Magnetospheric Particles and Earth

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Transcription:

Magnetospheric Particles and Earth Piergiorgio Picozza INFN and University of Rome Tor Vergata 12th AGILE Science Workshop Astro-Earth: Astrophysics and High-energy Terrestrial Phenomena ASI Headquarters May 8-9, 2014

The History

Van Allen Belts 350 km 70 o 610 km

Van Allen radiation belts A. Gyro B. Bounching C. Longitudinal drift A B C

Early Space Missions Electron and Proton flux variations below the radiation belts Electron Intercosmos Bulgaria-1300 and Meteor 3 Mariya Salyut 7 Mariya-2 MIR Gamma 1 GAMMA Astrophysical Station Meteor 3A Oreol 3

Single and Multiple Electron Bursts

Ionospheric-magnetosferic perturbation EME Natural emissions (earthquakes and volcanic eruptions) Anthropogenic emissions (PLHR, VLF & HF transmitters) ULF EME wave-trapped particle interaction?

Ground-based preseismic Ground based EME observations preseismic EME observations EQ EQ Loma Prieta earthquake, October 18, 1989, M=7.1 Spitak earthquake, December 7, 1988, M = 6.9

Wave particles interaction mechanism Schematic representation in a meridian plane of the trapped particle trajectories EM WAVES PROPAGATION INTO THE IONO- MAGNETOSPHERE EM WAVES GENERATE PERTURBATIONS IN THE LOWER IONOSPHERE EM WAVES INTERACT WITH CHARGED TRAPPED PARTICLES IN THE INNER RADIATION BELT mirror points lowering PBs stationary trajectory of trapped particles PARTICLE PITCH ANGLE CHANGES MIRROR POINTS LOWERING PARTICLE PRECIPITATION EARTHQUAKE PREPARATION AREA mirror points stationary lower boundary of the radiation belt geomagnetic field lines PBs PROPAGATE AROUND THE EARTH ALONG THE L-SHELL (LONGITUDINAL DRIFT) PBs DETECTABILITY AT ANY LONGITUDE

L = (L EQ L PB ) 0.1 H mirror 300 km T = T EQ T PB

Correlations between EQ & ps: T EQ-PB distributions After MIR mission 1985-2000 Altitude: 400 km Inclination: 51 Before E e : 20 200 MeV E p : 20 200 MeV After METEOR-3 mission 1985-1986 Altitude: 1250 km Inclination: 82 E e : 30 MeV Before After Before GAMMA-1 mission 1990-1992 Altitude: 350km Inclination: 51 E e : > 50 MeV

PET channel Level-2 data used for this study SAMPEX-PET Mission

SAMPEX Pointing Modes SAMPEX/PET has operated with three different pointing programs: ORR (original Orbit Rate Rotation) MORR (Modified Orbit Rate Rotation) 1 RPM (1 Rotation Per Minute) During the ORR pointing mode the PET yaw axis is substantially radial to the Earth. So, PET may detect particles with pitch angle in a wide range and, in particular, also in the loss cone (precipitating particles) or near to it. On the contrary, in the MORR mode the detector yaw axis is fundamentally perpendicular to the geomagnetic field lines, since it was implemented mainly to study particles with pitch angle near 90 (trapped particles). Measurements for PET values far from 90 are performed in periods during which PET yaw axis is parallel to the geomagnetic field (B), when B 0.3 G, and perpendicular to it, when B 0.3 G. Finally, in the 1 RPM mode the PET distribution is flat since the PET yaw axis, rotating continuously at 1 RPM, allows the particle detection at any pitch angle value.

PET/SAMPEX

Dependence of the T EQ-PB correlation on the PET yaw axis orientation MORR (1) 1 RPM MORR (2) N N N <N> + 2 <N> + 2 <N> <N> + 2 <N> <N> No correlation is obtained (that is, no relevant peak is observed) with PBEHI data collected in the other MORR(1), 1RPM, and MORR(2) pointing periods No correlation is obtained in the 4 pointing mode periods with PBELO data.

Correlations between EQ & ps: T EQ-PB distributions After MIR mission 1985-2000 Altitude: 400 km Inclination: 51 Before E e : 20 200 MeV E p : 20 200 MeV After METEOR-3 mission 1985-1986 Altitude: 1250 km Inclination: 82 E e : 30 MeV Before After Before GAMMA-1 mission 1990-1992 Altitude: 350km Inclination: 51 E e : > 50 MeV After ORR (Orbit Rate Rotation; July 1992 - May 1994) SAMPEX/PET Mission 1992-1999 Altitude: 520 740km Inclination: 82 Before 4 E e 15 MeV

Vittorio Sgrigna Piergiorgio Picozza Livio Conti

ESPERIA project

LAZIO & EGLE logo ENEIDE mission April 15-25 Roberto Vittori 2005 Esperia Geo-magnetometer for a Low-frequency wave Experiment

Photos LAZIO & EGLE

DEMETER Talk M. Parrot 29/06/2004 9/12/2010

The Resurs DK1 and VSPLESK ERA AGILE?

Conclusions PBs of precipitating high-energy Van Allen electrons appear to precede statistically by some hours the occurrence of moderate and strong EQs. No correlation was found between PBs and other nonseismic sources. Indication for a deeper investigation of the physical mechanisms under study.

The Next Future LIMADOU- CSES CHINA SEISMO-ELECTROMAGNETIC SATELLITE Talk R. Battiston

Thanks! http://spaceweather.roma2.infn.it