Titan Science Questions at the End of Cassini-Huygens

Total Page:16

File Type:pdf, Size:1020Kb

Titan Science Questions at the End of Cassini-Huygens Planetary Science Vision 2050 Workshop 2017 (LPI Contrib. No. 1989) 8156.pdf RIDDLES OF THE SPHINX: TITAN SCIENCE QUESTIONS AT THE END OF CASSINI-HUYGENS. C.A. Nixon1, R. K. Achterberg2, A. Buch3, R. N. Clark4, P. Coll5, F. M. Flasar1, A. G. Hayes6, L. Iess7, R. D. Lo- renz8, R. Lopes9, M. Mastrogiuseppe7, F. Raulin5, T. Smith8, A. Solomidou9, C. Sotin9, D. F. Strobel10, E. P. Turtle8, V. Vuitton11, R. West9, R. Yelle12. 1Planetary Systems Laboratory, NASA Goddard Space Flight Center, 8800 Greenbelt Road, Greenbelt, MD 20771, USA, [email protected]; 2Dept. of Astronomy, Univ. Maryland, Col- lege Park, MD 20742, USA; 3LGPM, Ecole Centrale Paris, Chatenay-Malabry, France; 4U.S. Geological Survey, Denver Federal Center, Denver, Colorado, USA; 5LISA, UPEC-UPD/CNRS/IPSL, Paris-Créteil, France; 6Dept. of Astronomy, Cornell Univ., Ithaca, New York, USA; 7Dipartimento di Ingegneria Meccanica e Aerospaziale, Univer- sità La Sapienza, via Eudossiana 18, 00184 Rome, Italy; 8Johns Hopkins Applied Physics Lab., Laurel, MD 20723, 9 10 USA; Caltech/Jet Propulsion Lab., 4800 Oak Grove Drive, Pasadena, CA 91109, USA; Dept. of Earth and Plane- tary Sciences, 3400 N. Charles Street, Johns Hopkins Univ., Baltimore, MD 21218, USA; 11UJF-Grenoble 1/CNRS- INSU, Institut de Planétologie et d’Astrophysique de Grenoble (IPAG) UMR 5274, Grenoble F-38041 ; 12Lunar and Planetary Lab., Dept. of Planetary Sciences, Univ. of Arizona, Tucson, Arizona, USA. Introduction: Since July 2004, the Cassini space- (1B) Why does Titan have an atmosphere, and how has craft has been orbiting Saturn, making repeated close it changed over time? encounters with Titan, its largest moon and the only (1C) What is the age of the features we see on Titan’s moon in the solar system to possess a dense atmos- surface? phere. By the end of the mission in September 2017, Interior and surface: Cassini will have amassed a vast wealth of scientific (2A) How thick is the icy shell and how deep is the ocean? data about Titan collected by 12 instruments during (2B) Is Titan geologically active today? 127 close flybys. These include: images and spectra (2C) What materials are exposed on the surface? from four remote sensing devices; particles and fields (2D) What factors influence the distribution of the measurements from six further instruments; and radar lakes and seas? and radio measurements of the atmosphere and surface (2E) What is the composition of the lakes and seas? at multiple wavelengths. (2F) What degree of prebiotic chemical complexity has In January 2005 the Huygens probe descended by been reached in surface environments? parachute to the surface, making the first in-situ meas- urements of the neutral atmosphere and surface with Lower and middle atmosphere: six on-board instruments, including winds, atmospher- (3A) How can we explain the observed variations in ic composition, temperature-pressure structure, hazes, Titan’s hydrogen profile? and surface characteristics. (3B) How can atmospheric models be reconciled with The international Cassini-Huygens mission has observations of clouds in the lower atmosphere? made huge advances in our understanding of this en- (3C) Why is the stratospheric axis tilted with respect to igmatic world, the greatest stride forward since the Titan’s solid body? Voyager 1 encounter of 1980. However it is clear in (3D) What is the reason for the detached haze layer? the closing stages of the mission that many mysteries Upper atmosphere and exosphere: remain. During a meeting of the Cassini-Huygens sci- (4A) What chemical processes lead to the formation of ence team in October 2016, Titan scientists were invit- complex molecules, including aromatics? ed to consider how many of the high-level questions (4B) How rapidly is Titan’s methane escaping into from the start of the mission have now been answered. space? The team concluded that while some of the pre-Cassini (4C) What gives rise to the observed electron density mysteries are now largely “solved”, some of the most profile? perplexing questions remain only partially understood, (4D) Do we see the expected nitrogen torus? while new riddles have also emerged from the data. Key Questions: the questions are divided into four Conclusions: In this paper we present a viewpoint broad thematic areas, while recognizing that in practice on the most important questions remaining for Titan these subject areas are all tied together: (1) history; (2) science at the end of the Cassini-Huygens mission. interior and surface; (3) lower and middle atmosphere; New data will be accumulated by powerful ground and (4) upper atmosphere and exosphere. space-based observatories in the years after Cassini; History: however, some of the most important questions will (1A) How did Titan form, and was this early or late in await new, focused spacecraft missions to Titan in the the solar system? decades from 2020 to 2050 to be more fully answered. .
Recommended publications
  • Saturn — from the Outside In
    Saturn — From the Outside In Saturn — From the Outside In Questions, Answers, and Cool Things to Think About Discovering Saturn:The Real Lord of the Rings Saturn — From the Outside In Although no one has ever traveled ing from Saturn’s interior. As gases in from Saturn’s atmosphere to its core, Saturn’s interior warm up, they rise scientists do have an understanding until they reach a level where the tem- of what’s there, based on their knowl- perature is cold enough to freeze them edge of natural forces, chemistry, and into particles of solid ice. Icy ammonia mathematical models. If you were able forms the outermost layer of clouds, to go deep into Saturn, here’s what you which look yellow because ammonia re- trapped in the ammonia ice particles, First, you would enter Saturn’s up- add shades of brown and other col- per atmosphere, which has super-fast ors to the clouds. Methane and water winds. In fact, winds near Saturn’s freeze at higher temperatures, so they equator (the fat middle) can reach turn to ice farther down, below the am- speeds of 1,100 miles per hour. That is monia clouds. Hydrogen and helium rise almost four times as fast as the fast- even higher than the ammonia without est hurricane winds on Earth! These freezing at all. They remain gases above winds get their energy from heat ris- the cloud tops. Saturn — From the Outside In Warm gases are continually rising in Earth’s Layers Saturn’s atmosphere, while icy particles are continually falling back down to the lower depths, where they warm up, turn to gas and rise again.
    [Show full text]
  • The Sun's Dynamic Atmosphere
    Lecture 16 The Sun’s Dynamic Atmosphere Jiong Qiu, MSU Physics Department Guiding Questions 1. What is the temperature and density structure of the Sun’s atmosphere? Does the atmosphere cool off farther away from the Sun’s center? 2. What intrinsic properties of the Sun are reflected in the photospheric observations of limb darkening and granulation? 3. What are major observational signatures in the dynamic chromosphere? 4. What might cause the heating of the upper atmosphere? Can Sound waves heat the upper atmosphere of the Sun? 5. Where does the solar wind come from? 15.1 Introduction The Sun’s atmosphere is composed of three major layers, the photosphere, chromosphere, and corona. The different layers have different temperatures, densities, and distinctive features, and are observed at different wavelengths. Structure of the Sun 15.2 Photosphere The photosphere is the thin (~500 km) bottom layer in the Sun’s atmosphere, where the atmosphere is optically thin, so that photons make their way out and travel unimpeded. Ex.1: the mean free path of photons in the photosphere and the radiative zone. The photosphere is seen in visible light continuum (so- called white light). Observable features on the photosphere include: • Limb darkening: from the disk center to the limb, the brightness fades. • Sun spots: dark areas of magnetic field concentration in low-mid latitudes. • Granulation: convection cells appearing as light patches divided by dark boundaries. Q: does the full moon exhibit limb darkening? Limb Darkening: limb darkening phenomenon indicates that temperature decreases with altitude in the photosphere. Modeling the limb darkening profile tells us the structure of the stellar atmosphere.
    [Show full text]
  • Our Atmosphere Greece Sicily Athens
    National Aeronautics and Space Administration Sardinia Italy Turkey Our Atmosphere Greece Sicily Athens he atmosphere is a life-giving blanket of air that surrounds our Crete T Tunisia Earth; it is composed of gases that protect us from the Sun’s intense ultraviolet Gulf of Gables radiation, allowing life to flourish. Greenhouse gases like carbon dioxide, Mediterranean Sea ozone, and methane are steadily increasing from year to year. These gases trap infrared radiation (heat) emitted from Earth’s surface and atmosphere, Gulf of causing the atmosphere to warm. Conversely, clouds as well as many tiny Sidra suspended liquid or solid particles in the air such as dust, smoke, and Egypt Libya pollution—called aerosols—reflect the Sun’s radiative energy, which leads N to cooling. This delicate balance of incoming and reflected solar radiation 200 km and emitted infrared energy is critical in maintaining the Earth’s climate Turkey Greece and sustaining life. Research using computer models and satellite data from NASA’s Earth Sicily Observing System enhances our understanding of the physical processes Athens affecting trends in temperature, humidity, clouds, and aerosols and helps us assess the impact of a changing atmosphere on the global climate. Crete Tunisia Gulf of Gables Mediterranean Sea September 17, 1979 Gulf of Sidra October 6, 1986 September 20, 1993 Egypt Libya September 10, 2000 Aerosol Index low high September 24, 2006 On August 26, 2007, wildfires in southern Greece stretched along the southwest coast of the Peloponnese producing Total Ozone (Dobson Units) plumes of smoke that drifted across the Mediterranean Sea as far as Libya along Africa’s north coast.
    [Show full text]
  • The Atmosphere!
    Activity 1 What’s Up? The Atmosphere! Atmosphere CHANGE IS IN THE AIR Forces of Change » Atmosphere » Activity 1 » Page 1 ACTIVITY 1 What’s Up? The Atmosphere! In one of 80 experiments performed on the space shuttle Columbia before its tragic loss during reentry in 2003, Israeli astronaut Ilan Ramon tracked desert dust in the atmosphere as it moved around the earth Photo © Ernest Hilsenrath. Overview Students learn the distinctions of each layer of the atmosphere and sketch the layers. Suggested Grade Level 6–8 National Standards National Science Education Standards Alignment Earth and Science Standard, Content Standard D: Grades 5–8 Structure of the Earth System: The atmosphere is a mixture of nitrogen, oxygen, and trace gases that include water vapor. The atmosphere has different properties at different elevations. Time One class period (40–50 minutes) Materials 1 Graph paper 1 Activity sheet Forces of Change » Atmosphere » Activity 1 » Page 2 ACTIVITY 1 OBJECTIVES Students will be able to: e Describe the main layers of Earth’s atmosphere, the proportion of each in the atmosphere, and what role each plays in atmospheric phenomena. r Define how the temperature varies from layer to layer of atmosphere. t Calculate the quantities of gases in a particular volume of air, such as their classroom. Background What we call the atmosphere comes in five main layers: exosphere, thermosphere, mesosphere, stratosphere, and troposphere. In the exosphere (640 to 64,000 km, or 400 to 40,000 mi), air dwin- dles to nothing as molecules drift into space. The thermosphere (80 to 640 km or 50 to 400 mi) is very hot despite being very thin because it The Aura Earth-observing satellite absorbs so much solar radiation.
    [Show full text]
  • Jupiter and Saturn
    Jupiter and Saturn 1 2 3 Guiding Questions 1. Why is the best month to see Jupiter different from one year to the next? 2. Why are there important differences between the atmospheres of Jupiter and Saturn? 3. What is going on in Jupiter’s Great Red Spot? 4. What is the nature of the multicolored clouds of Jupiter and Saturn? 5. What does the chemical composition of Jupiter’s atmosphere imply about the planet’s origin? 6. How do astronomers know about the deep interiors of Jupiter and Saturn? 7. How do Jupiter and Saturn generate their intense magnetic fields? 8. Why would it be dangerous for humans to visit certain parts of the space around Jupiter? 9. How was it discovered that Saturn has rings? 10.Are Saturn’s rings actually solid bands that encircle the planet? 11. How uniform and smooth are Saturn’s rings? 4 12.How do Saturn’s satellites affect the character of its rings? Jupiter and Saturn are the most massive planets in the solar system • Jupiter and Saturn are both much larger than Earth • Each is composed of 71% hydrogen, 24% helium, and 5% all other elements by mass • Both planets have a higher percentage of heavy elements than does the Sun • Jupiter and Saturn both rotate so rapidly that the planets are noticeably flattened 5 Unlike the terrestrial planets, Jupiter and Saturn exhibit differential rotation 6 Atmospheres • The visible “surfaces” of Jupiter and Saturn are actually the tops of their clouds • The rapid rotation of the planets twists the clouds into dark belts and light zones that run parallel to the equator • The
    [Show full text]
  • Nitrogen Dioxide Pollution As a Signature of Extraterrestrial Technology
    Draft version February 10, 2021 Typeset using LATEX default style in AASTeX63 Nitrogen Dioxide Pollution as a Signature of Extraterrestrial Technology Ravi Kopparapu ,1 Giada Arney,1 Jacob Haqq-Misra ,2 Jacob Lustig-Yaeger ,3 and Geronimo Villanueva 1 1NASA Goddard Space Flight Center 8800 Greenbelt Road Greenbelt, MD 20771, USA 2Blue Marble Space Institute of Science, Seattle, WA, USA 3Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA Submitted to ApJ ABSTRACT Nitrogen dioxide (NO2) on Earth today has biogenic and anthropogenic sources. During the COVID- 19 pandemic, observations of global NO2 emissions have shown significant decrease in urban areas. Drawing upon this example of NO2 as an industrial byproduct, we use a one-dimensional photo- chemical model and synthetic spectral generator to assess the detectability of NO2 as an atmospheric technosignature on exoplanets. We consider cases of an Earth-like planet around Sun-like, K-dwarf and M-dwarf stars. We find that NO2 concentrations increase on planets around cooler stars due to less short-wavelength photons that can photolyze NO2. In cloud-free results, present Earth-level NO2 on an Earth-like planet around a Sun-like star at 10pc can be detected with SNR ∼ 5 within ∼ 400 hours with a 15 meter LUVOIR-like telescope when observed in the 0:2 − 0:7µm range where NO2 has a strong absorption. However, clouds and aerosols can reduce the detectability and could mimic the NO2 feature. Historically, global NO2 levels were 3x higher, indicating the capability of detecting a 40-year old Earth-level civilization. Transit and direct imaging observations to detect infrared spectral signatures of NO2 on habitable planets around M-dwarfs would need several 100s of hours of obser- vation time, both due to weaker NO2 absorption in this region, and also because of masking features by dominant H2O and CO2 bands in the infrared part of the spectrum.
    [Show full text]
  • Morphology and Dynamics of the Venus Atmosphere at the Cloud Top Level As Observed by the Venus Monitoring Camera
    Morphology and dynamics of the Venus atmosphere at the cloud top level as observed by the Venus Monitoring Camera Von der Fakultät für Elektrotechnik, Informationstechnik, Physik der Technischen Universität Carolo-Wilhelmina zu Braunschweig zur Erlangung des Grades eines Doktors der Naturwissenschaften (Dr.rer.nat.) genehmigte Dissertation von Richard Moissl aus Grünstadt Bibliografische Information Der Deutschen Bibliothek Die Deutsche Bibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.ddb.de abrufbar. 1. Referentin oder Referent: Prof. Dr. Jürgen Blum 2. Referentin oder Referent: Dr. Horst-Uwe Keller eingereicht am: 24. April 2008 mündliche Prüfung (Disputation) am: 9. Juli 2008 ISBN 978-3-936586-86-2 Copernicus Publications, Katlenburg-Lindau Druck: Schaltungsdienst Lange, Berlin Printed in Germany Contents Summary 7 1 Introduction 9 1.1 Historical observations of Venus . .9 1.2 The atmosphere and climate of Venus . .9 1.2.1 Basic composition and structure of the Venus atmosphere . .9 1.2.2 The clouds of Venus . 11 1.2.3 Atmospheric dynamics at the cloud level . 12 1.3 Venus Express . 16 1.4 Goals and structure of the thesis . 19 2 The Venus Monitoring Camera experiment 21 2.1 Scientific objectives of the VMC in the context of this thesis . 21 2.1.1 UV Channel . 21 2.1.1.1 Morphology of the unknown UV absorber . 21 2.1.1.2 Atmospheric dynamics of the cloud tops . 21 2.1.2 The two IR channels . 22 2.1.2.1 Water vapor abundance and cloud opacity . 22 2.1.2.2 Surface and lower atmosphere .
    [Show full text]
  • Titan Fact Sheet Titan Is a Large Moon Orbiting the Planet Saturn, About
    Titan Fact Sheet Titan is a large moon orbiting the planet Saturn, about 866 million miles from the sun. The surface of Titan is hidden by the thick, hazy atmosphere, but in the past few years spacecraft have managed to collect images and other data that tell us about what lies beneath the haze. They found something that’s common on Earth but very unusual in the rest of the solar system: lakes and seas! Besides Earth, Titan is the only body in our solar system with enough liquid on its surface to fill lakes and seas. Titan’s lakes and seas are filled mainly with thick tar-like substances, such as methane and ethane. Titan also has methane gas in its atmosphere, just as Earth has water vapor in its atmosphere. Titan has summer and winter seasons when its surface becomes warmer and colder. However, because it is so far from the sun, even in summer Titan is very cold. Its average surface temperature is about -179 degrees Celsius or -290 degrees Fahrenheit. Titan Fact Sheet Titan is a large moon orbiting the planet Saturn, about 866 million miles from the sun. The surface of Titan is hidden by the thick, hazy atmosphere, but in the past few years spacecraft have managed to collect images and other data that tell us about what lies beneath the haze. They found something that’s common on Earth but very unusual in the rest of the solar system: lakes and seas! Besides Earth, Titan is the only body in our solar system with enough liquid on its surface to fill lakes and seas.
    [Show full text]
  • Extraterrestrial Life: Lecture #7 Next Homework
    Extraterrestrial Life: Lecture #7 Is the climate stable over geological time? Next homework: Thursday Feedback: if the surface temperature rises, does the concentration of greenhouse gases in the atmosphere: To first approximation: distance from star and luminosity of star determine the surface temperature and possibility • increase, possibly raising the temperature further? for liquid water on surface Positive feedback • decrease, offsetting the rise? Atmosphere (`greenhouse effect’) also plays an important Negative feedback role - warms Earth by ~20 degrees Celsius • water vapor Empirically, expect negative feedback to prevail on the increased concentration • carbon dioxide Earth - but may be different for other planets… warms the planet • methane Particulate matter (dust from volcanoes) cools Extraterrestrial Life: Spring 2008 Extraterrestrial Life: Spring 2008 Short term feedback processes Extent of ice cover also affects the climate via changes Short term feedbacks are mostly positive - destabilizing to the mean albedo e.g. water vapor: increased temperature leads to more If increased temperature leads evaporation from the oceans, increasing the atmospheric to less snow and ice, fraction concentration of water vapor of Solar energy that will be absorbed increases Water is a greenhouse gas, so this is positive feedback Positive feedback Role of clouds? Timescale: 1000s of years Timescale: essentially instantaneous Extraterrestrial Life: Spring 2008 Extraterrestrial Life: Spring 2008 Long term feedback processes Volcanic activity can
    [Show full text]
  • The Origin of Titan's Atmosphere: Some Recent Advances
    The origin of Titan’s atmosphere: some recent advances By Tobias Owen1 & H. B. Niemann2 1University of Hawaii, Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA 2Laboratory for Atmospheres, Goddard Space Fight Center, Greenbelt, MD 20771, USA It is possible to make a consistent story for the origin of Titan’s atmosphere starting with the birth of Titan in the Saturn subnebula. If we use comet nuclei as a model, Titan’s nitrogen and methane could easily have been delivered by the ice that makes up ∼50% of its mass. If Titan’s atmospheric hydrogen is derived from that ice, it is possible that Titan and comet nuclei are in fact made of the same protosolar ice. The noble gas abundances are consistent with relative abundances found in the atmospheres of Mars and Earth, the sun, and the meteorites. Keywords: Origin, atmosphere, composition, noble gases, deuterium 1. Introduction In this note, we will assume that Titan originated in Saturn’s subnebula as a result of the accretion of icy planetesimals: particles and larger lumps made of ice and rock. Alibert & Mousis (2007) reached this same point of view using an evolutionary, turbulent model of Saturn’s subnebula. They found that planetesimals made in the solar nebula according to their model led to a huge overabundance of CO on Titan. We obviously have no direct measurements of the composition of these planetes- imals. We can use comets as a guide, always remembering that comets formed in the solar nebula where conditions must have been different from those in Saturn’s subnebula, e.g., much colder.
    [Show full text]
  • Earth's Changing Atmosphere
    Earth’s Changing Atmosphere What will make this kite soar? Earth’s atmosphere is a blanket of gases that supports and protects life. Key Concepts SECTION Earth’s atmosphere 1 supports life. Learn about the materials that make up the atmosphere. SECTION The Sun supplies the 2 atmosphere’s energy. Learn how energy from the Sun affects the atmosphere. SECTION Gases in the atmosphere 3 absorb radiation. Learn about the ozone layer and the greenhouse effect. SECTION Human activities affect 4 the atmosphere. Learn about pollution, global warming, and changes in the ozone layer. Prepare and practice for the FCAT • Section Reviews, pp. 616, 623, 627, 635 • Chapter Review, pp. 638–640 • FCAT Practice, p. 641 CLASSZONE.COM • Florida Review: Content Review and FCAT Practice 608 Unit 5: Earth’s Atmosphere How Heavy Is Paper? Put a ruler on a table with one end off the edge. Tap on the ruler lightly and observe what happens. Then cover the ruler with a sheet of paper as shown. Tap again on the ruler and observe what happens. Observe and Think What happened to the ruler when you tapped lightly on it with and without the sheet of paper? Was the paper heavy enough by itself to hold the ruler down? How Does Heating Affect Air? Stretch the lip of a balloon over the neck of a small bottle. Next, fill a bowl with ice water and a second bowl with hot tap water. Place the bottle upright in the hot water. After 5 minutes, move the bottle to the cold water.
    [Show full text]
  • The Origin and Evolution of Titan's Atmosphere
    The origin and evolution! of Titan’s atmosphere Athena Coustenis Department of Space Research and Instrumentation in Astrophysics (LESIA) Paris-Meudon Observatory France [email protected] Saturn’s satellites Titan Through Time • Christianus Huygens discovers Titan, 1655 • Ground-based : " ! atmospheric limb darkening (Comas Solas, 1908) " ! CH4 detected (Kuiper, 1944) •! Voyager (1980) " ! mean distance from Saturn = 1,211,850 km (~ 3.1 x Earth-Moon distance) " ! orbital period= 15.94 days (Earth’s moon 27.3 days) " ! N2 detected as main component, CH4 second most abundant (Voyager, 1980) " ! mass = 1.35x 1023 kg (0.023 x Earth’s) " ! radius = 2575 km (0.98 Ganymede; 1.48 x Moon; 0.76 x Mars) " ! mean density = 1.88 g/cm3 (50% ice, 50% rock) " ! mean surface temperature = 93.5 K (-179.5 °C, -291 °F) " ! atmospheric pressure = 1.5 bars " ! atmospheric density = 4.4 x Earth’s atmosphere •! Ground-based and Earth-bound observatories (HST, ISO) – 1990s " ! Heterogeneous surface " ! Interesting atmospheric phenomena •! Cassini arrives at Saturn on 30 June 2004 •! Huygens lands on Titan 14 January 2005 " ! Ouaouh! Characteristic Ganymede Titan Enceladus Triton Pluto Rplanet 14.99 RJ 20.25 RS 3.95 RS 14.33 RN [39.53 AU] M [1022 kg] 14.82 13.5 0.011 2.14 1.31 Re [km] 2631 2575 252 1352 1150 ρ [kg/m3] 1936 1880 1608 2064 2030 g [m/s2] 1.43 1.35 0.12 0.78 0.4 TO [days] -- -- -- -- [248.5 yr] TS [days] 7.16 15.95 1.37 5.877 [6.38] i [deg] 0.18 0.33 0.02 157 17.14 0.005 e 0.001 0.029 0.000 0.25 A 0.4 0.2 1.4 0.4 0.52 ve [km/s] 2.75 2.64 0.235 ( < vT ! ) 1.50 1.1 Surface T [K] 110 94 114-157 38 40 P X 1.5 bar 16 µb 58 µb (var) H2O, N2 , CH4, Atmosphere O3, (H2O2-i) N2, CH4 N2, CH4 N2, CH4, (H2O-i) CO2, CO TITAN: WHY ARE WE INTERESTED? •!It is of general interest to the study of chemical evolution: –!N2, CH4 and other abundant organic gases (nitriles and hydrocarbons) are present in the atmosphere –!An orange-brown cloud deck globally covers the satellite, in which aerosol layers and, methane/ethane clouds are also present.
    [Show full text]