posted on 2018-01-23, 14:58authored byYa. A. Ilyushin, R. Orosei, O. Witasse, B. Sánchez-Cano
In this paper we present the CLUtter SIMulator (CLUSIM), a special program simulating radar side echoes from rough planetary surfaces using realistic topography data sets. A numerical model of realistic topography of the Martian surface, based on Mars Orbiter Laser Altimeter data, is developed. A specially developed computer routine for evaluation of wideband radar echoes reflected from rough surfaces, capable of aperture synthesis simulation, is described. A synthetic radargram for a portion of Mars Express (MEX) orbit 9466 is computed and validated against experimental data obtained by the MARSIS radar instrument. Finally, a previously developed ionospheric phase correction procedure is numerically tested with new simulated echo signals. Impact of the surface clutter on the ionospheric correction procedure is investigated with a direct numerical comparison to a known benchmark result, which shows robustness of the correction algorithm with respect to the surface clutter.
Funding
This work was supported by ESA-ESTEC Faculty and the Italian Space Agency (ASI) through contract I/032/12/1. Support from Russian Fundamental Research Fund with the grant 15-02-05476 and Russian Science Foundation with the grant 17-77-20087 is also kindly acknowledged. B. S. -C. acknowledges support through STFC grants ST/K001000/1 and ST/N000749/1. Y. I. is grateful to the administration of the Scientific Research Computing Center of the Moscow State University for granting the access to the computational resources of the parallel computing systems SKIF-GRID “Tchshebyshev” and “Lomonosov.”
History
Citation
Radio Science, 2017, 52 (9), pp. 1200-1213
Author affiliation
/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Physics and Astronomy
Version
VoR (Version of Record)
Published in
Radio Science
Publisher
American Geophysical Union (AGU), Wiley, International Union of Radio Science
MARSIS subsurface sounding data can be accessed through the Planetary Science Archive of ESA (https://www.cosmos.esa.int/web/psa/mars-express) or the PDS Geosciences Node of NASA (http://pds-geosciences.wustl.edu/missions/mars_express/marsis.htm). Laser altimetry data from MOLA instrument are available from the archive http://pds-geosciences.wustl.edu/missions/mgs/mola.html. Requests for any other data should be sent directly to the corresponding author (Ya, I.) ilyushin@phys.msu.ru