Yield Function of the DOSimetry TELescope Count and Dose Rates Aboard the International Space Station

The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar wind in the heliosphere and the Earth's magnetic field. For this reason, the ability of a particle to approach a spacecraft in low Earth orbit dep...

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Published inSpace Weather Vol. 19; no. 5
Main Authors Caprotti, A. S., Brüdern, M., Burmeister, S., Heber, B., Herbst, K.
Format Journal Article
LanguageEnglish
Published Washington John Wiley & Sons, Inc 01.05.2021
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Abstract The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar wind in the heliosphere and the Earth's magnetic field. For this reason, the ability of a particle to approach a spacecraft in low Earth orbit depends on its energy and the position of the spacecraft within the Earth's magnetosphere. Moreover, there are some areas (radiation belts) where the particles are trapped for a long time and, therefore, the flux of energetic particles is particularly high. Occasionally, solar energetic particles contribute to the energetic particle flux too. DOSimetry TELescope (DOSTEL) is one of the instruments aboard the International Space Station (ISS) that monitors the radiation field within the European module Columbus. Because being installed inside the ISS, particles produced by the interaction between the “primary” radiation and the ISS materials are also measured. To describe the observations in such a complex radiation field, we follow the method by Caballero‐Lopez and Moraal (2012, Journal of Geophysical Research, 117[A12], A12103. doi:10.1029/2012JA017794) to compute the so‐called yield function using precise measurements of the proton and helium energy spectra obtained by alpha magnet spectrometer and the systematic variation of the DOSTEL measurements within the Earth's magnetosphere. Key Points Energetic particles Influence of the Earth magnetosphere on the count‐ and dose rate aboard International Space Station (ISS) Yield function
AbstractList The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar wind in the heliosphere and the Earth's magnetic field. For this reason, the ability of a particle to approach a spacecraft in low Earth orbit depends on its energy and the position of the spacecraft within the Earth's magnetosphere. Moreover, there are some areas (radiation belts) where the particles are trapped for a long time and, therefore, the flux of energetic particles is particularly high. Occasionally, solar energetic particles contribute to the energetic particle flux too. DOSimetry TELescope (DOSTEL) is one of the instruments aboard the International Space Station (ISS) that monitors the radiation field within the European module Columbus. Because being installed inside the ISS, particles produced by the interaction between the “primary” radiation and the ISS materials are also measured. To describe the observations in such a complex radiation field, we follow the method by Caballero‐Lopez and Moraal (2012, Journal of Geophysical Research, 117[A12], A12103. doi:10.1029/2012JA017794) to compute the so‐called yield function using precise measurements of the proton and helium energy spectra obtained by alpha magnet spectrometer and the systematic variation of the DOSTEL measurements within the Earth's magnetosphere. Key Points Energetic particles Influence of the Earth magnetosphere on the count‐ and dose rate aboard International Space Station (ISS) Yield function
Abstract The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar wind in the heliosphere and the Earth's magnetic field. For this reason, the ability of a particle to approach a spacecraft in low Earth orbit depends on its energy and the position of the spacecraft within the Earth's magnetosphere. Moreover, there are some areas (radiation belts) where the particles are trapped for a long time and, therefore, the flux of energetic particles is particularly high. Occasionally, solar energetic particles contribute to the energetic particle flux too. DOSimetry TELescope (DOSTEL) is one of the instruments aboard the International Space Station (ISS) that monitors the radiation field within the European module Columbus. Because being installed inside the ISS, particles produced by the interaction between the “primary” radiation and the ISS materials are also measured. To describe the observations in such a complex radiation field, we follow the method by Caballero‐Lopez and Moraal (2012, Journal of Geophysical Research , 117[A12], A12103. doi:10.1029/2012JA017794) to compute the so‐called yield function using precise measurements of the proton and helium energy spectra obtained by alpha magnet spectrometer and the systematic variation of the DOSTEL measurements within the Earth's magnetosphere. Key Points Energetic particles Influence of the Earth magnetosphere on the count‐ and dose rate aboard International Space Station (ISS) Yield function
The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar wind in the heliosphere and the Earth's magnetic field. For this reason, the ability of a particle to approach a spacecraft in low Earth orbit depends on its energy and the position of the spacecraft within the Earth's magnetosphere. Moreover, there are some areas (radiation belts) where the particles are trapped for a long time and, therefore, the flux of energetic particles is particularly high. Occasionally, solar energetic particles contribute to the energetic particle flux too. DOSimetry TELescope (DOSTEL) is one of the instruments aboard the International Space Station (ISS) that monitors the radiation field within the European module Columbus. Because being installed inside the ISS, particles produced by the interaction between the “primary” radiation and the ISS materials are also measured. To describe the observations in such a complex radiation field, we follow the method by Caballero‐Lopez and Moraal (2012, Journal of Geophysical Research, 117[A12], A12103. doi:10.1029/2012JA017794) to compute the so‐called yield function using precise measurements of the proton and helium energy spectra obtained by alpha magnet spectrometer and the systematic variation of the DOSTEL measurements within the Earth's magnetosphere.
Author Herbst, K.
Caprotti, A. S.
Burmeister, S.
Brüdern, M.
Heber, B.
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  doi: 10.1029/2019JA027433
– year: 1970
  ident: e_1_2_12_13_1
  article-title: Coupling and barometer coefficients for measurements of cosmic ray variations at altitudes of 260‐400 mb
  publication-title: International Cosmic Ray Conference
  contributor:
    fullname: Dorman L. I.
– ident: e_1_2_12_20_1
  doi: 10.1002/2016JA022638
– ident: e_1_2_12_25_1
  doi: 10.1088/1742-6596/409/1/012003
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Snippet The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar wind in...
Abstract The Earth is constantly hit by energetic particles originating from galactic sources. The flux of these particles is altered by the magnetized solar...
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SubjectTerms Astronomical instruments
Dosimeters
Dosimetry
Earth magnetosphere
Earth orbits
energetic particle measurements
Energetic particles
Energy spectra
Fluctuations
Flux
galactic cosmic rays
Geomagnetic field
Heliosphere
Helium
International Space Station
Low earth orbits
Magnetic fields
Multinational space ventures
Radiation
Radiation belts
Solar energetic particles
Solar wind
Space stations
Spacecraft
Spacecraft modules
yield function
Title Yield Function of the DOSimetry TELescope Count and Dose Rates Aboard the International Space Station
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https://www.proquest.com/docview/2553333149
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