Ionizing particle fluxes in the near-ground atmosphere

Slides:



Advertisements
Similar presentations
23 rd ECRS The stratospheric polar vortex as a cause for the temporal variability of solar activity and galactic cosmic ray effects on the lower atmosphere.
Advertisements

GLAST The GLAST Balloon Flight experiment was performed with the collaboration of NASA Goddard Space Flight Center, Stanford Linear Accelerator Center,
21 ECRS, Kosice, 12/09/2008 Trapped charge particles measurements in the radiation belt by PAMELA instrument Vladimir V. Mikhailov (MEPHI) for PAMELA collaboration.
EAS EXPERIMENT ON BOARD OF THE AIRBUS A380 J. N. Capdevielle, F. Cohen, PCC, College de France K. Jedrzejczak, B. Szabelska, J. Szabelski, T. Wibig The.
SPHERE PEG GAY FAIRBURY JR SR HIGH SCHOOL. PROJECT SPHERE  Cherenkov light: radiation which is emitted whenever charged particles pass through matter.
PLANETOCOSMICS L. Desorgher, M. Gurtner, E.O. Flückiger, and P. Nieminen Physikalisches Institut, University of Bern ESA/ESTEC.
Riddles What happens when you throw a yellow rock into a purple stream? What starts with a T, ends with a T, and has T in it?
Cosmic v12/1/09Cosmic Pre-PDR 1 Cosmic Ray Experiment Team Cosmic Jace Boudreaux Allen Bordelon.
Radiation conditions during the GAMMA-400 observations:
RADAR Detection of Extensive Air Showers Nils Scharf III. Physikalisches Institut A Bad Honnef Nils Scharf III. Physikalisches Institut A Bad.
1 Seasonal variations of the muon flux seen by the muon detector BUST 1 Institute of Terrestrial Magnetism, Ionosphere and Radiowave Propagation RAN of.
The Relationship of Cosmic Rays to the Environment Erwin O. Flückiger Physikalisches Institut University of Bern ECRS 2008.
Cosmic Rays The discovery of cosmic rays Discoveries made with cosmic rays Cosmic rays in modern physics education Let’s count cosmic rays around us.
TAUP Conference, Sendai September The primary spectrum in the transition region between direct and indirect measurements (10 TeV – 10 PeV)
The PLANETOCOSMICS Geant4 application L. Desorgher Physikalisches Institut, University of Bern.
Cosmic-Ray Induced Neutrons: Recent Results from the Atmospheric Ionizing Radiation Measurements Aboard an ER-2 Airplane P. Goldhagen 1, J.M. Clem 2, J.W.
Atmospheric shower simulation studies with CORSIKA Physics Department Atreidis George ARISTOTLE UNIVERSITY OF THESSALONIKI.
Cosmic Ray flux modulation in different timescales observed with the CARPET detector between 2006 and 2012 (CASLEO, 2550 m, Rc = 9.65 GV) J.-P. Raulin,
Spectra of the Thunderstorm Correlated Electron and Gamma-Ray Measured at Aragats Bagrat Mailyan and Ashot Chilingarian.
Ch. 8.3 Pressure in Fluids. Pressure pressure – the amount of force applied to a given area – air, just like water, is a fluid (any substance that flows)
Neutron ‘thunder’ accompanying an extensive air shower Erlykin A.D. P.N.Lebedev Physical Institute, Moscow, Russia.
National Research Nuclear University MEPhI, Moscow, Russia
Properties of giant air showers and the problem of energy estimation of initial particles M.I. Pravdin for Yukutsk Collaboration Yu.G. Shafer Institute.
Exploitation of Space Ionizing Radiation Monitoring System in Russian Federal Space Agency STRUCTURE OF THE MONITORING SYSTEM The Monitoring System includes.
Interaction of solar and galactic cosmic rays with Earth’s atmosphere Contributors: Contributors: Rolf Bütikofer 1, Laurent Desorgher 1, Erwin Flückiger.
Cosmic Rays and Global Warming Cosmic Rays and Global Warming A.D.Erlykin 1,2, G. Gyalai 3, K. Kudela 3, T. Sloan 4 and A.W. Wolfendale 2 A.D.Erlykin 1,2,
Aa GLAST Particle Astrophysics Collaboration Instrument Managed and Integrated at SLAC/Stanford University The Gamma-ray Large Area Space Telescope (GLAST)
Trapped positrons and electrons observed by PAMELA Vladimir Mikhailov NRNU MEPHI, Moscow, Russia For PAMELA collaboration ICPPA 2015, PAMELA workshop,
Cosmic rays at sea level. There is in nearby interstellar space a flux of particles—mostly protons and atomic nuclei— travelling at almost the speed of.
Variations of Cosmic Rays during Thunderstorms N.S. Khaerdinov & A. S. Lidvansky Institute for Nuclear Research, Russian Academy of Sciences, Moscow, Russia.
Cosmic Rays2 The Origin of Cosmic Rays and Geomagnetic Effects.
It is considered that until now in the 24th cycle of solar activity 2 ground level enhancements of solar cosmic rays (GLEs) are registered: on May 17,
19.3 Detection of radioactivity
In high energy astrophysics observations, it is crucial to reduce the background effectively to achieve a high sensitivity, for the source intensity is.
What we do know about cosmic rays at energies above eV? A.A.Petrukhin Contents 4 th Round Table, December , Introduction. 2. How these.
NASA 2001 Mars Odyssey page 1 Workshop HEND Russian Aviation and Space Agency Institute for Space Research Signatures of ground water from maps.
AMIGA – A direct measurement of muons in Pierre Auger Observatory
SOLAR COSMIC RAYS AND OZONE LAYER OF THE EARTH (3D modeling) M27 Alexei Krivolutsky 1, Georgy Zakharov 1, Tatyana Vyushkova 1, Alexander Kuminov 1, and.
HIGH ENERGY POSITRON DETECTION VIA SYNCHROTRON RADIATION IN MAGENTOSPHERE “SONYA” project А.М. Гальпер 1, О.Ф. Прилуцкий 2, С.В. Колдашов 1, В.В. Михайлов.
The Course of Synoptic Meteorology
Measurement of high energy cosmic rays by the new Tibet hybrid experiment J. Huang for the Tibet ASγCollaboration a a Institute of high energy physics,
The “Carpet-2” multipurpose air shower array of the Baksan Neutrino Observatory INR of RAS A.U. Kudzhaev Institute for Nuclear Research, Russian Academy.
On behalf of the ARGO-YBJ collaboration
Paul Evenson University of Delaware
ATUL JAIN (CRL-TIFR, Ooty) on behalf of GRAPES-3 Collaboration
Search for Cosmic Ray Anisotropy with the Alpha Magnetic Spectrometer on the International Space Station G. LA VACCA University of Milano-Bicocca.
TREND workshop agenda 0. Introduction and round-table
Long-term variations of vector and tensor anisotropies of cosmic rays
Andrea Chiavassa Universita` degli Studi di Torino
STUDY of RADIATION RELATED with ATMOSPHERIC PRECIPITATIONS
A.S. Lidvansky, M.N. Khaerdinov, N.S. Khaerdinov
Department of Space Physics: Detached Laboratory at Lomnický štít (LS)
1 - Paul Scherrer Institut, 2 – SpaceIT, 3 - European Space Agency
Secondary positrons and electrons measured by PAMELA experiment
Vladimir Mikhailov (MEPhI) on behalf PAMELA collaboration
on behalf of the GAMMA Collaboration
Comparison Of High Energy Hadronic Interaction Models
Measurement of the Atmospheric Muon Charge Ratio by Using a Cosmic Ray Telescope Soheila Abdollahi (Imam Khomeini International University, Sharif University.
Comparison Of High Energy Hadronic Interaction Models
Cosmic Ray Showers Cosmic ray activity Figure 3:
N.S. Khaerdinov & A. S. Lidvansky
25.3 – Detecting Radioactivity
Measuring the cosmic radiation at different altitudes; an educational trip F.Riggi, 8° Conferenza dei Progetti del Centro Fermi, Erice, 6-8 Dicembre 2017.
Records of Cosmogenic Isotope Production Rates
Alexander Mishev & Ilya Usoskin
Composition of Cosmic Rays at Ultra High Energies
ICRC2003 OG Calculation of Cosmic-Ray Proton and Anti-proton Spatial Distribution in Magnetosphere Michio Fuki, Ayako Kuwahara, Nozomi, Sawada Faculty.
ATOC 4720: class 4 Variable constituents
ICRC2011, 32ND INTERNATIONAL COSMIC RAY CONFERENCE, BEIJING 2011
PH3520 / Particle Physics Autumn term 2010 – week 6
Presentation transcript:

Ionizing particle fluxes in the near-ground atmosphere BAZILEVSKAYA G.A., KRAINEV M.B., KVASHNIN A.N., MAKHMUTOV V.S., STOZHKOV Y.I., SVIRZHEVSKAYA A.K., SVIRZHEVSKY N.S. Lebedev Physical Institute, RAS, Leninsky prospect, 53, 119991, Moscow, Russia

Motivation and goal Ionization in the near-ground atmosphere is of interest for the cosmic ray physics and mechanisms of weather formation. There is a discrepancy between the results of charged particle fluxes observation and simulation near the ground. We try to understand the source of this discrepancy.

Long-term cosmic ray observations in the Earth’s atmosphere by Lebedev Physical Institute (Russia) Measurements with omnidirectional Geiger tubes and with Geiger tube telescopes beginning from 1957 Light balloon launchings several times a week at polar (Murmansk, Arctica, and Mirny, Antarctica) and mid-latitudes (Moscow region). Latitudinal surveys during sea expeditions. Here we use data of 1987 sea survey. Occasional measurements with a “B1” device with high statistics at polar (Arkhangelsk region) and mid-latitudes (Saratov region).

Radio-sound detectors

Stratos\Ser5708_1.xls

Main latitude surveys 19621965 19681969 19701971 19751976 19791980 19861987 Stratos\ISSI2007\MORSK871h.xls After Golenkov, A. E., Svirzhevskaya, A. K., Svirzhevsky, N. S., and Stozhkov, Yu. I.: 1990, Proc. 21st Int. Cosmic Ray Conf., Adelaide 7, 1417.

Stratos\photon\ФЭУ из Дис.xls

L. Desorgher et al., Int.J.Mod Phys. A, 20(29),6802-6804, 2005

Makhmutov , 2009

Discrepancy between the observed and simulated particle fluxes in the near-ground level (Bazilevskaya et al., 31 ICRC, Lodz, 2009) 13-14 km Cosmic ray fluxes and CRII normalized at averages for the whole period of observations 2.3 km Cosmic ray induced ionization: Usoskin et al. Acta Geophysica, 57(1), 88-101, DOI: 10.2478/s11600-008-0019-9, 2009.

Assumption: Ionizing radiation in the near-ground level (below 3 km – 700 g/cm2) Cosmic rays from the atmosphere Natural radioactivity

Approach A telescope is not sensitive to radioactivity. Sea water is much less radioactive than ground or rock. In Mirny, Antarctica, radioactivity is lower because the ground is mostly covered by glacier.

Data used Data of single Geiger counters Data of telescopes: Moscow and Murmansk regions 07.1957-2010. Mirny observatory, Antarctica, 03.1963-2009. Sea survey 1987. Arkhangelsk and Saratov regions, Set of 240 Geiger counters and a NaI scintillator (1970s, Charakhchyan et al., 1975, in Russian). Data of telescopes: Moscow and Murmansk regions, Mirny observatory, 1964-2009.

Stratos\Near_ground\sea_surv_1987.xls It is rightful to average the data of observations at various latitudes (various geomagnetic cutoffs) over sea at atmospheric pressures >400 g/cm2 (altitude < 7 km).

Stratos\Near_ground\compar_to_GEANT.xls

Stratos\STR\STR_season.xls

Ratio of count rates of an omnidirectional counter and a telescope Ratio for cosmic rays

There is a transition effect while cosmic ray particles pass through a boundary between air and soil (rock) because differences in the critical energy for electrons in these media. There is virtually no transition effect for cosmic rays passing from air to water.

Ionizing radiation in the near-ground level (below 3 km – 700 g/cm2) Cosmic rays from the atmosphere Natural radioactivity effect from the air-ground transition

Difference between observational data omnidirectional component) and GEANT 4 results (Desorgher et al., 2005): Contribution from the transition effect; Contribution from the natural radioactivity.

Difference between the observed X-ray fluxes at Arkhangelsk region and Mirny (Antarctida): 3. Contribution from the transition effect; 4. Contribution from the natural radioactivity.

Conclusion Difference between GEANT 4 results of Desorgher et al., 2005, and results of Makhmutov, 2009 is ~ 25% - need tuning. Divergence of results of GEANT 4 (Desorgher et al, 2005) from observations of omnidirectional fluxes of charged particles over ground begins at ~800 g/cm2 (altitude of ~2.1 km) and reaches ~30% at ~980 g/cm2 (altitude ~450 m). This is due to transition effect of cosmic rays between air and ground. Below ~ 500 m (pressure > ~970 g/cm2) the divergence is growing due to contribution of natural radioactivity which depends on location and changes with time. at

Conclusion (continuation) The observational results of omnidirectional charged particle fluxes over sea surface are virtually free from the transition effect. They are in reasonable agreement with the results of GEANT 4 simulation (Desorgher et al., 2005)

Conclusion (continuation) The results of X-ray observations over the ground surface demonstrate contributions from the CR transition effect (air-ground) and from natural radioactivity. The CR transition effect should be included into GEANT 4 simulations.

Thank you for your attention!

Измерения сцинтил. счетчиком у берегов Австралии на самолете. 916 811 715 630 г/см2 Измерения сцинтил. счетчиком у берегов Австралии на самолете. 5.06.59 – после 5 дней ветра с моря, остальные дни – ветер с континента. J.A. Walburton et al., Nature, 207(4993), 181, 1965

Stations of the cosmic ray measurements in the atmosphere Site of balloon launching Geographical coordinates Cutoff rigidity, GV McIlwain’s L-parameter Period of observations Olenya, Apatity (Murmansk region) 68º57'N 33º03'E 0.6 5.5 1957 – present time Dolgoprudny, Moscow region 5556'N 3731'E 2.35 2.6 Alma-Ata, Kazakhstan 4315'N 7655'E 6.7 1.8 1962- 1991 Mirny, Antarctica 6634'S 92º55'E 0.03 ~20 1963 –

The results of observations with a set of 240 Geiger tubes on the large-volume balloons (in Russian: А.Н. Чарахчьян, Г.А. Базилевская, А.Ф. Красоткин, Т.Н. Чарахчьян. Геомагнетизм и аэрономия, 15 (2), 197-202, 1975)