The Cool Tiny Beats Project - a High-Cadence HARPS Survey Searching for Short-Period Planets, Pulsations and Activity Signatures in M Stars
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Arxiv:2102.09424V2 [Astro-Ph.EP] 20 Feb 2021 the first Exoplanet
Draft version February 23, 2021 Typeset using LATEX twocolumn style in AASTeX63 Planets Across Space and Time (PAST). I. Characterizing the Memberships of Galactic Components and Stellar Ages: Revisiting the Kinematic Methods and Applying to Planet Host Stars Di-Chang Chen,1, 2 Ji-Wei Xie,1, 2 Ji-Lin Zhou,1, 2 Su-Bo Dong,3 Chao Liu,4, 5 Hai-Feng Wang,6 Mao-Sheng Xiang,7, 8 Yang Huang,9 Ali Luo,7 and Zheng Zheng10 1School of Astronomy and Space Science, Nanjing University, Nanjing 210023, China 2Key Laboratory of Modern Astronomy and Astrophysics, Ministry of Education, Nanjing 210023, China 3Kavli Institute for Astronomy and Astrophysics, Peking University, Beijing 100871, China 4Key Lab of Space Astronomy and Technology, National Astronomical Observatories, CAS, 100101, China 5University of Chinese Academy of Sciences, Beijing, 100049, China. 6South-Western Institute for Astronomy Research, Yunnan University, Kunming, 650500, China; LAMOST Fellow 7National Astronomical Observatories, Chinese Academy of Sciences, Beijing 100012, China 8Max-Planck Institute for Astronomy, K¨onigstuhl17, D-69117 Heidelberg, Germany 9South-Western Institute for Astronomy Research, Yunnan University, Kunming, 650500, China 10Department of Physics and Astronomy, University of Utah, Salt Lake City, UT 84112 ABSTRACT Over 4,000 exoplanets have been identified and thousands of candidates are to be confirmed. The relations between the characteristics of these planetary systems and the kinematics, Galactic compo- nents, and ages of their host stars have yet to be well explored. Aiming to addressing these questions, we conduct a research project, dubbed as PAST (Planets Across Space and Time). To do this, one of the key steps is to accurately characterize the planet host stars. -
Science Concept 5: Lunar Volcanism Provides a Window Into the Thermal and Compositional Evolution of the Moon
Science Concept 5: Lunar Volcanism Provides a Window into the Thermal and Compositional Evolution of the Moon Science Concept 5: Lunar volcanism provides a window into the thermal and compositional evolution of the Moon Science Goals: a. Determine the origin and variability of lunar basalts. b. Determine the age of the youngest and oldest mare basalts. c. Determine the compositional range and extent of lunar pyroclastic deposits. d. Determine the flux of lunar volcanism and its evolution through space and time. INTRODUCTION Features of Lunar Volcanism The most prominent volcanic features on the lunar surface are the low albedo mare regions, which cover approximately 17% of the lunar surface (Fig. 5.1). Mare regions are generally considered to be made up of flood basalts, which are the product of highly voluminous basaltic volcanism. On the Moon, such flood basalts typically fill topographically-low impact basins up to 2000 m below the global mean elevation (Wilhelms, 1987). The mare regions are asymmetrically distributed on the lunar surface and cover about 33% of the nearside and only ~3% of the far-side (Wilhelms, 1987). Other volcanic surface features include pyroclastic deposits, domes, and rilles. These features occur on a much smaller scale than the mare flood basalts, but are no less important in understanding lunar volcanism and the internal evolution of the Moon. Table 5.1 outlines different types of volcanic features and their interpreted formational processes. TABLE 5.1 Lunar Volcanic Features Volcanic Feature Interpreted Process -
Download Artist's CV
I N M A N G A L L E R Y Michael Jones McKean b. 1976, Truk Island, Micronesia Lives and works in New York City, NY and Richmond, VA Education 2002 MFA, Alfred University, Alfred, New York 2000 BFA, Marywood University, Scranton, Pennsylvania Solo Exhibitions 2018-29 (in progress) Twelve Earths, 12 global sites, w/ Fathomers, Los Angeles, CA 2019 The Commune, SuPerDutchess, New York, New York The Raw Morphology, A + B Gallery, Brescia, Italy 2018 UNTMLY MLDS, Art Brussels, Discovery Section, 2017 The Ground, The ContemPorary, Baltimore, MD Proxima Centauri b. Gleise 667 Cc. Kepler-442b. Wolf 1061c. Kepler-1229b. Kapteyn b. Kepler-186f. GJ 273b. TRAPPIST-1e., Galerie Escougnou-Cetraro, Paris, France 2016 Rivers, Carnegie Mellon University, Pittsburgh, PA Michael Jones McKean: The Ground, The ContemPorary Museum, Baltimore, MD The Drift, Pittsburgh, PA 2015 a hundred twenty six billion acres, Inman Gallery, Houston, TX three carbon tons, (two-person w/ Jered Sprecher) Zeitgeist Gallery, Nashville, TN 2014 we float above to spit and sing, Emerson Dorsch, Miami, FL Michael Jones McKean and Gilad Efrat, Inman Gallery, at UNTITLED, Miami, FL 2013 The Religion, The Fosdick-Nelson Gallery, Alfred University, Alfred, NY Seven Sculptures, (two person show with Jackie Gendel), Horton Gallery, New York, NY Love and Resources (two person show with Timur Si-Qin), Favorite Goods, Los Angeles, CA 2012 circles become spheres, Gentili APri, Berlin, Germany Certain Principles of Light and Shapes Between Forms, Bernis Center for ContemPorary Art, Omaha, NE -
Habitability of Planets on Eccentric Orbits: Limits of the Mean Flux Approximation
A&A 591, A106 (2016) Astronomy DOI: 10.1051/0004-6361/201628073 & c ESO 2016 Astrophysics Habitability of planets on eccentric orbits: Limits of the mean flux approximation Emeline Bolmont1, Anne-Sophie Libert1, Jeremy Leconte2; 3; 4, and Franck Selsis5; 6 1 NaXys, Department of Mathematics, University of Namur, 8 Rempart de la Vierge, 5000 Namur, Belgium e-mail: [email protected] 2 Canadian Institute for Theoretical Astrophysics, 60st St George Street, University of Toronto, Toronto, ON, M5S3H8, Canada 3 Banting Fellow 4 Center for Planetary Sciences, Department of Physical & Environmental Sciences, University of Toronto Scarborough, Toronto, ON, M1C 1A4, Canada 5 Univ. Bordeaux, LAB, UMR 5804, 33270 Floirac, France 6 CNRS, LAB, UMR 5804, 33270 Floirac, France Received 4 January 2016 / Accepted 28 April 2016 ABSTRACT Unlike the Earth, which has a small orbital eccentricity, some exoplanets discovered in the insolation habitable zone (HZ) have high orbital eccentricities (e.g., up to an eccentricity of ∼0.97 for HD 20782 b). This raises the question of whether these planets have surface conditions favorable to liquid water. In order to assess the habitability of an eccentric planet, the mean flux approximation is often used. It states that a planet on an eccentric orbit is called habitable if it receives on average a flux compatible with the presence of surface liquid water. However, because the planets experience important insolation variations over one orbit and even spend some time outside the HZ for high eccentricities, the question of their habitability might not be as straightforward. We performed a set of simulations using the global climate model LMDZ to explore the limits of the mean flux approximation when varying the luminosity of the host star and the eccentricity of the planet. -
Exoplanet.Eu Catalog Page 1 # Name Mass Star Name
exoplanet.eu_catalog # name mass star_name star_distance star_mass OGLE-2016-BLG-1469L b 13.6 OGLE-2016-BLG-1469L 4500.0 0.048 11 Com b 19.4 11 Com 110.6 2.7 11 Oph b 21 11 Oph 145.0 0.0162 11 UMi b 10.5 11 UMi 119.5 1.8 14 And b 5.33 14 And 76.4 2.2 14 Her b 4.64 14 Her 18.1 0.9 16 Cyg B b 1.68 16 Cyg B 21.4 1.01 18 Del b 10.3 18 Del 73.1 2.3 1RXS 1609 b 14 1RXS1609 145.0 0.73 1SWASP J1407 b 20 1SWASP J1407 133.0 0.9 24 Sex b 1.99 24 Sex 74.8 1.54 24 Sex c 0.86 24 Sex 74.8 1.54 2M 0103-55 (AB) b 13 2M 0103-55 (AB) 47.2 0.4 2M 0122-24 b 20 2M 0122-24 36.0 0.4 2M 0219-39 b 13.9 2M 0219-39 39.4 0.11 2M 0441+23 b 7.5 2M 0441+23 140.0 0.02 2M 0746+20 b 30 2M 0746+20 12.2 0.12 2M 1207-39 24 2M 1207-39 52.4 0.025 2M 1207-39 b 4 2M 1207-39 52.4 0.025 2M 1938+46 b 1.9 2M 1938+46 0.6 2M 2140+16 b 20 2M 2140+16 25.0 0.08 2M 2206-20 b 30 2M 2206-20 26.7 0.13 2M 2236+4751 b 12.5 2M 2236+4751 63.0 0.6 2M J2126-81 b 13.3 TYC 9486-927-1 24.8 0.4 2MASS J11193254 AB 3.7 2MASS J11193254 AB 2MASS J1450-7841 A 40 2MASS J1450-7841 A 75.0 0.04 2MASS J1450-7841 B 40 2MASS J1450-7841 B 75.0 0.04 2MASS J2250+2325 b 30 2MASS J2250+2325 41.5 30 Ari B b 9.88 30 Ari B 39.4 1.22 38 Vir b 4.51 38 Vir 1.18 4 Uma b 7.1 4 Uma 78.5 1.234 42 Dra b 3.88 42 Dra 97.3 0.98 47 Uma b 2.53 47 Uma 14.0 1.03 47 Uma c 0.54 47 Uma 14.0 1.03 47 Uma d 1.64 47 Uma 14.0 1.03 51 Eri b 9.1 51 Eri 29.4 1.75 51 Peg b 0.47 51 Peg 14.7 1.11 55 Cnc b 0.84 55 Cnc 12.3 0.905 55 Cnc c 0.1784 55 Cnc 12.3 0.905 55 Cnc d 3.86 55 Cnc 12.3 0.905 55 Cnc e 0.02547 55 Cnc 12.3 0.905 55 Cnc f 0.1479 55 -
Kuchner, M. & Seager, S., Extrasolar Carbon Planets, Arxiv:Astro-Ph
Extrasolar Carbon Planets Marc J. Kuchner1 Princeton University Department of Astrophysical Sciences Peyton Hall, Princeton, NJ 08544 S. Seager Carnegie Institution of Washington, 5241 Broad Branch Rd. NW, Washington DC 20015 [email protected] ABSTRACT We suggest that some extrasolar planets . 60 ML will form substantially from silicon carbide and other carbon compounds. Pulsar planets and low-mass white dwarf planets are especially good candidate members of this new class of planets, but these objects could also conceivably form around stars like the Sun. This planet-formation pathway requires only a factor of two local enhancement of the protoplanetary disk’s C/O ratio above solar, a condition that pileups of carbonaceous grains may create in ordinary protoplanetary disks. Hot, Neptune- mass carbon planets should show a significant paucity of water vapor in their spectra compared to hot planets with solar abundances. Cooler, less massive carbon planets may show hydrocarbon-rich spectra and tar-covered surfaces. The high sublimation temperatures of diamond, SiC, and other carbon compounds could protect these planets from carbon depletion at high temperatures. arXiv:astro-ph/0504214v2 2 May 2005 Subject headings: astrobiology — planets and satellites, individual (Mercury, Jupiter) — planetary systems: formation — pulsars, individual (PSR 1257+12) — white dwarfs 1. INTRODUCTION The recent discoveries of Neptune-mass extrasolar planets by the radial velocity method (Santos et al. 2004; McArthur et al. 2004; Butler et al. 2004) and the rapid development 1Hubble Fellow –2– of new technologies to study the compositions of low-mass extrasolar planets (see, e.g., the review by Kuchner & Spergel 2003) have compelled several authors to consider planets with chemistries unlike those found in the solar system (Stevenson 2004) such as water planets (Kuchner 2003; Leger et al. -
Simulating (Sub)Millimeter Observations of Exoplanet Atmospheres in Search of Water
University of Groningen Kapteyn Astronomical Institute Simulating (Sub)Millimeter Observations of Exoplanet Atmospheres in Search of Water September 5, 2018 Author: N.O. Oberg Supervisor: Prof. Dr. F.F.S. van der Tak Abstract Context: Spectroscopic characterization of exoplanetary atmospheres is a field still in its in- fancy. The detection of molecular spectral features in the atmosphere of several hot-Jupiters and hot-Neptunes has led to the preliminary identification of atmospheric H2O. The Atacama Large Millimiter/Submillimeter Array is particularly well suited in the search for extraterrestrial water, considering its wavelength coverage, sensitivity, resolving power and spectral resolution. Aims: Our aim is to determine the detectability of various spectroscopic signatures of H2O in the (sub)millimeter by a range of current and future observatories and the suitability of (sub)millimeter astronomy for the detection and characterization of exoplanets. Methods: We have created an atmospheric modeling framework based on the HAPI radiative transfer code. We have generated planetary spectra in the (sub)millimeter regime, covering a wide variety of possible exoplanet properties and atmospheric compositions. We have set limits on the detectability of these spectral features and of the planets themselves with emphasis on ALMA. We estimate the capabilities required to study exoplanet atmospheres directly in the (sub)millimeter by using a custom sensitivity calculator. Results: Even trace abundances of atmospheric water vapor can cause high-contrast spectral ab- sorption features in (sub)millimeter transmission spectra of exoplanets, however stellar (sub) millime- ter brightness is insufficient for transit spectroscopy with modern instruments. Excess stellar (sub) millimeter emission due to activity is unlikely to significantly enhance the detectability of planets in transit except in select pre-main-sequence stars. -
10/17/2015 1 the Origin of the Solar System Chapter 10
10/17/2015 Guidepost As you explore the origins and the materials that make up the solar system, you will discover the answers to several important questions: What are the observed properties of the solar system? Chapter 10 What is the theory for the origin of the solar system that explains the observed properties? The Origin of the Solar System How did Earth and the other planets form? What do astronomers know about other extrasolar planets orbiting other stars? In this and the following six chapters, we will explore in more detail the planets and other objects that make up our solar system, our home in the universe. A Survey of the Solar System Two Kinds of Planets The solar system consists of eight Planets of our solar system can be divided into two very major planets and several other different kinds: objects. Jovian (Jupiter- like) planets: The planets rotate on their axes and Jupiter, Saturn, revolve around the Sun. Uranus, Neptune The planets have elliptical orbits, sometimes inclined to the ecliptic, and all planets revolve in the same directly; only Venus and Uranus rotate in an alternate direction. Nearly all moons also revolve in the Terrestrial (Earthlike) same direction. planets: Mercury, Venus, Earth, Mars Terrestrial Planets Craters on Planets’ Surfaces Craters (like on our Four inner moon’s surface) are planets of the common throughout solar system the solar system. Relatively small in size Not seen on Jovian and mass planets because (Earth is the Surface of Venus they don’t have a largest and Rocky surface can not be seen solid surface. -
Proxima B: the Alien World Next Door - Is Anyone Home?
Proxima b: The Alien World Next Door - Is Anyone Home? Edward Guinan Biruni Observatory Dept. Astrophysics & Planetary Science th 40 Anniversary Workshop Villanova University 12 October, 2017 [email protected] Talking Points i. Planet Hunting: Exoplanets ii. Living with a Red Dwarf Program iii. Alpha Cen ABC -nearest Star System iv. Proxima Cen – the red dwarf star v. Proxima b Nearest Exoplanet vi. Can it support Life? vii. Planned Observations / Missions Planet Hunting: Finding Exoplanets A brief summary For citizen science projects: www.planethunters.org Early Thoughts on Extrasolar Planets and Life Thousands of years ago, Greek philosophers speculated… “There are infinite worlds both like and unlike this world of ours...We must believe that in all worlds there are living creatures and planets and other things we see in this world.” Epicurius c. 300 B.C First Planet Detected 51 Pegasi – November 1995 Mayer & Queloz / Marcy & Butler Credit: Charbonneau Many Exoplanets (400+) have been detected by the Spectroscopic Doppler Motion Technique (now can measure motions as low as 1 m/s (3.6 km/h = 2.3 mph)) Exoplanet Transit Eclipses Rp/Rs ~ [Depth of Eclipse] 1/2 Transit Eclipse Depths for Jupiter, Neptune and Earth for the Sun 0.01% (Earth-Sun) 0.15% (Neptune-Sun) 1.2% (Jupiter-Sun) Kepler Mission See: kepler.nasa.gov Has so far discovered 6000+ Confirmed & Candidate Exoplanets The Search for Planets Outside Our Solar System Exoplanet Census May 2017 Exoplanet Census (May-2017) Confirmed exoplanets: 3483+ (Doppler / Transit) 490+ Multi-planet Systems [April 2017] Exoplanet Candidates: 7900+ orbiting 2600+ stars (Mostly from the Kepler Mission) [May 2017] Other unconfirmed (mostly from CoRot)Exoplanets ~186+ Potentially Habitable Exoplanets: 51 (April 2017) Estimated Planets in the Galaxy ~ 50 -100 Billion! Most expected to be hosted by red dwarf stars Nomad (Free-floating planets) ~ 25 - 50 Billion Known planets with life: 1 so far. -
Arxiv:2103.02709V1
Draft version September 19, 2021 Typeset using LATEX default style in AASTeX63 A Gaussian Process Regression Reveals No Evidence for Planets Orbiting Kapteyn's Star Anna Bortle,1 Hallie Fausey,1 Jinbiao Ji,1 Sarah Dodson-Robinson,1 Victor Ramirez Delgado,1 and John Gizis1 1University of Delaware Department of Physics and Astronomy 217 Sharp Lab Newark, DE 19716 USA ABSTRACT Radial-velocity (RV) planet searches are often polluted by signals caused by gas motion at the star's surface. Stellar activity can mimic or mask changes in the RVs caused by orbiting planets, resulting in false positives or missed detections. Here we use Gaussian Process (GP) regression to disentangle the contradictory reports of planets vs. rotation artifacts in Kapteyn's star (Anglada-Escud´eet al. 2014; Robertson et al. 2015a; Anglada-Escud´eet al. 2016). To model rotation, we use joint quasi-periodic kernels for the RV and Hα signals, requiring that their periods and correlation timescales be the same. We find that the rotation period of Kapteyn's star is 125 days, while the characteristic active-region lifetime is 694 days. Adding a planet to the RV model produces a best-fit orbital period of 100 years, or 10 times the observing time baseline, indicating that the observed RVs are best explained by star rotation only. We also find no significant periodic signals in residual RV data sets constructed by subtracting off realizations of the best-fit rotation model and conclude that both previously reported \planets" are artifacts of the star's rotation and activity. Our results highlight the pitfalls of using sinusoids to model quasi-periodic rotation signals. -
Estudio Numérico De La Dinámica De Planetas
UNIVERSIDAD PEDAGOGICA´ NACIONAL FACULTAD DE CIENCIA Y TECNOLOG´IA ESTUDIO NUMERICO´ DE LA DINAMICA´ DE PLANETAS EXTRASOLARES Tesis presentada por Eduardo Antonio Mafla Mejia dirigida por: Camilo Delgado Correal Nestor Mendez Hincapie para obtener el grado de Licenciado en F´ısica 2015 Departamento de F´ısica I Dedico este trabajo a mi mam´a, quien me apoyo en mi deseo de seguir el camino de la educaci´on. Sin su apoyo este deseo no lograr´ıa ser hoy una realidad. RESUMEN ANALÍTICO EN EDUCACIÓN - RAE 1. Información General Tipo de documento Trabajo de Grado Acceso al documento Universidad Pedagógica Nacional. Biblioteca Central ESTUDIO NUMÉRICO DE LA DINÁMICA DE PLANETAS Título del documento EXTRASOLARES Autor(es) Mafla Mejia, Eduardo Antonio Director Méndez Hincapié, Néstor; Delgado Correal, Camilo Publicación Bogotá. Universidad Pedagógica Nacional, 2015. 61 p. Unidad Patrocinante Universidad Pedagógica Nacional DINÁMICA DE EXOPLANETAS, LEY GRAVITACIONAL DE NEWTON, Palabras Claves ESTUDIO NUMÉRICO. 2. Descripción Trabajo de grado que se propone evidenciar si el modelo matemático clásico newtoniano, y en consecuencia las tres leyes de Kepler, se puede generalizar a cualquier sistema planetario, o solo es válido para determinados casos particulares. Para lograr esto de comparar numéricamente los efectos de las diferentes correcciones que puede adoptar la ley de gravitación de Newton para modelar la dinámica de planetas extrasolares aplicándolos en los sistemas extrasolares Gliese 876 d, Gliese 436 b y el sistema Mercurio – Sol. En los exoplanetas examinados se encontró, que en un buen grado de aproximación, la dinámica de los exoplanetas se logran describir con el modelo newtoniano, y en consecuencia, modelar su movimiento usando las leyes de Kepler. -
Transition from Eyeball to Snowball Driven by Sea-Ice Drift on Tidally Locked Terrestrial Planets
Transition from Eyeball to Snowball Driven by Sea-ice Drift on Tidally Locked Terrestrial Planets Jun Yang1,*, Weiwen Ji1, & Yaoxuan Zeng1 1Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China. *Corresponding author: J.Y., [email protected] Tidally locked terrestrial planets around low-mass stars are the prime targets for future atmospheric characterizations of potentially habitable systems1, especially the three nearby ones–Proxima b2, TRAPPIST-1e3, and LHS 1140b4. Previous studies suggest that if these planets have surface ocean they would be in an eyeball-like climate state5-10: ice-free in the vicinity of the substellar point and ice-covered in the rest regions. However, an important component of the climate system–sea ice dynamics has not been well studied in previous studies. A fundamental question is: would the open ocean be stable against a globally ice-covered snowball state? Here we show that sea-ice drift cools the ocean’s surface when the ice flows to the warmer substellar region and melts through absorbing heat from the ocean and the overlying air. As a result, the open ocean shrinks and can even disappear when atmospheric greenhouse gases are not much more abundant than on Earth, turning the planet into a snowball state. This occurs for both synchronous rotation and spin- orbit resonances (such as 3:2). These results suggest that sea-ice drift strongly reduces the open ocean area and can significantly impact the habitability of tidally locked planets. 1 Sea-ice drift, driven by surface winds and ocean currents, transports heat and freshwater across the ocean surface, directly or indirectly influencing ice concentration, ice growth and melt, ice thickness, surface albedo, and air–sea heat exchange11,12.