Possible Sign of Life on Venus Stirs up Heated Debate
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Astronomy 330 HW 2 Presentations Outline
Astronomy 330 HW 2 •! Stanley Swat This class (Lecture 12): http://www.ufohowto.com/ Life in the Solar System •! Lucas Guthrie Next Class: http://www.crystalinks.com/abduction.html Life in the Solar System HW 5 is due Wednesday Music: We Are All Made of Stars– Moby Presentations Outline •! Daniel Borup •! Life on Venus? Futurama •! Life on Mars? Life in the Solar System? Earth – Venus comparison •! We want to examine in more detail the backyard of humans. •! What we find may change our estimates of ne. Radius 0.95 Earth Surface gravity 0.91 Earth Venus is the hottest Mass 0.81 Earth planet, the closest in Distance from Sun 0.72 AU size to Earth, the closest Average Temp 475 C in distance to Earth, and Year 224.7 Earth days the planet with the Length of Day 116.8 Earth days longest day. Atmosphere 96% CO2 What We Used to Think Turns Out that Venus is Hell Venus must be hotter, as it is closer the Sun, but the cloud •! The surface is hot enough to melt lead cover must reflect back a large amount of the heat. •! There is a runaway greenhouse effect •! There is almost no water In 1918, a Swedish chemist and Nobel laureate concluded: •! There is sulfuric acid rain •! Everything on Venus is dripping wet. •! Most of the surface is no doubt covered with swamps. •! Not a place to visit for Spring Break. •! The constantly uniform climatic conditions result in an entire absence of adaptation to changing exterior conditions. •! Only low forms of life are therefore represented, mostly no doubt, belonging to the vegetable kingdom; and the organisms are nearly of the same kind all over the planet. -
"Is There Life on Venus?" Pdf File
Home / Space / Specials Is there life on Venus? We call them "Martians" because, in science fiction, Mars has always been the natural home of extraterrestrials. In fact, of all the planets in the solar system, Mars is the prime candidate to host life, after Earth, of course. Indeed, Mars is on the outer edge of the habitable zone, that area around the Sun that delimits the space where the temperature is low enough to ensure that the water remains in a liquid state. And where there's water, it is well known, there's probably life. Yet it's cold on Mars today, and so far, all the probes and rovers we have sent to the surface of the red planet have found no signs of life. Planet Venus At the opposite end of the habitable belt there is Venus, similar in size and "geological" characteristics to our planet – that is, like Earth, it is a rocky planet. However, unlike Earth, Venus is probably one of the most inhospitable places in the Solar System: the temperature on the ground is about 500°C, higher than that recorded on Mercury, the planet closest to the Sun, so the Sun is not directly responsible for that infernal climate. The blame lies with the very extreme greenhouse effect on Venus. We know that the greenhouse effect is due to the presence of gases that trap solar radiation and heat the atmosphere. The main greenhouse gases are carbon dioxide (CO2), methane, water vapour and nitrogen oxides. On Earth we are rightly concerned because the amount of carbon dioxide is increasing due to human activities and with the increase in CO2, temperatures are rising. -
Lockheed Martin to Help NASA Uncover Mysteries of Venus with VERITAS and DAVINCI+ Spacecraft
Lockheed Martin to Help NASA Uncover Mysteries of Venus with VERITAS and DAVINCI+ Spacecraft June 2, 2021 Lockheed Martin has a major role in NASA's long-anticipated return to Venus DENVER, June 2, 2021 /PRNewswire/ -- To learn more about how terrestrial planets evolve over time, NASA selected the VERITAS and DAVINCI+ missions for its Discovery Program, both bound for Venus. Lockheed Martin will design, build and operate both spacecraft. The missions will launch in 2026 and 2030 respectively, and will combine to study Venus' dense atmosphere, topography and geologic processes in great depth. Both missions will aim to discover how Venus – which may have been the first potentially habitable planet in our solar system – became inhospitable to life. They represent NASA's return to Earth's sister planet after more than three decades. "We're very grateful for this opportunity to work with NASA and the missions' principal investigators to fully understand how rocky planets evolved and what it means for our planet, Earth," said Lisa Callahan, vice president and general manager of Lockheed Martin's Commercial Civil Space business. "Our team who designed these two spacecraft to study Venus in unprecedented detail – and yield answers to its greatest mysteries – is beyond excited!" The operations and science for DAVINCI+ – which stands for Deep Atmosphere Venus Investigation of Noble Gases, Chemistry and Imaging Plus – will be managed by NASA's Goddard Space Flight Center in Greenbelt, Maryland. VERITAS – which stands for Venus Emissivity, Radio Science, InSAR, Topography & Spectroscopy – will have its science and operations managed by NASA's Jet Propulsion Laboratory in Southern California. -
Hints of Life on Venus John I Davies
News Feature: Hints of life on Venus John I Davies On the 14th of September 2020, the world was briefly distracted from its many present troubles by an announcement from the Royal Astronomical Society, Hints of life on Venus (ras.ac.uk/news-and- press/news/hints-life-venus). Subsequent analysis has questioned the discovery of the spectroscopic signature of molecule Phospine, chemical formula PH3 (en.wikipedia.org/wiki/Phosphine). The problem remains unresolved and in situ examination might be the best way of solving the Synthesized false colour image of Venus, using 283-nm mystery. and 365-nm band images taken by the Venus Ultraviolet Imager (UVI). JAXA / ISAS / Akatsuki Project Team Here John Davies summarises the research and the Source: CBS News response by i4is and others. See also www.cbsnews.com/video/venus-potential-life- discovered-on-planet Discovery Two major classes of chemical process are known to produce phosphine elsewhere in the Solar system. One is the highly energetic convective storms found in the atmospheres of gas giants such as Jupiter and the other is from living processes on Earth. So have we found a biosignature on Venus? The paper in Nature Astronomy is - Greaves, JS, Richards, AMS, Bains, W et al. Phosphine gas in the cloud decks of Venus. Nature Astronomy (2020). doi.org/10.1038/s41550-020-1174-4. (Received 07 February 2020). The paper is available at - www.nature.com/articles/s41550-020-1174-4.pdf. The lead author is Jane S Greaves, of the universities of Cardiff and Cambridge, UK. Other authors are from Jodrell Bank, MIT, Cambridge University, Kyoto Sangyo University, Imperial College London, Cardiff University, The UK Open University and East Asian Observatory Hawaii. -
Constraints on a Potential Aerial Biosphere on Venus: I. Cosmic Rays ⇑ Lewis R
Icarus 257 (2015) 396–405 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Constraints on a potential aerial biosphere on Venus: I. Cosmic rays ⇑ Lewis R. Dartnell a, , Tom Andre Nordheim b,c, Manish R. Patel d,e, Jonathon P. Mason d, Andrew J. Coates b,c, Geraint H. Jones b,c a Space Research Centre, Department of Physics and Astronomy, University of Leicester, Leicester LE1 7RH, UK b Mullard Space Science Laboratory, University College London, Dorking, Surrey RH5 6NT, UK c Centre for Planetary Sciences at UCL/Birkbeck, University College London, Gower Street, London WC1E 6BT, UK d Department of Physical Sciences, The Open University, Milton Keynes, UK e Space Science and Technology Department, STFC Rutherford Appleton Laboratory, Chilton, Oxfordshire OX11 0QX, UK article info abstract Article history: While the present-day surface of Venus is certainly incompatible with terrestrial biology, the planet may Received 31 October 2014 have possessed oceans in the past and provided conditions suitable for the origin of life. Venusian life Revised 10 April 2015 may persist today high in the atmosphere where the temperature and pH regime is tolerable to terrestrial Accepted 7 May 2015 extremophile microbes: an aerial habitable zone. Here we argue that on the basis of the combined Available online 15 May 2015 biological hazard of high temperature and high acidity this habitable zone lies between 51 km (65 °C) and 62 km (À20 °C) altitude. Compared to Earth, this potential venusian biosphere may be exposed to Keywords: substantially more comic ionising radiation: Venus has no protective magnetic field, orbits closer to Astrobiology the Sun, and the entire habitable region lies high in the atmosphere – if this narrow band is sterilised Cosmic rays Exobiology there is no reservoir of deeper life that can recolonise afterwards. -
Our Solar System
This graphic of the solar system was made using real images of the planets and comet Hale-Bopp. It is not to scale! To show a scale model of the solar system with the Sun being 1cm would require about 64 meters of paper! Image credit: Maggie Mosetti, NASA This book was produced to commemorate the Year of the Solar System (2011-2013, a martian year), initiated by NASA. See http://solarsystem.nasa.gov/yss. Many images and captions have been adapted from NASA’s “From Earth to the Solar System” (FETTSS) image collection. See http://fettss.arc.nasa.gov/. Additional imagery and captions compiled by Deborah Scherrer, Stanford University, California, USA. Special thanks to the people of Suntrek (www.suntrek.org,) who helped with the final editing and allowed me to use Alphonse Sterling’s awesome photograph of a solar eclipse! Cover Images: Solar System: NASA/JPL; YSS logo: NASA; Sun: Venus Transit from NASA SDO/AIA © 2013-2020 Stanford University; permission given to use for educational and non-commericial purposes. Table of Contents Why Is the Sun Green and Mars Blue? ............................................................................... 4 Our Sun – Source of Life ..................................................................................................... 5 Solar Activity ................................................................................................................... 6 Space Weather ................................................................................................................. 9 Mercury -
Life on Venus, and How to Explore Venus with High-Temperature Electronics Carl-Mikael Zetterling [email protected]
Life on Venus, and How to Explore Venus with High-Temperature Electronics Carl-Mikael Zetterling [email protected] www.WorkingonVenus.se Outline Life on Venus (phosphine in the clouds) Previous missions to Venus Life on Venus (photos from the ground) High temperature electronics Future missions to Venus, including Working on Venus (KTH Project 2014 - 2018) www.WorkingonVenus.se 3 Phosphine gas in the cloud decks of Venus Trace amounts of phosphine (20 ppb, PH3) seen by the ALMA and JCMT telescopes, with millimetre wave spectral detection 4 Phosphine gas in the cloud decks of Venus 5 Phosphine gas in the cloud decks of Venus https://www.nature.com/articles/s41550-020-1174-4 https://arxiv.org/pdf/2009.06499.pdf https://www.nytimes.com/2020/09/14/science/venus-life- clouds.html?smtyp=cur&smid=fb-nytimesfindings https://www.scientificamerican.com/article/is-there-life-on- venus-these-missions-could-find-it/ 6 Did NASA detect phosphine 1978? Pioneer 13 Large Probe Neutral Mass Spectrometer (LNMS) https://www.livescience.com/life-on-venus-pioneer-13.html 7 Why Venus? From Wikimedia Commons, the free media repository Our closest planet, but least known Similar to earth in size and core, has an atmosphere Volcanoes Interesting for climate modeling Venus Long-life Surface Package (ultimate limit of global warming) C. Wilson, C.-M. Zetterling, W. T. Pike IAC-17-A3.5.5, Paper 41353 arXiv:1611.03365v1 www.WorkingonVenus.se 8 Venus Atmosphere 96% CO2 (Also sulphuric acids) Pressure of 92 bar (equivalent to 1000 m water) Temperature 460 °C From Wikimedia Commons, the free media repository Difficult to explore Life is not likely www.WorkingonVenus.se 9 Previous Missions Venera 1 – 16 (1961 – 1983) USSR Mariner 2 (1962) NASA, USA Pioneer (1978 – 1992) NASA, USA Magellan (1989) NASA, USA Venus Express (2005 - ) ESA, Europa From Wikimedia Commons, the free media repository Akatsuki (2010) JAXA, Japan www.WorkingonVenus.se 10 Steps to lunar and planetary exploration: 1. -
Types of Aliens
7/19/13 TYPES OF ALIENS TYPES OF ALIENS AGHARIANS - (or Aghartians) A group of Asiatic or Nordic humans who, sources claim, discovered a vast system of caverns below the region of the Gobi desert and surrounding areas thousands of years ago, and have since established a thriving kingdom within, one which has been interacting with other-planetary systems up until current times. ALPHA-DRACONIANS Reptilian beings who are said to have established colonies in Alpha Draconis. Like all reptilians, these claim to have originated on Terra thousands of years ago, a fact that they use to 'justify' their attempt to re-take the earth for their own. They are apparently a major part of a planned 'invasion' which is eventually turning from covert infiltration mode to overt invasion mode as the "window of opportunity" (the time span before International human society becomes an interplanetary and interstellar power) slowly begins to close. ---- They are attempting to keep the "window" open by suppressing advanced technology from the masses, which would lead to eventual Terran colonization of other planets by Earth and an eventual solution to the population, pollution, food and other environmental problems. Being that Terrans have an inbred "warrior" instinct the Draconians DO NOT want them/us to attain interstellar capabilities and therefore become a threat to their imperialistic agendas. Refer to Els ALTAIRIANS Alleged Reptilian inhabitants of the Altair stellar system in the constellation Aquila, in collaboration with a smaller Nordic human element and a collaborative Grey and Terran military presence. Headquarters of a collective known as the "Corporate", which maintains ties with the Ashtar and Draconian collectives (Draconian). -
^ Aw Ien Ticu T
next AL [ W J R e c k ’s week ^aw ienticut tc 00 p *— A L ’S iX c* UJ a <J. o “Lawrence-land’s Greatest Family Newspaper" c> J 13 (U Ui c* a 3 VOL. 77. NUMBER 16 LAWRENCE COLLEGE. APPLETON. WIS. Saturday, Febraury 8. 1958** Oi •'* r* i* • v> Petition Refused By ti> Ui K night, Loom er Cf o T Faculty; Referred To O VO Spark R. L. C. w o Standing Committee () (0 BY PETE NEGRONIDA Decision-Making Pointed Up As <-*■ The recent student petition concerning a pre-examin- tion reading period was denied by the faculty in its last for mal meeting of the semester just completed. “The main rea Union of Ethics And Religion son for the refusal,” stated Dean Marshall Hulbert (who presented the petition for the Committee on Administra Lawrence returned from its semester vacation this past tion), “was that there was no time to act on it.” week to be met by “Religion and Ethics,” the theme of this “The faculty does not op year’s Religion-in-Life Conference. Running from President Douglas M. Knight’s opening address pose a reading period per se,” last Monday night to the coffee-hour following the final address of he continued, “but it wanted Show Train Dr. Bernard M. Loomer on Wednesday evening, the conference en to look into it further before joyed one lively and well-attended session after another. taking action.” The reading CHRONOLOGY and Sage Halls, the fraternity period issue was turned over Ready To Go Film Classics will start its new Following Knight’s kickoff quadrangle, and the Art Center. -
The Combination Problem for Panpsychism: a Constitutive Russellian Solution
THE COMBINATION PROBLEM FOR PANPSYCHISM: A CONSTITUTIVE RUSSELLIAN SOLUTION AN INVESTIGATION INTO PHENOMENAL BONDING PANPSYCHISM AND COMPOSITE SUBJECTS OF EXPERIENCE Thesis submitted in accordance with the requirements of the University of Liverpool for the degree of Doctor of Philosophy by Gregory Edward Miller University of Liverpool September 2018 i Abstract In this thesis I argue for the following theory: constitutive Russellian phenomenal bonding panpsychism. To do so I do three main things: 1) I argue for Russellian panpsychism. 2) I argue for phenomenal bonding panpsychism. 3) I defend the resultant phenomenal bonding panpsychist model. The importance of arguing for (and defending) such a theory is that if it can be made to be viable, then it is proposed to be the most promising theory of the place of consciousness within nature (Chalmers, 2016a; Strawson, 2006a). This is because constitutive Russellian panpsychism has all the theoretical virtues of physicalism and dualism but does not face the problems they do (Alter and Nagasawa, 2015a; Chalmers, 2016a). The combination problem, however, is the most significant problem for the Russellian panpsychist (Chalmers, 2016b; Goff, 2017a), and, hence, in order to show the viability of the theory I address this problem. Moreover, I present a novel ‘mereological argument’ for panpsychism which makes it necessary that the Russellian panpsychist addresses (and solves) the combination problem. The focus of this thesis is therefore addressing this problem. I argue that the combination problem can indeed be solved. To do so I argue for the phenomenal bonding solution proposed by Goff (Goff, 2016, 2009a). I argue that this solution works and that we can form a positive concept of the phenomenal bonding relation (Miller, 2017). -
Venera-D Landing Sites Selection and Cloud Layer Habitability Workshop Report
1 Venera-D Landing Sites Selection and Cloud Layer Habitability Workshop Report IKI Moscow, Russia October 2-5, 2019 Space Science Research Institute (IKI), Russian Academy of Science, Roscosmos, and NASA http://venera-d.cosmos.ru/index.php?id=workshop2019&L=2 https://www.hou.usra.edu/meetings/venera-d2019/ 2 Table of Contents Introduction ...................................................................................................................................................... 6 Final Agenda .................................................................................................................................................. 10 Astrobiology Special Collection of papers from the workshop .................................................... 14 Technical Report: Venera-D Landing Site and Cloud Habitability Workshop ......................... 15 1.0 Missions to Venus .......................................................................................................................... 15 1.1 Past and Present ................................................................................................................................. 15 1.1.1 Available Instruments and Lessons Learned Surface Geology ........................................................... 15 1.1.2 Available Instruments and Lessons Learned for Cloud Habitability ............................................... 16 1.2 Future Missions .................................................................................................................................. -
What Makes a Planet Habitable?
Astron Astrophys Rev (2009) 17:181–249 DOI 10.1007/s00159-009-0019-z REVIEW ARTICLE What makes a planet habitable? H. Lammer · J. H. Bredehöft · A. Coustenis · M. L. Khodachenko · L. Kaltenegger · O. Grasset · D. Prieur · F. Raulin · P. Ehrenfreund · M. Yamauchi · J.-E. Wahlund · J.-M. Grießmeier · G. Stangl · C. S. Cockell · Yu.N.Kulikov · J. L. Grenfell · H. Rauer Received: 25 August 2008 / Revised: 2 February 2009 / Published online: 10 April 2009 © Springer-Verlag 2009 Abstract This work reviews factors which are important for the evolution of habitable Earth-like planets such as the effects of the host star dependent radiation and particle fluxes on the evolution of atmospheres and initial water inventories. We discuss the geodynamical and geophysical environments which are necessary for plan- ets where plate tectonics remain active over geological time scales and for planets H. Lammer (B) · M. L. Khodachenko · G. Stangl Space Research Institute, Austrian Academy of Sciences, Graz, Austria e-mail: [email protected] M. L. Khodachenko e-mail: [email protected] G. Stangl e-mail: [email protected] J. H. Bredehöft Institut für Angewandte und Physikalische Chemie, Universität Bremen, Bremen, Germany e-mail: [email protected] A. Coustenis Laboratoire d’Etudes Spatiales et d’Instrumentation en Astrophysique (LESIA), Observatoire de Meudon, Meudon, France e-mail: [email protected] L. Kaltenegger Harvard-Smithonian Center for Astrophysics, Cambridge, MA, USA e-mail: [email protected] O. Grasset UMR, Laboratoire de Planétologie et Géodynamique, Nantes, France e-mail: [email protected] 123 182 H.