Characterizing Habitable Exo-Moons
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Exomoon Habitability Constrained by Illumination and Tidal Heating
submitted to Astrobiology: April 6, 2012 accepted by Astrobiology: September 8, 2012 published in Astrobiology: January 24, 2013 this updated draft: October 30, 2013 doi:10.1089/ast.2012.0859 Exomoon habitability constrained by illumination and tidal heating René HellerI , Rory BarnesII,III I Leibniz-Institute for Astrophysics Potsdam (AIP), An der Sternwarte 16, 14482 Potsdam, Germany, [email protected] II Astronomy Department, University of Washington, Box 951580, Seattle, WA 98195, [email protected] III NASA Astrobiology Institute – Virtual Planetary Laboratory Lead Team, USA Abstract The detection of moons orbiting extrasolar planets (“exomoons”) has now become feasible. Once they are discovered in the circumstellar habitable zone, questions about their habitability will emerge. Exomoons are likely to be tidally locked to their planet and hence experience days much shorter than their orbital period around the star and have seasons, all of which works in favor of habitability. These satellites can receive more illumination per area than their host planets, as the planet reflects stellar light and emits thermal photons. On the contrary, eclipses can significantly alter local climates on exomoons by reducing stellar illumination. In addition to radiative heating, tidal heating can be very large on exomoons, possibly even large enough for sterilization. We identify combinations of physical and orbital parameters for which radiative and tidal heating are strong enough to trigger a runaway greenhouse. By analogy with the circumstellar habitable zone, these constraints define a circumplanetary “habitable edge”. We apply our model to hypothetical moons around the recently discovered exoplanet Kepler-22b and the giant planet candidate KOI211.01 and describe, for the first time, the orbits of habitable exomoons. -
The Subsurface Habitability of Small, Icy Exomoons J
A&A 636, A50 (2020) Astronomy https://doi.org/10.1051/0004-6361/201937035 & © ESO 2020 Astrophysics The subsurface habitability of small, icy exomoons J. N. K. Y. Tjoa1,?, M. Mueller1,2,3, and F. F. S. van der Tak1,2 1 Kapteyn Astronomical Institute, University of Groningen, Landleven 12, 9747 AD Groningen, The Netherlands e-mail: [email protected] 2 SRON Netherlands Institute for Space Research, Landleven 12, 9747 AD Groningen, The Netherlands 3 Leiden Observatory, Leiden University, Niels Bohrweg 2, 2300 RA Leiden, The Netherlands Received 1 November 2019 / Accepted 8 March 2020 ABSTRACT Context. Assuming our Solar System as typical, exomoons may outnumber exoplanets. If their habitability fraction is similar, they would thus constitute the largest portion of habitable real estate in the Universe. Icy moons in our Solar System, such as Europa and Enceladus, have already been shown to possess liquid water, a prerequisite for life on Earth. Aims. We intend to investigate under what thermal and orbital circumstances small, icy moons may sustain subsurface oceans and thus be “subsurface habitable”. We pay specific attention to tidal heating, which may keep a moon liquid far beyond the conservative habitable zone. Methods. We made use of a phenomenological approach to tidal heating. We computed the orbit averaged flux from both stellar and planetary (both thermal and reflected stellar) illumination. We then calculated subsurface temperatures depending on illumination and thermal conduction to the surface through the ice shell and an insulating layer of regolith. We adopted a conduction only model, ignoring volcanism and ice shell convection as an outlet for internal heat. -
Giant Planet Effects on Terrestrial Planet Formation and System Architecture
MNRAS 485, 541–549 (2019) doi:10.1093/mnras/stz385 Advance Access publication 2019 February 8 Giant planet effects on terrestrial planet formation and system architecture 1‹ 2 2,3 1 Anna C. Childs, Elisa Quintana, Thomas Barclay and Jason H. Steffen Downloaded from https://academic.oup.com/mnras/article-abstract/485/1/541/5309996 by NASA Goddard Space Flight Ctr user on 15 April 2020 1Department of Physics and Astronomy, University of Nevada, Las Vegas, NV 89154, USA 2NASA Goddard Space Flight Center, 8800 Greenbelt Road, Greenbelt, MD 20771, USA 3University of Maryland, Baltimore County, 1000 Hilltop Cir, Baltimore, MD 21250, USA Accepted 2019 February 4. Received 2019 January 16; in original form 2018 July 6 ABSTRACT Using an updated collision model, we conduct a suite of high-resolution N-body integrations to probe the relationship between giant planet mass and terrestrial planet formation and system architecture. We vary the mass of the planets that reside at Jupiter’s and Saturn’s orbit and examine the effects on the interior terrestrial system. We find that massive giant planets are more likely to eject material from the outer edge of the terrestrial disc and produce terrestrial planets that are on smaller, more circular orbits. We do not find a strong correlation between exterior giant planet mass and the number of Earth analogues (analogous in mass and semimajor axis) produced in the system. These results allow us to make predictions on the nature of terrestrial planets orbiting distant Sun-like star systems that harbour giant planet companions on long orbits – systems that will be a priority for NASA’s upcoming Wide-Field Infrared Survey Telescope (WFIRST) mission. -
Outer Planets: the Ice Giants
Outer Planets: The Ice Giants A. P. Ingersoll, H. B. Hammel, T. R. Spilker, R. E. Young Exploring Uranus and Neptune satisfies NASA’s objectives, “investigation of the Earth, Moon, Mars and beyond with emphasis on understanding the history of the solar system” and “conduct robotic exploration across the solar system for scientific purposes.” The giant planet story is the story of the solar system (*). Earth and the other small objects are leftovers from the feast of giant planet formation. As they formed, the giant planets may have migrated inward or outward, ejecting some objects from the solar system and swallowing others. The giant planets most likely delivered water and other volatiles, in the form of icy planetesimals, to the inner solar system from the region around Neptune. The “gas giants” Jupiter and Saturn are mostly hydrogen and helium. These planets must have swallowed a portion of the solar nebula intact. The “ice giants” Uranus and Neptune are made primarily of heavier stuff, probably the next most abundant elements in the Sun – oxygen, carbon, nitrogen, and sulfur. For each giant planet the core is the “seed” around which it accreted nebular gas. The ice giants may be more seed than gas. Giant planets are laboratories in which to test our theories about geophysics, plasma physics, meteorology, and even oceanography in a larger context. Their bottomless atmospheres, with 1000 mph winds and 100 year-old storms, teach us about weather on Earth. The giant planets’ enormous magnetic fields and intense radiation belts test our theories of terrestrial and solar electromagnetic phenomena. -
Activity 16: Planets and Their Features Mercury Mercury Is an Extreme Planet
Activity 16: Planets And Their Features Mercury Mercury.is.an.extreme.planet..It.is.the.fastest.of.all.the.planets..It.is.one.of.the.hottest. planets,.and.it.is.also.one.of.the.coldest!.It.may.be.the.site.of.the.largest.crash.in.the. history.of.the.solar.system..Mercury.may.also.have.the.strangest.view.of.the.sun.in.the. whole.universe! Mercury.zooms.around.the.sun.at.a.speed.of.48.kilometres.per.second,.or.half.as.fast. again.as.the.Earth.travels. At.certain.times.and.places,.Mercury’s.surface.temperature.can.rise.to.twice.the. temperature.inside.an.oven.when.you.are.baking.a.cake..On.the.other.hand,.in.the. shadow.of.its.North.Pole.craters,.Mercury.has.ice.like.our.North.Pole.does. Since.Mercury.is.so.close.to.the.sun,.we.have.never.been.able.to.see.it.in.any.detail..Even. with.the.most.powerful.telescope,.Mercury.looks.like.a.blurry.white.ball..It.wasn’t.until.1974. that.we.really.began.to.learn.about.Mercury..In.1974.and.1975,.Mariner.10.flew.by.Mercury.three.times.and.sent.back. about.12,000.images. These.pictures.combined.to.give.a.map.of.about.45%.of.Mercury’s.surface,.and.what.they.show.us.is.a.planet.covered. with.craters,.much.like.our.moon..Mercury’s.largest.land.feature.is.the.Caloris.Basin,.a.crater.formed.by.a.collision.with.a. meteorite.long.ago..The.size.of.the.Caloris.Basin,.about.1350.kilometres.in.diameter,.suggests.that.this.may.have.been. -
Abstracts of the 50Th DDA Meeting (Boulder, CO)
Abstracts of the 50th DDA Meeting (Boulder, CO) American Astronomical Society June, 2019 100 — Dynamics on Asteroids break-up event around a Lagrange point. 100.01 — Simulations of a Synthetic Eurybates 100.02 — High-Fidelity Testing of Binary Asteroid Collisional Family Formation with Applications to 1999 KW4 Timothy Holt1; David Nesvorny2; Jonathan Horner1; Alex B. Davis1; Daniel Scheeres1 Rachel King1; Brad Carter1; Leigh Brookshaw1 1 Aerospace Engineering Sciences, University of Colorado Boulder 1 Centre for Astrophysics, University of Southern Queensland (Boulder, Colorado, United States) (Longmont, Colorado, United States) 2 Southwest Research Institute (Boulder, Connecticut, United The commonly accepted formation process for asym- States) metric binary asteroids is the spin up and eventual fission of rubble pile asteroids as proposed by Walsh, Of the six recognized collisional families in the Jo- Richardson and Michel (Walsh et al., Nature 2008) vian Trojan swarms, the Eurybates family is the and Scheeres (Scheeres, Icarus 2007). In this theory largest, with over 200 recognized members. Located a rubble pile asteroid is spun up by YORP until it around the Jovian L4 Lagrange point, librations of reaches a critical spin rate and experiences a mass the members make this family an interesting study shedding event forming a close, low-eccentricity in orbital dynamics. The Jovian Trojans are thought satellite. Further work by Jacobson and Scheeres to have been captured during an early period of in- used a planar, two-ellipsoid model to analyze the stability in the Solar system. The parent body of the evolutionary pathways of such a formation event family, 3548 Eurybates is one of the targets for the from the moment the bodies initially fission (Jacob- LUCY spacecraft, and our work will provide a dy- son and Scheeres, Icarus 2011). -
Simon Porter , Will Grundy
Post-Capture Evolution of Potentially Habitable Exomoons Simon Porter1,2, Will Grundy1 1Lowell Observatory, Flagstaff, Arizona 2School of Earth and Space Exploration, Arizona State University [email protected] and spin vector were initially pointed at random di- Table 1: Relative fraction of end states for fully Abstract !"# $%& " '(" !"# $%& # '(# rections on the sky. The exoplanets had a ran- evolved exomoon systems dom obliquity < 5 deg and was at a stellarcentric The satellites of extrasolar planets (exomoons) Star Planet Moon Survived Retrograde Separated Impacted distance such that the equilibrium temperature was have been recently proposed as astrobiological tar- Earth 43% 52% 21% 35% equal to Earth. The simulations were run until they Jupiter Mars 44% 45% 18% 37% gets. Triton has been proposed to have been cap- 5 either reached an eccentricity below 10 or the pe- Titan 42% 47% 21% 36% tured through a momentum-exchange reaction [1], − Sun Earth 52% 44% 17% 30% riapse went below the Roche limit (impact) or the and it is possible that a similar event could allow Neptune Mars 44% 45% 18% 36% apoapse exceeded the Hill radius. Stars used were Titan 45% 47% 19% 35% a giant planet to capture a formerly binary terres- Earth 65% 47% 3% 31% the Sun (G2), a main-sequence F0 (1.7 MSun), trial planet or planetesimal. We therefore attempt to Jupiter Mars 59% 46% 4% 35% and a main-sequence M0 (0.47 MSun). Exoplan- Titan 61% 48% 3% 34% model the dynamical evolution of a terrestrial planet !"# $%& " !"# $%& " ' F0 ets used had the mass of either Jupiter or Neptune, Earth 77% 44% 4% 18% captured into orbit around a giant planet in the hab- and exomoons with the mass of Earth, Mars, and Neptune Mars 67% 44% 4% 28% itable zone of a star. -
Gravitational Microlensing by Exoplanets and Exomoons
INTERNATIONAL SPACE SCIENCE INSTITUTE SPATIUM Published by the Association Pro ISSI No. 45, May 2020 Gravitational Microlensing by Exoplanets and Exomoons 200216_Spatium_45_2020_(001_016).indd 1 16.05.20 11:11 Editorial Since Copernicus (1473–1543) was world view abruptly. They seemed not able to measure brightness not to be inhabited as previously Impressum variations of the stars due to Earth’s assumed, and life appeared not to revolutionary motion around the be a matter of course. Astrophys- Sun, he inferred that stars must be ics and interdisciplinary science ISSN 2297–5888 (Print) very far away from Earth. During recognised the very special condi- ISSN 2297–590X (Online) the 16th and 17th Centuries schol- tions required to create life. More- ars began gradually to realise that over, these conditions need to be Spatium the Universe, i.e., the sphere of very selective and restricting, de- Published by the fixed stars enclosing our Solar pending not only on physical and Association Pro ISSI System, might not be finite but chemical parameters but particu- infinite. Philosophical arguments larly on stable and stabilising hab- by Thomas Digges (1546–1595) or itable environments in space and Giordano Bruno (1548–1600) sup- on ground. ported this view. Galileo (1564– Today, the existence of extra-ter- Association Pro ISSI 1642) provided evidence from ob- restrial life seems to be quite likely Hallerstrasse 6, CH-3012 Bern servations of the Milky Way using for statistical reasons. However, it Phone +41 (0)31 631 48 96 his telescope. is very hard to find evidence from see In his Cosmotheoros posthumously bio-markers identified in exoplan- www.issibern.ch/pro-issi.html published in 1698, Christiaan Huy- etary spectra as long as it is not clear for the whole Spatium series gens (1629–1695) estimated the dis- what life actually is. -
The Nature of the Giant Exomoon Candidate Kepler-1625 B-I René Heller
A&A 610, A39 (2018) https://doi.org/10.1051/0004-6361/201731760 Astronomy & © ESO 2018 Astrophysics The nature of the giant exomoon candidate Kepler-1625 b-i René Heller Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077 Göttingen, Germany e-mail: [email protected] Received 11 August 2017 / Accepted 21 November 2017 ABSTRACT The recent announcement of a Neptune-sized exomoon candidate around the transiting Jupiter-sized object Kepler-1625 b could indi- cate the presence of a hitherto unknown kind of gas giant moon, if confirmed. Three transits of Kepler-1625 b have been observed, allowing estimates of the radii of both objects. Mass estimates, however, have not been backed up by radial velocity measurements of the host star. Here we investigate possible mass regimes of the transiting system that could produce the observed signatures and study them in the context of moon formation in the solar system, i.e., via impacts, capture, or in-situ accretion. The radius of Kepler-1625 b suggests it could be anything from a gas giant planet somewhat more massive than Saturn (0:4 MJup) to a brown dwarf (BD; up to 75 MJup) or even a very-low-mass star (VLMS; 112 MJup ≈ 0:11 M ). The proposed companion would certainly have a planetary mass. Possible extreme scenarios range from a highly inflated Earth-mass gas satellite to an atmosphere-free water–rock companion of about +19:2 180 M⊕. Furthermore, the planet–moon dynamics during the transits suggest a total system mass of 17:6−12:6 MJup. -
On the Detection of Exomoons in Photometric Time Series
On the Detection of Exomoons in Photometric Time Series Dissertation zur Erlangung des mathematisch-naturwissenschaftlichen Doktorgrades “Doctor rerum naturalium” der Georg-August-Universität Göttingen im Promotionsprogramm PROPHYS der Georg-August University School of Science (GAUSS) vorgelegt von Kai Oliver Rodenbeck aus Göttingen, Deutschland Göttingen, 2019 Betreuungsausschuss Prof. Dr. Laurent Gizon Max-Planck-Institut für Sonnensystemforschung, Göttingen, Deutschland und Institut für Astrophysik, Georg-August-Universität, Göttingen, Deutschland Prof. Dr. Stefan Dreizler Institut für Astrophysik, Georg-August-Universität, Göttingen, Deutschland Dr. Warrick H. Ball School of Physics and Astronomy, University of Birmingham, UK vormals Institut für Astrophysik, Georg-August-Universität, Göttingen, Deutschland Mitglieder der Prüfungskommision Referent: Prof. Dr. Laurent Gizon Max-Planck-Institut für Sonnensystemforschung, Göttingen, Deutschland und Institut für Astrophysik, Georg-August-Universität, Göttingen, Deutschland Korreferent: Prof. Dr. Stefan Dreizler Institut für Astrophysik, Georg-August-Universität, Göttingen, Deutschland Weitere Mitglieder der Prüfungskommission: Prof. Dr. Ulrich Christensen Max-Planck-Institut für Sonnensystemforschung, Göttingen, Deutschland Dr.ir. Saskia Hekker Max-Planck-Institut für Sonnensystemforschung, Göttingen, Deutschland Dr. René Heller Max-Planck-Institut für Sonnensystemforschung, Göttingen, Deutschland Prof. Dr. Wolfram Kollatschny Institut für Astrophysik, Georg-August-Universität, Göttingen, -
Fifth Giant Ex-Planet of the Solar System: Characteristics and Remnants
Fifth giant ex-planet of the Solar System: characteristics and remnants Yury I. Rogozin* Abstract In recent years it has coming to light that the early outer Solar System likely might have somewhat more planets than today. However, to date there is unknown what a former giant planet might in fact have represented and where its orbit may certainly have located. Using the originally suggested relations, we have found the reasonable orbital and physical characteristics of the icy giant ex-planet, which in the past may have orbited the Sun about in the halfway between Saturn and Uranus. Validity of the results obtained here is supported by a feasibility of these relations to other objects of the outer Solar System. A possible linkage between the fifth giant ex-planet and the puzzling objects of the outer Solar System such as the Saturn’s rings and the irregular moons Triton and Phoebe existing today is briefly discussed. Keywords: planets and satellites; individuals: fifth giant ex-planet, Saturn´s rings, Triton, Phoebe 1 Introduction According to the existing ideas of the formation of the Solar System its planetary structure is held unchanged during about 4.5 billion years. Such a static situation of the things had been embodied, particularly, in offered in 1766 Titius-Bode’s rule of the orbital distances for known at that time the seven planets from Mercury to Uranus. As it is known, the conformity to this rule for planets Neptune and Pluto discovered subsequently has appeared much worse than for before known seven planets. However, the essential departures of the real orbital distances from this rule for these two planets so far have not obtained any explained justifying within the framework of such conservative insights into a structure of the Solar System. -
THE SEARCH for EXOMOON RADIO EMISSIONS by JOAQUIN P. NOYOLA Presented to the Faculty of the Graduate School of the University Of
THE SEARCH FOR EXOMOON RADIO EMISSIONS by JOAQUIN P. NOYOLA Presented to the Faculty of the Graduate School of The University of Texas at Arlington in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY THE UNIVERSITY OF TEXAS AT ARLINGTON December 2015 Copyright © by Joaquin P. Noyola 2015 All Rights Reserved ii Dedicated to my wife Thao Noyola, my son Layton, my daughter Allison, and our future little ones. iii Acknowledgements I would like to express my sincere gratitude to all the people who have helped throughout my career at UTA, including my advising professors Dr. Zdzislaw Musielak (Ph.D.), and Dr. Qiming Zhang (M.Sc.) for their advice and guidance. Many thanks to my committee members Dr. Andrew Brandt, Dr. Manfred Cuntz, and Dr. Alex Weiss for your interest and for your time. Also many thanks to Dr. Suman Satyal, my collaborator and friend, for all the fruitful discussions we have had throughout the years. I would like to thank my wife, Thao Noyola, for her love, her help, and her understanding through these six years of marriage and graduate school. October 19, 2015 iv Abstract THE SEARCH FOR EXOMOON RADIO EMISSIONS Joaquin P. Noyola, PhD The University of Texas at Arlington, 2015 Supervising Professor: Zdzislaw Musielak The field of exoplanet detection has seen many new developments since the discovery of the first exoplanet. Observational surveys by the NASA Kepler Mission and several other instrument have led to the confirmation of over 1900 exoplanets, and several thousands of exoplanet potential candidates. All this progress, however, has yet to provide the first confirmed exomoon.