Spatial and Temporal Variability of the Gamma Radiation from Earth's Atmosphere during a Solar Cycle

Details Spatial and Temporal Variability of the Gamma Radiation from Earth's Atmosphere during a Solar Cycle Spatial and Temporal Variability of the Gamma Radiation from Earth's Atmosphere during a Solar Cycle

2003-08-21

arxiv.org/abs/physics/0308082v1

J.Geophys.Res. 108A12 (2003) 1435

Physics

Space Physics

11 pages, 12 figs., J. Geophys. Res. in press

Scientific paper

The Solar Maximum Mission satellite's Gamma Ray Spectrometer observed Earth's atmosphere for most of the period 1980-1989. Its 28deg orbit ensured that a range of geomagnetic latitudes (geomagnetic cutoff rigidities) was sampled. We measured the variation with time and rigidity of albedo gamma-ray lines at 1.6 MeV, 2.3 MeV and 4.4 MeV which are diagnostic of Galactic cosmic radiation penetrating the cutoff and of the secondary neutrons produced in the atmosphere. We found that the gamma-ray line intensities varied inversely with solar activity and cutoff rigidity, as expected. The line ratio (1.6 MeV + 2.3 MeV)/4.4 MeV was remarkably constant (close to 0.39) at all times and rigidities; the former two lines are produced by 5-10 MeV secondary neutrons causing excitation and de-excitation of 14N, while the latter is produced by more energetic (>20 MeV) neutrons inducing spallation. We infer that the shape of the secondary neutron energy spectrum is virtually constant everywhere and at all times. We also measured the intensity of the 0.511 MeV electron-positron annihilation line. This line too varies with solar cycle and cutoff rigidity, but its fall-off from low to high rigidity is less marked than that of the nuclear lines. This results from the energy dependences of the cross sections for positron production and for the hadronic processes which which produce secondary neutrons.

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