.46 ± 0.06stat7.89/6
2007–2015a4.04 ± 0.22stat0.912.15 ± 0.06stat6.73/6
Power-law fit
Data setN0E0Γχ2/NDF
(×10−12 cm−2 s−1)(TeV)
2007–20083.19 ± 0.23stat1.112.43 ± 0.09stat4.03/5
2008–20153.42 ± 0.29stat0.692.63 ± 0.14stat3.39/4
2007–20152.65 ± 0.14stat0.912.46 ± 0.06stat7.89/6
2007–2015a4.04 ± 0.22stat0.912.15 ± 0.06stat6.73/6

Note.Deabsorbed using the Franceschini et al. (2008) EBL model.

Table 2.

Spectral analysis of 1ES 2344+514 broken down into observation periods. The systematic errors on N0 and Γ are estimated to be 20 per cent and 0.20, respectively.

Power-law fit
Data setN0E0Γχ2/NDF
(×10−12 cm−2 s−1)(TeV)
2007–20083.19 ± 0.23stat1.112.43 ± 0.09stat4.03/5
2008–20153.42 ± 0.29stat0.692.63 ± 0.14stat3.39/4
2007–20152.65 ± 0.14stat0.912.46 ± 0.06stat7.89/6
2007–2015a4.04 ± 0.22stat0.912.15 ± 0.06stat6.73/6
Power-law fit
Data setN0E0Γχ2/NDF
(×10−12 cm−2 s−1)(TeV)
2007–20083.19 ± 0.23stat1.112.43 ± 0.09stat4.03/5
2008–20153.42 ± 0.29stat0.692.63 ± 0.14stat3.39/4
2007–20152.65 ± 0.14stat0.912.46 ± 0.06stat7.89/6
2007–2015a4.04 ± 0.22stat0.912.15 ± 0.06stat6.73/6

Note.Deabsorbed using the Franceschini et al. (2008) EBL model.

The systematic errors quoted are the standard VERITAS errors of 20 per cent on the flux normalization and 0.20 on the index for a power-law function (Madhavan 2013). The 2007–2008 data set is found to be in good agreement with the previously published spectrum, when statistical and systematic uncertainties are considered.

The spectral points for the combined 2007–2015 data set, excluding the flare night of MJD 54441, along with the best-fit power law and the 95 per cent confidence interval (statistical errors only) on the fit, are shown in Fig. 2. Points are shown when the significance exceeds 2σ in a bin and there are at least five ‘on’ events, otherwise upper limits are presented. We extrapolate the confidence interval obtained from the best-fit function out to the final energy bin (between 8 and 13 TeV) and find agreement between the model and upper limit.

The differential energy spectrum of 1ES 2344+514 fitted with a power law with a 95 per cent statistical confidence band plotted as a shaded region. The deabsorbed energy spectrum is obtained using the Franceschini et al. (2008) EBL model. Details of the fits can be found in Table 2. Points failing to meet a threshold significance of 2σ or with less than 5 ‘on’ events are plotted as upper limits and are not included in the fit.
Figure 2.

The differential energy spectrum of 1ES 2344+514 fitted with a power law with a 95 per cent statistical confidence band plotted as a shaded region. The deabsorbed energy spectrum is obtained using the Franceschini et al. (2008) EBL model. Details of the fits can be found in Table 2. Points failing to meet a threshold significance of 2σ or with less than 5 ‘on’ events are plotted as upper limits and are not included in the fit.

To investigate the intrinsic spectrum of the source, we deabsorbed the observed 2007–2015 spectrum using the EBL model of Franceschini, Rodighiero & Vaccari (2008). This deabsorbed spectrum is then fitted with a power-law function (see Table 2) and a power law with an exponential cut-off function of the form
\begin{equation*} \frac{{\rm d}N}{{\rm d}E} = N_0 \left(\frac{E}{E_0}\right)^{-\Gamma } \text{e}^{-\frac{E}{E_{\text{c}}} }, \end{equation*}
where Ec is the cut-off energy. The power law with an exponential cut-off is well fitted with a χ2/NDF = 2.56/5 and parameters N0 = (5.19 ± 1.99stat) × 10−13 cm−2 s−1, Γ = 1.82 ± 0.19stat, E0 = 3.3 TeV and Ec = 4.38 ± 2.42stat TeV. To test whether the power law with an exponential cut-off model provides a significantly improved fit, we apply a nested F-test, which results in an F-statistic of 8.13, corresponding to a 2.1σ improvement over the power-law model.

5 DISCUSSION AND CONCLUSIONS

We have presented the results of VERITAS observations of 1ES 2344+514 using all good-weather data taken between 2007 and 2015, including data taken under moderate moonlight with a reduced high voltage supplied to the PMTs. This extended data set incorporates 30.1 additional hours of monitoring data beyond the 2007 data set already published by VERITAS in Acciari et al. (2011). 1ES 2344+514 is detected at greater than 20σ above background in the overall data set, with the mean 2008–2015 flux showing a significant (8.3σ) ∼70 per cent decrease from ∼13 per cent to ∼4 per cent of the Crab nebula flux. There is evidence for flux variability from season to season, and within seasons, but no new significant flaring activity was observed. The observations, when combined with other VHE observations, indicate that there is not a steady baseline flux level for the VHE emission from this object. The observed flickering variability is not uncommon for BL Lac objects and indicates that the VHE emission is not from a large-scale structure within the galaxy, but instead from a compact region most probably within the jet, with variability possibly caused by turbulence in the jet or variations in the electron supply (see for e.g. Howard et al. 2004).

The first study of the location and extension of the VHE γ-ray emission with VERITAS of 1ES 2344+514 was conducted. The best-fit coordinates (J2000) were found to be

 RA: (23h 47΄ 4) ± (0 h 0΄ 2 )stat ± (0 h 0΄ 3 )sys,

 Dec.: (+51° 42΄ 49) ± (0° 0΄ 16 )stat ± (0° 0΄ 25 )sys.

The location of the source is consistent with the radio location of RA: 23h 47΄ 04.837, Dec.: +51° 42΄ 17.881 (J2000), reported by Petrov et al. (2008), when the statistical and systematic errors are taken into account. The fitted extension is consistent with a point source convolved with the point-spread function of VERITAS, revealing no evidence for extended halo-type emission that might be expected from magnetically broadened cascades. A recent dedicated VERITAS analysis of the spatial extents of other BL Lac objects also found no evidence for extended emission (Archambault et al. 2017b), so this result on 1ES 2344+514 is not unexpected.

The observed time-averaged spectrum is best fitted by a power law with an index of Γ = 2.46 ± 0.06stat ± 0.20sys. The spectrum extends to at least 8 TeV and is approaching a region where absorption due to the EBL is starting to become significant (the optical depth for 8 TeV photons due to EBL absorption is 1.3 for a source at a redshift of z = 0.044 according to the Franceschini et al. (2008) model). The EBL-deabsorbed spectrum was fitted with both a power law and a power law with an exponential cut-off; the power law gave a satisfactory fit (χ2/NDF of 6.73/6) with a spectral index of Γ = 2.15 ± 0.06stat ± 0.20sys, while the power law with an exponential cut-off yielded only a marginal (2.1σ) improvement to the fit. The lack of significant evidence for the curvature in the VHE spectrum, coupled with the observed ‘harder when brighter’ behaviour some HBLs have displayed, makes future flaring activity for this source of great interest due to the hard deabsorbed spectral index. The spectral index obtained indicates that the higher-energy peak of the broad-band SED (i.e. the inverse-Compton component) is near or below the lowest energy VERITAS point at 200 GeV.

While only marginal evidence is seen in the VERITAS data, curvature or a cut-off is expected to occur at some point in the intrinsic VHE spectrum of a BL Lac object if the emission is produced by the inverse-Compton mechanism. In one-zone SSC models, a single population of relativistic electrons with a spectrum that softens with increasing energy is utilized to produce a synchrotron spectrum that matches the observed optical–X-ray SED. Commonly, this electron distribution is described by a broken power law between Lorentz factors γmin and γmax with a break at γb (e.g. Katarzyński, Sol & Kus 2001). This is in turn Doppler boosted by a factor δ/(1 + z), where δ = γ−1(1 − βcos θ) and β is the relativistic velocity, to higher frequencies in the frame of the observer by the bulk relativistic motion of the jet. The resulting synchrotron spectrum follows power laws for corresponding frequencies between γmin and γb and between γb and γmax, with the latter power-law index being softer to account for the cooling and escape of the electrons. The frequency range of the synchrotron radiation produced depends on the strength of the magnetic field and γ (the synchrotron critical frequency for a single electron νch ∝ γ2B), but decreases sharply beyond that corresponding to γmax, hence terminating the synchrotron spectrum. Typically, the electrons boost, via the inverse-Compton mechanism, the energy of the synchrotron photons they produced by a factor of γ2, with the interaction rate governed approximately by the Thomson cross-section. For combinations of large-electron Lorentz factors and high target synchrotron photon frequencies, the energies of the synchrotron photons in the electron rest frame may be comparable to the electron rest mass. This limits the boost in energy to γm0c2 and the Klein–Nishina cross-section applies, which results in a decreased interaction rate and a softening of the inverse-Compton spectrum at the highest energies. Thus, there are a variety of combinations of electrons and soft photon energies that could produce the VHE emission and result in a particular spectral shape over the range in which we have measured it. It is difficult to constrain the models from observations in one band alone, and constraints on the model parameter space require contemporaneous measurements of both the synchrotron and inverse-Compton components and any associated time lags between variability in the different emission bands. While many models involve numerical calculations, analytic approaches for constraining parameters can be found in, for example, Tavecchio, Maraschi & Ghisellini (1998).

VERITAS will continue to monitor 1ES 2344+514 as part of the blazar science working group's long-term plan over the coming years and will provide and respond to alerts should flaring activity occur. In the absence of flaring activity, continued observations will increase the photon statistics available to extend the spectrum to higher energies to allow for models of the emission of BL Lac objects in quiescent states to be constrained, and will allow further studies of the characteristics and implications of its temporal, spatial and spectral properties to be conducted.

Being one of the first VHE-detected blazars, 1ES 2344+514 receives significant multiwavelength monitoring from instruments across the electromagnetic spectrum. The VERITAS data presented here represent the most comprehensive VHE study of this object to date. The VERITAS observations have significant contemporaneous optical (e.g. Tuorla2) and Swift XRT X-ray (>144 exposures since September 20073, many of which taken simultaneously with VERITAS) data available, in addition to the almost-continuous Fermi-LAT coverage. The combining of these data sets, along with others from additional instruments, can prove useful for understanding the underlying processes in 1ES 2344+514, and HBLs in general, and is encouraged.

Acknowledgments

This research is supported by grants from the U.S. Department of Energy Office of Science, the U.S. National Science Foundation and the Smithsonian Institution, and by NSERC in Canada. We acknowledge the excellent work of the technical support staff at the Fred Lawrence Whipple Observatory and at the collaborating institutions in the construction and operation of the instrument. S. O'Brien is funded by a UCD Research Scholarship. The VERITAS Collaboration is grateful to Trevor Weekes for his seminal contributions and leadership in the field of VHE gamma-ray astrophysics, which made this study possible.

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