“Beagle-2 Aftermath” : Lessons Learned and the Post-Landing Phase
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Planetary Report Report
The PLANETARYPLANETARY REPORT REPORT Volume XXIX Number 1 January/February 2009 Beyond The Moon From The Editor he Internet has transformed the way science is On the Cover: Tdone—even in the realm of “rocket science”— The United States has the opportunity to unify and inspire the and now anyone can make a real contribution, as world’s spacefaring nations to create a future brightened by long as you have the will to give your best. new goals, such as the human exploration of Mars and near- In this issue, you’ll read about a group of amateurs Earth asteroids. Inset: American astronaut Peggy A. Whitson who are helping professional researchers explore and Russian cosmonaut Yuri I. Malenchenko try out training Mars online, encouraged by Mars Exploration versions of Russian Orlan spacesuits. Background: The High Rovers Project Scientist Steve Squyres and Plane- Resolution Camera on Mars Express took this snapshot of tary Society President Jim Bell (who is also head Candor Chasma, a valley in the northern part of Valles of the rovers’ Pancam team.) Marineris, on July 6, 2006. Images: Gagarin Cosmonaut Training This new Internet-enabled fun is not the first, Center. Background: ESA nor will it be the only, way people can participate in planetary exploration. The Planetary Society has been encouraging our members to contribute Background: their minds and energy to science since 1984, A dust storm blurs the sky above a volcanic caldera in this image when the Pallas Project helped to determine the taken by the Mars Color Imager on Mars Reconnaissance Orbiter shape of a main-belt asteroid. -
Esa Publications
number 172 | 4th quarter 2017 bulletin → united space in europe European Space Agency The European Space Agency was formed out of, and took over the rights and The ESA headquarters are in Paris. obligations of, the two earlier European space organisations – the European Space Research Organisation (ESRO) and the European Launcher Development The major establishments of ESA are: Organisation (ELDO). The Member States are Austria, Belgium, Czech Republic, Denmark, Estonia, Finland, France, Germany, Greece, Hungary, Ireland, Italy, ESTEC, Noordwijk, Netherlands. Luxembourg, the Netherlands, Norway, Poland, Portugal, Romania, Spain, Sweden, Switzerland and the United Kingdom. Slovenia is an Associate Member. Canada ESOC, Darmstadt, Germany. takes part in some projects under a cooperation agreement. Bulgaria, Cyprus, Malta, Latvia, Lithuania and Slovakia have cooperation agreements with ESA. ESRIN, Frascati, Italy. ESAC, Madrid, Spain. In the words of its Convention: the purpose of the Agency shall be to provide for and to promote, for exclusively peaceful purposes, cooperation among European EAC, Cologne, Germany. States in space research and technology and their space applications, with a view to their being used for scientific purposes and for operational space applications ECSAT, Harwell, United Kingdom. systems: ESEC, Redu, Belgium. → by elaborating and implementing a long-term European space policy, by recommending space objectives to the Member States, and by concerting the policies of the Member States with respect to other national -
Retour Des Réponses Le 06/01/2020 À [email protected] PARTIE I
Episode 2 – Énoncé des énigmes le 04/11/2019 ; retour des réponses le 06/01/2020 à [email protected] PARTIE I – Questions à choix multiples – Trouver la bonne réponse pour chacune des questions ! Question 1. Comparons nos deux planètes telluriques voisines La Terre et Mars. Quelle est la réponse fausse parmi les suivantes ? o Le diamètre de la planète Mars est plus petit que celui de la Terre o Ces deux planètes rocheuses ont la même masse volumique o Ces deux planètes sont rocheuses et ont chacune au moins un satellite o L’atmosphère de Mars est 61 fois plus fine que celle de la Terre o la gravité de surface sur Mars est seulement 38 % de celle de la Terre Question 2. Il n'y a pas que sur la Terre qu'il y a des volcans. Le volcanisme de la planète Mars serait apparu il y a près de quatre milliards d'années. Il aurait connu son intensité maximale à entre 3,7 et 3,2 Ga, puis se serait progressivement affaibli. Il a produit de nombreux volcans tels que Olympus Mons, Pavonis Mons, Ascraeus Mons, Elysium Mons, Arsia Mons. Localisez chacun de ces volcans sur la carte ci dessous : o volcan 1 > o volcan 2 > o volcan 3 > o volcan 4 > o volcan 5 > Question 3. Classez ces volcans par altitude. Le plus haut en premier (A), le moins haut en dernier (E) o volcan A le plus haut > o volcan B > o volcan C > o volcan D > o volcan E le moins haut > Question 4. -
Exploration of Mars by the European Space Agency 1
Exploration of Mars by the European Space Agency Alejandro Cardesín ESA Science Operations Mars Express, ExoMars 2016 IAC Winter School, November 20161 Credit: MEX/HRSC History of Missions to Mars Mars Exploration nowadays… 2000‐2010 2011 2013/14 2016 2018 2020 future … Mars Express MAVEN (ESA) TGO Future ESA (ESA- Studies… RUSSIA) Odyssey MRO Mars Phobos- Sample Grunt Return? (RUSSIA) MOM Schiaparelli ExoMars 2020 Phoenix (ESA-RUSSIA) Opportunity MSL Curiosity Mars Insight 2020 Spirit The data/information contained herein has been reviewed and approved for release by JPL Export Administration on the basis that this document contains no export‐controlled information. Mars Express 2003-2016 … First European Mission to orbit another Planet! First mission of the “Rosetta family” Up and running since 2003 Credit: MEX/HRSC First European Mission to orbit another Planet First European attempt to land on another Planet Original mission concept Credit: MEX/HRSC December 2003: Mars Express Lander Release and Orbit Insertion Collission trajectory Bye bye Beagle 2! Last picture Lander after release, release taken by VMC camera Insertion 19/12/2003 8:33 trajectory Credit: MEX/HRSC Beagle 2 was found in January 2015 ! Only 6km away from landing site OK Open petals indicate soft landing OK Antenna remained covered Lessons learned: comms at all time! Credit: MEX/HRSC Mars Express: so many missions at once Mars Mission Phobos Mission Relay Mission Credit: MEX/HRSC Mars Express science investigations Martian Moons: Phobos & Deimos: Ionosphere, surface, -
Mars Exploration - a Story Fifty Years Long Giuseppe Pezzella and Antonio Viviani
Chapter Introductory Chapter: Mars Exploration - A Story Fifty Years Long Giuseppe Pezzella and Antonio Viviani 1. Introduction Mars has been a goal of exploration programs of the most important space agencies all over the world for decades. It is, in fact, the most investigated celestial body of the Solar System. Mars robotic exploration began in the 1960s of the twentieth century by means of several space probes sent by the United States (US) and the Soviet Union (USSR). In the recent past, also European, Japanese, and Indian spacecrafts reached Mars; while other countries, such as China and the United Arab Emirates, aim to send spacecraft toward the red planet in the next future. 1.1 Exploration aims The high number of mission explorations to Mars clearly points out the impor- tance of Mars within the Solar System. Thus, the question is: “Why this great interest in Mars exploration?” The interest in Mars is due to several practical, scientific, and strategic reasons. In the practical sense, Mars is the most accessible planet in the Solar System [1]. It is the second closest planet to Earth, besides Venus, averaging about 360 million kilometers apart between the furthest and closest points in its orbit. Earth and Mars feature great similarities. For instance, both planets rotate on an axis with quite the same rotation velocity and tilt angle. The length of a day on Earth is 24 h, while slightly longer on Mars at 24 h and 37 min. The tilt of Earth axis is 23.5 deg, and Mars tilts slightly more at 25.2 deg [2]. -
A Singular Seasonally Recurrent Double Vortex on Mars
A singular seasonally recurrent double vortex on Mars Agustín Sanchez-Lavega1, A. Garro1, R. Hueso1, T. del Rio-Gaztelurrutia1, Hao Chen Chen1, I. Ordoñez-Etxeberria1, A. Cardesin-Moinelo2, D. Titov3, S. Wood4, M. Dias-Almeida5 1. Dpto. Física Aplicada I, Universidad del País Vasco UPV/EHU, Bilbao, Spain. 2. European Space Agency - ESAC, Madrid, Spain. 3. European Space Agency - ESTEC, Noorwijk, Netherlands. 4. European Space Agency - ESOC, Darmstadt, Germany. 5. Dias Almeida Data Processing and Systems, Ittigen, Switzerland From Mars Express to Exomars – 28 February 2018 Visual Monitoring Camera (VMC) – Mars Express (MEx) VMC * Beagle descent * Outreach Science Instrument (*) Detector • CMOS • Bayer RGB (COLOR) • Wavelength: 400-650 nm VMC/MEx (June-July 2012) Additional images used in this study (NASA – PDS) MARCI/Mars Reconnaissance Orbiter Navigation PLIA software MOC/Mars Global Surveyor (*) Sánchez-Lavega A. et al., Limb clouds and dust on Mars from images obtained by the Visual Monitoring Camera (VMC) onboard Mars Express, Icarus, 299, 194 (2018). PLIA software: Hueso et al., Adv. Space Res. , 2010 From Mars Express to Exomars – 28 February 2018 Vortex properties MEx-VMC June 18, 2012 The vortex repeat in location and date Latitude: 60°N Longitude: 70W – 110W ( 800 Km East of PHOENIX lander) LS = 120-140° (Northern summer solstice: LS =90°) Size (each vortex): 600 - 800 km Wavelength 90 Wavenumber m = 4 From Mars Express to Exomars – 28 February 2018 Vortex Motion June 15-23 (2012) - MEx/VMC 1- UTC: 12-06-15 / 05:26:12 Local -
First Year of Coordinated Science Observations by Mars Express and Exomars 2016 Trace Gas Orbiter
MANUSCRIPT PRE-PRINT Icarus Special Issue “From Mars Express to ExoMars” https://doi.org/10.1016/j.icarus.2020.113707 First year of coordinated science observations by Mars Express and ExoMars 2016 Trace Gas Orbiter A. Cardesín-Moinelo1, B. Geiger1, G. Lacombe2, B. Ristic3, M. Costa1, D. Titov4, H. Svedhem4, J. Marín-Yaseli1, D. Merritt1, P. Martin1, M.A. López-Valverde5, P. Wolkenberg6, B. Gondet7 and Mars Express and ExoMars 2016 Science Ground Segment teams 1 European Space Astronomy Centre, Madrid, Spain 2 Laboratoire Atmosphères, Milieux, Observations Spatiales, Guyancourt, France 3 Royal Belgian Institute for Space Aeronomy, Brussels, Belgium 4 European Space Research and Technology Centre, Noordwijk, The Netherlands 5 Instituto de Astrofísica de Andalucía, Granada, Spain 6 Istituto Nazionale Astrofisica, Roma, Italy 7 Institut d'Astrophysique Spatiale, Orsay, Paris, France Abstract Two spacecraft launched and operated by the European Space Agency are currently performing observations in Mars orbit. For more than 15 years Mars Express has been conducting global surveys of the surface, the atmosphere and the plasma environment of the Red Planet. The Trace Gas Orbiter, the first element of the ExoMars programme, began its science phase in 2018 focusing on investigations of the atmospheric composition with unprecedented sensitivity as well as surface and subsurface studies. The coordination of observation programmes of both spacecraft aims at cross calibration of the instruments and exploitation of new opportunities provided by the presence of two spacecraft whose science operations are performed by two closely collaborating teams at the European Space Astronomy Centre (ESAC). In this paper we describe the first combined observations executed by the Mars Express and Trace Gas Orbiter missions since the start of the TGO operational phase in April 2018 until June 2019. -
Planet Mars III 28 March- 2 April 2010 POSTERS: ABSTRACT BOOK
Planet Mars III 28 March- 2 April 2010 POSTERS: ABSTRACT BOOK Recent Science Results from VMC on Mars Express Jonathan Schulster1, Hannes Griebel2, Thomas Ormston2 & Michel Denis3 1 VCS Space Engineering GmbH (Scisys), R.Bosch-Str.7, D-64293 Darmstadt, Germany 2 Vega Deutschland Gmbh & Co. KG, Europaplatz 5, D-64293 Darmstadt, Germany 3 Mars Express Spacecraft Operations Manager, OPS-OPM, ESA-ESOC, R.Bosch-Str 5, D-64293, Darmstadt, Germany. Mars Express carries a small Visual Monitoring Camera (VMC), originally to provide visual telemetry of the Beagle-2 probe deployment, successfully release on 19-December-2003. The VMC comprises a small CMOS optical camera, fitted with a Bayer pattern filter for colour imaging. The camera produces a 640x480 pixel array of 8-bit intensity samples which are recoded on ground to a standard digital image format. The camera has a basic command interface with almost all operations being performed at a hardware level, not featuring advanced features such as patchable software or full data bus integration as found on other instruments. In 2007 a test campaign was initiated to study the possibility of using VMC to produce full disc images of Mars for outreach purposes. An extensive test campaign to verify the camera’s capabilities in-flight was followed by tuning of optimal parameters for Mars imaging. Several thousand images of both full- and partial disc have been taken and made immediately publicly available via a web blog. Due to restrictive operational constraints the camera cannot be used when any other instrument is on. Most imaging opportunities are therefore restricted to a 1 hour period following each spacecraft maintenance window, shortly after orbit apocenter. -
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Download DARWIN, Beagle Diary.Pdf
CHARLES DARWIN'S BEAGLE DIARY Edited by Richard Darwin Keynes, CBE, ScD, FRS Emeritus Professor of Physiology in the University of Cambridge, and Fellow of Churchill College CAMBRIDGE UNIVERSITY PRESS [page iv] PUBLISHED BY THE PRESS SYNDICATE OF THE UNIVERSITY OF CAMBRIDGE The Pitt Building, Trumpington Street, Cambridge, United Kingdom CAMBRIDGE UNIVERSITY PRESS The Edinburgh Building, Cambridge CB2 2RU, UK 40 West 20th Street, New York, NY 10011–4211, USA 10 Stamford Road, Oakleigh, VIC 3166, Australia Ruiz de Alarcón 13, 28014 Madrid, Spain Dock House, The Waterfront, Cape Town 8001, South Africa http://www.cambridge.org © Cambridge University Press 1988 September 7th, 1835 The Beagle sailed for the Galapagos: 15th on the 15th she was employed in surveying the outer coast of Chatham Isd1 the S. Eastern one of the Archipelago. |604| 1 The Spanish name of Chatham Island now used is Isla San Cristobal. 16th The next day we ran near Hoods Isd1 & there left a Whale boat. — In the evening the Yawl was also sent away on a surveying cruize of some length. — The weather, now & during the passage, has continued as on the coast of Peru, a steady, gentle breeze of wind & gloomy sky. — We landed for an hour on the NW end of Chatham Isd. — These islands at a distance have a sloping uniform outline, excepting where broken by sundry paps & hillocks. — The whole is black Lava, completelycovered by small leafless brushwood & low trees. — The fragments of Lava where most porous are reddish & like cinders; the stunted trees show [page] 352 GALAPAGOS ISDS SEPTEMBER 1835 Chart of the Galapagos Islands (from part of a map in Narrative 1). -
Phoenix Descending NASA’S Mars Strategy Goes from “Follow the Water” to “Arrive at the Ice”
NEWS NATURE|Vol 453|8 May 2008 Phoenix descending NASA’s Mars strategy goes from “follow the water” to “arrive at the ice”. Since 2001, the slogan for from hardware and software. NASA’s Mars programme has “We may not succeed, but we NASA been “follow the water”. deserve to succeed,” he says. With Phoenix, a US$420- Engineers at the Jet Propul- million mission to the edge of sion Laboratory in Pasadena, the planet’s north ice cap, the California, which runs most of agency hopes to finally touch NASA’s planetary missions, will its quarry, in the form of dirty have their last chance to tweak water ice scraped from the the trajectory on 24 May. The subsurface and melted in the next day, Phoenix is expected probe’s on-board ovens. to use the planet’s atmosphere, If all goes as planned, Phoenix and its own heat shielding, will reach the end of its 680- parachutes and retrorockets, to million-kilometre, 10-month- slow itself down from an orbital long journey on 25 May. Its speed of 20,000 kilometres per landing site is in a region where hour to a soft, safe landing at NASA’s orbiting Mars Odyssey just 2.4 metres per second. spacecraft has detected gamma-ray and neu- Phoenix, a 350-kilogram lander, inherited Smith and his team hope that the ice and soil tron signatures suggesting a significant amount hardware from the Mars Surveyor Lander, a samples they will study with the spacecraft’s of hydrogen — thought to be a constituent of mission cancelled in 2000 after the failure of mass-spectrometer and chemical analysis sys- frozen water — near the surface. -
1 Archives of Natural History, 47, 147-165. Accepted Version. Robert
Archives of Natural History, 47, 147-165. Accepted version. Robert McCormick’s geological collections from Antarctica and the Southern Ocean, 1839–1843 PHILIP STONE British Geological Survey, The Lyell Centre, Research Avenue South, Edinburgh EH14 4AP, Scotland, UK (e-mail: [email protected]) ABSTRACT: Robert McCormick (1800–1890) took part in three mid-nineteenth- century British Polar expeditions, two to the Arctic and one to the Antarctic. The latter, from 1839 to 1843 and led by James Clark Ross, is the best known. McCormick served as senior surgeon on HMS Erebus and was responsible for the collection of zoological and geological specimens. Despite the novelty and potential scientific importance of these early geological collections from Antarctica and remote islands in the Southern Ocean, they received surprisingly little attention at the time. Ross deposited an official collection with the British Museum in 1844, soon after the expedition’s return, and this was supplemented by McCormick’s personal collection, bequeathed in 1890. McCormick had contributed brief and idiosyncratic geological notes to the expedition report published by Ross in 1847, but it was not until 1899 that an informed description of the Antarctic rocks was published, and only in 1921 were McCormick’s palaeobotanical specimens from Kerguelen examined. His material from other Southern Ocean islands received even less attention; had it been utilized at the time it would have supplemented the better-known collections made by the likes of Charles Darwin. In later life, McCormick became increasingly embittered over the lack of recognition afforded to him for his work in the Polar regions.