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Evidence for Thermal-Stress-Induced Rockfalls on Mars Impact Crater Slopes
Icarus 342 (2020) 113503 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Evidence for thermal-stress-induced rockfalls on Mars impact crater slopes P.-A. Tesson a,b,*, S.J. Conway b, N. Mangold b, J. Ciazela a, S.R. Lewis c, D. M�ege a a Space Research Centre, Polish Academy of Science, Wrocław, Poland b Laboratoire de Plan�etologie et G�eodynamique UMR 6112, CNRS, Nantes, France c School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK ARTICLE INFO ABSTRACT Keywords: Here we study rocks falling from exposed outcrops of bedrock, which have left tracks on the slope over which Mars, surface they have bounced and/or rolled, in fresh impact craters (1–10 km in diameter) on Mars. The presence of these Thermal stress tracks shows that these rocks have fallen relatively recently because aeolian processes are known to infill Ices topographic lows over time. Mapping of rockfall tracks indicate trends in frequency with orientation, which in Solar radiation � � turn depend on the latitudinal position of the crater. Craters in the equatorial belt (between 15 N and 15 S) Weathering exhibit higher frequencies of rockfall on their north-south oriented slopes compared to their east-west ones. � Craters >15 N/S have notably higher frequencies on their equator-facing slopes as opposed to the other ori entations. We computed solar radiation on the surface of crater slopes to compare insolation patterns with the spatial distribution of rockfalls, and found statistically significant correlations between maximum diurnal inso lation and rockfall frequency. -
Revolutionizing Solar System Science with WFIRST
! Revolutionizing Solar System Science with WFIRST Bryan J. Holler WFIRST Solar System Working Group (SSWG) Stefanie Milam Ernesto Palomba James Bauer Silvia Protopapa Charles Alcock Lynnae Quick Michele Bannister Darin Ragozzine Gordon Bjoraker Vishnu Reddy Dennis Bodewits Jason Rhodes Amanda Bosh Andy Rivkin Marc Buie Gal Sarid Tony Farnham Amanda Sickafoose Nader Haghighipour Amy Simon Paul Harderson Cristina Thomas Alan Harris David Trilling Henry Hsieh Robert West Michael Kelley With thanks to: Matthew Knight Christopher Hirata Emily Kramer Jason Kalirai Andrea Longobardo Jeff Kruk Conor Nixon Ed Nelan “Observations of XYZ will provide valuable information for understanding the origin and evolution of the solar system.” -Every solar system proposal Not to scale! Discovery Characterization WFIRST mission assumptions No IFC No moving target tracking Passive cooling Surveys not yet finalized Descope effects on solar system science Holler et al. (2018) NASA/JPL/K. McGill Estimated detection limits (1000 sec, 5-σ) Holler et al. (2018) Mining the astrophysics surveys Microlensing survey 8 Size-Frequency Distribution 44,555 Main Belt Asteroids 6 4 Log Frequency 2 0 0 5 10 15 20 25 30 Diameter (km) 120 ~1500 asteroids per W149 AB mag 100 square degree 80 ≈ 60 Johnson V Vega 40 Frequency per square degree 20 mag 0 15 20 25 30 35 W149(AB) magnitude Microlensing survey (cont.) • Gould (2014) claims: • Detection of KBOs down to V=30.2 • Detection of KBO satellites w/n 10 mas of primary down to V=31.0 • Cadence of microlensing survey could result in the construction of rotation light curves High-Latitude Survey (HLS) • DES and LSST can reach r<24.5 • WFIRST will be able to reach r<27 • Observe targets 3x smaller at a particular distance or 3x farther away for a particular size Spergel et al. -
Habitability of Mars: How Welcoming Are the Surface and Subsurface to Life on the Red Planet?
geosciences Review Habitability of Mars: How Welcoming Are the Surface and Subsurface to Life on the Red Planet? Aleksandra Checinska Sielaff and Stephanie A. Smith * Youth and Families Program Unit, Washington State University, Pullman, WA 99163, USA * Correspondence: [email protected] Received: 31 July 2019; Accepted: 20 August 2019; Published: 22 August 2019 Abstract: Mars is a planet of great interest in the search for signatures of past or present life beyond Earth. The years of research, and more advanced instrumentation, have yielded a lot of evidence which may be considered by the scientific community as proof of past or present habitability of Mars. Recent discoveries including seasonal methane releases and a subglacial lake are exciting, yet challenging findings. Concurrently, laboratory and environmental studies on the limits of microbial life in extreme environments on Earth broaden our knowledge of the possibility of Mars habitability. In this review, we aim to: (1) Discuss the characteristics of the Martian surface and subsurface that may be conducive to habitability either in the past or at present; (2) discuss laboratory-based studies on Earth that provide us with discoveries on the limits of life; and (3) summarize the current state of knowledge in terms of direction for future research. Keywords: Mars; habitability; surface; subsurface; water; organics; methane; life; microorganisms; lichens; bryophytes 1. Introduction “The Earth remains the only inhabited world known so far, but scientists are finding that the universe -
Amazonian Northern Mid-Latitude Glaciation on Mars: a Proposed Climate Scenario Jean-Baptiste Madeleine, François Forget, James W
Amazonian Northern Mid-Latitude Glaciation on Mars: A Proposed Climate Scenario Jean-Baptiste Madeleine, François Forget, James W. Head, Benjamin Levrard, Franck Montmessin, Ehouarn Millour To cite this version: Jean-Baptiste Madeleine, François Forget, James W. Head, Benjamin Levrard, Franck Montmessin, et al.. Amazonian Northern Mid-Latitude Glaciation on Mars: A Proposed Climate Scenario. Icarus, Elsevier, 2009, 203 (2), pp.390-405. 10.1016/j.icarus.2009.04.037. hal-00399202 HAL Id: hal-00399202 https://hal.archives-ouvertes.fr/hal-00399202 Submitted on 11 Apr 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Amazonian Northern Mid-Latitude 2 Glaciation on Mars: 3 A Proposed Climate Scenario a a b c 4 J.-B. Madeleine , F. Forget , James W. Head , B. Levrard , d a 5 F. Montmessin , and E. Millour a 6 Laboratoire de M´et´eorologie Dynamique, CNRS/UPMC/IPSL, 4 place Jussieu, 7 BP99, 75252, Paris Cedex 05, France b 8 Department of Geological Sciences, Brown University, Providence, RI 02912, 9 USA c 10 Astronomie et Syst`emes Dynamiques, IMCCE-CNRS UMR 8028, 77 Avenue 11 Denfert-Rochereau, 75014 Paris, France d 12 Service d’A´eronomie, CNRS/UVSQ/IPSL, R´eduit de Verri`eres, Route des 13 Gatines, 91371 Verri`eres-le-Buisson Cedex, France 14 Pages: 43 15 Tables: 1 16 Figures: 13 Email address: [email protected] (J.-B. -
OPAG Update to the Planetary Science Advisory Committee (PAC)
OPAG Update to the Planetary Science Advisory Committee (PAC) ? Linda Spilker OPAG Vice-Chair, JPL PAC Meeting September 24, 2019 Large KBOs: Outer Planets Assessment Group (OPAG) Charter https://www.lpi.usra.edu/opag/ • NASA's community-based forum to provide science input for planning and prioritizing outer planet exploration activities for the next several decades • Evaluates outer solar system exploration goals, objectives, investigations and required measurements on the basis of the widest possible community outreach • Meets twice per year, summer and winter – Next meeting: Feb. 3-4, 2020, LPI, Houston, TX • OPAG documents are inputs to the Decadal Surveys • OPAG and Small Bodies Assessment Group (SBAG) have Joint custody of Pluto system and other planets among Kuiper Belt Objects KBO planets OPAG Steering Committee Jeff Moore Linda Spilker OPAG Chair OPAG Vice-Chair * =New Member Ames Research Center Jet Propulsion Lab Alfred McEwen Lynnae Quick* Kathleen Mandt* University of Arizona NASA Goddard Applied Physics Laboratory OPAG Steering Committee Scott Edgington Amanda Hendrix Mark Hofstadter Jet Propulsion Lab Planetary Science Institute Jet Propulsion Lab Terry Hurford Carol Paty Goddard Space Flight Center Georgia Institute of Technology OPAG Steering Committee Morgan Cable* Britney Schmidt Kunio Sayanagi Jet Propulsion Lab Georgia Institute of Technology Hampton University * =New Member Tom Spilker* Abigail Rymer* Consultant Applied Physics Lab Recent and Upcoming OPAG-related Meetings • OPAG Subsurface Needs for Ocean Worlds -
Widespread Crater-Related Pitted Materials on Mars: Further Evidence for the Role of Target Volatiles During the Impact Process ⇑ Livio L
Icarus 220 (2012) 348–368 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Widespread crater-related pitted materials on Mars: Further evidence for the role of target volatiles during the impact process ⇑ Livio L. Tornabene a, , Gordon R. Osinski a, Alfred S. McEwen b, Joseph M. Boyce c, Veronica J. Bray b, Christy M. Caudill b, John A. Grant d, Christopher W. Hamilton e, Sarah Mattson b, Peter J. Mouginis-Mark c a University of Western Ontario, Centre for Planetary Science and Exploration, Earth Sciences, London, ON, Canada N6A 5B7 b University of Arizona, Lunar and Planetary Lab, Tucson, AZ 85721-0092, USA c University of Hawai’i, Hawai’i Institute of Geophysics and Planetology, Ma¯noa, HI 96822, USA d Smithsonian Institution, Center for Earth and Planetary Studies, Washington, DC 20013-7012, USA e NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA article info abstract Article history: Recently acquired high-resolution images of martian impact craters provide further evidence for the Received 28 August 2011 interaction between subsurface volatiles and the impact cratering process. A densely pitted crater-related Revised 29 April 2012 unit has been identified in images of 204 craters from the Mars Reconnaissance Orbiter. This sample of Accepted 9 May 2012 craters are nearly equally distributed between the two hemispheres, spanning from 53°Sto62°N latitude. Available online 24 May 2012 They range in diameter from 1 to 150 km, and are found at elevations between À5.5 to +5.2 km relative to the martian datum. The pits are polygonal to quasi-circular depressions that often occur in dense clus- Keywords: ters and range in size from 10 m to as large as 3 km. -
Volcanism on Mars
Author's personal copy Chapter 41 Volcanism on Mars James R. Zimbelman Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC, USA William Brent Garry and Jacob Elvin Bleacher Sciences and Exploration Directorate, Code 600, NASA Goddard Space Flight Center, Greenbelt, MD, USA David A. Crown Planetary Science Institute, Tucson, AZ, USA Chapter Outline 1. Introduction 717 7. Volcanic Plains 724 2. Background 718 8. Medusae Fossae Formation 725 3. Large Central Volcanoes 720 9. Compositional Constraints 726 4. Paterae and Tholi 721 10. Volcanic History of Mars 727 5. Hellas Highland Volcanoes 722 11. Future Studies 728 6. Small Constructs 723 Further Reading 728 GLOSSARY shield volcano A broad volcanic construct consisting of a multitude of individual lava flows. Flank slopes are typically w5, or less AMAZONIAN The youngest geologic time period on Mars identi- than half as steep as the flanks on a typical composite volcano. fied through geologic mapping of superposition relations and the SNC meteorites A group of igneous meteorites that originated on areal density of impact craters. Mars, as indicated by a relatively young age for most of these caldera An irregular collapse feature formed over the evacuated meteorites, but most importantly because gases trapped within magma chamber within a volcano, which includes the potential glassy parts of the meteorite are identical to the atmosphere of for a significant role for explosive volcanism. Mars. The abbreviation is derived from the names of the three central volcano Edifice created by the emplacement of volcanic meteorites that define major subdivisions identified within the materials from a centralized source vent rather than from along a group: S, Shergotty; N, Nakhla; C, Chassigny. -
A New Model of the Crustal Magnetic Field of Mars Using MGS and MAVEN
RESEARCH ARTICLE A New Model of the Crustal Magnetic Field of Mars Using 10.1029/2018JE005854 MGS and MAVEN Key Points: 1 1 2 3 • MGS and MAVEN magnetic field Benoit Langlais , Erwan Thébault , Aymeric Houliez , Michael E. Purucker , 4 measurements are combined into a and Robert J. Lillis high-resolution magnetic field model • The new model extends up to SH 1Laboratoire de Planétologie et Géodynamique, Université de Nantes, Université d'Angers, CNRS, UMR 6112, Nantes, degree 134, corresponding to 160-km France, 2Observatoire Royal de Belgique, Uccle, Belgium, 3Planetary Magnetospheres Laboratory, NASA Goddard horizontal resolution at the Martian Space Flight Center, Greenbelt, MD, USA, 4Space Science Laboratory, University of California, Berkeley, CA, USA surface • It enables local studies, where geologic and magnetic features can be compared Abstract While devoid of an active magnetic dynamo field today, Mars possesses a remanent magnetic field that may reach several thousand nanoteslas locally. The exact origin and the events that have shaped the crustal magnetization remain largely enigmatic. Three magnetic field data sets from two spacecraft Supporting Information: • Supporting Information S1 collected over 13 cumulative years have sampled the Martian magnetic field over a range of altitudes •TableS1 from 90 up to 6,000 km: (a) Mars Global Surveyor (MGS) magnetometer (1997–2006), (b) MGS Electron Reflectometer (1999–2006), and (c) Mars Atmosphere and Volatile EvolutioN (MAVEN) magnetometer Correspondence to: (2014 to today). In this paper we combine these complementary data sets for the first time to build a new B. Langlais, model of the Martian internal magnetic field. This new model improves upon previous ones in several [email protected] aspects: comprehensive data coverage, refined data selection scheme, modified modeling scheme, discrete-to-continuous transformation of the model, and increased model resolution. -
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, -
The Need for a Large-Scale, Integrated Approach to Ocean World Modeling
The need for a large-scale, integrated approach to Ocean World Modeling Submitted by: William Farrell,NASA/Goddard Space Flight Center, 301-286-4446, [email protected] * Orenthal Tucker, NASA/Goddard Space Flight Center* Marc Neveu, NASA/Goddard Space Flight Center* Dina Bower, NASA/Goddard Space Flight Center * Lynnae Quick, NASA/Goddard Space Flight Center* Joseph Renaud, NASA/Goddard Space Flight Center* Robert Tyler, NASA/Goddard Space Flight Center* Louis-Alexandre Couston, British Antarctic Survey, Cambridge UK Conor Nixon, NASA/Goddard Space Flight Center* Paul Romani, NASA/Goddard Space Flight Center * Reggie Hudson, NASA/Goddard Space Flight Center * Cesare Grava, Southwest Research Institute Denis Felikson, NASA Postdoc Program, NASA/Goddard Space Flight Center* Erica Nathan, Brown University Geronimo Villanueva, NASA/Goddard Space Flight Center* Veronica Allen, NASA Postdoc Program, NASA/Goddard Space Flight Center* Shawn Domagal-Goldman, NASA/Goddard Space Flight Center* Jennifer Eigenbrode, NASA/Goddard Space Flight Center* Bethany Theiling, NASA/Goddard Space Flight Center* Gordon Bjoraker, NASA/Goddard Space Flight Center* Krista Soderlund, University of Texas, Austin *Members of NASA/GSFC’s Ocean worlds Science, Exploration and ANalog (OSEAN) team Italics indicates key contribution to paper as part of the principal writing team 0 1. Motivation The past decade has seen greatly enhanced scientific and political interest in new generation studies of the now known-to-be- numerous Ocean Worlds in our solar system. -
Geology of Alba Mons, Mars: Results from 1:1M-Scale Geologic Mapping
50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 2160.pdf GEOLOGY OF ALBA MONS, MARS: RESULTS FROM 1:1M-SCALE GEOLOGIC MAPPING. David A. Crown1, Daniel C. Berman1, Stephen P. Scheidt1, and Ernst Hauber3, 1Planetary Science Institute, 1700 E. Ft. Lowell Rd., Suite 106, Tucson, Arizona 85719 ([email protected]); 2Institute of Planetary Research, German Aerospace Center, Berlin, Germany. Introduction: Imaging and topographic datasets distribution and local slope, and the occurrence of are being used to produce two 1:1M-scale geologic dendritic networks on the highest local slopes, suggest maps of Alba Mons in order to document the volcanic control by topography rather than variations in evolution and geologic history of the northernmost substrate properties. volcano in the Tharsis region. We utilize geologic 2) Alba Mons’ western flank is dominated by lava mapping of Alba Mons’ summit region (245-255°E, flows and lava tube systems [24-26]. Their distribution 32.5-47.5°N) and western flank (230-245°E, 37.5- is consistent with the broad shape of the volcano and 47.5°N) to characterize volcanic, tectonic, and local slopes (i.e., at 50 km scale), although some lava erosional processes and derive age constraints from flow paths have been deflected by local obstacles, cross-cutting relationships and crater size-frequency including pre-existing craters and volcanic flows. distributions. Although local relationships are complex, lava flows Mapping Methodology and Datasets: Geologic generally seem to post-date adjacent lava tube systems. mapping uses THEMIS, HRSC, CTX, and HiRISE 3) Individual lava flows are typically elongate with images supported by HRSC and MOLA topography. -
Abstract STUBBLEFIELD, RASHONDA KIAM. Extensional Tectonics at Alba Mons, Mars
Abstract STUBBLEFIELD, RASHONDA KIAM. Extensional Tectonics at Alba Mons, Mars: A Case Study for Local versus Regional Stress Fields. (Under the direction of Dr. Paul K. Byrne). Alba Mons is a large shield volcano on Mars, the development of which appears to be responsible for tectonic landforms oriented radially and circumferentially to the shield. These landforms include those interpreted as extensional structures, such as normal faults and systems of graben. These structures, however, may also be associated with broader, regional stress field emanating from the volcano-tectonic Tharsis Rise, to the south of Alba Mons and centered on the equator. In this study, I report on structural and statistical analyses for normal faults proximal to Alba Mons (in a region spanning 95–120° W and 14–50° N) and test for systematic changes in fault properties with distance from the volcano and from Tharsis. A total of 11,767 faults were mapped for this study, and these faults were all measured for strike, length, and distance from Alba Mons and Tharsis. Additional properties were qualitatively and quantitatively analyzed within a subset of 62 faults, and model ages were obtained for two areas with crater statistics. Distinguishing traits for each structure population include fault properties such as strike, vertical displacement (i.e., throw) distribution profiles, displacement–length (Dmax/L) scaling, and spatial (i.e., cross-cutting) relationships with adjacent faults with different strikes. The only statistically significant correlation in these analyses was between study fault strike with distance from Tharsis. The lack of trends in the data suggest that one or more geological processes is obscuring the expected similarities in properties for these fault systems, such as volcanic resurfacing, mechanical restriction, or fault linkage.