Christopher W. Hamilton, Alfred S. McEwen, Laszlo Keszthelyi, Lynn M. Carter, Ashley G. Davies, Katherine de Kleer, Kandis Lea Jessup, Xianzhe Jia, James T. Keane, Kathleen Mandt, Francis Nimmo, Chris Paranicas, Ryan S. Park, Jason E. Perry, Anne Pommier, Jani Radebaugh, Sarah S. Sutton, Audrey Vorburger, Peter Wurz, Cauê Borlina, Amanda F. Haapala, Daniella N. DellaGiustina, Brett W. Denevi, Sarah M. Hörst, Sascha Kempf, Krishan K. Khurana, Justin J. Likar, Adam Masters, Olivier Mousis, Anjani T. Polit, Aditya Bhushan, Michael Bland, Isamu Matsuyama, John Spencer
{"title":"Comparing NASA Discovery and New Frontiers Class Mission Concepts for the Io Volcano Observer (IVO)","authors":"Christopher W. Hamilton, Alfred S. McEwen, Laszlo Keszthelyi, Lynn M. Carter, Ashley G. Davies, Katherine de Kleer, Kandis Lea Jessup, Xianzhe Jia, James T. Keane, Kathleen Mandt, Francis Nimmo, Chris Paranicas, Ryan S. Park, Jason E. Perry, Anne Pommier, Jani Radebaugh, Sarah S. Sutton, Audrey Vorburger, Peter Wurz, Cauê Borlina, Amanda F. Haapala, Daniella N. DellaGiustina, Brett W. Denevi, Sarah M. Hörst, Sascha Kempf, Krishan K. Khurana, Justin J. Likar, Adam Masters, Olivier Mousis, Anjani T. Polit, Aditya Bhushan, Michael Bland, Isamu Matsuyama, John Spencer","doi":"arxiv-2408.08334","DOIUrl":null,"url":null,"abstract":"Jupiter's moon Io is a highly compelling target for future exploration that\noffers critical insight into tidal dissipation processes and the geology of\nhigh heat flux worlds, including primitive planetary bodies, such as the early\nEarth, that are shaped by enhanced rates of volcanism. Io is also important for\nunderstanding the development of volcanogenic atmospheres and mass-exchange\nwithin the Jupiter System. However, fundamental questions remain about the\nstate of Io's interior, surface, and atmosphere, as well as its role in the\nevolution of the Galilean satellites. The Io Volcano Observer (IVO) would\naddress these questions by achieving the following three key goals: (A)\nDetermine how and where tidal heat is generated inside Io; (B) Understand how\ntidal heat is transported to the surface of Io; and (C) Understand how Io is\nevolving. IVO was selected for Phase A study through the NASA Discovery program\nin 2020 and, in anticipation of a New Frontiers 5 opportunity, an enhanced\nIVO-NF mission concept was advanced that would increase the Baseline mission\nfrom 10 flybys to 20, with an improved radiation design; employ a Ka-band\ncommunications to double IVO's total data downlink; add a wide angle camera for\ncolor and stereo mapping; add a dust mass spectrometer; and lower the altitude\nof later flybys to enable new science. This study compares and contrasts the\nmission architecture, instrument suite, and science objectives for Discovery\n(IVO) and New Frontiers (IVO-NF) missions to Io, and advocates for continued\nprioritization of Io as an exploration target for New Frontiers.","PeriodicalId":501423,"journal":{"name":"arXiv - PHYS - Space Physics","volume":"205 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-08-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Space Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2408.08334","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Jupiter's moon Io is a highly compelling target for future exploration that
offers critical insight into tidal dissipation processes and the geology of
high heat flux worlds, including primitive planetary bodies, such as the early
Earth, that are shaped by enhanced rates of volcanism. Io is also important for
understanding the development of volcanogenic atmospheres and mass-exchange
within the Jupiter System. However, fundamental questions remain about the
state of Io's interior, surface, and atmosphere, as well as its role in the
evolution of the Galilean satellites. The Io Volcano Observer (IVO) would
address these questions by achieving the following three key goals: (A)
Determine how and where tidal heat is generated inside Io; (B) Understand how
tidal heat is transported to the surface of Io; and (C) Understand how Io is
evolving. IVO was selected for Phase A study through the NASA Discovery program
in 2020 and, in anticipation of a New Frontiers 5 opportunity, an enhanced
IVO-NF mission concept was advanced that would increase the Baseline mission
from 10 flybys to 20, with an improved radiation design; employ a Ka-band
communications to double IVO's total data downlink; add a wide angle camera for
color and stereo mapping; add a dust mass spectrometer; and lower the altitude
of later flybys to enable new science. This study compares and contrasts the
mission architecture, instrument suite, and science objectives for Discovery
(IVO) and New Frontiers (IVO-NF) missions to Io, and advocates for continued
prioritization of Io as an exploration target for New Frontiers.