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Browse and search white papers and mission & technology studies received by the Planetary Science Decadal Survey. Click here for basic user instructions.
Total results: 198
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Dana M. Hurley
Co-Authors: David J. Lawrence, Raul Baragiola, D. Benjamin Bussey, Anthony Colaprete, M. Darby Dyar, Anthony F. Egan, Richard C. Elphic, William Farrell, William Feldman, James R. Gaier, Jacob Grimes, Jasper S. Halekas, Erika Harnett, James N. Head, Jennifer Heldmann, Amanda Hendrix, Charles A. Hibbitts, Kurt D. Retherford, Catherine Neish, Sarah Noble, Carle Pieters, Paul D. Spudis, Timothy J. Stubbs, Bradley J. Thomson, Kris Zacny
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Lunar Polar Volatiles and Associated Processes |
A landed/mobile mission to a lunar permanently shadowed region (PSR) should identify the composition, abundance, and distribution of volatiles in lunar PSRs. The next step is obtaining a detailed understanding of the transport/deposition/retention system to unravel the history of polar volatiles. |
Inner Planets: Mercury, Venus, and the Moon. |
Johns Hopkins University/
Applied Physics Laboratory |
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| Naoya Imae |
Supporting the sample return from Mars |
I heartfully indicate the support on the sample return mission from Mars, and the indispensable facilities in laboratories. Because the sample return mission is the keys of essential problems for Planetary Science. |
Mars: Not Phobos and Deimos. |
National Institute of Polar Research |
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Bruce Jakosky
Co-Authors: Richard W. Zurek, Jan Amend, Michael H. Carr, Daniel J. McCleese, John F. Mustard, Kenneth Nealson, Roger Summons |
Update: Are There Signs of Life on Mars? A Scientific Rationale for a Mars Sample-Return Campaign As The Next Step in Solar System Exploration |
Update: Discussion of the scientific rationale for Mars sample return as the next step in understanding solar-system exploration and Mars astrobiology. Sample return is discussed in the context of a Mars exploration program and the fiscal reality of the Mars program. |
Mars: Not Phobos and Deimos. |
University of Colorado |
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Jeffrey R. Johnson
Co-Authors: B. Archinal, R. Kirk, L. Gaddis, J. Anderson, B. Bussey, R. Beyer, L. Bleamaster, W. Patterson, J. Gillis-Davis, T. Watters, P. Schenk, B. Denevi |
The Importance of a Planetary Cartography Program: Status and Recommendations for NASA 2013-2023 |
We describe 7 areas where greater attention should be paid to data returned from planetary missions, beyond minimum “mission success”. The alternative is duplication of efforts and greater chances for errors, thereby diminishing the cost return and scientific potential provided by planetary data. |
Inner Planets: Mercury, Venus, and the Moon.
Mars: Not Phobos and Deimos.
Satellites: Galilean satellites, Titan, and the other satellites of the giant planets.
Primitive Bodies: Asteroids, comets, Phobos, Deimos, Pluto/Charon and other Kuiper belt objects, meteorites, and interplanetary dust. |
United States Geological Survey |
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Jeffrey R. Johnson
Co-Authors: Tori Hoehler, Frances Westall, Scot Rafkin, Paul Withers, Jeffrey Plescia, Victoria Hamilton, Abhi Tripathi, Darlene Lim |
Summary of the Mars Science Goals, Objectives, Investigations, and Priorities |
This document reflects the synthesis of recent MEPAG Goals Committee activities, MEPAG Science Analysis Groups, workshops, feedback, and discussion of these topics at recent MEPAG meetings. It was prepared by the MEPAG Goals and Executive Committees with assistance of many Mars community members. |
Mars: Not Phobos and Deimos. |
United States Geological Survey |
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Brad Jolliff
Co-Authors: Noah Petro, Leon Alkalai, Carlton Allen, Irene Antonenko, Lars Borg, William Bottke, Barbara Cohen, Michael Duke, Amy Fagan, Bernard Foing, Lisa Gaddis, John Gruener, Justin Hagerty, James Head III, Harold Hiesinger, Peter Isaacson, Randy Korotev, Georgiana Kramer, Samuel Lawrence, Gary Lofgren, Tomas Magna, Clive Neal, Marc Norman, Larry Nyquist, Gordon Osinski, Dimitri Papanastassiou, Carle Pieters, Bhairavi Shankar, Tim Swindle, G. Jeffrey Taylor, Allan Treiman, Paul Warren, Mark Wieczorek, Ryan Zeigler, Nicolle Zellner
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Constraining Solar System impact history and evolution of the terrestrial planets with exploration of and samples from the Moon’s South Pole-Aitken Basin |
A fundamental issue of Solar System science is determining the early history of the terrestrial planets, including giant impact bombardment and the evolution of differentiated crust. Exploration and sampling of the Moon’s South Pole–Aitken Basin can illuminate these formative planetary processes. |
Inner Planets: Mercury, Venus, and the Moon. |
Washington University,
Goddard Space Flight Center |
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Thomas D. Jones
Co-Authors: Rob R. Landis, David J. Korsmeyer, Paul A. Abell, Daniel R. Adamo |
Strengthening U.S. Exploration Policy via Human Expeditions to Near-Earth Objects |
By conducting a series of piloted Near-Earth Object (NEO) missions beginning about 2020, the U.S. will reinforce the scientific, economic, programmatic, operations, planetary defense, and public outreach elements of its human exploration program. |
Primitive Bodies: Asteroids, comets, Phobos, Deimos, Pluto/Charon and other Kuiper belt objects, meteorites, and interplanetary dust. |
Association of Space Explorers |
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| Rhawn Joseph |
Life on Earth Came From Other Planets |
Life on Earth Came From Other Planets, reviews the evidence presented in over 100 peer reviewed scientific papers published in prestigious scientific journals, and explains how life on Earth originated on other planets. The entire 45 page paper will be published in the journal, Cosmology, on 12/2009 |
None of the above. |
BrainMind.com |
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| Rhawn Joseph |
Life on Earth Came From Other Planets - 7 Page Summary/Press release |
If life were to appear on a desert island we wouldn''t claim it was assembled in an organic soup or created by God; we''d conclude it washed to shore or fell from the sky. The Earth too, is an island, orbiting in a sea of space and this is how life on our planet began. |
None of the above. |
BrainMind.com |
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| Michael J. Kavaya |
Mars Orbiting Pulsed Doppler Wind Lidar for Characterization of Wind and Dust |
Technology is described which is well developed and on a path for space. This technology could be used in Mars orbit to provide a global climatology of wind and relative dust as a function of location and altitude. |
Mars: Not Phobos and Deimos. |
NASA Langley Research Center |
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| Robert M. Kelso |
A commercially-leveraged, science-focused, lunar exploration program |
Summarizes the NASA work in assessing use of commercially-demonstrated landers and comm systems to enable early access to the lunar surface for science and exploration. |
Inner Planets: Mercury, Venus, and the Moon. |
NASA Headquarters |
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Krishan Khurana
Co-Authors: V. Angelopoulos, Charles W. Carlson, Gregory T. Delory, William M. Farrell, Robert E. Grimm, Ian Garrick-Bethell, Jasper S. Halekas, L. L. Hood, M. Horanyi, Robert J.Lillis, Robert P. Lin, Clive R. Neal, M. E. Purucker, Chris T. Russell, Gerry Schubert, D. G. Sibeck, Pavel Travnicek
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Lunar Science with ARTEMIS: A Journey from the Moon’s Exosphere to its Core [version 2] |
This white paper describes the planetary science objectives to be achieved by ARTEMIS, a two-spacecraft constellation en route to the Moon, and presents recommendations pertaining to future lunar science. [version 2] |
Inner Planets: Mercury, Venus, and the Moon. |
IGPP/UCLA |
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Georgiana Young Kramer
Co-Authors: David Blewett, Lon Hood, Jasper Halekas, Sarah Noble, Bernard Ray Hawke, Gunther Kletetschka, Erika Harnett, and Ian Garrick-Bethell |
The Lunar Swirls |
The lunar swirls are high albedo curvilinear surface features coincident with regions of strong remanent magnetism. Investigating the lunar swirls is important to understand the Earth-Moon system, the interaction of planetary surfaces with the solar wind, and how to best explore our solar system. |
Inner Planets: Mercury, Venus, and the Moon. |
Bear Fight Center |
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Kimberly R. Kuhlman
Co-Authors: Alberto Behar, Jack Jones, Penelope Boston, Jeffrey Antol, Gregory Hajos, Warren Kelliher, Max Coleman, Ronald Crawford, Lynn Rothschild, Martin Buehler, Greg Bearman, Daniel W. Wilson, Christopher P. McKay
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Tumbleweed: A New Paradigm for Surveying the Surface of Mars |
Tumbleweeds are lightweight, highly configurable and inexpensive wind-driven vehicles that could enable long-range surveys of the surface of Mars. Their analytical capabilities can be optimized for measurements for astrobiology or in situ resources over relatively large swaths of terrain. |
Mars: Not Phobos and Deimos. |
Planetary Science Institute |
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E. Robert Kursinski
Co-Authors: James Lyons, Claire Newman, Mark Richardson |
A Dual Satellite Mission Concept for Martian Climate and Chemistry |
mm-wavelength satellite to satellite occultations combined with solar occultation and thermal IR emission aerosol measurements will tightly and uniquely constrain processes to answer key open questions about the chemistry and climate of Mars. |
Mars: Not Phobos and Deimos. |
University of Arizona |
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Dante S. Lauretta
Co-Authors: Paul Abell, Carlton Allen, Ariel Anbar, Olivier Barnouin-Jha, M. Antonella Barucci, E. Beau Bierhaus,
Richard P. Binzel, William F. Bottke, Steven R. Chesley, Beth E. Clark, Edward Cloutis, Harold C. Connolly, Jr., Michael J. Drake, Jason P. Dworkin, M. Darby Dyar, Jack Farmer, Rebecca Ghent, Daniel P. Glavin, Nader Haghighipour, Vicky E. Hamilton, Carl W. Hergenrother, Kip Hodges, Lindsay P. Keller, Detlef Koschny, John Marshall, Scott Messenger, Steven Mielke, Keiko Nakamura-Messenger, Joseph A. Nuth, Dennis Reuter, Frans J. M. Rietmeijer, Kevin Righter, Waddell Robey, Michal Rozyczka, Nicolaus Copernicus, Farid Salama, Scott A. Sandford, Daniel J. Scheeres, Everett Shock,
Steve Vance, Brian D. Wade, Kosei E. Yamaguchi
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Astrobiology Research Priorities for Primitive Asteroids |
Study of primitive asteroids is fundamental to understanding the origin, distribution, and evolution of volatile and organic compounds in the early Solar System. This paper outlines six major research focus areas and recommends three mission concepts, which are listed in priority order. |
Primitive Bodies: Asteroids, comets, Phobos, Deimos, Pluto/Charon and other Kuiper belt objects, meteorites, and interplanetary dust. |
University of Arizona |
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Samuel J. Lawrence
Co-Authors: Georgiana Y. Kramer, Bradley L. Jolliff, B. Ray Hawke, Mark S. Robinson, Justin J. Hagerty, G. Jeffrey Taylor, Jeffrey Plescia, W. Brent Garry, Julie D. Stopar, Brett W. Denevi, S. E. Braden, L. R. Ostrach, David T. Blewett, Tomas Magna, Thomas R. Watters, Lisa R. Gaddis, Rongxing Li, Clive R. Neal, Jeffrey Gillis-Davis |
Sampling the Age Extremes of Lunar Volcanism: the Youngest and Oldest Lunar Basalts |
Automated sample return missions to the youngest (Procellarum) and oldest (cryptomaria) basalts on the lunar surface will help improve our absolute chronology for the inner Solar System by providing the timing for the beginning and end of lunar basaltic volcanism. |
Inner Planets: Mercury, Venus, and the Moon. |
Arizona State University |
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Robert J. Lillis
Co-Authors: J. Arkani-Hamed, D. A. Brain, J. C. Cain, J. E. P. Connerney, G. T. Delory, J. Espley, M. Fuller, J. Gattecceca, J. S. Halekas, L. L. Hood, C. L. Johnson, D. Jurdy, G. Kletetschka, B. Langlais, R. P. Lin, K. L. Louzada, M. Manga, C. Milbury, D. Mozzoni, M. Purucker, D. Ravat, J. H. Roberts, P. Rochette, C.T. Russell, S. Smrekar, S. T. Stewart, S. Vennerstrom, B. P. Weiss, K. Whaler |
Mars'' Ancient Dynamo and Crustal Remanent Magnetism |
Mars'' crustal magnetization is unique and enigmatic. It is pertinent to Mars science questions as diverse as the structure of the interior and the evolution of climate. To study it, we recommend 1) extending the MAVEN mission, 2) rover-mounted surface magnetometers and 3) oriented sample return. |
Mars: Not Phobos and Deimos. |
University of California Berkeley |
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Sanjay S. Limaye
Co-Authors: Mark Allen, Sushil Atreya, Kevin H. Baines, Jean-Loup Bertaux, Gordon Bjoraker, Jacques Blamont, Mark Bullock, Eric Chassefiere, Gordon Chin, Curt Covey, David Grinspoon, Samuel Gulkis, Viktor Kerzhanovich, Stephen Lewis, Kevin McGouldrick, W. J. Markiewicz, Rosalyn A. Pertzborn, Christopher Rozoff, Giuseppe Piccioni, Gerald Schubert, Lawrence A. Sromovsky, Colin F. Wilson, Yuk Yung |
Venus Atmosphere: Major Questions and Required Observations |
This paper describes the major questions about the atmosphere of Venus and the observations required to understand it. “How Does Venus atmosphere work?” A dedicated and renewed exploration effort is required to address this fundamental question. Key questions requiring new observations include: H |
Inner Planets: Mercury, Venus, and the Moon. |
University of Wiscosin - Madison |
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Amy S. Lo
Co-Authors: Howard Eller, Dean Dailey, Eric Drucker, James Wehner |
Secondary Payloads Using LCROSS Architecture |
The ESPA architecture used by the LCROSS mission enables two capable missions for the cost of one launch. This paper describes our approach for leveraging the capability of the new generation of EELVs to enable secondary planetary missions at well below the cost of an independently launched mission. |
Inner Planets: Mercury, Venus, and the Moon.
Mars: Not Phobos and Deimos.
Primitive Bodies: Asteroids, comets, Phobos, Deimos, Pluto/Charon and other Kuiper belt objects, meteorites, and interplanetary dust. |
Northrop Grumman Aerospace Systems |
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These documents have been prepared in coordination with the National Academies of Science in support of the National Academies Planetary Science Decadal Survey. These documents are being made available for information purposes only, and any views and opinions expressed herein do not necessarily state or reflect those of NASA, JPL, or the California Institute of Technology.
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