Appendix I Authors and Editors
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Mathématiques Et Espace
Atelier disciplinaire AD 5 Mathématiques et Espace Anne-Cécile DHERS, Education Nationale (mathématiques) Peggy THILLET, Education Nationale (mathématiques) Yann BARSAMIAN, Education Nationale (mathématiques) Olivier BONNETON, Sciences - U (mathématiques) Cahier d'activités Activité 1 : L'HORIZON TERRESTRE ET SPATIAL Activité 2 : DENOMBREMENT D'ETOILES DANS LE CIEL ET L'UNIVERS Activité 3 : D'HIPPARCOS A BENFORD Activité 4 : OBSERVATION STATISTIQUE DES CRATERES LUNAIRES Activité 5 : DIAMETRE DES CRATERES D'IMPACT Activité 6 : LOI DE TITIUS-BODE Activité 7 : MODELISER UNE CONSTELLATION EN 3D Crédits photo : NASA / CNES L'HORIZON TERRESTRE ET SPATIAL (3 ème / 2 nde ) __________________________________________________ OBJECTIF : Détermination de la ligne d'horizon à une altitude donnée. COMPETENCES : ● Utilisation du théorème de Pythagore ● Utilisation de Google Earth pour évaluer des distances à vol d'oiseau ● Recherche personnelle de données REALISATION : Il s'agit ici de mettre en application le théorème de Pythagore mais avec une vision terrestre dans un premier temps suite à un questionnement de l'élève puis dans un second temps de réutiliser la même démarche dans le cadre spatial de la visibilité d'un satellite. Fiche élève ____________________________________________________________________________ 1. Victor Hugo a écrit dans Les Châtiments : "Les horizons aux horizons succèdent […] : on avance toujours, on n’arrive jamais ". Face à la mer, vous voyez l'horizon à perte de vue. Mais "est-ce loin, l'horizon ?". D'après toi, jusqu'à quelle distance peux-tu voir si le temps est clair ? Réponse 1 : " Sans instrument, je peux voir jusqu'à .................. km " Réponse 2 : " Avec une paire de jumelles, je peux voir jusqu'à ............... km " 2. Nous allons maintenant calculer à l'aide du théorème de Pythagore la ligne d'horizon pour une hauteur H donnée. -
Lurking in the Shadows: Wide-Separation Gas Giants As Tracers of Planet Formation
Lurking in the Shadows: Wide-Separation Gas Giants as Tracers of Planet Formation Thesis by Marta Levesque Bryan In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California 2018 Defended May 1, 2018 ii © 2018 Marta Levesque Bryan ORCID: [0000-0002-6076-5967] All rights reserved iii ACKNOWLEDGEMENTS First and foremost I would like to thank Heather Knutson, who I had the great privilege of working with as my thesis advisor. Her encouragement, guidance, and perspective helped me navigate many a challenging problem, and my conversations with her were a consistent source of positivity and learning throughout my time at Caltech. I leave graduate school a better scientist and person for having her as a role model. Heather fostered a wonderfully positive and supportive environment for her students, giving us the space to explore and grow - I could not have asked for a better advisor or research experience. I would also like to thank Konstantin Batygin for enthusiastic and illuminating discussions that always left me more excited to explore the result at hand. Thank you as well to Dimitri Mawet for providing both expertise and contagious optimism for some of my latest direct imaging endeavors. Thank you to the rest of my thesis committee, namely Geoff Blake, Evan Kirby, and Chuck Steidel for their support, helpful conversations, and insightful questions. I am grateful to have had the opportunity to collaborate with Brendan Bowler. His talk at Caltech my second year of graduate school introduced me to an unexpected population of massive wide-separation planetary-mass companions, and lead to a long-running collaboration from which several of my thesis projects were born. -
The Dunhuang Chinese Sky: a Comprehensive Study of the Oldest Known Star Atlas
25/02/09JAHH/v4 1 THE DUNHUANG CHINESE SKY: A COMPREHENSIVE STUDY OF THE OLDEST KNOWN STAR ATLAS JEAN-MARC BONNET-BIDAUD Commissariat à l’Energie Atomique ,Centre de Saclay, F-91191 Gif-sur-Yvette, France E-mail: [email protected] FRANÇOISE PRADERIE Observatoire de Paris, 61 Avenue de l’Observatoire, F- 75014 Paris, France E-mail: [email protected] and SUSAN WHITFIELD The British Library, 96 Euston Road, London NW1 2DB, UK E-mail: [email protected] Abstract: This paper presents an analysis of the star atlas included in the medieval Chinese manuscript (Or.8210/S.3326), discovered in 1907 by the archaeologist Aurel Stein at the Silk Road town of Dunhuang and now held in the British Library. Although partially studied by a few Chinese scholars, it has never been fully displayed and discussed in the Western world. This set of sky maps (12 hour angle maps in quasi-cylindrical projection and a circumpolar map in azimuthal projection), displaying the full sky visible from the Northern hemisphere, is up to now the oldest complete preserved star atlas from any civilisation. It is also the first known pictorial representation of the quasi-totality of the Chinese constellations. This paper describes the history of the physical object – a roll of thin paper drawn with ink. We analyse the stellar content of each map (1339 stars, 257 asterisms) and the texts associated with the maps. We establish the precision with which the maps are drawn (1.5 to 4° for the brightest stars) and examine the type of projections used. -
On the Metallicity of Open Clusters II. Spectroscopy
Astronomy & Astrophysics manuscript no. OCMetPaper2 c ESO 2013 November 12, 2013 On the metallicity of open clusters II. Spectroscopy U. Heiter1, C. Soubiran2, M. Netopil3, and E. Paunzen4 1 Institutionen för fysik och astronomi, Uppsala universitet, Box 516, 751 20 Uppsala, Sweden e-mail: [email protected] 2 Université Bordeaux 1, CNRS, Laboratoire d’Astrophysique de Bordeaux UMR 5804, BP 89, 33270 Floirac, France 3 Institut für Astrophysik der Universität Wien, Türkenschanzstrasse 17, 1180 Wien, Austria 4 Department of Theoretical Physics and Astrophysics, Masaryk University, Kotlárskᡠ267/2, 611 37 Brno, Czech Republic Received 29 August 2013 / Accepted 20 October 2013 ABSTRACT Context. Open clusters are an important tool for studying the chemical evolution of the Galactic disk. Metallicity estimates are available for about ten percent of the currently known open clusters. These metallicities are based on widely differing methods, however, which introduces unknown systematic effects. Aims. In a series of three papers, we investigate the current status of published metallicities for open clusters that were derived from a variety of photometric and spectroscopic methods. The current article focuses on spectroscopic methods. The aim is to compile a comprehensive set of clusters with the most reliable metallicities from high-resolution spectroscopic studies. This set of metallicities will be the basis for a calibration of metallicities from different methods. Methods. The literature was searched for [Fe/H] estimates of individual member stars of open clusters based on the analysis of high-resolution spectra. For comparison, we also compiled [Fe/H] estimates based on spectra with low and intermediate resolution. -
Ix Ophiuchi: a High-Velocity Star Near a Molecular Cloud G
The Astronomical Journal, 130:815–824, 2005 August # 2005. The American Astronomical Society. All rights reserved. Printed in U.S.A. IX OPHIUCHI: A HIGH-VELOCITY STAR NEAR A MOLECULAR CLOUD G. H. Herbig Institute for Astronomy, University of Hawaii, 2680 Woodlawn Drive, Honolulu, HI 96822 Received 2005 March 24; accepted 2005 April 26 ABSTRACT The molecular cloud Barnard 59 is probably an outlier of the Upper Sco/ Oph complex. B59 contains several T Tauri stars (TTSs), but outside its northwestern edge are three other H -emission objects whose nature has been unclear: IX, KK, and V359 Oph. This paper is a discussion of all three and of a nearby Be star (HD 154851), based largely on Keck HIRES spectrograms obtained in 2004. KK Oph is a close (1B6) double. The brighter component is an HAeBe star, and the fainter is a K-type TTS. The complex BVR variations of the unresolved pair require both components to be variable. V359 Oph is a conventional TTS. Thus, these pre-main-sequence stars continue to be recognizable as such well outside the boundary of their parent cloud. IX Oph is quite different. Its absorption spec- trum is about type G, with many peculiarities: all lines are narrow but abnormally weak, with structures that depend on ion and excitation level and that vary in detail from month to month. It could be a spectroscopic binary of small amplitude. H and H are the only prominent emission lines. They are broad, with variable central reversals. How- ever, the most unusual characteristic of IX Oph is the very high (heliocentric) radial velocity: about À310 km sÀ1, common to all spectrograms, and very different from the radial velocity of B59, about À7kmsÀ1. -
Program and Abstract Book
Program and Abstract Book Precision Asteroseismology: Celebration of the Scientific Opus of Wojtek Dziembowski Date: 19 – 23 August 2013, Location: WrocÃlaw (Poland) Scientific Organizing Committee: Annie Baglin (France) Bill Chaplin (UK) Jørgen Christensen-Dalsgaard (Denmark) Margarida Cunha (Portugal) Jadwiga Daszy´nska-Daszkiewicz (Chair, Poland) Gilles Fontaine (Canada) Joyce Guzik (USA) Marcella Marconi (Italy) Karen Pollard (New Zealand) Hiromoto Shibahashi (Chair, Japan) Juan Carlos Su´arez(Spain) Werner Weiss (Austria) Local Organizing Committee: Urszula Bąk-Stęślicka Barbara Cader-Sroka Jadwiga Daszyńska-Daszkiewicz (Chair) Zbigniew Kołaczkowski Grzegorz Kopacki Andrzej Pigulski (Chair) Marek Stęślicki Przemysław Walczak 1 2 PROGRAM OF THE SYMPOSIUM DAY 1. August 19, Monday Session 1. Introduction Chair: Jadwiga Daszy´nska-Daszkiewicz 8:00 – 9:00 Registration and setting up posters 9:00 – 9:20 Welcome and opening 9:20 – 10:20 An overview of the scientific career of Wojtek Dziem- bowski by Douglas Gough (30 min) & Alexey Pamyatnykh (30 min) 10:20 – 10:50 Coffee break Chair: Jørgen Christensen-Dalsgaard 10:50 – 11:30 Introductory talk: What can we expect from precision asteroseismology (Gerald Handler) Session 2. Observations: from ground to space 11:30 – 12:00 Pulsating variables from the OGLE and Araucaria pro- jects (Grzegorz Pietrzy´nski,invited) 12:00 – 12:30 A review of pulsating stars from the ASAS data (Andrzej Pigulski, invited) 12:30 – 12:45 Asteroseismology with SuperWASP (Barry Smalley) 12:45 – 13:00 A new class of low amplitude -
Program and Abstracts of 2017 Congress / Programme Et Résumés
1 Sponsors | Commanditaires Gold Sponsors | Commanditaires d’or Silver Sponsors | Commanditaires d’argent Other Sponsors | Les autres Commanditaires 2 Contents Sponsors | Commanditaires .......................................................................................................................... 2 Welcome from the Premier of Ontario .......................................................................................................... 5 Bienvenue du premier ministre de l'Ontario .................................................................................................. 6 Welcome from the Mayor of Toronto ............................................................................................................ 7 Mot de bienvenue du maire de Toronto ........................................................................................................ 8 Welcome from the Minister of Fisheries, Oceans and the Canadian Coast Guard ...................................... 9 Mot de bienvenue de ministre des Pêches, des Océans et de la Garde côtière canadienne .................... 10 Welcome from the Minister of Environment and Climate Change .............................................................. 11 Mot de bienvenue du Ministre d’Environnement et Changement climatique Canada ................................ 12 Welcome from the President of the Canadian Meteorological and Oceanographic Society ...................... 13 Mot de bienvenue du président de la Société canadienne de météorologie et d’océanographie ............. -
Naming the Extrasolar Planets
Naming the extrasolar planets W. Lyra Max Planck Institute for Astronomy, K¨onigstuhl 17, 69177, Heidelberg, Germany [email protected] Abstract and OGLE-TR-182 b, which does not help educators convey the message that these planets are quite similar to Jupiter. Extrasolar planets are not named and are referred to only In stark contrast, the sentence“planet Apollo is a gas giant by their assigned scientific designation. The reason given like Jupiter” is heavily - yet invisibly - coated with Coper- by the IAU to not name the planets is that it is consid- nicanism. ered impractical as planets are expected to be common. I One reason given by the IAU for not considering naming advance some reasons as to why this logic is flawed, and sug- the extrasolar planets is that it is a task deemed impractical. gest names for the 403 extrasolar planet candidates known One source is quoted as having said “if planets are found to as of Oct 2009. The names follow a scheme of association occur very frequently in the Universe, a system of individual with the constellation that the host star pertains to, and names for planets might well rapidly be found equally im- therefore are mostly drawn from Roman-Greek mythology. practicable as it is for stars, as planet discoveries progress.” Other mythologies may also be used given that a suitable 1. This leads to a second argument. It is indeed impractical association is established. to name all stars. But some stars are named nonetheless. In fact, all other classes of astronomical bodies are named. -
Make ''Girl Scout'' Mean Health! Strength!
Gl Vol. 4 APRIL.19!7 No.4 Make ''Girl Scout'' Mean Health! Strength! Joy! By Sally Lucas Jean, Health Consultant HAIRS and tables were beinc cardully ar The table is set for the purpose of feeding the fam ranced by teVeral girls in Girl Scout uni Oy; what is to be placed in the dishes l The interest of form as a visitor entered the CIOIIIIDunity the occasion is one that should not be lost; stress the bOUle of a c:rowded district one eveninc riaht foods and the vital part played by diet in accom • not long ago. They retUmecl the ltranl pliabing our desired goals. Make the lesson a definite er"s peetiog cordillly and one girl stepped forward of one; mention the details of a good menu and be sure it ferittl to -call the --captain, no 'WIS -engqecl in an ad is a well balanced meal, including mOk in some form, joining room. The visitor, really wanting an oppor green vegetables or fruit, perhaps both. The imagina tunity to be with the girls, said she would wait. After tion of the girls will quickly fill the plates, cups and her coat had been taken and the moat comfortable chair gl..es with the foods indicated. Very little guidance sugested, the girls went on with their preparations for wm prepare them to present a good breakfast, lunch or the meeting. Girl Scout hoste~~eal dinner menu for a faau1y of two adults and three chO A aal1 bed was 10, 10 carefully lifted from a doeet, dren. -
Matching the Spectral Energy Distribution and P Mode Oscillation Frequencies of the Rapidly Rotating Delta Scuti Star Α Ophiuchi with a 2D Rotating Stellar Model
Matching the Spectral Energy Distribution and p Mode Oscillation Frequencies of the Rapidly Rotating Delta Scuti Star α Ophiuchi with a 2D Rotating Stellar Model Robert G. Deupree, Diego Castañeda, Fernando Peña, and C. Ian Short Institute for Computational Astrophysics and Department of Astronomy and Physics, Saint Mary’s University, Halifax, NS B3H 3C3 Canada; [email protected] ABSTRACT Spectral energy distributions are computed using 2D rotating stellar models and NLTE plane parallel model atmospheres. A rotating, 2D stellar model has been found which matches the observed ultraviolet and visible spectrum of α Oph. The SED match occurs for the interferometrically deduced surface shape and inclination, and is different from the SED produced by spherical models. The p mode oscillation frequencies in which the latitudinal variation is modelled by a linear combination of eight Legendre polynomials were computed for this model. The five highest and seven of the nine highest amplitude modes show agreement between computed axisymmetric, equatorially symmetric mode frequencies and the mode frequencies observed by MOST to within the observational error. Including nonaxisymmetric modes up through |m| = 2 and allowing the possibility that the eight lowest amplitude modes could be produced by modes which are not equatorially symmetric produces matches for 24 out of the 35 MOST modes to within the observational error and another eight modes to within twice the observational error. The remaining three observed modes can be fit within 4.2 times the observational error, but even these may be fit to within the observational error if the criteria for computed modes are expanded. -
Global Scale Impacts
Global Scale Impacts Erik Asphaug Arizona State University Gareth Collins Imperial College, London Martin Jutzi University of Bern Global scale impacts modify the physical or thermal state of a substantial fraction of a target asteroid. Specific effects include accretion, family formation, reshaping, mixing and layering, shock and frictional heating, fragmentation, material compaction, dilatation, stripping of mantle and crust, and seismic degradation. Deciphering the complicated record of global scale impacts, in asteroids and meteorites, will lead us to understand the original planet-forming process and its resultant populations, and their evolution in time as collisions became faster and fewer. We provide a brief overview of these ideas, and an introduction to models. 1. Introduction v1 < v2 are the velocities of the target and projectile in the center of mass frame. If the energy is sufficiently intense, The most important parameter governing the global ex- Q > Q , then shattering occurs, breaking the solid bonds tent of an impact is the mass ratio of the projectile to the S∗ of the asteroid into pieces no larger than M =2. If gravita- target, γ = M =M . In the case of a cratering event this 1 2 1 tionally bound (ejected at < v ) then shattering produces ratio is small, and there is a well-defined geometric locus. esc a rubble pile as defined below; otherwise if fragments are Crater scaling then becomes a powerful tool (e.g. Housen escaping, the result is a collection of new asteroids. This et al. 1983) that allows simple analytical approaches to be is the classic example of hitting something so hard that applied to determine whether an impact ‘goes global’ – for you break it. -
Description of Map Units Northeast Asia Geodynamics Map
DESCRIPTION OF MAP UNITS NORTHEAST ASIA GEODYNAMICS MAP OVERLAP ASSEMBLAGES (Arranged alphabetically by map symbol) ad Adycha intermountain sedimentary basin (Miocene and Pliocene) (Yakutia) Basin forms a discontinuous chain along the foot of southwestern slope of Chersky Range in the Yana and Adycha Rivers basins. Contain Miocene and Pliocene sandstone, pebble gravel conglomerate, claystone, and minor boulder gravel conglomerate that range up to 400 m thick. REFERENCES: Grinenko and others, 1998. ag Agul (Rybinsk) molasse basin (Middle Devonian to Early Carboniferous) (Eastern Sayan) Consists of Middle Devonian through Early Carboniferous aerial and lacustrine sand-silt-mudstone, conglomerate, marl, and limestone with fauna and flora. Tuff, tuffite, and tuffaceous rock occur in Early Carboniferous sedimentary rocks. Ranges up to 2,000 m thick in southwestern margin of basin. Unconformably overlaps Early Devonian rocks of South Siberian volcanic-plutonic belt and Precambrian and early Paleozoic rocks of the Siberian Platform and surrounding fold belts. REFERENCES: Yanov, 1956; Graizer, Borovskaya, 1964. ags Argun sedimentary basin (Early Paleozoic) (Northeastern China) Occurs east of the Argun River in a discontinuously exposed, northeast-trending belt and consists of Cambrian and Ordovician marine, terrigenous detrital, and carbonate rocks. Cambrian units are composed of of feldspar- quartz sandstone, siltstone, shale and limestone and contain abundant Afaciacyathus sp., Bensocyathus sp., Robustocyathus yavorskii, Archaeocyathus yavorskii(Vologalin), Ethomophyllum hinganense Gu,o and other fossils. Ordovicain units consist of feldspar-quartz sandstone, siltstone, fine-grained sandstone and phylitic siltstone, and interlayered metamorphosed muddy siltstone and fine-grained sandstone with brachiopods, corals, and trilobites. Total thickness ranges up to 4,370 m. Basin unconformably overlies the Argunsky metamorphic terrane.