Engineering Models for Titan's Atmosphere
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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. -
Titan and the Moons of Saturn Telesto Titan
The Icy Moons and the Extended Habitable Zone Europa Interior Models Other Types of Habitable Zones Water requires heat and pressure to remain stable as a liquid Extended Habitable Zones • You do not need sunlight. • You do need liquid water • You do need an energy source. Saturn and its Satellites • Saturn is nearly twice as far from the Sun as Jupiter • Saturn gets ~30% of Jupiter’s sunlight: It is commensurately colder Prometheus • Saturn has 82 known satellites (plus the rings) • 7 major • 27 regular • 4 Trojan • 55 irregular • Others in rings Titan • Titan is nearly as large as Ganymede Titan and the Moons of Saturn Telesto Titan Prometheus Dione Titan Janus Pandora Enceladus Mimas Rhea Pan • . • . Titan The second-largest moon in the Solar System The only moon with a substantial atmosphere 90% N2 + CH4, Ar, C2H6, C3H8, C2H2, HCN, CO2 Equilibrium Temperatures 2 1/4 Recall that TEQ ~ (L*/d ) Planet Distance (au) TEQ (K) Mercury 0.38 400 Venus 0.72 291 Earth 1.00 247 Mars 1.52 200 Jupiter 5.20 108 Saturn 9.53 80 Uranus 19.2 56 Neptune 30.1 45 The Atmosphere of Titan Pressure: 1.5 bars Temperature: 95 K Condensation sequence: • Jovian Moons: H2O ice • Saturnian Moons: NH3, CH4 2NH3 + sunlight è N2 + 3H2 CH4 + sunlight è CH, CH2 Implications of Methane Free CH4 requires replenishment • Liquid methane on the surface? Hazy atmosphere/clouds may suggest methane/ ethane precipitation. The freezing points of CH4 and C2H6 are 91 and 92K, respectively. (Titan has a mean temperature of 95K) (Liquid natural gas anyone?) This atmosphere may resemble the primordial terrestrial atmosphere. -
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. -
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. -
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. -
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 -
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. -
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 . -
The Lakes and Seas of Titan • Explore Related Articles • Search Keywords Alexander G
EA44CH04-Hayes ARI 17 May 2016 14:59 ANNUAL REVIEWS Further Click here to view this article's online features: • Download figures as PPT slides • Navigate linked references • Download citations The Lakes and Seas of Titan • Explore related articles • Search keywords Alexander G. Hayes Department of Astronomy and Cornell Center for Astrophysics and Planetary Science, Cornell University, Ithaca, New York 14853; email: [email protected] Annu. Rev. Earth Planet. Sci. 2016. 44:57–83 Keywords First published online as a Review in Advance on Cassini, Saturn, icy satellites, hydrology, hydrocarbons, climate April 27, 2016 The Annual Review of Earth and Planetary Sciences is Abstract online at earth.annualreviews.org Analogous to Earth’s water cycle, Titan’s methane-based hydrologic cycle This article’s doi: supports standing bodies of liquid and drives processes that result in common 10.1146/annurev-earth-060115-012247 Annu. Rev. Earth Planet. Sci. 2016.44:57-83. Downloaded from annualreviews.org morphologic features including dunes, channels, lakes, and seas. Like lakes Access provided by University of Chicago Libraries on 03/07/17. For personal use only. Copyright c 2016 by Annual Reviews. on Earth and early Mars, Titan’s lakes and seas preserve a record of its All rights reserved climate and surface evolution. Unlike on Earth, the volume of liquid exposed on Titan’s surface is only a small fraction of the atmospheric reservoir. The volume and bulk composition of the seas can constrain the age and nature of atmospheric methane, as well as its interaction with surface reservoirs. Similarly, the morphology of lacustrine basins chronicles the history of the polar landscape over multiple temporal and spatial scales. -
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. -
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 -
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.