cosmic ray - wikipedia, the free encyclopedia
TRANSCRIPT
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The energy spectrum for cosmic rays
cini makes a
asurement in 1910.
osmic raym Wikipedia, the free encyclopedia
edirected from Cosmic rays)
smic rays are very high-energy particles, mainly originating outside the Solar System.[1] They may produce showers of
ondary particles that penetrate and impact the Earth's atmosphere and sometimes even reach the surface. Comprised
marilyof high-energy protons and atomic nuclei, their origin has, until recently, been a mystery. With data from the Fermi
ce telescope published in February 2013,[2] it is now known that cosmic rays primarily originate from the supernovae of
ssive stars.[3]
e term ray is a historical accident, as cosmic rays were at first, and wrongly, thought to be mostly electromagnetic
iation. In modern common usage[4] high-energy particles with intrinsic mass are known as "cosmic" rays, and photons,
ch are quanta of electromagnetic radiation (and so have no intrinsic mass) are known by their common names, such as
mma rays" or "X-rays", depending on their frequencies.
mic rays attract great interest practically, due to the damage they inflict on microelectronics and life outside the protection
n atmosphere and magnetic field, and scientifically, because the energies of the most energetic ultra-high-energy cosmic
s (UHECRs) have been observed to approach 3 1020 eV,[5] about 40 million times the energy of particles accelerated by
Large Hadron Collider.[6] At 50 J,[7] the highest-energy ultra-high-energy cosmic rays have energies comparable to the
etic energy of a 90-kilometre-per-hour (56 mph) baseball. As a result of these discoveries, there has been interest in
estigating cosmic rays of even greater energies.[8] Most cosmic rays, however, do not have such extreme energies; the
rgy distribution of cosmic rays peaks at 0.3 gigaelectronvolts (4.8 1011 J).[9]
primary cosmic rays, which originate outside of Earth's atmosphere, about 99% are the nuclei (stripped of their electron
lls) of well-known atoms, and about 1% are solitary electrons (similar to beta particles). Of the nuclei, about 90% are
ple protons, i. e. hydrogen nuclei; 9% are alpha particles, and 1% are the nuclei of heavier elements. [10] A very small
tion are stable particles of antimatter, such as positrons or antiprotons, and the precise nature of this remaining fraction is
area of active research.
Contents
1 History
1.1 Discovery
1.2 Identification
1.3 Energy distribution
2 Sources of cosmic rays
3 Types
3.1 Primary cosmic rays
3.2 Secondarycosmic rays
3.3 Cosmic-ray flux
4 Detection methods
5 Effects
5.1 Changes in atmospheric chemistry
5.2 Role in ambient radiation
5.3 Effect on electronics
5.4 Significance to space travel
5.5 Role in lightning
5.6 Role in climate change
5.6.1 Suggested mechanisms
5.6.2 Geochemical and astrophysical evidence
6 Research and experiments
6.1 Ground-based
6.2 Satellite
6.3 Balloon-borne
7 See also
8 Notes
9 References
10 External links
istory
er the discovery of radioactivity by Henri Becquerel in 1896, it was generally believed that atmospheric electricity, ionization of the air, was caused only by radiation from radioactive
ments in the ground or the radioactive gases or isotopes of radon they produce. Measurements of ionization rates at increasing heights above the ground during the decade from 1900 to
0 showed a decrease that could be explained as due to absorption of the ionizing radiation by the intervening air.
scovery
909 Theodor Wulf developed an electrometer, a device to measure the rate of ion production inside a hermetically sealed container, and used it to show higher levels of radiation at the
of the Eiffel Tower than at its base. However, his paper published in Physikalische Zeitschriftwas not widely accepted. In 1911 Domenico Pacini observed simultaneous variations of
rate of ionization over a lake, over the sea, and at a depth of 3 meters from the surface. Pacini concluded from the decrease of radioactivity underwater that a certain part of the
ization must be due to sources other than the radioactivity of the Earth.[11]
Then, in 1912, Victor Hess carried three enhanced-accuracy Wulf electrometers[12] to an altitude of 5300 meters in a free balloon flight. He found the
ionization rate increased approximately fourfold over the rate at ground level.[12] Hess also ruled out the Sun as the radiation's source by making a balloon
ascent during a near-total eclipse. With the moon blocking much of the Sun's visible radiation, Hess still measured rising radiation at rising altitudes.[12] He
concluded "The results of my observation are best explained by the assumption that a radiation of very great penetrating power enters our atmosphere from
above." In 19131914, Werner Kolhrster confirmed Victor Hess' earlier results by measuring the increased ionization rate at an altitude of 9 km.
Hess received the Nobel Prize in Physics in 1936 for his discovery.[13][14]
The Hess balloon flight took place on 7 August 1912. By sheer coincidence, exactly 100 years later on 7 August 2012,
the Mars Science Laboratory rover used its Radiation Assessment Detector (RAD) instrument to begin measuring the
iation levels on another planet for the first time.
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Increase of ionization with altitude as
measured by Hess in 1912 (left) and
by Kolhrster (right)
Hess lands after his balloon flight in
1912.
Primary cosmic particle collides with a moleculeof atmosphere.
entification
he 1920s the term "cosmic rays" was coined by Robert Millikan who made measurements of ionization due to cosmic rays from deep under
er to high altitudes and around the globe. Millikan believed that his measurements proved that the primary cosmic rays were gamma rays, i.e.,
rgetic photons. And he proposed a theory that they were produced in interstellar space as by-products of the fusion of hydrogen atoms into the
vier elements, and that secondaryelectrons were produced in the atmosphere by Compton scattering of gamma rays. But then, in 1927, J. Clay
nd evidence,[15] later confirmed in many experiments, of a variation of cosmic ray intensity with latitude, which indicated that the primary
mic rays are deflected by the geomagnetic field and must therefore be charged particles, not photons. In 1929, Bothe and Kolhrster discovered
rged cosmic-ray particles that could penetrate 4.1 cm of gold.[16] Charged particles of such high energy could not possibly be produced by
tons from Millikan's proposed interstellar fusion process.
930, Bruno Rossi predicted a difference between the intensities of cosmic rays arriving from the east and the west that depends upon the charge
he primary particles - the so-called "east-west effect."[17] Three independent experiments[18][19][20] found that the intensity is, in fact, greater
m the west, proving that most primaries are positive. During the years from 1930 to 1945, a wide variety of investigations confirmed that the
mary cosmic rays are mostly protons, and the secondary radiation produced in the atmosphere is primarilyelectrons, photons and muons. In
8, observations with nuclear emulsions carried by balloons to near the top of the atmosphere showed that approximately 10% of the primaries
helium nuclei (alpha particles) and 1% are heavier nuclei of the elements such as carbon, iron, and lead.[21][21]
ring a test of his equipment for measuring the east-west effect, Rossi observed that the rate of near-simultaneous discharges of two widely
arated Geiger counters was larger than the expected accidental rate. In his report on the experiment, Rossi wrote "... it seems that once in a while
recording equipment is struck by very extensive showers of particles, which causes coincidences between the counters, even placed at large
ances from one another."[20] In 1937 Pierre Auger, unaware of Rossi's earlier report, detected the same phenomenon and investigated it in some
ail. He concluded that high-energy primary cosmic-ray particles interact with air nuclei high in the atmosphere, initiating a cascade of secondary
ractions that ultimately yield a shower of electrons, and photons that reach ground level.
viet physicist Sergey Vernov was the first to use radiosondes to perform cosmic ray readings with an instrument carried to high altitude by a
oon. On 1 April 1935, he took measurements at heights up to 13.6 kilometers using a pair of Geiger counters in an anti-coincidence circuit to
id counting secondaryray showers.[22][23]
mi J. Bhabha derived an expression for the probability of scattering positrons by electrons, a process now known as Bhabha scattering. His
sic paper, jointly with Walter Heitler, published in 1937 described how primary cosmic rays from space interact with the upper atmosphere to
duce particles observed at the ground level. Bhabha and Heitler explained the cosmic ray shower formation by the cascade production of gamma rays and positive and negative electron
rs.
ergy distribution
asurements of the energy and arrival directions of the ultra-high energy primary cosmic rays by the techniques of "density sampling" and "fast timing" of extensive air showers were
t carried out in 1954 by members of the Rossi Cosmic Ray Group at the Massachusetts Institute of Technology.[24] The experiment employed eleven scintillation detectors arranged
hin a circle 460 meters in diameter on the grounds of the Agassiz Station of the Harvard College Observatory. From that work, and from many other experiments carried out all over
world, the energy spectrum of the primary cosmic rays is now known to extend beyond 1020 eV. A huge air shower experiment called the Auger Project is currently operated at a site
he pampas of Argentina by an international consortium of physicists, led by James Cronin, 1980 Nobel Prize in Physics of the University of Chicago and Alan Watson of the
versity of Leeds. Their aim is to explore the properties and arrival directions of the very highest-energy primary cosmic rays.[25] The results are expected to have important
plications for particle physics and cosmology, due to a theoretical GreisenZatsepinKuzmin limit to the energies of cosmic rays from long distances (about 160 million light years)
ch occurs above 1020 eV because of interactions with the remnant photons from the big bang origin of the universe.
November, 2007 preliminary results were announced showing direction of origination of the 27 highest energy events were strongly correlated with the locations of active galactic
lei (AGNs), where bare protons are believed to be accelerated by strong magnetic fields associated with the large black holes at the AGN centers to energies of 1020 eV and higher.[26]
h-energy gamma rays (>50 MeV photons) were finally discovered in the primary cosmic radiation by an MIT experiment carried on the OSO-3 satellite in 1967.[27] Components of
h galactic and extra-galactic origins were separately identified at intensities much less than 1% of the primary charged particles. Since then, numerous satellite gamma-ray observatories
e mapped the gamma-ray sky. The most recent is the Fermi Observatory, which has produced a map showing a narrow band of gamma ray intensity produced in discrete and diffuse
rces in our galaxy, and numerous point-like extra-galactic sources distributed over the celestial sphere.
ources of cosmic rays
ly speculation on the sources of cosmic rays included a 1948 proposal by Horace W. Babcock that magnetic variable stars could be a source of cosmic rays.[28] Subsequently in 1951,
Sediko et al. identified the Crab Nebula as a source of cosmic rays.[29] Subsequently, a wide variety of potential sources for cosmic rays began to surface, including supernovae, active
actic nuclei, quasars, and gamma-ray bursts.[30]
er experiments have helped to identify the sources of cosmic rays with greater certainty. In 2009, a paper presented at the International Cosmic Ray Conference (ICRC) by scientists at
Pierre Auger Observatory showed ultra-high energy cosmic rays (UHECRs) originating from a location in the sky very close to the radio galaxy Centaurus A, although the authors
cificallystated that further investigation would be required to confirm Cen A as a source of cosmic rays.[31]
However, no correlation was found between the incidence of gamma-raysts and cosmic rays, causing the authors to set a lower limit of 106 erg cm2 on the flux of 1 GeV-1 TeV cosmic rays from gamma-ray bursts.[32]
2009, supernovae were said to have been "pinned down" as a source of cosmic rays, a discovery made by a group using data from the Very Large Telescope.[33] This analysis, however,
disputed in 2011 with data from PAMELA, which revealed that "spectral shapes of [hydrogen and helium nuclei] are different and cannot be described well bya single power law",
gesting a more complex process of cosmic ray formation.[34] In February 2013, though, research analyzing data from Fermi revealed through an observation of neutral pion decay that
ernovae were indeed a source of cosmic rays, with each explosion producing roughly 3 1042 - 3 1043 J of cosmic rays.[2][3] However, supernovae do not produce all cosmic rays,
the proportion of cosmic rays that they do produce is a question which cannot be answered without further study.[35]
ypes
mic rays originate as primary cosmic rays, which are those originally produced in various astrophysical processes.
mary cosmic rays are composed primarily of protons and alpha particles (99%), with a small amount of heavier
lei (~1%) and an extremely minute proportion of positrons and antiprotons.[10] Secondary cosmic rays, caused by a
ay of primary cosmic rays as they impact an atmosphere, include neutrons, pions, positrons, and muons. Of these
r, the latter three were first detected in cosmic rays.
imary cosmic rays
mary cosmic rays primarily originate from outside our Solar System and sometimes even the MilkyWay. When they
ract with Earth's atmosphere, they are converted to secondary particles. The mass ratio of helium to hydrogen
lei, 28%, is about the same as the primordial elemental abundance ratio of these elements, 24%.[36] The remaining
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The moon in cosmic rays
e Moon'scosmic rayshadow,as
en in secondarymuons detected
0 m below ground, at the
udan 2 detector
e moon as seen by the Compton
amma RayObservatory, in
mma rays with energies greater
an 20 MeV. Theseare produced
cosmic raybombardment on its
rface.[39]
An overview of the space environment shows the relationship between
the solar activity and galactic cosmicrays.[41]
The VERITAS arrayof air Cherenkov telescopes.
tion is made up of the other heavier nuclei that are nuclear synthesis end products, products of the Big Bang[citation needed], primarily lithium, beryllium, and boron. These light nuclei
ear in cosmic rays in much greater abundance (~1%) than in the solar atmosphere, where they are only about 1011 as abundant as helium.
s abundance difference is a result of the way secondary cosmic rays are formed. Carbon and oxygen nuclei collide with interstellar matter to form lithium, beryllium and boron in a
cess termed cosmic ray spallation. Spallation is also responsible for the abundances of scandium, titanium, vanadium, and manganese ions in cosmic rays produced by collisions of iron
nickel nuclei with interstellar matter.[37]
ellite experiments have found evidence of a few antiprotons and positrons in primary cosmic rays, although there is no evidence of complex antimatter atomic nuclei, such as anti-
um nuclei (anti-alpha) particles. Antiprotons arrive at Earth with a characteristic energy maximum of 2 GeV, indicating their production in a fundamentally different process from
mic ray protons.[38]
Secondary cosmic rays
When cosmic rays enter the Earth's atmosphere they collide with molecules, mainly oxygen and nitrogen. The interaction produce a cascade of lighter
particles, a so-called air shower.[40] All of the produced particles stay within about one degree of the primary particle's path.
Typical particles produced in such collisions are neutrons and charged mesons such as positive or negative pions and kaons. Some of these
subsequently decay into muons, which are able to reach the surface of the Earth, and even penetrate for some distance into shallow mines. The muons
can be easily detected by many types of particle detectors, such as cloud chambers, bubble chambers or scintillation detectors. The observation of a
secondary shower of particles in multiple detectors at the same time is an indication that all of the particles came from that event.
Cosmic rays impacting other planetary bodies in the Solar System are detected indirectly byobserving high energy gamma ray emissions by gamma-
ray telescope. These are distinguished from radioactive decay processes bytheir higher energies above about 10 MeV.
Cosmic-ray flux
The flux of incoming cosmic rays at the upper atmosphere is dependent on the
solar wind, the Earth's magnetic field, and the energy of the cosmic rays. At
distances of ~94 AU from the Sun, the solar wind undergoes a transition, called
the termination shock, from supersonic to subsonic speeds. The region between the
termination shock and the heliopause acts as a barrier to cosmic rays, decreasing
the flux at lower energies ( 1 GeV) by about 90%. However, the strength of thesolar wind is not constant, and hence it has been observed that cosmic ray flux is
correlated with solar activity.
In addition, the Earth's magnetic field acts to deflect cosmic rays from its surface,
giving rise to the observation that the flux is apparently dependent on latitude,
longitude, and azimuth angle. The magnetic field lines deflect the cosmic rays
towards the poles, giving rise to the aurorae.
The combined effects of all of the factors mentioned contribute to the flux of cosmic rays at Earth's surface. For 1 GeV particles, the rate of arrival is
about 10,000 per square meter per second. At 1 TeV the rate is 1 particle per square meter per second. At 10 PeV there are only a few particles per
square meter per year. Particles above 10 EeV arrive only at a rate of about one particle per square kilometer per year, and above 100 EeV at a rate of
about one particle per square kilometer per century.[42]
In the past, it was believed that the cosmic ray flux remained fairly constant over time. However, recent research suggests 1.5 to 2-fold millennium-
escale changes in the cosmic ray flux in the past forty thousand years.[43]
e magnitude of the energy of cosmic ray flux in interstellar space is very comparable to that of other deep space energies: cosmic ray energy density averages about one electron-volt per
ic centimeter of interstellar space, or ~1 eV/cm3, which is comparable to the energy density of visible starlight at 0.3 eV/cm3, the galactic magnetic field energy density (assumed 3
rogauss) which is ~0.25 eV/cm3, or the cosmic microwave background (CMB) radiation energy density at ~ 0.25 eV/cm3.[44]
etection methods
ere are several ground-based methods of detecting cosmic rays currently in use. The
t detection method is called the air Cherenkov telescope, designed to detect low-
rgy (
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ffects
anges in atmospheric chemistry
mic rays ionize the nitrogen and oxygen molecules in the atmosphere, which leads to a number of chemical reactions. One of the reactions results in ozone depletion. Cosmic rays are
o responsible for the continuous production of a number of unstable isotopes in the Earth's atmosphere, such as carbon-14, via the reaction:
n + 14N p + 14C
mic rays kept the level of carbon-14[50] in the atmosphere roughly constant (70 tons) for at least the past 100,000 years, until the beginning of above-ground nuclear weapons testing in
early 1950s. This is an important fact used in radiocarbon dating used in archaeology.
action products of primary cosmic rays, radioisotope half-lifetime, and production reaction.[51]
Tritium (12.3 years): 14N(n, 3H)12C (Spallation)Beryllium-7 (53.3 days)
Beryllium-10 (1.39 million years): 14N(n,p )10Be (Spallation)
Carbon-14 (5730 years): 14N(n, p)14C (Neutron activation)
Sodium-22 (2.6 years)
Sodium-24 (15 hours)
Magnesium-28 (20.9 hours)
Silicon-31 (2.6 hours)
Silicon-32 (101 years)
Phosphorus-32 (14.3 days)
Sulfur-35 (87.5 days)
Sulfur-38 (2.8 hours)
Chlorine-34 m (32 minutes)
Chlorine-36 (300,000 years)
Chlorine-38 (37.2 minutes)
Chlorine-39 (56 minutes)
Argon-39 (269 years)
Krypton-85 (10.7 years)
le in ambient radiation
mic rays constitute a fraction of the annual radiation exposure of human beings on the Earth, averaging 0.39 mSv out of a total of 3 mSv per year (13% of total background) for the
th's population. However, the background radiation from cosmic rays increases with altitude, from 0.3 mSv per year for sea-level areas to 1.0 mSv per year for higher-altitude cities,
ing cosmic radiation exposure to a quarter of total background radiation exposure for populations of said cities. Airline crews flying long distance high-altitude routes can be exposed
.2 mSv of extra radiation each year due to cosmic rays, nearly doubling their total ionizing radiation exposure.
Average annual radiation exposure (millisieverts)
Radiation UNSCEAR[52][53] Princeton[54] Wa State[55] MEXT[56]
Type Sourc eWorld
averageTypical range USA USA Japan Remark
atural
Air 1.26 0.2-10.0a 2.29 2.00 0.40 Primarily from Radon, (a)depends on indoor accumulation of radon gas.
Internal 0.29 0.2-1.0b 0.16 0.40 0.40 Mainlyfrom radioisotopes in food (40K, 14C, etc.) (b)depends on diet.
Terrestrial 0.48 0.3-1.0c 0.19 0.29 0.40 (c)Depends on soil composition and building material of structres.
Cosmic 0.39 0.3-1.0d 0.31 0.26 0.30 (d)Generally increases with elevation.
Subtotal 2.40 1.0-13.0 2.95 2.95 1.50
tificial
Medical 0.60 0.03-2.0 3.00 0.53 2.30
Fallout 0.007 0 - 1+ - - 0.01Peaked in 1963 with a spike in 1986; still high near nuclear test and accident sites.
For the United States, fallout is incorporated into other categories.
others 0.0052 0-20 0.25 0.13 0.001Average annual occupational exposure is 0.7 mSv; mining workers have higher exposure.
Populations near nuclear plants have an additional ~0.02 mSv of exposure annually.
Subtotal 0.6 0 to tens 3.25 0.66 2.311
Total 3.00 0 to tens 6.20 3.61 3.81
Figures are for the time before the Fukushima Daiichi nuclear disaster. Human-made values by UNCEAR are from the Japanese National Institute of Radiological Sciences, which summarized the UNCEAR data.
fect on electronics
mic rays have sufficient energy to alter the states of elements in electronic integrated circuits, causing transient errors to occur, such as corrupted data in electronic memory devices, or
orrect performance of CPUs, often referred to as "soft errors" (not to be confused with software errors caused by programming mistakes/bugs). This has been a problem in extremely
h-altitude electronics, such as in satellites, but with transistors becoming smaller and smaller, this is becoming an increasing concern in ground-level electronics as well.[57] Studies by
M in the 1990s suggest that computers typically experience about one cosmic-ray-induced error per 256 megabytes of RAM per month.[58] To alleviate this problem, the Intel
poration has proposed a cosmic ray detector that could be integrated into future high-density microprocessors, allowing the processor to repeat the last command following a cosmic-
event.[59]
mic rays are suspected as a possible cause of an in-flight incident in 2008 where an Airbus A330 airliner of Qantas twice plunged hundreds of feet after an unexplained malfunction in
flight control system. Many passengers and crew members were injured, some seriously. After this incident, the accident investigators determined that the airliner's flight control system
received a data spike that could not be explained, and that all systems were in perfect working order. This has prompted a software upgrade to all A330 and A340 airliners, worldwide,
hat any data spikes in this system are filtered out electronically.[60]
gnificance to space travel
Main article: Health threat from cosmic rays
actic cosmic rays are one of the most important barriers standing in the way of plans for interplanetary travel by crewed spacecraft. Cosmic rays also pose a threat to electronics placed
ard outgoing probes. In 2010, a malfunction aboard the Voyager 2 space probe was credited to a single flipped bit, probably caused by a cosmic ray. Strategies such as physical or
gnetic shielding for spacecraft have been considered in order to minimize the damage to electronics and human beings caused by cosmic rays.[61][62]
le in lightning
mic rays have been implicated in the triggering of electrical breakdown in lightning. It has been proposed that essentially all lightning is triggered through a relativistic process,
naway breakdown", seeded by cosmic ray secondaries. Subsequent development of the lightning discharge then occurs through "conventional breakdown" mechanisms.[63]
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Carbondioxide concentrationson 500
million year scale.[66][68]
Climate change on 500 millionyear
scale
le in climate change
ole of cosmic rays directly or via solar-induced modulations in climate change was suggested by Edward P. Ney in 1959[64] and by Robert E. Dickinson in 1975.[65] In recent years, the
a has been revived, most notably by Henrik Svensmark; the most recent IPCC study disputed the mechanism,[66] while the most comprehensive review of the topic to date states that
le the amount of influence extraterrestrial factors have on Earth's climate is unclear, "evidence for the cosmic ray forcing is increasing as is the understanding of its physical
nciples."[67]
ggested mechanisms
nrik Svensmark has argued that because solar variations modulate the cosmic ray flux on Earth, they would consequently affect the rate of cloud
mation and hence the climate. Cosmic rays have been experimentally determined capable of producing ultra-small aerosol particles;[69] however,
se are orders of magnitude smaller than cloud condensation nuclei.
cording to a report about the ongoing CERN CLOUD research project,[70] detecting any cosmic ray forcing is challenging, since on geological
escales changes in the Sun's magnetic activity, Earth's magnetic field, and the galactic environment must all be taken into account. Empirically,
reased galactic cosmic ray (GCR) flux seem to be associated with a cooler climate and a weakening of monsoon rainfalls, or vice versa .[70]
ims have been made of identification of GCR climate signals in atmospheric parameters such as high-latitude precipitation and Svensmark's
ual cloud cover variations.
ious proposals have been made for the mechanism by which cosmic rays might affect clouds, including ion mediated nucleation and indirect
ects on current flow density in the global electric circuit, as suggested byBrian Tinsley[71] and Fangqun Yu.[72] Other studies refer to the
mation of relativelyhighly charged aerosols and cloud droplets at cloud boundaries, with an indirect effect on ice particle formation and altering aerosol interaction with cloud droplets.
Kirkby (2009) reviews developments and describes further cloud nucleation mechanisms that appear energetically favorable and depend on GCRs.[73][74] However, the many
cesses which cause cosmic rays to seed clouds have yet to be definitely identified.[67]
ochemical and astrophysical evidence
Shaviv has argued that climate signals on geological time scales are attributable to changing positions of the galactic spiral arms of the Milky
y Galaxy, and that cosmic ray flux variability is the dominant "climate driver" over these time periods.[75] Nir Shaviv and Jan Veizer in 2003[68]
ue, that in contrast to a carbon based scenario, the model and proxybased estimates of atmospheric CO2
levels especially for the early
nerozoic (see diagrams) do not show correlation with the paleoclimate picture that emerged from geological criteria, while cosmic ray flux does.
e 2007 IPCC synthesis report, however, strongly attributes a major role in the ongoing global warming to human-produced gases such as carbon
xide, nitrous oxide, and halocarbons, and has stated that models including natural forcings only (including aerosol forcings, which cosmic rays
considered by some to contribute to) would result in far less warming than has actually been observed or predicted in models including
hropogenic forcings.[76] The IPCC synthesis report only covers present and future changes in the Earth's climate, and does not mention
eoclimate or the influences which cosmic rays may have had on it.
omprehensive study of different research institutes was published 2007 by Scherer et al.[67] The study combines geochemical evidence both on
perature, cosmic rays influence and as well astrophysical deliberations suggesting a major role in climate variability over different geological time scales. Proxy data of CRF influence
mprise among others isotopic evidence in sediments on the Earth and as well changes in iron meteorites.
esearch and experiments
See also: Cosmic-ray observatory
ere are a number of cosmic-ray research initiatives.
ound-based
Akeno Giant Air Shower Array
CHICOS
High Energy Stereoscopic System
High Resolution Fly's Eye Cosmic Ray Detector
MAGIC
MARIACHI
Pierre Auger Observatory
Telescope Array Project
Washington Large Area Time Coincidence Array
CLOUD
Spaceship Earth
Milagro
NMDB
KASCADE
GAMMA
GRAPES-3
HEGRA
Chicago Air Shower Array
IceCube
tellite
PAMELA
Alpha Magnetic Spectrometer
ACE (Advanced Composition Explorer)
Voyager 1 and Voyager 2
CassiniHuygens
HEAO 1, HEAO 2, HEAO 3
Fermi Gamma-ray Space Telescope
Solar and Heliospheric Observatory
Interstellar Boundary Explorer
Langton Ultimate Cosmic-Ray Intensity Detector
lloon-borne
BESS
Advanced Thin Ionization Calorimeter
TRACER (cosmic ray detector)
TIGER (http://tiger.gsfc.nasa.gov)
Cosmic Ray Energetics And Mass (CREAM) (http://cosmicray.umd.edu/cream/)
PERDaix
HEAT (High Energy Antimatter Telescope) (http://adsabs.harvard.edu/
abs/1995psu..reptR....B)
e also
Environmental radioactivity
Forbush decrease
Gilbert Jerome Perlow
Extragalactic cosmic ray
Solar energetic particle
Track Imaging Cherenkov Experiment
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rieved from "http://en.wikipedia.org/w/index.php?title=Cosmic_ray&oldid=554255155"
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