We present a precise measurement of downward going albedo proton fluxes for kinetic energy above ∼70 MeV performed by the Payload for Antimatter Matter Exploration and Light-nuclei Astrophysics (PAMELA) experiment at an altitude between 350 and 610 km. On the basis of a trajectory tracing simulation, the analyzed protons were classified into quasi-trapped, concentrating in the magnetic equatorial region, and untrapped spreading over all latitudes, including both short-lived (precipitating) and long-lived (pseudotrapped) components. In addition, features of the penumbra region around the geomagnetic cutoff were investigated in detail. PAMELA results significantly improve the characterization of the high-energy albedo proton populations at low-Earth orbits.

Reentrant albedo proton fluxes measured by the PAMELA experiment / O., A., G. C., B., G. A., B., R., B., M., B., E. A., B., M., B., V., B., S., B., A., B., F., C., D., C., P., C., M., C., G., C., C., D.D., C., D.S., N., D.S., V., D.F., V., F., et al.. - In: JOURNAL OF GEOPHYSICAL RESEARCH. SPACE PHYSICS. - ISSN 2169-9402. - STAMPA. - 120:5(2015), pp. 3728-3738. [10.1002/2015JA021019]

Reentrant albedo proton fluxes measured by the PAMELA experiment

MUNINI, RICCARDO;
2015-01-01

Abstract

We present a precise measurement of downward going albedo proton fluxes for kinetic energy above ∼70 MeV performed by the Payload for Antimatter Matter Exploration and Light-nuclei Astrophysics (PAMELA) experiment at an altitude between 350 and 610 km. On the basis of a trajectory tracing simulation, the analyzed protons were classified into quasi-trapped, concentrating in the magnetic equatorial region, and untrapped spreading over all latitudes, including both short-lived (precipitating) and long-lived (pseudotrapped) components. In addition, features of the penumbra region around the geomagnetic cutoff were investigated in detail. PAMELA results significantly improve the characterization of the high-energy albedo proton populations at low-Earth orbits.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11368/2847408
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