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      Investigating Europa’s Habitability with the Europa Clipper

      review-article
      1 , , 2 , 3 , 4 , 4 , 1 , 5 , 6 , 6 , 7 , 6 , 8 , 9 , 1 , 10 , 1 , 1 , 1 , 3 , 11 , 1 , 12 , 1 , 13 , 14 , 12 , 15 , 16 , 1 , 17 , 18 , 1 , 1 , 19 , 20 , 9 , 1
      Space Science Reviews
      Springer Netherlands
      Europa, Ocean worlds, Ice, Habitability, Jupiter

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          Abstract

          The habitability of Europa is a property within a system, which is driven by a multitude of physical and chemical processes and is defined by many interdependent parameters, so that its full characterization requires collaborative investigation. To explore Europa as an integrated system to yield a complete picture of its habitability, the Europa Clipper mission has three primary science objectives: (1) characterize the ice shell and ocean including their heterogeneity, properties, and the nature of surface–ice–ocean exchange; (2) characterize Europa’s composition including any non-ice materials on the surface and in the atmosphere, and any carbon-containing compounds; and (3) characterize Europa’s geology including surface features and localities of high science interest. The mission will also address several cross-cutting science topics including the search for any current or recent activity in the form of thermal anomalies and plumes, performing geodetic and radiation measurements, and assessing high-resolution, co-located observations at select sites to provide reconnaissance for a potential future landed mission. Synthesizing the mission’s science measurements, as well as incorporating remote observations by Earth-based observatories, the James Webb Space Telescope, and other space-based resources, to constrain Europa’s habitability, is a complex task and is guided by the mission’s Habitability Assessment Board (HAB).

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          The rise of oxygen in Earth's early ocean and atmosphere.

          The rapid increase of carbon dioxide concentration in Earth's modern atmosphere is a matter of major concern. But for the atmosphere of roughly two-and-half billion years ago, interest centres on a different gas: free oxygen (O2) spawned by early biological production. The initial increase of O2 in the atmosphere, its delayed build-up in the ocean, its increase to near-modern levels in the sea and air two billion years later, and its cause-and-effect relationship with life are among the most compelling stories in Earth's history.
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                Author and article information

                Contributors
                Steven.D.Vance@jpl.nasa.gov
                Journal
                Space Sci Rev
                Space Sci Rev
                Space Science Reviews
                Springer Netherlands (Dordrecht )
                0038-6308
                1572-9672
                29 November 2023
                29 November 2023
                2023
                : 219
                : 8
                : 81
                Affiliations
                [1 ]GRID grid.20861.3d, ISNI 0000000107068890, Jet Propulsion Laboratory, , California Institute of Technology, ; Pasadena, CA USA
                [2 ]Applied Physics Laboratory, Johns Hopkins University, ( https://ror.org/00za53h95) Laurel, MD USA
                [3 ]School of Earth & Space Exploration and School of Molecular Sciences, Arizona State University, ( https://ror.org/03efmqc40) Tempe, AZ USA
                [4 ]Department of Astronomy and Department of Earth & Atmospheric Sciences, Cornell University, ( https://ror.org/05bnh6r87) Ithaca, NY USA
                [5 ]Department of Earth and Planetary Sciences and McDonnell Center for the Space Sciences, Washington University in St. Louis, ( https://ror.org/01yc7t268) Saint Louis, MO USA
                [6 ]School of Earth and Atmospheric Sciences, Georgia Institute of Technology, ( https://ror.org/01zkghx44) Atlanta, GA USA
                [7 ]Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, ( https://ror.org/03zbnzt98) Woods Hole, MA USA
                [8 ]Honeybee Robotics, ( https://ror.org/01yhhvk26) Altadena, CA USA
                [9 ]Institute for Geophysics, John A. and Katherine G. Jackson School of Geosciences, University of Texas at Austin, ( https://ror.org/00hj54h04) Austin, TX USA
                [10 ]Beyond Center, Arizona State University, ( https://ror.org/03efmqc40) Tempe, AZ USA
                [11 ]NASA Goddard Space Flight Center, ( https://ror.org/0171mag52) Greenbelt, MD USA
                [12 ]Southwest Research Institute, ( https://ror.org/03tghng59) San Antonio, TX USA
                [13 ]Planetary Science Institute, ( https://ror.org/05vvg9554) Tucson, AZ USA
                [14 ]Dept. of Earth and Environmental Sciences, University of Illinois Chicago, ( https://ror.org/02mpq6x41) Chicago, USA
                [15 ]GRID grid.5399.6, ISNI 0000 0001 2176 4817, Aix Marseille Université, CNRS, LAM (Laboratoire d’Astrophysique de Marseille), ; Marseille, France
                [16 ]Impacts and Astromaterials Research Centre, Department of Earth Science and Engineering, Imperial College London, ( https://ror.org/041kmwe10) London, United Kingdom
                [17 ]GRID grid.205975.c, ISNI 0000 0001 0740 6917, Department of Earth and Planetary Sciences, , University of California, ; Santa Cruz, CA USA
                [18 ]Lunar and Planetary Laboratory, University of Arizona, ( https://ror.org/03m2x1q45) Tucson, AZ USA
                [19 ]Department of Climate and Space Sciences and Engineering, University of Michigan, ( https://ror.org/00jmfr291) Ann Arbor, MI USA
                [20 ]Institut für Geologische Wissenschaften, Freie Universität Berlin, ( https://ror.org/046ak2485) Berlin, Germany
                Article
                1025
                10.1007/s11214-023-01025-2
                10687213
                38046182
                32846904-35e6-4c54-89d1-5ebb0f7b010a
                © The Author(s) 2023

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 22 October 2022
                : 3 November 2023
                Funding
                Funded by: FundRef http://dx.doi.org/10.13039/100020017, Planetary Science Division;
                Award ID: 80NM0018D0004
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100000781, European Research Council;
                Award ID: 724908-Habitat OASIS
                Award Recipient :
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                © Springer Nature B.V. 2023

                europa,ocean worlds,ice,habitability,jupiter
                europa, ocean worlds, ice, habitability, jupiter

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