Introduction to the New Rover Reference Surface Mission
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Mawrth Vallis, Mars: a Fascinating Place for Future in Situ Exploration
Mawrth Vallis, Mars: a fascinating place for future in situ exploration François Poulet1, Christoph Gross2, Briony Horgan3, Damien Loizeau1, Janice L. Bishop4, John Carter1, Csilla Orgel2 1Institut d’Astrophysique Spatiale, CNRS/Université Paris-Sud, 91405 Orsay Cedex, France 2Institute of Geological Sciences, Planetary Sciences and Remote Sensing Group, Freie Universität Berlin, Germany 3Purdue University, West Lafayette, USA. 4SETI Institute/NASA-ARC, Mountain View, CA, USA Corresponding author: François Poulet, IAS, Bâtiment 121, CNRS/Université Paris-Sud, 91405 Orsay Cedex, France; email: [email protected] Running title: Mawrth: a fascinating place for exploration 1 Abstract After the successful landing of the Mars Science Laboratory rover, both NASA and ESA initiated a selection process for potential landing sites for the Mars2020 and ExoMars missions, respectively. Two ellipses located in the Mawrth Vallis region were proposed and evaluated during a series of meetings (3 for Mars2020 mission and 5 for ExoMars). We describe here the regional context of the two proposed ellipses as well as the framework of the objectives of these two missions. Key science targets of the ellipses and their astrobiological interests are reported. This work confirms the proposed ellipses contain multiple past Martian wet environments of subaerial, subsurface and/or subaqueous character, in which to probe the past climate of Mars, build a broad picture of possible past habitable environments, evaluate their exobiological potentials and search for biosignatures in well-preserved rocks. A mission scenario covering several key investigations during the nominal mission of each rover is also presented, as well as descriptions of how the site fulfills the science requirements and expectations of in situ martian exploration. -
Atmospheric Dust on Mars: a Review
47th International Conference on Environmental Systems ICES-2017-175 16-20 July 2017, Charleston, South Carolina Atmospheric Dust on Mars: A Review François Forget1 Laboratoire de Météorologie Dynamique (LMD/IPSL), Sorbonne Universités, UPMC Univ Paris 06, PSL Research University, Ecole Normale Supérieure, Université Paris-Saclay, Ecole Polytechnique, CNRS, Paris, France Luca Montabone2 Laboratoire de Météorologie Dynamique (LMD/IPSL), Paris, France & Space Science Institute, Boulder, CO, USA The Martian environment is characterized by airborne mineral dust extending between the surface and up to 80 km altitude. This dust plays a key role in the climate system and in the atmospheric variability. It is a significant issue for any system on the surface. The atmospheric dust content is highly variable in space and time. In the past 20 years, many investigations have been conducted to better understand the characteristics of the dust particles, their distribution and their variability. However, many unknowns remain. The occurrence of local, regional and global-scale dust storms are better documented and modeled, but they remain very difficult to predict. The vertical distribution of dust, characterized by detached layers exhibiting large diurnal and seasonal variations, remains quite enigmatic and very poorly modeled. Nomenclature Ls = Solar Longitude (°) MY = Martian year reff = Effective radius τ = Dust optical depth (or dust opacity) CDOD = Column Dust Optical Depth (i.e. τ integrated over the atmospheric column) IR = Infrared LDL = Low Dust Loading (season) HDL = High Dust Loading (season) MGS = Mars Global Surveyor (NASA spacecraft) MRO = Mars Reconnaissance Orbiter (NASA spacecraft) MEX = Mars Express (ESA spacecraft) TES = Thermal Emission Spectrometer (instrument aboard MGS) THEMIS = Thermal Emission Imaging System (instrument aboard NASA Mars Odyssey spacecraft) MCS = Mars Climate Sounder (instrument aboard MRO) PDS = Planetary Data System (NASA data archive) EDL = Entry, Descending, and Landing GCM = Global Climate Model I. -
March 21–25, 2016
FORTY-SEVENTH LUNAR AND PLANETARY SCIENCE CONFERENCE PROGRAM OF TECHNICAL SESSIONS MARCH 21–25, 2016 The Woodlands Waterway Marriott Hotel and Convention Center The Woodlands, Texas INSTITUTIONAL SUPPORT Universities Space Research Association Lunar and Planetary Institute National Aeronautics and Space Administration CONFERENCE CO-CHAIRS Stephen Mackwell, Lunar and Planetary Institute Eileen Stansbery, NASA Johnson Space Center PROGRAM COMMITTEE CHAIRS David Draper, NASA Johnson Space Center Walter Kiefer, Lunar and Planetary Institute PROGRAM COMMITTEE P. Doug Archer, NASA Johnson Space Center Nicolas LeCorvec, Lunar and Planetary Institute Katherine Bermingham, University of Maryland Yo Matsubara, Smithsonian Institute Janice Bishop, SETI and NASA Ames Research Center Francis McCubbin, NASA Johnson Space Center Jeremy Boyce, University of California, Los Angeles Andrew Needham, Carnegie Institution of Washington Lisa Danielson, NASA Johnson Space Center Lan-Anh Nguyen, NASA Johnson Space Center Deepak Dhingra, University of Idaho Paul Niles, NASA Johnson Space Center Stephen Elardo, Carnegie Institution of Washington Dorothy Oehler, NASA Johnson Space Center Marc Fries, NASA Johnson Space Center D. Alex Patthoff, Jet Propulsion Laboratory Cyrena Goodrich, Lunar and Planetary Institute Elizabeth Rampe, Aerodyne Industries, Jacobs JETS at John Gruener, NASA Johnson Space Center NASA Johnson Space Center Justin Hagerty, U.S. Geological Survey Carol Raymond, Jet Propulsion Laboratory Lindsay Hays, Jet Propulsion Laboratory Paul Schenk, -
Open Research Online Oro.Open.Ac.Uk
Open Research Online The Open University’s repository of research publications and other research outputs Oxia Planum: The Landing Site for the ExoMars “Rosalind Franklin” Rover Mission: Geological Context and Prelanding Interpretation Journal Item How to cite: Quantin-Nataf, Cathy; Carter, John; Mandon, Lucia; Thollot, Patrick; Balme, Matthew; Volat, Matthieu; Pan, Lu; Loizeau, Damien; Millot, Cédric; Breton, Sylvain; Dehouck, Erwin; Fawdon, Peter; Gupta, Sanjeev; Davis, Joel; Grindrod, Peter M.; Pacifici, Andrea; Bultel, Benjamin; Allemand, Pascal; Ody, Anouck; Lozach, Loic and Broyer, Jordan (2021). Oxia Planum: The Landing Site for the ExoMars “Rosalind Franklin” Rover Mission: Geological Context and Prelanding Interpretation. Astrobiology, 21(3) For guidance on citations see FAQs. c 2020 Cathy Quantin-Nataf et al. https://creativecommons.org/licenses/by/4.0/ Version: Version of Record Link(s) to article on publisher’s website: http://dx.doi.org/doi:10.1089/ast.2019.2191 Copyright and Moral Rights for the articles on this site are retained by the individual authors and/or other copyright owners. For more information on Open Research Online’s data policy on reuse of materials please consult the policies page. oro.open.ac.uk ASTROBIOLOGY Volume 21, Number 3, 2021 Research Article Mary Ann Liebert, Inc. DOI: 10.1089/ast.2019.2191 Oxia Planum: The Landing Site for the ExoMars ‘‘Rosalind Franklin’’ Rover Mission: Geological Context and Prelanding Interpretation Cathy Quantin-Nataf,1 John Carter,2 Lucia Mandon,1 Patrick Thollot,1 Matthew Balme,3 Matthieu Volat,1 Lu Pan,1 Damien Loizeau,1,2 Ce´dric Millot,1 Sylvain Breton,1 Erwin Dehouck,1 Peter Fawdon,3 Sanjeev Gupta,4 Joel Davis,5 Peter M. -
Blocks Size Frequency Distribution in the Enceladus Tiger Stripes Area: Implications on Their Formative Processes
universe Article Blocks Size Frequency Distribution in the Enceladus Tiger Stripes Area: Implications on Their Formative Processes Maurizio Pajola 1,* , Alice Lucchetti 1 , Lara Senter 2 and Gabriele Cremonese 1 1 INAF-Astronomical Observatory of Padova, Vicolo dell’Osservatorio 5, 35122 Padova, Italy; [email protected] (A.L.); [email protected] (G.C.) 2 Department of Physics and Astronomy “G. Galilei”, Università di Padova, 35122 Padova, Italy; [email protected] * Correspondence: [email protected] Abstract: We study the size frequency distribution of the blocks located in the deeply fractured, geologically active Enceladus South Polar Terrain with the aim to suggest their formative mechanisms. Through the Cassini ISS images, we identify ~17,000 blocks with sizes ranging from ~25 m to 366 m, and located at different distances from the Damascus, Baghdad and Cairo Sulci. On all counts and for both Damascus and Baghdad cases, the power-law fitting curve has an index that is similar to the one obtained on the deeply fractured, actively sublimating Hathor cliff on comet 67P/Churyumov- Gerasimenko, where several non-dislodged blocks are observed. This suggests that as for 67P, sublimation and surface stresses favor similar fractures development in the Enceladus icy matrix, hence resulting in comparable block disaggregation. A steeper power-law index for Cairo counts may suggest a higher degree of fragmentation, which could be the result of localized, stronger tectonic disruption of lithospheric ice. Eventually, we show that the smallest blocks identified are located Citation: Pajola, M.; Lucchetti, A.; from tens of m to 20–25 km from the Sulci fissures, while the largest blocks are found closer to the Senter, L.; Cremonese, G. -
Rapid Single Image-Based DTM Estimation from Exomars TGO Cassis Images Using Generative Adversarial U-Nets
remote sensing Article Rapid Single Image-Based DTM Estimation from ExoMars TGO CaSSIS Images Using Generative Adversarial U-Nets Yu Tao 1,* , Siting Xiong 2, Susan J. Conway 3, Jan-Peter Muller 1 , Anthony Guimpier 3, Peter Fawdon 4, Nicolas Thomas 5 and Gabriele Cremonese 6 1 Mullard Space Science Laboratory, Imaging Group, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK; [email protected] 2 College of Civil and Transportation Engineering, Shenzhen University, Shenzhen 518060, China; [email protected] 3 Laboratoire de Planétologie et Géodynamique, CNRS, UMR 6112, Universités de Nantes, 44300 Nantes, France; [email protected] (S.J.C.); [email protected] (A.G.) 4 School of Physical Sciences, Open University, Walton Hall, Milton Keynes MK7 6AA, UK; [email protected] 5 Physikalisches Institut, Universität Bern, Sidlerstrasse 5, 3012 Bern, Switzerland; [email protected] 6 INAF, Osservatorio Astronomico di Padova, 35122 Padova, Italy; [email protected] * Correspondence: [email protected] Abstract: The lack of adequate stereo coverage and where available, lengthy processing time, various artefacts, and unsatisfactory quality and complexity of automating the selection of the best set of processing parameters, have long been big barriers for large-area planetary 3D mapping. In this paper, Citation: Tao, Y.; Xiong, S.; Conway, we propose a deep learning-based solution, called MADNet (Multi-scale generative Adversarial S.J.; Muller, J.-P.; Guimpier, A.; u-net with Dense convolutional and up-projection blocks), that avoids or resolves all of the above Fawdon, P.; Thomas, N.; Cremonese, G. -
The Surface of Mars Michael H. Carr Index More Information
Cambridge University Press 978-0-521-87201-0 - The Surface of Mars Michael H. Carr Index More information Index Accretion 277 Areocentric longitude Sun 2, 3 Acheron Fossae 167 Ares Vallis 114, 116, 117, 231 Acid fogs 237 Argyre 5, 27, 159, 160, 181 Acidalia Planitia 116 floor elevation 158 part of low around Tharsis 85 floor Hesperian in age 158 Admittance 84 lake 156–8 African Rift Valleys 95 Arsia Mons 46–9, 188 Ages absolute 15, 23 summit caldera 46 Ages, relative, by remote sensing 14, 23 Dikes 47 Alases 176 magma supply rate 51 Alba Patera 2, 17, 48, 54–7, 92, 132, 136 Arsinoes Chaos 115, 117 low slopes 54 Ascreus Mons 46, 49, 51 flank fractures 54 summit caldera 49 fracture ring 54 flank vents 49 dikes 55 rounded terraces 50 pit craters 55, 56, 88 Asteroids 24 sheet flows 55, 56 Astronomical unit 1, 2 Tube-fed flows 55, 56 Athabasca Vallis 59, 65, 122, 125, 126 lava ridges 55 Atlantis Chaos 151 dilatational faults 55 Atmosphere collapse 262 channels 56, 57 Atmosphere, chemical composition 17 pyroclastic deposits 56 circulation 8 graben 56, 84, 86 convective boundary layer 9 profile 54 CO2 retention 260 Albedo 1, 9, 193 early Mars 263, 271 Albor Tholus 60 eddies 8 ALH84001 20, 21, 78, 267, 273–4, 277 isotopic composition 17 Alpha Particle X-ray Spectrometer 232 mass 16 Alpha Proton-ray Spectrometer 231 meridional flow 1 Alpheus Colles 160 pressure variations and range 5, 16 AlQahira 122 temperatures 6–8 Amazonian 277 scale height 5, 16 Amazonis Planitia 45, 64, 161, 195 water content 11 flows 66, 68 column water abundance 174 low -
PS4: Biosignature Modification in the Oxia Planum Region
Biosignature modification in the Oxia Planum region. Supervision team: Victoria Pearson, Nisha Ramkissoon, Peter Fawdon and Manish Patel External collaborator: Andrew Coates (UCL), Matt Gunn (Aberystwyth University), Ian Hutchinson (University of Leicester) Lead contact: Victoria Pearson [email protected] Description: ESA’s ExoMars 2020 Rosalind Franklin rover is expected to land on Mars in mid-2021, with a primary objective to search for signs of life. A landing site, Oxia Planum, has been selected that is rich in clay minerals, indicative of an environment that has been subjected to aqueous alteration in the past [1-3]. The prior presence of water may indicate that this region was once habitable, but any biosignatures (geochemical indicators for life) left behind may have been modified or even obliterated by subsequent surface processing, such as impact cratering, desiccation and diagenetic aqueous alteration [4]. This project aims to determine the effects of such processing on biosignatures within an Oxia Planum-like environment. It will combine orbital and rover data to develop an Oxia Planum simulant, which will then be used in laboratory simulation experiments to identify how biosignatures could be modified after they experience the types of processing seen at Oxia Planum. The project will begin with the design and production of a prototype Oxia Planum simulant based on existing data obtained from orbiting spacecraft. This prototype will be characterised and tested using instruments akin to those onboard the rover, specifically the Raman Laser Spectrometer (RLS) and infrared spectrometer for ExoMars (ISEM). Once data is returned from the ISEM, RLS and MicrOMEGA (micro Observatoire pour la Minéralogie l’Eau, la Glace et l’Activite) instruments aboard the ExoMars rover, the simulant will be refined, and a final version produced. -
Using Band Ratioed Cassis Imagery and Analysis of Fracture Morphology to Characterise Oxia Planum’S Clay-Bearing Unit
EPSC Abstracts Vol. 14, EPSC2020-877, 2020 https://doi.org/10.5194/epsc2020-877 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Using band ratioed CaSSIS imagery and analysis of fracture morphology to characterise Oxia Planum’s clay-bearing unit Adam Parkes Bowen1, Lucia Mandon2, John Bridges1, Cathy Quantin-Nataf2, Livio Tornabene3, James Page4, Jemima Briggs1, Nicolas Thomas5, and Gabriele Cremonese6 1Space Research Centre, University of Leicester, Leicester, United Kingdom of Great Britain and Northern Ireland ([email protected]) 2LGLTPE, Université de Lyon 1, Lyon, France ([email protected]) 3Centre for Planetary Science and Exploration, University of Western Ontario, Canada ([email protected]) 4Department of Physics, Imperial College London, London, United Kingdom of Great Britain and Northern Ireland 5Physikalisches Institut, Universität Bern, Bern, Switzerland ([email protected]) 6Istituto Nazionale di Astrofisica (INAF), Osservatorio Astronomico di Padova (OAPD), Padova, Italy ([email protected]) Introduction: In an effort to aid the characterisation of Oxia Planum, selected as the Rosalind Franklin rover’s landing site partly due to its extensive Noachian-era clay deposits [1, 2], a comparison of fractured terrains at Oxia and Gale Crater along with an analysis of Colour and Stereo Surface Imaging System (CaSSIS) [3] imagery are currently underway. An analysis of fractured terrains is a useful tool for determining the history and material properties of Oxia, as the form a fracture network takes varies depending both on the mechanisms which generated it as well as the materials within which the fracturing occurred [4-6]. -
The Mars Global Surveyor Mars Orbiter Camera: Interplanetary Cruise Through Primary Mission
p. 1 The Mars Global Surveyor Mars Orbiter Camera: Interplanetary Cruise through Primary Mission Michael C. Malin and Kenneth S. Edgett Malin Space Science Systems P.O. Box 910148 San Diego CA 92130-0148 (note to JGR: please do not publish e-mail addresses) ABSTRACT More than three years of high resolution (1.5 to 20 m/pixel) photographic observations of the surface of Mars have dramatically changed our view of that planet. Among the most important observations and interpretations derived therefrom are that much of Mars, at least to depths of several kilometers, is layered; that substantial portions of the planet have experienced burial and subsequent exhumation; that layered and massive units, many kilometers thick, appear to reflect an ancient period of large- scale erosion and deposition within what are now the ancient heavily cratered regions of Mars; and that processes previously unsuspected, including gully-forming fluid action and burial and exhumation of large tracts of land, have operated within near- contemporary times. These and many other attributes of the planet argue for a complex geology and complicated history. INTRODUCTION Successive improvements in image quality or resolution are often accompanied by new and important insights into planetary geology that would not otherwise be attained. From the variety of landforms and processes observed from previous missions to the planet Mars, it has long been anticipated that understanding of Mars would greatly benefit from increases in image spatial resolution. p. 2 The Mars Observer Camera (MOC) was initially selected for flight aboard the Mars Observer (MO) spacecraft [Malin et al., 1991, 1992]. -
OXIA PLANUM, a CLAY-LADEN LANDING SITE PROPOSED for the EXOMARS ROVER MISSION: AQUEOUS MINERALOGY and ALTERATION SCENARIOS. J. Carter1 and C
47th Lunar and Planetary Science Conference (2016) 2064.pdf OXIA PLANUM, A CLAY-LADEN LANDING SITE PROPOSED FOR THE EXOMARS ROVER MISSION: AQUEOUS MINERALOGY AND ALTERATION SCENARIOS. J. Carter1 and C. Quantin2 and P. Thollot2 and D. Loizeau2 and A. Ody2 and L. Lozach2, 1Institut d‟Astrophysique Spatiale, CNRS/Université Paris-Saclay, France. 2LGLTPE, Université de Lyon, France. [email protected], Introduction: The ExoMars rover mission goals ridge outside of the Oxia Planum lower unit, and fur- are to sample ancient, aqueously altered terrains to ther east at Mawrth Vallis. To the limit of sensitivity search for traces of extinct life and characterize the provided by orbital instruments, the clays at Oxia are water history of Early Mars [1]. These objectives as the most representative of Mars in terms of geographic well as EDL requirements translate into stringent con- distribution [5] but many large clay units are found to straints for finding suitable landing sites, which are be more nontronite-rich instead (Mawrth Vallis, Nili potentially met at only four locations, recently down- Fossae, Meridiani Planum [6,7,8]). The spectral uni- selected to 3 [2]. Along with the SE Mawrth Vallis formity, seldom observed elsewhere at similar resolu- Plateaus [3] and the Aram Dorsum plains [4], Oxia tion, likely indicates that a single formation or trans- Planum was selected as a final candidate for a 2020 formation process is responsible, independently of the launch and is the prime target for the 2018 launch win- duration and intensity of water-rock interactions. Punc- dow. Here, we report the discovery of this site and de- tures by small impact craters observed with HiRISE scribe its aqueous mineralogy. -
Infiltration of Martian Outflow Channel Floodwaters Into Lowland Cavernous Systems J
GEOPHYSICAL RESEARCH LETTERS, VOL. 39, L22201, doi:10.1029/2012GL053225, 2012 Infiltration of Martian outflow channel floodwaters into lowland cavernous systems J. Alexis P. Rodriguez,1 Mary Bourke,1,2 Kenneth L. Tanaka,3 Hideaki Miyamoto,4 Jeffrey Kargel,5 Victor Baker,5 Alberto G. Fairén,6 Richard J. Davies,7 Lynne Bridget,8 Rogelio Linares Santiago,9 Mario Zarroca Hernández,9 and Daniel C. Berman1 Received 24 July 2012; revised 9 October 2012; accepted 10 October 2012; published 30 November 2012. [1] The hydrosphere of Mars has remained mostly con- 1. Introduction cealed within the subsurface for the past 3.5 Gyr. Localized [2] The Martian outflow channels were excavated by the rupturing of the permafrost-capped crust led to voluminous largest estimated flood volumes in our solar system [Carr, groundwater discharges that carved some of the largest 1979; Clifford and Parker, 2001; Tanaka et al., 2005]. These known channels in the solar system. However, our knowl- edge of the nature of the flows and their ultimate fate remains waters were released from aquifers [Carr, 1979; Clifford and Parker, 2001] and/or surface lakes [Irwin et al., 2004] and incomplete, partly because diagnostic landforms at outflow may have resulted in the formation of transient oceans [Parker channel termini have been largely destroyed or buried. The et al., 1993; Fairén,2003],lakes[Fairén, 2003], continental- Hebrus Valles outflow channels were excavated by fluid dis- scale ice sheets [Kargel et al., 1995], and regionally extensive charges that emanated from two point sources, and they debris flow deposits [Tanaka et al., 2001].