Abstract

New estimation of fundamental geodetic parameters and global and local topography of planets and satellites provide basic coordinate systems for mapping as well as opportunities for studies of processes on their surfaces. The main targets of our study are Europa, Ganymede, Calisto and Io (satellites of Jupiter), Enceladus (a satellite of Saturn), terrestrial planetary bodies, including Mercury, the Moon and Phobos, one of the Martian satellites. In particular, based on new global shape models derived from three-dimensional control point networks and processing of high-resolution stereo images, we have carried out studies of topography and morphology. As a visual representation of the results, various planetary maps with different scale and thematic direction were created. For example, for Phobos we have produced a new atlas with 43 maps, as well as various wall maps (different from the maps in the atlas by their format and design): basemap, topography and geomorphological maps. In addition, we compiled geomorphologic maps of Ganymede on local level, and a global hypsometric Enceladus map. Mercury’s topography was represented as a hypsometric globe for the first time. Mapping of the Moon was carried out using new images with super resolution (0.5-1 m/pixel) for activity regions of the first Soviet planetary rovers (Lunokhod-1 and -2). New results of planetary mapping have been demonstrated to the scientific community at planetary map exhibitions (Planetary Maps Exhibitions, 2015), organized by MExLab team in frame of the International Map Year, which is celebrated in 2015-2016. Cartographic products have multipurpose applications: for example, the Mercury globe is popular for teaching and public outreach, the maps like those for the Moon and Phobos provide cartographic support for Solar system exploration.

Highlights

  • Planetary mapping in Russia has been initiated during the early ambitious Soviet space program (Shevchenko et al, 2016)

  • Modern planetary cartography integrates the different scientific and technologic tasks: to establish the coordinate system and provide basic maps derived from photogrammetric image processing; to study planetary surface feature characteristics using GIS-tools; to use new possibilities to publish various types of planetary cartography products such as digital maps, online maps, as well as access to spatial data via a geoportal, for example, Planetary Data system or Planetary geoportal of the Extraterrestrial laboratory

  • The Lunar Reconnaissance Orbiter (LRO) was launched on June 18, 2009 and provided data with highest resolution

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Summary

INTRODUCTION

Planetary mapping in Russia has been initiated during the early ambitious Soviet space program (Shevchenko et al, 2016). To present the results of new planetary research and to support the planning of future missions we have prepared various online and printed maps of planets and their satellites. Mapping of planetary surface is a research process developed for going beyond the standard image analysis, so many maps are created as results of various studies. Modern planetary cartography integrates the different scientific and technologic tasks: to establish the coordinate system and provide basic maps derived from photogrammetric image processing (global and local DEMs, orthomosaics); to study planetary surface feature characteristics using GIS-tools; to use new possibilities to publish various types of planetary cartography products such as digital maps (http://astrogeology.usgs.gov/), online maps (http://bit.ly/Lunohod_1), as well as access to spatial data via a geoportal, for example, Planetary Data system (http://wms.lroc.asu.edu/lroc) or Planetary geoportal of the MIIGAiK. Planetary mapping is based on results of photogrammetric image processing and spatial analysis of remote sensing data from different missions: archive images from Galileo (19942003), Voyager (1979-1981), Mars Global Surveyor (20012007), MESSENGER (2011-2015), as well as images from ongoing missions Lunar and Reconnaissance Orbiter, Mars Express, Mars Reconnaissance Orbiter, and Cassini

Phobos
The Moon
Mercury
CONCLUSION
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