2020
DOI: 10.1051/swsc/2020031
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On-orbit calibration of geostationary electron and proton flux observations for augmentation of an existing empirical radiation model

Abstract: Challenges faced in the quantitative use of long-term radiation belt data sets include establishing their relative accuracy and correcting for on-orbit degradation. An existing empirical model of energetic plasmas (0.001–40 keV) in geosynchronous orbit has been extended in energy to several hundred keV by incorporating observations from the Geostationary Operational Environmental Satellite (GOES) 13 and 15 magnetospheric electron detector (MAGED) and magnetospheric proton detector (MAGPD). In order to ensure t… Show more

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Cited by 7 publications
(5 citation statements)
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“…The calibration method is the same as that of similar particle detectors [18][19][20][21][22]. The calibration items include the energy spectral range, energy linearity, energy resolution, particle flux accuracy and a test of sensor thickness, size, field of view and particle identification capability.…”
Section: Ground Calibration 41 Calibration Methodsmentioning
confidence: 99%
“…The calibration method is the same as that of similar particle detectors [18][19][20][21][22]. The calibration items include the energy spectral range, energy linearity, energy resolution, particle flux accuracy and a test of sensor thickness, size, field of view and particle identification capability.…”
Section: Ground Calibration 41 Calibration Methodsmentioning
confidence: 99%
“…The calibration method is the same as that of similar particle detectors [11][12][13][14][15]. The calibration items include the energy spectra range, energy linearity, energy resolution, particle flux accuracy and the test of the sensor thickness, size, field of view, and the particle identification capability etc.al.…”
Section: Calibration Methodsmentioning
confidence: 99%
“…Note that west is lower than east-facing detector flux due to the finite proton gyroradius at these energies, so lower energy protons gyrate from higher L and higher from lower L into west and east facing detectors respectively, with flux higher at lower energies. condition for the subsequent radial diffusion calculation, the GOES EPS measurements were augmented with 80-800 keV measurements from the GOES Magnetospheric Proton Detector (Rodriguez et al, 2020). Assuming zero proton flux above the P1 channel midpoint energy (∼2.5 MeV), we find that the P1 effective energy is approximately 1 MeV during quiet solar periods.…”
Section: Appendix Amentioning
confidence: 99%