EGU24-13328, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-13328
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Inter-Calibration of Solar Orbiter’s Heavy Ion Sensor and Suprathermal Ion Spectrograph

Benjamin Alterman1, Robert Allen2, Ryan Dewey3, Stefano Livi1,3, Jim Raines3, Susan Lepri3, Sarah Spitzer3,10, Chris Bert3, Christopher Owen4, George Ho1, Antoinette Galvin5, Lynn Kistler5, Frederic Allegrini1, Keiichi Ogasawara1, Peter Wurz6, Mark Philips1, Raffaella D'Amicis7, Glen Mason2, Robert F. Wimmer-Schweingruber8, and Javier Rodriquez-Pacheco9
Benjamin Alterman et al.
  • 1Southwest Research Institute, Space Science and Engineering, San Antonio, United States of America (blaltermanphd@gmail.com)
  • 2Johns Hopkins University Applied Physics Laboratory, Laurel, USA
  • 3Climate and Space Sciences, University of Michigan, Ann Arbor, USA
  • 4Mullard Space Science Laboratory, University College London, Dorking, UK
  • 5University of New Hampshire, Durham, USA
  • 6University of Bern, Bern, Switzerland
  • 7Institute for Space Astrophysics and Planetology, Rome, Italy
  • 8für Experimentelle und Angewandte Physik, Christian-Albrechts-Universität zu Kiel, Kiel, Germany
  • 9Space Research Group, Universidad de Alcalá, Alcalá de Henares, Madrid, Spain
  • 10Weizmann Institute of Science, Rehovot, Israel

The distribution of charged particles in the heliosphere covers more than 16 orders of magnitude in particle flux and more than 6 orders of magnitude in energy. While the majority of these particles are ionized hydrogen (protons) and fully ionized helium (alpha particles), heavier ions are also present. Because of the large parameter space that must be covered, different instruments are required and these instruments must be optimized to specific energy and particle flux ranges. They must also be designed to target specific ion species. To properly characterize the means by which different energy ranges are populated, the observations from these different instruments must be intercalibrated.

We present initial progress intercalibrating observations from Solar Orbiter’s Heavy Ion Sensor (HIS) and Suprathermal Ion Spectrograph (SIS). HIS is a heavy ion composition experiment that targets the solar wind through the low energy range of suprathermal energies with mass and charge state resolution. SIS covers the suprathermal and low range energetic particles with high mass resolution but without charge state resolution. Together, these two sensors cover heavy ion composition from solar wind to suprathermal energies. During advantageous conditions, proton distributions across both instruments are also available. Properly intercalibrated observations across these instruments enable studies of charged particle energization across the energy ranges, which is essential for characterizing a wide range of phenomena in heliosphere.

How to cite: Alterman, B., Allen, R., Dewey, R., Livi, S., Raines, J., Lepri, S., Spitzer, S., Bert, C., Owen, C., Ho, G., Galvin, A., Kistler, L., Allegrini, F., Ogasawara, K., Wurz, P., Philips, M., D'Amicis, R., Mason, G., Wimmer-Schweingruber, R. F., and Rodriquez-Pacheco, J.: Inter-Calibration of Solar Orbiter’s Heavy Ion Sensor and Suprathermal Ion Spectrograph, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-13328, https://doi.org/10.5194/egusphere-egu24-13328, 2024.