Comparative Planetology of Exoplanets and the Solar System
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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. -
OCEANOGRAPHY an Additional 1.4 Tg of Carbon Per Year Atmospheric CO2 Concentrations from Ice Loss and Ocean Life Over This Period
research highlights OCEANOGRAPHY an additional 1.4 Tg of carbon per year atmospheric CO2 concentrations from Ice loss and ocean life over this period. A rise in phytoplankton Antarctic ice cores. They found that Glob. Biogeochem. Cycles http://doi.org/p27 (2013) productivity in the surface waters of the two younger periods of enhanced the Laptev, East Siberian, Chukchi and mixing coincided with a steep increase in Beaufort seas was responsible for the atmospheric CO2 levels, and the oldest with increase in carbon uptake. In contrast, net a small, temporary rise. carbon uptake declined in the Barents Sea, The team concluded that enhanced where a warming-induced outgassing of vertical mixing in these intervals brought surface-water CO2 countered the rise in CO2-rich waters from the deep ocean to the primary production. surface, allowing CO2 to escape from these The findings suggest that the continued upwelled waters to the atmosphere. AN decline of Arctic sea ice cover could be accompanied by a rise in the oceanic uptake PLANETARY SCIENCE of carbon dioxide, although uncertainties Weighing Phobos in the response of physical, chemical and Icarus http://doi.org/p26 (2013) biological processes to sea ice loss hinder reliable predictions at this stage. AA PALAEOCEANOGRAPHY Southern upwelling Nature Commun. 4, 2758 (2013). At the end of the last glacial period about 20,000 years ago, atmospheric CO2 concentrations rose in several steps. Radiocarbon measurements from a marine sediment core suggest that the upwelling of © FRANS LANTING STUDIO / ALAMY © FRANS LANTING STUDIO carbon-rich waters in the Southern Ocean contributed to the CO2 rise. -
A Review of Possible Planetary Atmospheres in the TRAPPIST-1 System
Space Sci Rev (2020) 216:100 https://doi.org/10.1007/s11214-020-00719-1 A Review of Possible Planetary Atmospheres in the TRAPPIST-1 System Martin Turbet1 · Emeline Bolmont1 · Vincent Bourrier1 · Brice-Olivier Demory2 · Jérémy Leconte3 · James Owen4 · Eric T. Wolf5 Received: 14 January 2020 / Accepted: 4 July 2020 / Published online: 23 July 2020 © The Author(s) 2020 Abstract TRAPPIST-1 is a fantastic nearby (∼39.14 light years) planetary system made of at least seven transiting terrestrial-size, terrestrial-mass planets all receiving a moderate amount of irradiation. To date, this is the most observationally favourable system of po- tentially habitable planets known to exist. Since the announcement of the discovery of the TRAPPIST-1 planetary system in 2016, a growing number of techniques and approaches have been used and proposed to characterize its true nature. Here we have compiled a state- of-the-art overview of all the observational and theoretical constraints that have been ob- tained so far using these techniques and approaches. The goal is to get a better understanding of whether or not TRAPPIST-1 planets can have atmospheres, and if so, what they are made of. For this, we surveyed the literature on TRAPPIST-1 about topics as broad as irradiation environment, planet formation and migration, orbital stability, effects of tides and Transit Timing Variations, transit observations, stellar contamination, density measurements, and numerical climate and escape models. Each of these topics adds a brick to our understand- ing of the likely—or on the contrary unlikely—atmospheres of the seven known planets of the system. -
The Detectability and Constraints of Biosignature Gasses in the Near & Mid-Infrared from Transit Transmission Spectroscopy B
The Detectability and Constraints of Biosignature Gasses in the Near & Mid-Infrared from Transit Transmission Spectroscopy by Luke Tremblay A Thesis Presented in Partial Fulfillment of the Requirements for the Degree Master of Science Approved November 2019 by the Graduate Supervisory Committee: Michael Line, Chair Evgenya Schkolnik Sara Walker ARIZONA STATE UNIVERSITY December 2019 ABSTRACT The James Webb Space Telescope (JWST ) is expected to revolutionize the cur- rent understanding of Jovian worlds over the coming decade. However, as the field pushes towards characterizing cooler, smaller, \terrestrial-like" planets, dedicated next-generation facilities will be required to tease out the small spectral signatures indicative of biological activity. Here, the feasibility of determining atmospheric prop- erties, from near to mid-infrared transmission spectra, of transiting temperate ter- restrial M-dwarf companions, has been evaluated. Specifically, atmospheric retrievals were utilized to explore the trade space between spectral resolution, wavelength cover- age, and signal-to-noise on the ability to both detect molecular species and constrain their abundances. Increasing spectral resolution beyond R=100 for near-infrared wavelengths, shorter than 5µm, proves to reduce the degeneracy between spectral features of different molecules and thus greatly benefits the abundance constraints. However, this benefit is greatly diminished beyond 5µm as any overlap between broad features in the mid-infrared does not deconvolve with higher resolutions. Additionally, the inclusion of features beyond 11µm did not meaningfully improve the detection sig- nificance nor abundance constraints results. The findings of this study indicate that an instrument with continuous wavelength coverage from approximately 2-11µm and with a resolution of R'50-300, would be capable of detecting H2O, CO2, CH4,O3, and N2O in the atmosphere of an Earth-analog transiting an M-dwarf (magK =8.0) within 50 transits, and obtain better than an order-of-magnitude constraint on each of their abundances. -
THE EARTH's GRAVITY OUTLINE the Earth's Gravitational Field
GEOPHYSICS (08/430/0012) THE EARTH'S GRAVITY OUTLINE The Earth's gravitational field 2 Newton's law of gravitation: Fgrav = GMm=r ; Gravitational field = gravitational acceleration g; gravitational potential, equipotential surfaces. g for a non–rotating spherically symmetric Earth; Effects of rotation and ellipticity – variation with latitude, the reference ellipsoid and International Gravity Formula; Effects of elevation and topography, intervening rock, density inhomogeneities, tides. The geoid: equipotential mean–sea–level surface on which g = IGF value. Gravity surveys Measurement: gravity units, gravimeters, survey procedures; the geoid; satellite altimetry. Gravity corrections – latitude, elevation, Bouguer, terrain, drift; Interpretation of gravity anomalies: regional–residual separation; regional variations and deep (crust, mantle) structure; local variations and shallow density anomalies; Examples of Bouguer gravity anomalies. Isostasy Mechanism: level of compensation; Pratt and Airy models; mountain roots; Isostasy and free–air gravity, examples of isostatic balance and isostatic anomalies. Background reading: Fowler §5.1–5.6; Lowrie §2.2–2.6; Kearey & Vine §2.11. GEOPHYSICS (08/430/0012) THE EARTH'S GRAVITY FIELD Newton's law of gravitation is: ¯ GMm F = r2 11 2 2 1 3 2 where the Gravitational Constant G = 6:673 10− Nm kg− (kg− m s− ). ¢ The field strength of the Earth's gravitational field is defined as the gravitational force acting on unit mass. From Newton's third¯ law of mechanics, F = ma, it follows that gravitational force per unit mass = gravitational acceleration g. g is approximately 9:8m/s2 at the surface of the Earth. A related concept is gravitational potential: the gravitational potential V at a point P is the work done against gravity in ¯ P bringing unit mass from infinity to P. -
Composition and Accretion of the Terrestrial Planets
Lunar and Planetary Science XXXI 1546.pdf COMPOSITION AND ACCRETION OF THE TERRESTRIAL PLANETS. Edward R. D. Scott and G. Jeffrey Taylor, Hawai’i Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, Univer- sity of Hawai’i at Manoa, Honolulu, Hawai’i 96822, USA; [email protected] Abstract: Compositional variations among the spread gravitational mixing of the embryos and their four terrestrial planets are generally attributed to giant 20 impacts [1] rather than to primordial chemical varia- Fig. 2 tions among planetesimals [e.g., 2]. This is largely be- Mars cause modeling suggests that each terrestrial planet ac- 15 creted material from the whole of the inner solar sys- tem [1], and because Mercury’s high density is attrib- 10 Venus Earth uted to mantle stripping in a giant impact [3] and not to its position as the innermost planet [4]. However, Mer- Mercury cury’s high concentration of metallic iron and low con- 5 centration of oxidized iron are comparable to those in recently discovered metal-rich chondrites [5-7]. Since E 0 chondrites are linked isotopically with the Earth, we 0 0.5 1 1.5 2 suggest that Mercury may have formed from metal-rich chondritic material. Venus and Earth have similar con- Semi-major Axis (AU) centrations of metallic and oxidized iron that are inter- fragments, which ensured that each terrestrial planet mediate between those of Mercury and Mars consistent formed from material originally located throughout the with wide, overlapping accretion zones [1]. However, inner solar system (0.5 to 2.5 AU). -
POSSIBLE STRUCTURE MODELS for the TRANSITING SUPER-EARTHS:KEPLER-10B and 11B
43rd Lunar and Planetary Science Conference (2012) 1290.pdf POSSIBLE STRUCTURE MODELS FOR THE TRANSITING SUPER-EARTHS:KEPLER-10b AND 11b. P. Futó1 1 Department of Physical Geography, University of West Hungary, Szombathely, Károlyi Gáspár tér, H- 9700, Hungary ([email protected]) Introduction:Up to january of 2012,10 super- The planet Kepler-11b has a large radius (1.97 R⊕) for Earths have been announced by Kepler-mission [1] its mass (4.3 M⊕),therefore this planet must have a that is designed to detect hundreds of transiting exo- spherical shell that is composed of low-density materi- planets.Kepler was launched on 6th March,2009 and the als.Considering the planet's average density,it must primary purpose of its scientific program is to search have a metallic core with different possible fractional for terrestrial-sized planets in the habitable zone of mass.Accordinghly,I have made a possible structure Solar-like stars.For the case of high number of discov- model for Kepler-11b in which the selected core mass eries we will be able to estimate the frequency of fraction is 32.59% (similarly to that of Earth) and the Earth-sized planets in our galaxy.Results of the Kepler- water ice layer has a relatively great fractional 's measurements show that the small-sized planets are volume.For case of the selected composition, the icy frequent in the spiral galaxies.A catalog of planetary surface sublimated to form a water vapor as the planet candidates,including objects with small-sized candidate moved inward the central star during its migration. -
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. -
Planetary Science
Scientific Research National Aeronautics and Space Administration Planetary Science MSFC planetary scientists are active in Peering into the history The centerpiece of the Marshall efforts is research at Marshall, building on a long history of the solar system the Marshall Noble Gas Research Laboratory of scientific support to NASA’s human explo- (MNGRL), a unique facility within NASA. Noble- ration program planning, whether focused Marshall planetary scientists use multiple anal- gas isotopes are a well-established technique on the Moon, asteroids, or Mars. Research ysis techniques to understand the formation, for providing detailed temperature-time histories areas of expertise include planetary sample modification, and age of planetary materials of rocks and meteorites. The MNGRL lab uses analysis, planetary interior modeling, and to learn about their parent planets. Sample Ar-Ar and I-Xe radioactive dating to find the planetary atmosphere observations. Scientists analysis of this type is well-aligned with the formation age of rocks and meteorites, and at Marshall are involved in several ongoing priorities for scientific research and analysis Ar/Kr/Ne cosmic-ray exposure ages to under- planetary science missions, including the Mars in NASA’s Planetary Science Division. Multiple stand when the meteorites were launched from Exploration Rovers, the Cassini mission to future missions are poised to provide new their parent planets. Saturn, and the Gravity Recovery and Interior sample-analysis opportunities. Laboratory (GRAIL) mission to the Moon. Marshall is the center for program manage- ment for the Agency’s Discovery and New Frontiers programs, providing programmatic oversight into a variety of missions to various planetary science destinations throughout the solar system, from MESSENGER’s investiga- tions of Mercury to New Frontiers’ forthcoming examination of the Pluto system. -
On the Use of Planetary Science Data for Studying Extrasolar Planets a Science Frontier White Paper Submitted to the Astronomy & Astrophysics 2020 Decadal Survey
On the Use of Planetary Science Data for Studying Extrasolar Planets A science frontier white paper submitted to the Astronomy & Astrophysics 2020 Decadal Survey Thematic Area: Planetary Systems Principal Author Daniel J. Crichton Jet Propulsion Laboratory, California Institute of Technology [email protected] 818-354-9155 Co-Authors: J. Steve Hughes, Gael Roudier, Robert West, Jeffrey Jewell, Geoffrey Bryden, Mark Swain, T. Joseph W. Lazio (Jet Propulsion Laboratory, California Institute of Technology) There is an opportunity to advance both solar system and extrasolar planetary studies that does not require the construction of new telescopes or new missions but better use and access to inter-disciplinary data sets. This approach leverages significant investment from NASA and international space agencies in exploring this solar system and using those discoveries as “ground truth” for the study of extrasolar planets. This white paper illustrates the potential, using phase curves and atmospheric modeling as specific examples. A key advance required to realize this potential is to enable seamless discovery and access within and between planetary science and astronomical data sets. Further, seamless data discovery and access also expands the availability of science, allowing researchers and students at a variety of institutions, equipped only with Internet access and a decent computer to conduct cutting-edge research. © 2019 California Institute of Technology. Government sponsorship acknowledged. Pre-decisional - For planning -
Biosignatures Search in Habitable Planets
galaxies Review Biosignatures Search in Habitable Planets Riccardo Claudi 1,* and Eleonora Alei 1,2 1 INAF-Astronomical Observatory of Padova, Vicolo Osservatorio, 5, 35122 Padova, Italy 2 Physics and Astronomy Department, Padova University, 35131 Padova, Italy * Correspondence: [email protected] Received: 2 August 2019; Accepted: 25 September 2019; Published: 29 September 2019 Abstract: The search for life has had a new enthusiastic restart in the last two decades thanks to the large number of new worlds discovered. The about 4100 exoplanets found so far, show a large diversity of planets, from hot giants to rocky planets orbiting small and cold stars. Most of them are very different from those of the Solar System and one of the striking case is that of the super-Earths, rocky planets with masses ranging between 1 and 10 M⊕ with dimensions up to twice those of Earth. In the right environment, these planets could be the cradle of alien life that could modify the chemical composition of their atmospheres. So, the search for life signatures requires as the first step the knowledge of planet atmospheres, the main objective of future exoplanetary space explorations. Indeed, the quest for the determination of the chemical composition of those planetary atmospheres rises also more general interest than that given by the mere directory of the atmospheric compounds. It opens out to the more general speculation on what such detection might tell us about the presence of life on those planets. As, for now, we have only one example of life in the universe, we are bound to study terrestrial organisms to assess possibilities of life on other planets and guide our search for possible extinct or extant life on other planetary bodies. -
Abstracts Connecting to the Boston University Network
20th Cambridge Workshop: Cool Stars, Stellar Systems, and the Sun July 29 - Aug 3, 2018 Boston / Cambridge, USA Abstracts Connecting to the Boston University Network 1. Select network ”BU Guest (unencrypted)” 2. Once connected, open a web browser and try to navigate to a website. You should be redirected to https://safeconnect.bu.edu:9443 for registration. If the page does not automatically redirect, go to bu.edu to be brought to the login page. 3. Enter the login information: Guest Username: CoolStars20 Password: CoolStars20 Click to accept the conditions then log in. ii Foreword Our story starts on January 31, 1980 when a small group of about 50 astronomers came to- gether, organized by Andrea Dupree, to discuss the results from the new high-energy satel- lites IUE and Einstein. Called “Cool Stars, Stellar Systems, and the Sun,” the meeting empha- sized the solar stellar connection and focused discussion on “several topics … in which the similarity is manifest: the structures of chromospheres and coronae, stellar activity, and the phenomena of mass loss,” according to the preface of the resulting, “Special Report of the Smithsonian Astrophysical Observatory.” We could easily have chosen the same topics for this meeting. Over the summer of 1980, the group met again in Bonas, France and then back in Cambridge in 1981. Nearly 40 years on, I am comfortable saying these workshops have evolved to be the premier conference series for cool star research. Cool Stars has been held largely biennially, alternating between North America and Europe. Over that time, the field of stellar astro- physics has been upended several times, first by results from Hubble, then ROSAT, then Keck and other large aperture ground-based adaptive optics telescopes.