Modeling the variations of Dose Rate measured by RAD during the first MSL Martian year: 2012-2014
arXiv:1507.03473 · doi:10.1088/0004-637X/810/1/24
Abstract
The Radiation Assessment Detector (RAD), on board Mars Science Laboratory's (MSL) rover Curiosity, measures the {energy spectra} of both energetic charged and neutral particles along with the radiation dose rate at the surface of Mars. With these first-ever measurements on the Martian surface, RAD observed several effects influencing the galactic cosmic ray (GCR) induced surface radiation dose concurrently: [a] short-term diurnal variations of the Martian atmospheric pressure caused by daily thermal tides, [b] long-term seasonal pressure changes in the Martian atmosphere, and [c] the modulation of the primary GCR flux by the heliospheric magnetic field, which correlates with long-term solar activity and the rotation of the Sun. The RAD surface dose measurements, along with the surface pressure data and the solar modulation factor, are analysed and fitted to empirical models which quantitatively demonstrate} how the long-term influences ([b] and [c]) are related to the measured dose rates. {Correspondingly we can estimate dose rate and dose equivalents under different solar modulations and different atmospheric conditions, thus allowing empirical predictions of the Martian surface radiation environment.
References in corpus (1)
Cited by in corpus (8)
- Dependence of the Martian radiation environment on atmospheric depth: Modeling and measurement
- Implementation and validation of the GEANT4/AtRIS code to model the radiation environment at Mars
- A generalized approach to model the spectra and radiation dose rate of solar particle events on the surface of Mars
- Measurements of Forbush decreases at Mars: both by MSL on ground and by MAVEN in orbit
- Measurements of the neutral particle spectra on Mars by MSL/RAD from 2015-11-15 to 2016-01-15
- Ready functions for calculating the Martian radiation environment
- Modeling the effectiveness of radiation shielding materials for astronaut protection on Mars
- Using Forbush decreases to derive the transit time of ICMEs propagating from 1 AU to Mars