5 results on '"Vance, Steven"'
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2. The NASA Roadmap to Ocean Worlds
- Author
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Hendrix, Amanda R, Hurford, Terry A, Barge, Laura M, Bland, Michael T, Bowman, Jeff S, Brinckerhoff, William, Buratti, Bonnie J, Cable, Morgan L, Castillo-Rogez, Julie, Collins, Geoffrey C, Diniega, Serina, German, Christopher R, Hayes, Alexander G, Hoehler, Tori, Hosseini, Sona, Howett, Carly JA, McEwen, Alfred S, Neish, Catherine D, Neveu, Marc, Nordheim, Tom A, Patterson, G Wesley, Patthoff, D Alex, Phillips, Cynthia, Rhoden, Alyssa, Schmidt, Britney E, Singer, Kelsi N, Soderblom, Jason M, and Vance, Steven D
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Astronomical Sciences ,Physical Sciences ,Life Below Water ,Exobiology ,Oceans and Seas ,Planets ,United States ,United States National Aeronautics and Space Administration ,Roadmap ,Enceladus ,Titan ,Europa ,Triton ,NASA ,NASA. ,Astronomical and Space Sciences ,Geochemistry ,Geology ,Astronomy & Astrophysics ,Astronomical sciences - Abstract
In this article, we summarize the work of the NASA Outer Planets Assessment Group (OPAG) Roadmaps to Ocean Worlds (ROW) group. The aim of this group is to assemble the scientific framework that will guide the exploration of ocean worlds, and to identify and prioritize science objectives for ocean worlds over the next several decades. The overarching goal of an Ocean Worlds exploration program as defined by ROW is to "identify ocean worlds, characterize their oceans, evaluate their habitability, search for life, and ultimately understand any life we find." The ROW team supports the creation of an exploration program that studies the full spectrum of ocean worlds, that is, not just the exploration of known ocean worlds such as Europa but candidate ocean worlds such as Triton as well. The ROW team finds that the confirmed ocean worlds Enceladus, Titan, and Europa are the highest priority bodies to target in the near term to address ROW goals. Triton is the highest priority candidate ocean world to target in the near term. A major finding of this study is that, to map out a coherent Ocean Worlds Program, significant input is required from studies here on Earth; rigorous Research and Analysis studies are called for to enable some future ocean worlds missions to be thoughtfully planned and undertaken. A second finding is that progress needs to be made in the area of collaborations between Earth ocean scientists and extraterrestrial ocean scientists.
- Published
- 2019
3. Ice-Ocean Exchange Processes in the Jovian and Saturnian Satellites
- Author
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Soderlund, Krista M., Kalousová, Klára, Buffo, Jacob J., Glein, Christopher R., Goodman, Jason C., Mitri, Giuseppe, Patterson, G. Wesley, Postberg, Frank, Rovira-Navarro, Marc, Rückriemen, Tina, Saur, Joachim, Schmidt, Britney E., Sotin, Christophe, Spohn, Tilman, Tobie, Gabriel, Van Hoolst, Tim, Vance, Steven D., and Vermeersen, Bert
- Published
- 2020
- Full Text
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4. Science Objectives for Flagship-Class Mission Concepts for the Search for Evidence of Life at Enceladus.
- Author
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MacKenzie, Shannon M., Neveu, Marc, Davila, Alfonso F., Lunine, Jonathan I., Cable, Morgan L., Phillips-Lander, Charity M., Eigenbrode, Jennifer L., Waite, J. Hunter, Craft, Kate L., Hofgartner, Jason D., McKay, Chris P., Glein, Christopher R., Burton, Dana, Kounaves, Samuel P., Mathies, Richard A., Vance, Steven D., Malaska, Michael J., Gold, Robert, German, Christopher R., and Soderlund, Krista M.
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SEA ice , *PLANETARY science , *UNDERWATER exploration , *ASTROBIOLOGY , *OCEAN - Abstract
Cassini revealed that Saturn's Moon Enceladus hosts a subsurface ocean that meets the accepted criteria for habitability with bio-essential elements and compounds, liquid water, and energy sources available in the environment. Whether these conditions are sufficiently abundant and collocated to support life remains unknown and cannot be determined from Cassini data. However, thanks to the plume of oceanic material emanating from Enceladus' south pole, a new mission to Enceladus could search for evidence of life without having to descend through kilometers of ice. In this article, we outline the science motivations for such a successor to Cassini, choosing the primary science goal to be determining whether Enceladus is inhabited and assuming a resource level equivalent to NASA's Flagship-class missions. We selected a set of potential biosignature measurements that are complementary and orthogonal to build a robust case for any life detection result. This result would be further informed by quantifications of the habitability of the environment through geochemical and geophysical investigations into the ocean and ice shell crust. This study demonstrates that Enceladus' plume offers an unparalleled opportunity for in situ exploration of an Ocean World and that the planetary science and astrobiology community is well equipped to take full advantage of it in the coming decades. [ABSTRACT FROM AUTHOR]
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- 2022
- Full Text
- View/download PDF
5. Geophysical Investigations of Habitability in Ice-Covered Ocean Worlds
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William T. Pike, Fabio Cammarano, Ralph D. Lorenz, Jennifer M. Jackson, Sharon Kedar, Gabriel Tobie, Christophe Sotin, Steven D. Vance, Bruce Banerdt, Simon Stähler, Bruce G. Bills, Mark P. Panning, Shunichi Kamata, Hsin-Hua Huang, Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Institute of Geophysics [ETH Zürich], Department of Earth Sciences [Swiss Federal Institute of Technology - ETH Zürich] (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), Dipartimento di Scienze Geologiche [Roma TRE], Università degli Studi Roma Tre, NASA, Jet Prop Lab, CALTECH, 4800 Oak Grove Dr, Pasadena, CA 91109 USA, Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Department of Electrical and Electronic Engineering [London] (DEEE), Imperial College London, Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan, Vance, Steven D., Panning, Mark P., Stähler, Simon, Cammarano, Fabio, Bills, Bruce G., Tobie, Gabriel, Kamata, Shunichi, Kedar, Sharon, Sotin, Christophe, Pike, William T., Lorenz, Ralph, Huang, Hsin-Hua, Jackson, Jennifer M., and Banerdt, Bruce
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Mineral hydration ,010504 meteorology & atmospheric sciences ,Ice V ,Geophysics ,01 natural sciences ,Jupiter ,symbols.namesake ,13. Climate action ,Space and Planetary Science ,Geochemistry and Petrology ,Lithosphere ,[SDU]Sciences of the Universe [physics] ,0103 physical sciences ,Earth and Planetary Sciences (miscellaneous) ,symbols ,Seawater ,14. Life underwater ,Love number ,Enceladus ,Titan (rocket family) ,010303 astronomy & astrophysics ,Geology ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences - Abstract
Geophysical measurements can reveal the structures and thermal states of icy ocean worlds. The interior density, temperature, sound speed, and electrical conductivity thus characterize their habitability. We explore the variability and correlation of these parameters using 1-D internal structure models. We invoke thermodynamic consistency using available thermodynamics of aqueous MgSO_4, NaCl (as seawater), and NH_3; pure water ice phases I, II, III, V, and VI; silicates; and any metallic core that may be present. Model results suggest, for Europa, that combinations of geophysical parameters might be used to distinguish an oxidized ocean dominated by MgSO_4 from a more reduced ocean dominated by NaCl. In contrast with Jupiter's icy ocean moons, Titan and Enceladus have low-density rocky interiors, with minimal or no metallic core. The low-density rocky core of Enceladus may comprise hydrated minerals or anhydrous minerals with high porosity. Cassini gravity data for Titan indicate a high tidal potential Love number (k_2 > 0.6), which requires a dense internal ocean (ρ_(ocean) >1,200 kg m^(−3)) and icy lithosphere thinner than 100 km. In that case, Titan may have little or no high-pressure ice, or a surprisingly deep water-rock interface more than 500 km below the surface, covered only by ice VI. Ganymede's water-rock interface is the deepest among known ocean worlds, at around 800 km. Its ocean may contain multiple phases of high-pressure ice, which will become buoyant if the ocean is sufficiently salty. Callisto's interior structure may be intermediate to those of Titan and Europa, with a water-rock interface 250 km below the surface covered by ice V but not ice VI.
- Published
- 2018
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