Introduction
γ-ray bursts (GRBs) are a phenomenon in which gamma rays from the depths of the universe suddenly increase on a short-time scale; they are the most violent explosion phenomenon after the Big Bang. Theoretically, the prompt emission of the GRB is generated by the energy dissipation process inside the relativistic jet, whereas the multi-band afterglow emission is generated by the external shock caused by the collision between the relativistic jet and the external medium. Therefore, gamma bursts are used to study the emergence of compact celestial bodies (black holes with constant star mass and neutron stars), gravitational wave radiation, relativistic shock waves, extremely high-energy cosmic rays, high-energy neutrinos, and other extreme objects in astronomical laboratories for scientific phenomena and high-precision testing of basic physical principles; they are also important probes for early universe star formation and evolution, high-redshift galaxies, and high-redshift cosmology.
The first γ-ray burst (GRB) was discovered by the Vela U.S. military satellites in 1967 and was recognized early as being of extrasolar origin [1]. A bimodal structure (first reported in [2]) in the duration distribution of GRBs was detected by the Burst and Transient Source Experiment (BATSE) onboard the Compton Gamma Ray Observatory (CGRO) [3], based on which GRBs are currently commonly classified as short (with a duration T90 < 2 s, SGRBs) and long (with T90 > 2 s, LGRBs) [4]. BATSE observations have also confirmed that GRBs have an isotropic angular distribution in the sky [3, 5-8]. GRB970508, with 0.835 < z ≤ 2.3, was placed at a cosmological distance of at least 2.9 Gpc, which was later corroborated by the first redshift measurement [9]. Subsequently, the progenitors of LGRBs were associated with supernovae (SNe) [10-14] related to the collapse of massive stars. The first direct detection of gravitational waves (GWs) by the Laser-Interferometer Gravitational-Wave Observatory, termed GW150914, was interpreted as a merger of two stellar-mass black holes (BHs) with masses and was, by itself, a discovery of prime importance [15]. It became especially interesting in light of the discovery of a weak transient source lasting 1 s in [16] and detected by Fermi/GBM [17] only 0.4 s after the GW150914 (termed GW150914-GBM). The highest-energy GRB photon ever recorded by Fermi-LAT thus far had been emitted by GRB 130427A in the early afterglow phase and had an energy of 95 GeV (128 GeV in the rest frame during a redshift z=0.34) [18]. While LAT-detected GRBs commonly exhibit photon energies of a few hundred MeV, higher energies are relatively rare. Although satellite experiments have provided a vast number of exciting results, they are limited by their effective areas and have difficulty detecting higher-energy photons in the prompt emissions of GRBs.
Recently, sub-TeV energy γ rays were successfully observed by the Major Atmospheric Gamma Imaging Cherenkov (MAGIC) and High Energy Stereoscopic System (H.E.S.S.) telescopes approximately 1 min after the GRB 190114C burst and 10 h after the end of the prompt-emission phase of GRB 180720B [19, 20, 21]. These events were unique, as researchers were able to observe them for the first time in afterglow emission photons with sub-TeV energies. Soon thereafter, the H.E.S.S. collaboration announced the detection of photons with energies up to 4 TeV high from GRB 190829A between 4 h and 56 h after the trigger [22]. Additionally, MAGIC reported the detection of hundreds of GeV γ-ray emissions from GRB 201216C in the afterglow phase [23]. Along with GRB 160821B and GRB 201015A, from which over 100 GeV of emissions at the ≤ 3σ level have been reported [24, 25], six GRBs have been reported with VHE afterglow emissions. Imaging atmospheric Cherenkov telescopes (IACTs) have been making great progress in the observations of VHE emissions in the afterglow phase. However, it is challenging for IACTs to perform conduct prompt-phase observation. They have a narrow field of view (FoV) and need to slew because a GRB does not typically enter their FoV within the first seconds of the prompt phase occurring, even if they have larger effective areas (unless the GRB occurs in their FoV, which has a very small probability).
Traditional extended air shower (EAS) experiments, for example, the High-Altitude Water Cherenkov Observatory [26] and the Large High Altitude Air Shower Observatory [27], which have wide FoVs, high duty cycles, and large effective areas, have not yet detected GRBs. In general, the energy thresholds of the EAS experiments are also higher than those of the IACT experiments.
The detection of high-energy photons in the prompt phase of the GRB is conducive to understanding the acceleration mechanisms and energetics because it constrains the progenitors, jet feeding mechanism, and extragalactic background light (EBL)-induced absorption of high-energy photons, which limits the Lorentz invariance violation (LIV). Therefore, it is important to search for prompt VHE emissions from GRBs using ground-based instruments that can achieve excellent sensitivity and a low-energy threshold over a wide FoV. The high-altitude detection of astronomical radiation (HADAR) experiment is a new observation instrument that uses a large-dimensional refractive water lens as a light collector to observe Cherenkov light induced by VHE cosmic rays (CRs) and γ rays in the atmosphere. In 2016, a prototype experiment was conducted and was successfully operated at the Yangbajing Observatory (4300 m above sea level, 90.522° E, 30.102°N, 606 g/cm2) in Tibet, China. Cosmic rays were successfully detected. More detailed information is available in [28, 29].
However, the bottleneck in wide-FoV Cherenkov technology is caused by the high rate of night-sky background (NSB) noise from random stars overwhelming the Cherenkov light signal from a GRB. Consequently, images of air showers recorded by telescopes are indistinguishable, and the fitting of a Hillas ellipse with the fired photomultiplier tubes (PMTs) on the camera, a critical step in event reconstruction, cannot be precisely performed. In this study, we propose a novel method that considers the spatial properties of GRBs and the temporal characteristics of Cherenkov radiation to reject NSB noise.
The remainder of this paper is organized as follows. Section 2 describes the HADAR experiment in detail. Section 3 presents a novel trigger method for wide-view IACT experiments, and Sect. 4 includes the results of the novel trigger method. Section 5 presents the conclusions of the study.
Imaging Atmospheric Cherenkov Technique and the HADAR Experiment
Imaging Atmospheric Cherenkov Technique (IACT)
Cherenkov radiation is produced when an energetically charged particle moves through a dielectric medium at a velocity higher than the speed of light. The electric field of the particle polarizes the adjacent molecules in the medium. Once the particle has passed, the molecules return to their original dipole configuration by releasing a brief pulse of continuum electromagnetic radiation that peaks at the UV and blue wavelengths.
The radiation fans out in the shape of a cone along the direction of the particle's path. The emission of molecules in the wake of the particle interferes constructively via the Huygens-Fresnel principle. The opening angle of this cone for a medium with refractive index n is given by
The change in the refractive index n as a function of atmospheric depth means that the light pool at the ground level takes the shape of a flattened disk or pancake. When a γ-ray above 1.022 MeV (2Mec2) interacts with the nucleus of an oxygen or nitrogen atom in the upper atmosphere, it spontaneously produces electron-positron pairs. Conservation of momentum dictates that these particles travel close to the incident direction of the γ-ray at nearly the speed of light, thereby producing Cherenkov radiation in their wake above the threshold energy. γ rays are not the only sources of particle showers in the atmosphere. Cosmic rays that pass through the atmosphere also induce extensive air showers (EASs).
The method for imaging Cherenkov radiation in the atmosphere consists of a large optical collection dish comprising tessellated mirror facets focused onto a multi-pixel camera box. The pixels contain PMTs that can register single photons with a time resolution comparable to that of Cherenkov flash (a few nanoseconds). The PMTs and their associated back-end electronics record images of the air shower as a signal above the ambient night-sky background in real time as it progresses; when the radiation reaches the ground, its intensity is quite faint, only 100 photons/m2 originating from a 1 TeV γ ray; therefore, multiple imaging atmospheric Cherenkov telescopes (IACTs) are often evenly distributed around a site to maximize the effective area of the array.
HADAR experiment
The HADAR instrument was configured with four water-lens telescopes that employed the imaging atmospheric Cherenkov technique, whose main task is to measure Cherenkov light induced by 10 GeV to 100 TeV CRs and γ rays in the atmosphere. The four water-lens telescopes were square-shaped with a side length of 100 m. The side length was selected because the Cherenkov light pool generally has a radius of approximately 125 m [30]. To perform joint observations, plastic scintillation detectors of the Yangbajing hybrid array were added to the telescope system. A water-lens telescope consists mainly of an acrylic spherical cap lens with a diameter of 5 m, a cylindrical tank with a radius of 4 m and a height of 7 m, and a camera with an array of 18961 PMTs with 5 cm diameters. The steel tank, containing an absorption layer in the inside wall and a thermal insulation material coated on the outer wall, is filled with purified water to reflect radiation emissions to the PMTs. The PMTs are placed in the focal plane of the lens and arranged as a series of concentric ring matrices supported by a stainless steel space frame. The details of the profile structure of a water-lens telescope and the instrument layout can be found in [31].
Focal length (FL) is one of the most important parameters of a lens. The value of the FL measured by ZEMAX was Fexp = 690 ± 1.5 cm [32]. The parameters used in the ZEMAX simulation were the same as the geometric parameters of the lens. Thus, the focal ratio N = F/Φ = 1.38. As a pathfinder experiment, the HADAR was designed to explore the processing technique of a wide FoV water lens. Hence, we chose a commercial material, acrylic, as the shell of the prototype water lens instead of high-UV-transparent materials. The absorption of acrylic and purified water can be ignored in the water-lens optical system at wavelengths between 400 nm and 500 nm. Because the camera did not occlude the lens, the telescope could obtain a wide FoV for observation. The camera was designed on a curved surface to ensure that the light incident at a large angle could be clearly focused. The light parallel to the main optical axis of the telescope at 0-30° was well focused.
trigger algorithm
GRB jets are usually unresolved and are viewed as point sources by instruments that are observational rather than intrinsic. This is because of their intrinsically small size, especially at early times, and their cosmological distances, which result in very small angular sizes [33]. Therefore, the GRB signal exhibits spatial characteristics. The main high-rate noise is NSB noise, which is emitted from random stars because IACTs can only make observations on clear and moonless nights. In contrast, NSB is isotropic and has no spatial characteristics.
Generally, H.E.S.S. or MAGIC telescopes are equipped with a large optical reflecting dish. These telescopes must rotate with the gamma source when they make scientific observations because they have a narrow FoV. However, owing to the small FoV, the night sky background noise received by the mirror is significantly lesser. After a simple cut on pixels (e.g., image cleaning), a clearer Cherenkov image caused by CR or γ rays can be obtained on the camera. However, this trigger method cannot be directly applied to experiments with a wide FoV, such as the HADAR. Because HADAR telescopes have a wide FoV, this introduces a significant amount of NSB noise. The challenge for the HADAR experiment is determining how to reject the high rate of NSB noise from random stars. For high-energy events, the effect of the NSB noise can be ignored because high-energy events generate many Cherenkov photons. The signal is not overwhelmed by the noise. However, low-energy events do not generate as many photons as high-energy events. It is difficult to distinguish which PMTs have been triggered by noise, and which have been triggered by Cherenkov photons. Clear images cannot be obtained. Therefore, to make better scientific observations using HADAR, we improved the trigger method.
As shown in Fig. 1, on a clear and moonless night, a GRB appeared at δ(i,j) on the celestial sphere, which was in the FoV of the HADAR experiment. High-energy γ rays from the GRB entered and interacted with the Earth's atmosphere. They produced a large number of electron–positron pairs with enormous velocities. When electron–positron pairs travel faster than light in the Earth's atmosphere, their passage causes a brief flash of light: Cherenkov light. The photons from the Cherenkov radiation were collected by the lens and focused on by the camera (this was the signal of interest). Simultaneously, the photons from the random stars also entered the lens and were recorded by the camera (this was the main noise). At low energy, the crucial signals from the GRB were submerged by NSB noise.
-202203/1001-8042-33-03-003/alternativeImage/1001-8042-33-03-003-F001.jpg)
The trigger algorithm used by HADAR was as follows: (1) one PMT was fired if ≥ 9 photoelectrons were collected by the PMT within the time window; (2) if the number of adjacent triggered PMTs on the camera was n ≥ 3, a telescope was considered to be triggered; (3) an event was recorded if ≥ 2 telescopes were triggered in a time window of 20 ns (to reconstruct the event); (4) a 10 × 10 PMT matrix was selected from the camera with adjacent triggered PMTs as the center. Subsequently, all fired PMTs in the matrix were used to fit the Hillas ellipse (a key step for event reconstruction). The area enclosed by the ellipse is denoted as δ′ (i′,j′). Other PMTs outside the matrix were masked to reduce the trigger rate of the NSB noise. As previously mentioned, GRBs have distinct spatial properties. Therefore, to perform detection even at low energies, a map between δ (i,j), the position of the GRB on the celestial sphere, and δ′ (i′,j′), where the signals were large and concentrated on the camera, could be constructed as follows:
Because the atmospheric index of refraction was very close to 1, the Cherenkov light almost kept pace with radiating charged particles. Near the edge of the "light pool", most of the light from the γ ray shower arrived within 2 ns. Thus, a very short temporal window was possible, allowing for suppression of the dominant NSB. The number of background photons is given as follows:
Result
After applying the new trigger method, the NSB was suppressed and the angular resolution and effective area were significantly improved.
In Fig. 2, the black line represents the time distribution of all photons (including NSB and Cherenkov photons) received by all PMTs. The NSB overwhelmed the Cherenkov signals of interest. After selecting the area δ′ (i′,j′) with the strongest signal on the camera (blue line), the NSB was suppressed, and the Cherenkov signal was well preserved compared to the case that only included Cherenkov signals (red line).
-202203/1001-8042-33-03-003/alternativeImage/1001-8042-33-03-003-F002.jpg)
In addition, the angular resolution was improved and the effective area increased. Fitting a Hillas ellipse is a critical step for event reconstruction in IACTs. However, while applying all PMTs of one camera, it becomes a challenge to fit a Hillas ellipse with fired PMTs because many of them are fired by the NSB. This results in a significant difference between the reconstructed and real directions. Therefore, the angular resolution was > 1° at E< 200 GeV, as indicated by the black line in Fig. 3, when applying all PMTs of one camera. As the energy increased, the angular resolution gradually approached < 1°. This was because the Cherenkov signals became stronger and were no longer submerged by the NSB. The angular resolution improved considerably after selecting δ′ (i′,j′) on the camera, as indicated by the red line. After selection, the fired PMTs could be fitted by a qualified ellipse that contained the essential parameters for event reconstruction at low energy. Furthermore, the angular resolution of the high-energy event was also improved. In contrast to the blue line, which corresponds to the case with only Cherenkov photons, the red line indicates that the NSB has a certain influence on the event reconstruction.
-202203/1001-8042-33-03-003/alternativeImage/1001-8042-33-03-003-F003.jpg)
Figure 4 shows the effective area of the HADAR experiment. The simulated area was 800 × 800 m2. The black line was the effective area before PMT selection. At E < 200 GeV, almost every event triggered the telescope array because the NSB was introduced heavily, resulting in many PMTs being fired. After PMT selection, because the NSB was suppressed and Cherenkov photons were lower in low energy, the probability of event triggering the telescope array became lower, which was almost the same as the case with only Cherenkov photons, as shown by the red and blue lines. Aside from the angular resolution, when E > 300 GeV, the effective area was almost the same in the three cases.
-202203/1001-8042-33-03-003/alternativeImage/1001-8042-33-03-003-F004.jpg)
Conclusion
Unlike the afterglow theory, which is relatively simple and well-tested by data, the GRB prompt-emission theory is much more complicated. Thus, more experimental data are required for prompt GRB emissions. The HADAR experiment provides an effective solution for detecting GRB prompt emissions on the ground. Unlike satellite experiments with small effective areas and traditional IACTs with narrow FoVs, the HADAR experiment has a large effective area and wide FoV. The wide FoV allows telescopes to cover a larger area of the celestial sphere and observe GRBs without slewing. However, a wide FoV introduces considerable noise from the NSB, making it difficult to observe low-energy events.
To solve this problem, the GRB's spatial properties and temporal structure of atmospheric Cherenkov radiation were fully utilized. At the coordinates δ′ (i′,j′), a stronger and concentrated signal on the camera was selected and mapped to δ (i,j), the position of the GRB on the celestial sphere. To fully record the Cherenkov signal while introducing as little noise as possible, a 20-ns integration temporal window was selected. After applying the new trigger method, the angular resolution of low-energy events significantly improved, and the angular resolution was < 1° at 10 GeV. Moreover, the trigger rate of the telescope array was significantly reduced at low energy because the NSB noise was suppressed. This method can be used in all the wide-FoV IACT experiments. As the angular resolution and effective area of HADAR have improved, HADAR’s capacity to observe GRBs increases the detection rate to at least one GRB per year. We hope that future experimental observations can confirm the progress of physics in the prompt phase and relevant parameters.
Observation of gamma-ray bursts of cosmic origin
. Astrophys. J. 182, 85-88 (1973). doi: 10.1086/181225Catalog of cosmic gamma-ray bursts from the KONUS experiment data—parts I and II
. Astrophys. Space Sci. 80, 3-83 (1981). doi: 10.1007/BF00649140Spatial distribution of gamma-ray bursts observed by BATSE
. Nature 355,143-145 (1992). doi: 10.1038/355143a0Identification of two classes of gamma-ray bursts
, Astrophys. J. 413, 101-104 (1993). doi: 10.1086/186969A test of the galactic origin of gamma-ray bursts
. Astrophys. J. 348, 485-494 (1990). doi: 10.1086/168257Cosmological gamma-ray bursts
. Acta Astron. 41, 257-267, (1991).γ-ray bursts
. Annu. Rev. Astron. Astrophys. 33, 415-458 (1995). doi: 10.1146/annurev.aa.33.090195.002215BATSE observations of the large-scale isotropy of gamma-ray bursts
. Astrophys. J. 459, 40 (1996). doi: 10.1086/176867Spectral constraints on the redshift of the optical counterpart to the γ-ray burst of 8 May 1997
. Nature 387, 878-880 (1997). doi: 10.1038/43132A very energetic supernova associated with the γ-ray burst of 29 March 2003
. Nature 423, 847-850, (2003). doi: 10.1038/nature01750SN 2003lw and GRB 031203: a bright supernova for a faint gamma-ray burst
. Astrophys. J. 609, L5-L8, (2004). doi: 10.1086/422684The supernova-gamma-ray burst connection
. Annu. Rev. Astron. Astrophys. 44, 507-556, (2006). doi: 10.1146/annurev.astro.43.072103.150558Spectroscopic evidence for SN 2010ma associated with GRB 101219B
. Astrophys. J. Lett. 735, L24 (2011). doi: 10.1088/2041-8205/735/1/L24GRB 120422A/SN 2012bz: bridging the gap between low- and high-luminosity gamma-ray bursts
. Astron. Astrophys. 566, A102 (2014). doi: 10.1051/0004-6361/201423387Observation of gravitational waves from a binary black hole merger
. Phys. Rev. Lett. 116, 061102 (2016). doi: 10.1103/PhysRevLett.116.061102Fermi GBM observations of ligo gravitational-wave event GW150914
, Astrophys. J. Lett. 826, L6 (2016). doi: 10.3847/2041-8205/826/1/L6The third fermi GBM gamma-ray burst catalog: the first six years
. Astrophys. J. Suppl. Ser. 223, 28 (2016). doi: 10.3847/0067-0049/223/2/28Fermi-LAT Observations of the Gamma-Ray Burst GRB 130427A
. Science 343, 42-47 (2014). doi: 10.1126/science.1242353Observation of inverse Compton emission from a long γ-ray burst
. Nature 575, 459-463 (2019). doi: 10.1038/s41586-019-1754-6Teraelectronvolt emission from the γ-ray burst GRB 190114C
. Nature 575, 455-458 (2019). doi: 10.1038/s41586-019-1750-xA very-high-energy component deep in the gamma-ray burst afterglow
. Nature 575, 464-467 (2019). doi: 10.1038/s41586-019-1743-9Revealing x-ray and gamma ray temporal and spectral similarities in the GRB 190829A afterglow
. Science 372, 1081-1085 (2021). doi: 10.1126/science.abe8560GRB 201216C: Fermi GBM detection
. GRB Coordinates Network, Circular Service, No. 29073 (2020)MAGIC observations of the nearby short gamma-ray burst GRB 160821B
. Astrophys. J. 908, 90 (2021). doi: 10.3847/1538-4357/abd249.MAGIC observations of GRB 201015A: hint of very high energy gamma-ray signal
. GRB Coordinates Network, No. 28659 (2020)The high altitude water Cherenkov (HAWC) observatory
. Nucl. Part. Phys. Proc. 279-281, 87-94 (2016) doi: 10.1016/j.nuclphysbps.2016.10.013.The large high altitude air shower observation
. (2019). arXiv:1905.02773Wide field-of-view atmospheric Cherenkov telescope based on refractive lens
. J. Instrum. 12, P09023 (2017). doi: 10.1088/1748-0221/12/09/p09023.Performance of a wide field-of-view atmospheric Cherenkov telescope prototype based on a refractive lens
. Nucl. Instrum. Methods. Phys. Res. A, 927, 46-53 (2019). doi: 10.1016/j.nima.2019.02.020.Imaging very high energy gamma-ray telescopes
. Exp. Astron. 25, 173-191 (2019). doi: 10.1007/s10686-009-9151-z.Prospects of γ-ray bursts detecting at very high energy with the High Altitude Detection of Astronomical Radiation experiment
. https://doi.org/10.3847/1538-4357/ac2df7ZEMAX homepage
, https://www.zemax.com.Gamma-ray burst jets and their radio observations
. Publications of the Astronomical Society of Australia,31, E008 (2014). doi: 10.1017/pasa.2013.44