The Martian Surface Radiation Environment: Zenith Angle Dependence of Fluxes of Different Secondary Particle Species Produced in the Mars Atmosphere
- 1Christian-Albrechts-Universität zu Kiel, Institut für Experimentelle und Angewandte Physik, Physik, Germany (khaksari@physik.uni-kiel.de)
- 2NASA Goddard Space Flight Center, Greenbelt, MD, USA
- 3The Aerospace Corporation, Los Angeles, CA, United States
- 4University of Maryland, Baltimore County, Baltimore, MD, USA
- 5School of Earth and Space Sciences, University of Science and Technology of China, Hefei, PR China
- 6CAS Center for Excellence in Comparative Planetology, USTC, Hefei, PR China
- 7Solar System Science & Exploration Division, Southwest Research Institute, Boulder, CO, USA
- 8Leidos Corporation, Houston, TX, USA
- 9German Aerospace Center (DLR), Institute of Aerospace Medicine, Cologne, Germany
Understanding the zenith angle dependence of the Martian surface radiation environment is crucial for planning future human exploration missions to Mars. In our previous research (Wimmer et al. 2015; Guo et al. 2021; Khaksarighiri et al. 2023) we extensively studied the zenith-angle dependence of the Martian surface radiation dose rate. Leveraging the same validated radiation model, calibrated with data from the Radiation Assessment Detector (RAD) on Mars, we calculated the flux of secondary downward particles reaching to the surface of Mars from various zenith angles resulting from the interaction of primary particles with the Martian atmosphere.
These flux of secondary particles, coming from different zenith angles, can be integrated into a comprehensive topographic map of Mars, providing a detailed depiction of the global radiation landscape.
The construction of this radiation map requires careful consideration of various factors, including atmospheric column density, local and large-scale topography offering potential shielding effects, and the input spectrum is affected by heliospheric modulation. Additionally, accounting for seasonal pressure cycles and daily atmospheric surface pressure due to thermal tides is essential. Our model specifically focused on the influence of zenith angle on atmospheric column depth and simulations tailored to the Gale Crater region, a region explored by the Curiosity rover.
Applying this methodology allows us to create lookup tables of all secondary particles reaching the Martian surface from various zenith angles and evaluate the atmospheric impact. Employing these matrices alongside the incident spectrum enables the calculation of secondary particle flux from all zenith angles on the Martian surface.
This method provides valuable insights into the fluctuations in radiation flux on Mars, facilitating thorough assessments of potential radiation hazards. Mission planners can leverage these data, obtaining vital information to identify secure landing areas and sheltered regions for astronauts on the Martian surface.
How to cite: Khaksarighiri, S., Wimmer-Schweingruber, R. F., stubbs, T. J., Phipps, P. H., Looper, M. D., Guo, J., Ehresmann, B., Hassler, D. M., Matthiä, D., Zeitlin, C., Löwe, J. L., Berger, T., Löffler, S., and Reitz, G.: The Martian Surface Radiation Environment: Zenith Angle Dependence of Fluxes of Different Secondary Particle Species Produced in the Mars Atmosphere, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-10518, https://doi.org/10.5194/egusphere-egu24-10518, 2024.
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