Diurnal variations of energetic particle radiation at the surface of Mars as observed by the Mars Science Laboratory Radiation Assessment Detector. Issue 6 (18th June 2014)

• Record Type: Journal Article
• Authors: Rafkin, Scot C. R.; Zeitlin, Cary; Ehresmann, Bent; Hassler, Don; Guo, Jingnan; Köhler, Jan; Wimmer‐Schweingruber, Robert; Gomez‐Elvira, Javier; Harri, Ari‐Matti; Kahanpää, Henrik; Brinza, David E.; Weigle, Gerald; Böttcher, Stephan; Böhm, Eckart; Burmeister, Söenke; Martin, Cesar; Reitz, Güenther; Cucinotta, Francis A.; Kim, Myung‐Hee; Grinspoon, David; Bullock, Mark A.; Posner, Arik
• Is Part Of: Journal of geophysical research. Volume 119:Issue 6(2014:Jun.)
• Page Start: 1345
• Page End: 1358
• Publication Date: 2014-06-18
• Subjects: Mars -- radiation -- space weather -- atmosphere -- Mars Science Laboratory; Planets -- Periodicals; Geophysics -- Periodicals; 559.9
• DOI: 10.1002/2013JE004525
• Languages: English
• ISSNs: 2169-9097

Abstract

Abstract: The Radiation Assessment Detector onboard the Mars Science Laboratory rover Curiosity is detecting the energetic particle radiation at the surface of Mars. Data collected over the first 350 Martian days of the nominal surface mission show a pronounced diurnal cycle in both the total dose rate and the neutral particle count rate. The diurnal variations detected by the Radiation Assessment Detector were neither anticipated nor previously considered in the literature. These cyclic variations in dose rate and count rate are shown to be the result of changes in atmospheric column mass driven by the atmospheric thermal tide that is characterized through pressure measurements obtained by the Rover Environmental Monitoring Station, also onboard the rover. In addition to bulk changes in the radiation environment, changes in atmospheric shielding forced by the thermal tide are shown to disproportionately affect heavy ions compared to H and He nuclei. Key Points: Dose rate is inversely related to variations in atmospheric column mass Neutral count rate is proportional to variations in atmospheric mass Heavy ions are disproportionately affected by atmospheric shielding