In gamma-ray astronomy, gamma-ray bursts (GRBs) are extremely energetic explosions that have been observed in distant galaxies. They are the brightest electromagnetic events known to occur in the universe. Bursts can last from ten milliseconds to several hours. After an initial flash of gamma rays, a longer-lived "afterglow" is usually emitted at longer wavelengths (X-ray, ultraviolet, optical, infrared, microwave and radio).
The intense radiation of most observed GRBs is thought to be released during a supernova or superluminous supernova as a high-mass star implodes to form a neutron star or a black hole.
A subclass of GRBs (the "short" bursts) appear to originate from the merger of binary neutron stars.
The cause of the precursor burst observed in some of these short events
may be the development of a resonance between the crust and core of
such stars as a result of the massive tidal forces experienced in the
seconds leading up to their collision, causing the entire crust of the
star to shatter.
The sources of most GRBs are billions of light years away from Earth, implying that the explosions are both extremely energetic (a typical burst releases as much energy in a few seconds as the Sun will in its entire 10-billion-year lifetime) and extremely rare (a few per galaxy per million years). All observed GRBs have originated from outside the Milky Way galaxy, although a related class of phenomena, soft gamma repeater flares, are associated with magnetars
within the Milky Way. It has been hypothesized that a gamma-ray burst
in the Milky Way, pointing directly towards the Earth, could cause a mass extinction event.
GRBs were first detected in 1967 by the Vela satellites, which had been designed to detect covert nuclear weapons tests; this was declassified and published in 1973. Following their discovery, hundreds of theoretical models were proposed to explain these bursts, such as collisions between comets and neutron stars.
Little information was available to verify these models until the 1997
detection of the first X-ray and optical afterglows and direct
measurement of their redshifts using optical spectroscopy, and thus their distances and energy outputs. These discoveries, and subsequent studies of the galaxies and supernovae associated with the bursts, clarified the distance and luminosity of GRBs, definitively placing them in distant galaxies.
History
Gamma-ray bursts were first observed in the late 1960s by the U.S. Vela satellites, which were built to detect gamma radiation pulses emitted by nuclear weapons tested in space. The United States suspected that the Soviet Union might attempt to conduct secret nuclear tests after signing the Nuclear Test Ban Treaty in 1963. On July 2, 1967, at 14:19 UTC, the Vela 4 and Vela 3 satellites detected a flash of gamma radiation unlike any known nuclear weapons signature. Uncertain what had happened but not considering the matter particularly urgent, the team at the Los Alamos National Laboratory, led by Ray Klebesadel,
filed the data away for investigation. As additional Vela satellites
were launched with better instruments, the Los Alamos team continued to
find inexplicable gamma-ray bursts in their data. By analyzing the
different arrival times of the bursts as detected by different
satellites, the team was able to determine rough estimates for the sky positions of sixteen bursts and definitively rule out a terrestrial or solar origin. The discovery was declassified and published in 1973.
Most early theories of gamma-ray bursts posited nearby sources within the Milky Way Galaxy. From 1991, the Compton Gamma Ray Observatory (CGRO) and its Burst and Transient Source Explorer (BATSE) instrument, an extremely sensitive gamma-ray detector, provided data that showed the distribution of GRBs is isotropic—not biased towards any particular direction in space.
If the sources were from within our own galaxy they would be strongly
concentrated in or near the galactic plane. The absence of any such
pattern in the case of GRBs provided strong evidence that gamma-ray
bursts must come from beyond the Milky Way. However, some Milky Way models are still consistent with an isotropic distribution.
In October 2018, astronomers reported that GRB 150101B, a
gamma-ray burst event detected in 2015, may be directly related to the
historic GW170817, a gravitational wave event detected in 2017, and associated with the merger of two neutron stars. The similarities between the two events, in terms of gamma ray, optical and x-ray emissions, as well as to the nature of the associated host galaxies, are "striking", suggesting the two separate events may both be the result of the merger of neutron stars, and both may be a kilonova, which may be more common in the universe than previously understood, according to the researchers.
In November 2019, astronomers reported a notable gamma ray burst explosion, named GRB 190114C, initially detected in January 2019, that, so far, has been determined to have had the highest energy, 1 Tera electron volts (Tev), ever observed for such a cosmic event.
Counterpart objects as candidate sources
For
decades after the discovery of GRBs, astronomers searched for a
counterpart at other wavelengths: i.e., any astronomical object in
positional coincidence with a recently observed burst. Astronomers
considered many distinct classes of objects, including white dwarfs, pulsars, supernovae, globular clusters, quasars, Seyfert galaxies, and BL Lac objects. All such searches were unsuccessful,
and in a few cases particularly well-localized bursts (those whose
positions were determined with what was then a high degree of accuracy)
could be clearly shown to have no bright objects of any nature
consistent with the position derived from the detecting satellites. This
suggested an origin of either very faint stars or extremely distant
galaxies.
Even the most accurate positions contained numerous faint stars and
galaxies, and it was widely agreed that final resolution of the origins
of cosmic gamma-ray bursts would require both new satellites and faster
communication.
Afterglow
Several models for the origin of gamma-ray bursts postulated that the
initial burst of gamma rays should be followed by slowly fading
emission at longer wavelengths created by collisions between the burst ejecta and interstellar gas.
This fading emission would be called the "afterglow". Early searches
for this afterglow were unsuccessful, largely because it is difficult to
observe a burst's position at longer wavelengths immediately after the
initial burst. The breakthrough came in February 1997 when the satellite
BeppoSAX detected a gamma-ray burst (GRB 970228)
and when the X-ray camera was pointed towards the direction from which
the burst had originated, it detected fading X-ray emission. The William Herschel Telescope identified a fading optical counterpart 20 hours after the burst.[30]
Once the GRB faded, deep imaging was able to identify a faint, distant
host galaxy at the location of the GRB as pinpointed by the optical
afterglow.
Because of the very faint luminosity of this galaxy, its exact
distance was not measured for several years. Well after then, another
major breakthrough occurred with the next event registered by BeppoSAX, GRB 970508.
This event was localized within four hours of its discovery, allowing
research teams to begin making observations much sooner than any
previous burst. The spectrum of the object revealed a redshift of z = 0.835, placing the burst at a distance of roughly 6 billion light years from Earth.
This was the first accurate determination of the distance to a GRB, and
together with the discovery of the host galaxy of 970228 proved that
GRBs occur in extremely distant galaxies.
Within a few months, the controversy about the distance scale ended:
GRBs were extragalactic events originating within faint galaxies at
enormous distances. The following year, GRB 980425 was followed within a day by a bright supernova (SN 1998bw),
coincident in location, indicating a clear connection between GRBs and
the deaths of very massive stars. This burst provided the first strong
clue about the nature of the systems that produce GRBs.
BeppoSAX functioned until 2002 and CGRO
(with BATSE) was deorbited in 2000. However, the revolution in the
study of gamma-ray bursts motivated the development of a number of
additional instruments designed specifically to explore the nature of
GRBs, especially in the earliest moments following the explosion. The
first such mission, HETE-2,
was launched in 2000 and functioned until 2006, providing most of the
major discoveries during this period. One of the most successful space
missions to date, Swift, was launched in 2004 and as of 2018 is still operational.
Swift is equipped with a very sensitive gamma ray detector as well as
on-board X-ray and optical telescopes, which can be rapidly and
automatically slewed to observe afterglow emission following a burst. More recently, the Fermi mission was launched carrying the Gamma-Ray Burst Monitor,
which detects bursts at a rate of several hundred per year, some of
which are bright enough to be observed at extremely high energies with
Fermi's Large Area Telescope.
Meanwhile, on the ground, numerous optical telescopes have been built
or modified to incorporate robotic control software that responds
immediately to signals sent through the Gamma-ray Burst Coordinates Network.
This allows the telescopes to rapidly repoint towards a GRB, often
within seconds of receiving the signal and while the gamma-ray emission
itself is still ongoing.
New developments since the 2000s include the recognition of short
gamma-ray bursts as a separate class (likely from merging neutron stars
and not associated with supernovae), the discovery of extended, erratic
flaring activity at X-ray wavelengths lasting for many minutes after
most GRBs, and the discovery of the most luminous (GRB 080319B) and the former most distant (GRB 090423) objects in the universe. The most distant known GRB, GRB 090429B, is now the most distant known object in the universe.
Classification
The light curves of gamma-ray bursts are extremely diverse and complex. No two gamma-ray burst light curves are identical,
with large variation observed in almost every property: the duration of
observable emission can vary from milliseconds to tens of minutes,
there can be a single peak or several individual subpulses, and
individual peaks can be symmetric or with fast brightening and very slow
fading. Some bursts are preceded by a "precursor" event, a weak burst
that is then followed (after seconds to minutes of no emission at all)
by the much more intense "true" bursting episode. The light curves of some events have extremely chaotic and complicated profiles with almost no discernible patterns.
Although some light curves can be roughly reproduced using certain simplified models,
little progress has been made in understanding the full diversity
observed. Many classification schemes have been proposed, but these are
often based solely on differences in the appearance of light curves and
may not always reflect a true physical difference in the progenitors of
the explosions. However, plots of the distribution of the observed
duration for a large number of gamma-ray bursts show a clear bimodality,
suggesting the existence of two separate populations: a "short"
population with an average duration of about 0.3 seconds and a "long"
population with an average duration of about 30 seconds.
Both distributions are very broad with a significant overlap region in
which the identity of a given event is not clear from duration alone.
Additional classes beyond this two-tiered system have been proposed on
both observational and theoretical grounds.
Short gamma-ray bursts
Events with a duration of less than about two seconds are classified
as short gamma-ray bursts. These account for about 30% of gamma-ray
bursts, but until 2005, no afterglow had been successfully detected from
any short event and little was known about their origins.
Since then, several dozen short gamma-ray burst afterglows have been
detected and localized, several of which are associated with regions of
little or no star formation, such as large elliptical galaxies and the central regions oflarge galaxy clusters.
This rules out a link to massive stars, confirming that short events
are physically distinct from long events. In addition, there has been no
association with supernovae.
The true nature of these objects was initially unknown, and the
leading hypothesis was that they originated from the mergers of binary
neutron stars or a neutron star with a black hole. Such mergers were theorized to produce kilonovae, and evidence for a kilonova associated with GRB 130603B was seen. The mean duration of these events of 0.2 seconds suggests (because of causality)
a source of very small physical diameter in stellar terms; less than
0.2 light-seconds (about 60,000 km or 37,000 miles—four times the
Earth's diameter). The observation of minutes to hours of X-ray flashes
after a short gamma-ray burst is consistent with small particles of a
primary object like a neutron star initially swallowed by a black hole
in less than two seconds, followed by some hours of lesser energy
events, as remaining fragments of tidally disrupted neutron star
material (no longer neutronium) remain in orbit to spiral into the black hole, over a longer period of time. A small fraction of short gamma-ray bursts are probably produced by giant flares from soft gamma repeaters in nearby galaxies.
The origin of short GRBs in kilonovae was confirmed when short GRB 170817A was detected only 1.7 s after the detection of gravitational wave GW170817, which was a signal from the merger of two neutron stars.
Long gamma-ray bursts
Most
observed events (70%) have a duration of greater than two seconds and
are classified as long gamma-ray bursts. Because these events constitute
the majority of the population and because they tend to have the
brightest afterglows, they have been observed in much greater detail
than their short counterparts. Almost every well-studied long gamma-ray
burst has been linked to a galaxy with rapid star formation, and in many
cases to a core-collapse supernova as well, unambiguously associating long GRBs with the deaths of massive stars. Long GRB afterglow observations, at high redshift, are also consistent with the GRB having originated in star-forming regions.
Ultra-long gamma-ray bursts
These
events are at the tail end of the long GRB duration distribution,
lasting more than 10,000 seconds. They have been proposed to form a
separate class, caused by the collapse of a blue supergiant star, a tidal disruption event or a new-born magnetar.
Only a small number have been identified to date, their primary
characteristic being their gamma ray emission duration. The most studied
ultra-long events include GRB 101225A and GRB 111209A.
The low detection rate may be a result of low sensitivity of current
detectors to long-duration events, rather than a reflection of their
true frequency. A 2013 study,
on the other hand, shows that the existing evidence for a separate
ultra-long GRB population with a new type of progenitor is inconclusive,
and further multi-wavelength observations are needed to draw a firmer
conclusion.
Energetics and beaming
Gamma-ray bursts are very bright as observed from Earth despite their typically immense distances. An average long GRB has a bolometric
flux comparable to a bright star of our galaxy despite a distance of
billions of light years (compared to a few tens of light years for most
visible stars). Most of this energy is released in gamma rays, although
some GRBs have extremely luminous optical counterparts as well. GRB 080319B, for example, was accompanied by an optical counterpart that peaked at a visible magnitude of 5.8,
comparable to that of the dimmest naked-eye stars despite the burst's
distance of 7.5 billion light years. This combination of brightness and
distance implies an extremely energetic source. Assuming the gamma-ray
explosion to be spherical, the energy output of GRB 080319B would be
within a factor of two of the rest-mass energy of the Sun (the energy which would be released were the Sun to be converted entirely into radiation).
Gamma-ray bursts are thought to be highly focused explosions, with most of the explosion energy collimated into a narrow jet.
The approximate angular width of the jet (that is, the degree of spread
of the beam) can be estimated directly by observing the achromatic "jet
breaks" in afterglow light curves: a time after which the slowly
decaying afterglow begins to fade rapidly as the jet slows and can no
longer beam its radiation as effectively. Observations suggest significant variation in the jet angle from between 2 and 20 degrees.
Because their energy is strongly focused, the gamma rays emitted
by most bursts are expected to miss the Earth and never be detected.
When a gamma-ray burst is pointed towards Earth, the focusing of its
energy along a relatively narrow beam causes the burst to appear much
brighter than it would have been were its energy emitted spherically.
When this effect is taken into account, typical gamma-ray bursts are
observed to have a true energy release of about 1044 J, or about 1/2000 of a Solar mass (M☉) energy equivalent—which is still many times the mass-energy equivalent of the Earth (about 5.5 × 1041 J). This is comparable to the energy released in a bright type Ib/c supernova and within the range of theoretical models. Very bright supernovae have been observed to accompany several of the nearest GRBs.
Additional support for focusing of the output of GRBs has come from
observations of strong asymmetries in the spectra of nearby type Ic supernova and from radio observations taken long after bursts when their jets are no longer relativistic.
Short (time duration) GRBs appear to come from a lower-redshift
(i.e. less distant) population and are less luminous than long GRBs.
The degree of beaming in short bursts has not been accurately measured,
but as a population they are likely less collimated than long GRBs or possibly not collimated at all in some cases.
Progenitors
Because of the immense distances of most gamma-ray burst sources from
Earth, identification of the progenitors, the systems that produce
these explosions, is challenging. The association of some long GRBs with
supernovae and the fact that their host galaxies are rapidly
star-forming offer very strong evidence that long gamma-ray bursts are
associated with massive stars. The most widely accepted mechanism for
the origin of long-duration GRBs is the collapsar model, in which the core of an extremely massive, low-metallicity, rapidly rotating star collapses into a black hole in the final stages of its evolution. Matter near the star's core rains down towards the center and swirls into a high-density accretion disk. The infall of this material into a black hole drives a pair of relativistic jets
out along the rotational axis, which pummel through the stellar
envelope and eventually break through the stellar surface and radiate as
gamma rays. Some alternative models replace the black hole with a newly
formed magnetar,
although most other aspects of the model (the collapse of the core of a
massive star and the formation of relativistic jets) are the same.
The closest analogs within the Milky Way galaxy of the stars producing long gamma-ray bursts are likely the Wolf–Rayet stars, extremely hot and massive stars, which have shed most or all of their hydrogen to radiation pressure. Eta Carinae and WR 104 have been cited as possible future gamma-ray burst progenitors. It is unclear if any star in the Milky Way has the appropriate characteristics to produce a gamma-ray burst.
The massive-star model probably does not explain all types of
gamma-ray burst. There is strong evidence that some short-duration
gamma-ray bursts occur in systems with no star formation and no massive
stars, such as elliptical galaxies and galaxy halos.
The favored theory for the origin of most short gamma-ray bursts is the
merger of a binary system consisting of two neutron stars. According to
this model, the two stars in a binary slowly spiral towards each other
because gravitational radiation releases energy until tidal forces
suddenly rip the neutron stars apart and they collapse into a single
black hole. The infall of matter into the new black hole produces an
accretion disk and releases a burst of energy, analogous to the
collapsar model. Numerous other models have also been proposed to
explain short gamma-ray bursts, including the merger of a neutron star
and a black hole, the accretion-induced collapse of a neutron star, or
the evaporation of primordial black holes.
An alternative explanation proposed by Friedwardt Winterberg
is that in the course of a gravitational collapse and in reaching the
event horizon of a black hole, all matter disintegrates into a burst of
gamma radiation.
Tidal disruption events
This new class of GRB-like events was first discovered through the detection of GRB 110328A by the Swift Gamma-Ray Burst Mission
on 28 March 2011. This event had a gamma-ray duration of about 2 days,
much longer than even ultra-long GRBs, and was detected in X-rays for
many months. It occurred at the center of a small elliptical galaxy at
redshift z = 0.3534. There is an ongoing debate as to whether the
explosion was the result of stellar collapse or a tidal disruption event
accompanied by a relativistic jet, although the latter explanation has
become widely favoured.
A tidal disruption event of this sort is when a star interacts with a supermassive black hole,
shredding the star, and in some cases creating a relativistic jet which
produces bright emission of gamma ray radiation. The event GRB 110328A
(also denoted Swift J1644+57) was initially argued to be produced by the
disruption of a main sequence star by a black hole of several million
times the mass of the Sun, although it has subsequently been argued that the disruption of a white dwarf by a black hole of mass about 10 thousand times the Sun may be more likely.
Emission mechanisms
The means by which gamma-ray bursts convert energy into radiation
remains poorly understood, and as of 2010 there was still no generally
accepted model for how this process occurs.
Any successful model of GRB emission must explain the physical process
for generating gamma-ray emission that matches the observed diversity of
light curves, spectra, and other characteristics.
Particularly challenging is the need to explain the very high
efficiencies that are inferred from some explosions: some gamma-ray
bursts may convert as much as half (or more) of the explosion energy
into gamma-rays. Early observations of the bright optical counterparts to GRB 990123 and to GRB 080319B, whose optical light curves were extrapolations of the gamma-ray light spectra, have suggested that inverse Compton may be the dominant process in some events. In this model, pre-existing low-energy photons
are scattered by relativistic electrons within the explosion,
augmenting their energy by a large factor and transforming them into
gamma-rays.
The nature of the longer-wavelength afterglow emission (ranging from X-ray through radio)
that follows gamma-ray bursts is better understood. Any energy released
by the explosion not radiated away in the burst itself takes the form
of matter or energy moving outward at nearly the speed of light. As this
matter collides with the surrounding interstellar gas, it creates a relativistic shock wave
that then propagates forward into interstellar space. A second shock
wave, the reverse shock, may propagate back into the ejected matter.
Extremely energetic electrons within the shock wave are accelerated by
strong local magnetic fields and radiate as synchrotron emission across most of the electromagnetic spectrum.
This model has generally been successful in modeling the behavior of
many observed afterglows at late times (generally, hours to days after
the explosion), although there are difficulties explaining all features
of the afterglow very shortly after the gamma-ray burst has occurred.
Alternative explanations
Rather
than cataclysmic explosions, it has been suggested that gamma ray
bursts could conceivably represent optical illusions caused by constant
emitters entering into the region of space-time occupied by a gamma
emitter.
Rate of occurrence and potential effects on life
Gamma ray bursts can have harmful or destructive effects on life.
Considering the universe as a whole, the safest environments for life
similar to that on Earth are the lowest density regions in the outskirts
of large galaxies. Our knowledge of galaxy
types and their distribution suggests that life as we know it can only
exist in about 10% of all galaxies. Furthermore, galaxies with a
redshift, z, higher than 0.5 are unsuitable for life as we know it, because of their higher rate of GRBs and their stellar compactness.
All GRBs observed to date have occurred well outside the Milky
Way galaxy and have been harmless to Earth. However, if a GRB were to
occur within the Milky Way and its emission were beamed straight towards
Earth, the effects could be harmful and potentially devastating for the
ecosystems. Currently, orbiting satellites detect on average approximately one GRB per day. The closest observed GRB as of March 2014 was GRB 980425, located 40 megaparsecs (130,000,000 ly) away (z=0.0085) in an SBc-type dwarf galaxy. GRB 980425 was far less energetic than the average GRB and was associated with the Type Ib supernova SN 1998bw.
Estimating the exact rate at which GRBs occur is difficult; for a galaxy of approximately the same size as the Milky Way,
estimates of the expected rate (for long-duration GRBs) can range from
one burst every 10,000 years, to one burst every 1,000,000 years.
Only a small percentage of these would be beamed towards Earth.
Estimates of rate of occurrence of short-duration GRBs are even more
uncertain because of the unknown degree of collimation, but are probably
comparable.
Since GRBs are thought to involve beamed emission along two jets
in opposing directions, only planets in the path of these jets would be
subjected to the high energy gamma radiation.
Although nearby GRBs hitting Earth with a destructive shower of
gamma rays are only hypothetical events, high energy processes across
the galaxy have been observed to affect the Earth's atmosphere.
Effects on Earth
Earth's
atmosphere is very effective at absorbing high energy electromagnetic
radiation such as x-rays and gamma rays, so these types of radiation
would not reach any dangerous levels at the surface during the burst
event itself. The immediate effect on life on Earth from a GRB within a
few kiloparsecs
would only be a short increase in ultraviolet radiation at ground
level, lasting from less than a second to tens of seconds. This
ultraviolet radiation could potentially reach dangerous levels depending
on the exact nature and distance of the burst, but it seems unlikely to
be able to cause a global catastrophe for life on Earth.
The long-term effects from a nearby burst are more dangerous. Gamma rays cause chemical reactions in the atmosphere involving oxygen and nitrogen molecules, creating first nitrogen oxide then nitrogen dioxide gas. The nitrogen oxides cause dangerous effects on three levels. First, they deplete ozone,
with models showing a possible global reduction of 25–35%, with as much
as 75% in certain locations, an effect that would last for years. This
reduction is enough to cause a dangerously elevated UV index at the surface. Secondly, the nitrogen oxides cause photochemical smog, which darkens the sky and blocks out parts of the sunlight spectrum. This would affect photosynthesis,
but models show only about a 1% reduction of the total sunlight
spectrum, lasting a few years. However, the smog could potentially cause
a cooling effect on Earth's climate, producing a "cosmic winter"
(similar to an impact winter,
but without an impact), but only if it occurs simultaneously with a
global climate instability. Thirdly, the elevated nitrogen levels in the
atmosphere would wash out and produce nitric acid rain. Nitric acid
is toxic to a variety of organisms, including amphibian life, but
models predict that it would not reach levels that would cause a serious
global effect. The nitrates might in fact be of benefit to some plants.
All in all, a GRB within a few kiloparsecs, with its energy
directed towards Earth, will mostly damage life by raising the UV levels
during the burst itself and for a few years thereafter. Models show
that the destructive effects of this increase can cause up to 16 times
the normal levels of DNA damage. It has proved difficult to assess a
reliable evaluation of the consequences of this on the terrestrial
ecosystem, because of the uncertainty in biological field and laboratory
data.
Hypothetical effects on Earth in the past
GRBs close enough to affect life in some way might occur once every five million years or so – around a thousand times since life on Earth began.
The major Ordovician–Silurian extinction events 450 million years ago may have been caused by a GRB. The late Ordovician species of trilobites that spent portions of their lives in the plankton
layer near the ocean surface were much harder hit than deep-water
dwellers, which tended to remain within quite restricted areas. This is
in contrast to the usual pattern of extinction events, wherein species
with more widely spread populations typically fare better. A possible
explanation is that trilobites remaining in deep water would be more
shielded from the increased UV radiation associated with a GRB. Also
supportive of this hypothesis is the fact that during the late
Ordovician, burrowing bivalve species were less likely to go extinct than bivalves that lived on the surface.
A case has been made that the 774–775 carbon-14 spike was the result of a short GRB, though a very strong solar flare is another possibility.
GRB candidates in the Milky Way
No gamma-ray bursts from within our own galaxy, the Milky Way, have been observed,
and the question of whether one has ever occurred remains unresolved.
In light of evolving understanding of gamma-ray bursts and their
progenitors, the scientific literature records a growing number of
local, past, and future GRB candidates. Long duration GRBs are related
to superluminous supernovae, or hypernovae, and most luminous blue variables (LBVs), and rapidly spinning Wolf–Rayet stars
are thought to end their life cycles in core-collapse supernovae with
an associated long-duration GRB. Knowledge of GRBs, however, is from
metal-poor galaxies of former epochs of the universe's evolution, and it is impossible to directly extrapolate to encompass more evolved galaxies and stellar environments with a higher metallicity, such as the Milky Way.
WR 104: A nearby GRB candidate
A Wolf–Rayet star
in WR 104, about 8,000 light-years (2,500 pc) away, is considered a
nearby GRB candidate that could have destructive effects on terrestrial
life. It is expected to explode in a core-collapse-supernova at some
point within the next 500,000 years and it is possible that this
explosion will create a GRB. If that happens, there is a small chance
that Earth will be in the path of its gamma ray jet.