Capabilities of the Space Instrument PAMELA for Solar Research Roberta Sparvoli ON BEHALF OF THE PAMELA COLLABORATION University of Rome ‘‘Tor Vergata’’,

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Capabilities of the Space Instrument PAMELA for Solar Research Roberta Sparvoli ON BEHALF OF THE PAMELA COLLABORATION University of Rome ‘‘Tor Vergata’’, Department of Physics, I Rome, Italy INFN, Sezione di Rome ‘‘Tor Vergata’’, I Rome, Italy 11 th European Spaceweather Week, November 2014 Liege, Belgium

Russia Moscow St. Petersburg Italy BariFlorenceFrascatiTriesteNaplesRome Sweden KTH, Stockholm Germany Siegen USA New Mexico New Hampshire PAMELA COLLABORATION

Direct detection of CRs in space Main focus on antiparticles (antiprotons and positrons) Launch from Baykonur PAMELA on board of Russian satellite Resurs DK1 Orbital parameters: - inclination ~70 o (  low energy) - altitude ~ km (elliptical) – now 500 km (circular)  Launched on 15th June 2006  PAMELA in continuous data-taking mode since then! PAMELA MISSION

GF: 21.5 cm 2 sr Mass: 470 kg Size: 130x70x70 cm 3 Power Budget: 360W Spectrometer microstrip silicon tracking system + permanent magnet - Magnetic rigidity  R = pc/Ze - Z sign - Z value from dE/dx Time-Of-Flight plastic scintillators + PMT - Trigger - Albedo rejection - Mass identification up to 1 GeV - Z identification from dE/dx Electromagnetic calorimeter W/Si sampling (16.3 X0, 0.6 λI) - Discrimination e + / p, anti-p / e - - Direct E measurement for e - Neutron detector plastic scintillators + PMT - High-energy e/h discrimination + - PAMELA INSTRUMENT

PAMELA ORBIT Semi-polar orbit (70°) outside the atmosphere 1)Different trigger configuration  optimal response to higher rates during Solar Particle Events 2)Collecting solar particles down to 80 MeV and up to several GeVs  ideal for Ground Level Enhancement studies 3)Over 30 polar passes every day  good capabilities in catching the onset of an event

Antiproton flux + antiproton/proton ratio (100 MeV- 200 GeV) Positron flux + positron/electron ratio (100 MeV-200 GeV) Electron flux (1 – 500 GeV) Proton and helium flux (1 GeV – 1.2 TeV) B/C ratio (500 MeV – 100 GeV) H and He isotope flux AntiHe/He Proton flux vs. time – solar modulation Trapped antiproton flux SEP data (13 December 2006 event) PAMELA published results

PAMELA SOLAR MODULATION STUDIES

The evolution of the proton energy spectrum as particle intensities approached the period of minimum solar activity, from July 2006 (violet), to December 2009 (red). The region between the blue and red curves indicates the spread in proton fluxes during this time. SOLAR MODULATION : PROTON SPECTRA

LIS based on that by Langner and Potgieter, modified at high energies to match PAMELA data SOLAR MODULATION : LIS SPECTRA

Charge-dependent solar modulatWork in progress PAMELA POSITRON low energy PAMELA ELECTRON to POSITRON low energy PRELIMINARY CHARGE DEPENDENT SOLAR MODULATION

PAMELA SEP STUDIES

Adriani et al. - ApJ , 2011 SEP from Dec. 13, 2006

EVENTS UNDER STUDY 1/2 M8.7 01/23/ UTC AR1402 X1.7 01/27/ UTC AR1402 X5.4 03/07/ UTC AR1429 M5.1 05/17/ UTC AR1476

EVENTS UNDER STUDY 2/2 M6.9 07/08/ UTC AR1515 M2.6 07/07/ UTC AR1515 M2.0 06/07/ UTC AR1227 M5.0 05/22/ UTC AR1745

FLUENCES Events measured by PAMELA Differences in a)Shape b)Duration c)Strength d)Rigidity threshol d January 2012March2012 May 2012June 2011 July2012May 2013

2012 May 17 th 2012 March 7 th 2012 January 27 th 2012 January 23 rd COMPLETING THE SPECTRUM PAMELA bridges the gap below ACE, GOES and many others and above the Neutron Monitors to obtain a complete spectrum

PAMELA can measure energy (or rigidity) spectra with very high precision (up to several hundreds of Gev) AND in a very narrow time window  well-suited for acceleration and propagation mechanisms Time averaged spectra (on a proper time window) measured by PAMELA can be fitted to extract parameter information and decide which mechanism better fits the data points 1. DIFFUSIVE SHOCK ACCELERATION 2. STOCHASTIC ACCELERATION ACCELERATION MECHANISMS

γ = 6.0 ± 0.9 E 0 = 0.17 ± 0.02 γ = 3.6 ± 0.9 E 0 = 0.25 ± 0.02 γ = 2.7 ± 0.8 E 0 = 0.11 ± 0.07 γ = 2.9 ± 0.8 E 0 = 0.99 ± 0.02 γ = 2.5 ± 0.7 E 0 = 0.15 ± 0.03 γ = 2.8 ± 0.5 E 0 = 0.21 ± 0.04

αT = ± αT = ± αT = ± αT = ± αT = ± αT = ± 0.003

FORBUSH DECREASE STUDY PAMELA studied also Forbush decrease (up to about 30 GV) for different particles Comparison between daily proton fluxes normalized to quite sun condition for the 2006 December 13 th event Time dependence of rigidity range between 1.57 GV and 5.70 GV of the flux normalized to quiet sun.

HELIUM/PROTON COMPARISON Comparing proton & Helium measurements Helium spectra measured from 0.7 GV Z identification allows good separation between samples Different behaviour during solar events? Study of charge/mass dependence of acceleration mechanisms Time (dd/mm )

Both tracker silicon layers and TOF scintillatiing layer perform excellent charge separation. No possibility to confuse the two species, due to charge consistency requests. Particle Selection for SEP’s events Proton selection bands ToF Tracker

HELIUM ENHANCEMENT p/He ratio during the 2012 March 7 th event The Helium enhancement (He/p > 15% ) has been associated with large flare The ratio decreases respect to the quiet Sun condition The ratio tends to become normal again after 5 days

ONSETS Onset time as a function of the velocity dispersion Combined data sets from various instruments: o PAMELA protons o PAMELA helium o WIND/LEMT He,Fe and O o Oulu Linear fit is performed The horizontal marks indicate o onset of the flare (blue) o CME-driven shock (green), o type II radio emission (black) o onset of hard X-ray (red) PAMELA can give useful information to infer the mechanisms of acceleration May 17 th 2012

SITE OF ACCELERATION It is possible to determine where the different acceleration mechanisms take place If CME-driven shock  site of the SPR time provides the altitude (respect to the center of the Sun) at which particles were injected Using the CME height versus time measurements from SOHO/LASCO the altitude of the possible CME driven shock has been extrapolated Site of acceleration as a function of time

We compare the derived accelerated ion population at the Sun (obtained by Fermi γ measurement) with the ion population directly measured in space by PAMELA COMPARING POPULATION SUN-EARTH Derived accelerated proton fluence (> 500 MeV) based on from a standard γ-ray production model Particle density measured by PAMELA (> 200 & > 500 MeV)

GOES STEREO A Area below the curve gives the filling factor COMPARING POPULATION SUN-EARTH PAMELA offers for the first time a unique opportunity to observe high-energy SEPs with ion energies that are know to produce the high-energy gamma-ray emission observed by FERMI/LAT, enabling the possibility to determine a connection, if any, between particles at the Sun and those in space. A multi-point observations of GOES, STEREO A & STEREO B (> 10 MeV) is used to obtain a filling factor and calculate the differential number of particles (dN p ) and then obtain a volume-integrated density (N p )

Results of the deduced number of accelerated ions at the Sun and measured by PAMELA The total number of protons ( > 500 MeV) is 15 × the protons measured by PAMELA (for the 7 March 2012 event) 1.Populations are unrelated? 2.Ions at the Sun are accelerated by stochastic acceleration at the Sun and do not escape? 3.Protons measured in space accelerated by a separate mechanism (CME shock?) COMPARING POPULATION SUN-EARTH

March 7 th event was not well-connected  underestimated the total number of protons in space No conclusion on timing of particle injection A more straightforward comparison can be obtained with SEP events that are well connected (like May 17 th, under study) COMPARING POPULATION SUN-EARTH

ANISOTROPY STUDIES PAMELA innovative aspects include the possibility of measuring the pitch-angle distributions, essential for the interpretation of solar events. A key ingredient is the use of back-tracing techniques, based on a realistic description of the magnetosphere, in order to reconstruct particle trajectories, identify asymptotic arrival directions and thus reconstruct the pitch angles. PAMELA data con be combined with data from NMs and other satellite-based detectors, in order to model the directional distribution of solar events, estimating the role of local transport phenomena.

THE ANISOTROPY OF 2012 MAY 17 th 60 rigidity bins ( GV) x 850 time bins = 52k trajectories asymptotic vertical looking directions

THE ANISOTROPY OF 2012 MAY 17 th flight data: count distributions

THE ANISOTROPY OF 2012 MAY 17 th Flux distribution as a function of pitch- angle in 10 bins of rigidity. The galactic background (estimated during a similar orbit of May 16 th ) is subtracted Flux distribution as a function of rigidity in 10 bins of pitch-angle. The galactic background (estimated during a similar orbit of May 16 th ) is subtracted

THE ANISOTROPY OF 2012 MAY 17 th SEP observations from PAMELA during the 2012 May 17 SEP event that exhibit differential anisotropies and thus transport features over the instrument rigidity range. SEP protons exhibit two distinct pitch angle distributions; a low-energy population that extends to 90° and a high energy population that is beamed at high energies (> 1 GeV), consistent with neutron monitor observations. In order to explain a low-energy SEP population that exhibits significant scattering or redistribution accompanied by a high energy population that reaches the Earth unhindered by dispersive transport effects, it is possible to postulate that the scattering or redistribution takes place locally. This could be the first definitive observations of the effects of solar energetic particle transport within the Earth’s magnetosheath.

SEARCH FOR SOLAR NEUTRONS 1/2 Solar neutrons can be produced by any solar event PAMELA Neutron Detector (ND) sensitivity threshold to neutrons flux Search of ND counts increasing after events near equator on solar side of the Earth (4-10 min time interval) in comparison with counts during 1 orbit before the event (a shift on East ~25° must be considered) Possible effect of Geomagnetic cutoff change by the trajectory shift ~25° June 7t h 2011 December 13 rd 2006

SEARCH FOR SOLAR NEUTRONS 2/2 December 13 rd 2006 December 12 th 2006 June 7 th 2011June 6 th 2011

PAMELA OVERALL RESULTS Results span 4 decades in energy and 13 in fluxes ! PAMELA data public and available at (ASI data Centre)

PAMELA has been in orbit and studying cosmic rays for more than 8 years. Its operation time will continue until Though conceived primarily for high energy cosmic ray studies, PAMELA has unique features suitable for solar research, and has already provided valuable data. One article about the 13 Dec SEP event already published. A new article “How the Earth’s Magnetosheath effects Solar Energetic Particles” (with US theoreticians) just submitted to Science. CONCLUSIONS (1)

Since several years, PAMELA started collaborations with solar physicists all over the world: North-West Univ. (South-Africa) for solar modulation, Univ. of Kiel for gradients in heliosphere, GSCF, NMSU, NHU (Usa) for SEP analysis with NM, FERMI collaboration for joint analysis. PAMELA is collaborating especially with solar and radiation groups of Univ. of Tor Vergata (Rome), IAPS/INAF (Rome) and Kapodistrian University of Athens (Greece) groups for joint analysis. See our poster Multiplatform observations of the Earth’s particle radiation environment during the 17 May 2012 SEP event (Laurenza M. et al., Poster 8.02). CONCLUSIONS (2)

“The PAMELA Space Mission: Heralding a New Era in Precision Cosmic Ray Physics” Physics Reports 544 (2014), pp Summarizes published and unpublished (but final) PAMELA results. PAMELA on PHYSICS REPORTS