ABSTRACT

1. Titan’s Greenhouse Effect and Climate:Lessons from the Earth’s Cooler CousinA White Paper Submission to the NRC Planetary Science Decadal SurveyConor A. Nixon1,*, Athena Coustenis2, Jonathan I. Lunine3, Ralph Lorenz4, Carrie M. Anderson5, F. Michael Flasar5, Christophe Sotin6, J. Hunter Waite Jr.7, V. Malathy Devi8, Olivier Mousis9, Kim R. Reh6, Konstantinos Kalogerakis10, A. James Friedson6, Henry Roe11, Yuk L. Yung12, Valeria Cottini1, Giorgos Bampasides13, Richard K. Achterberg1, Nicholas A. Teanby14, Gordon L. Bjoraker5, Eric H. Wilson6, Tilak Hewagama1, Mark A. Gurwell15, Roger Yelle3, Mark A. Allen6, Nathan J. Strange6, Linda J. Spilker6, Glenn Orton6, Candice J. Hansen6, Jason W. Barnes16, Jason M. Soderblom3, Vladimir B. Zivkovic17, Anezina Solomonidou13, David L. Huestis10, Mark A. Smith3, David H. Atkinson18, Patrick G. J. Irwin14, Mathieu Hirtzig2, Simon B. Calcutt14, Timothy A. Livengood5, Sandrine Vinatier5, Theodore Kostiuk5, Antoine Jolly19, Nasser Moazzen-Ahmadi20, Darrell F. Strobel21, Mao-Chang Liang22, Patricia M. Beauchamp6, Remco de Kok23, Robert Pappalardo6, Imke de Pater24, Véronique Vuitton25, Paul N. Romani5, Robert A. West6, Lucy H. Norman26, Mary Ann H. Smith27, Kathleen Mandt7, Sebastien Rodriguez28, Máté Ádámkovics24, Jean-Marie Flaud29, Kurt K. Klaus30, Michael Wong31, Jean-Pierre Lebreton32, Neil Bowles14, Marina Galand33, Linda R. Brown6, F. Javier Martin-Torres12 .1Univ. Maryland, *conor.a.nixon@nasa.gov, 2Obs. Paris, 3Univ. Arizona, 4APL, 5NASA GSFC, 6Caltech/JPL, 7SWRI, 8Coll. Wm. and Mary, 9Obs. Besançon, 10SRI, 11Lowell Obs., 12Cal. Inst. Tech, 13Univ. Athens, 14Univ. Oxford, 15Harvard-Smithsonian, 16Univ. Idaho (Physics), 17Univ. N. Dakota, 18Univ Idaho (E.Eng.), 19LISA Univ. Paris, 20Univ. Calgary, 21JHU, 22Academica Sinica, 23SRON, 24UC Berkeley, 25Lab. Plan. Grenoble, 26UCL, 27NASA LRC, 28CEA/Univ. Paris, 29CNRS/Univ. Paris, 30Boeing, 31STScI, 32ESA/ESTEC, 33Imperial Coll. 4. THE FATE OF THE ATMOSPHERE ABSTRACT • Titan’s upper atmosphere functions as a vast chemical factory, turning the raw materials (N2, CH4, H2O) into more complex molecules and haze. • These condense and fall from the atmosphere, the net effect is an irreversible depletion of methane. • This poster is a response to a ‘call for white papers’ by the Decadal Survey for Planetary Science conducted by theSpace Studies Board of the US National Academiesto inform prioritization of future funding for research, including missions. • In this poster we show that Titan is an atmospheric ‘greenhouse world’, like the Earth, Mars and Venus. • Study of Earth’s planetary ‘cousins’, including Titan, has great potential to inform us about the nature of the greenhouse effect and long-term climate changeon our world. • See the final box for our on how best to address this important topic. • The CH4 inventory will last just ~107Myr, unless resupplied. • Possible mechanisms include volcanism or outgassingfrom the interior, or comets. • If all the CH4 is periodically removed, then the atmosphere may collapse and freeze out on the surface. Graphic: NASA TSSM Final Report/J. Lunine. 1. GREENHOUSE EFFECT: HOW DOES IT WORK? 2. ANTI-GREENHOUSE EFFECT • OUR RECOMMENDATIONS: • We recommend that the following steps be taken by the NRC Decadal Survey for Planetary Science, to continue critical research into the subject of Titan’s climatology: • Endorse: the strong positive findings of the recent Senior Review of the Cassini Solstice Mission, to continue the mission until 2017. • Urgethat a successor Titan-focused mission be given very high priority for near-term development and launch. • Recommendcontinued funding for strong ground-based, airborne and space-based observing campaigns for continuous, long-term Titan monitoring. • Supportcontinued funding for applicable NASA R&A programs and the NSF Planetary Astronomy Program; and for associated laboratory experiments, modeling and theoretical calculations. • Proposethat a dedicated NASA outer planetary flagship mission program be initiated, analogous to the Mars and lunar programs, to encompass the continued operations of Cassini, and follow-on flagship missions. 3. SEASONAL CHANGE: SMILE OR FROWN? • Key molecules in Titan’s atmosphere are more transparent to visible light than to infrared radiation. • When sunlight reaches Titan’s surface, some re-radiated thermal energy is trapped, warming the lower atmosphere and surface. • A feedback loop also exists, whereby small increases in H2, which is not limited by saturation, causes more CH4 to be retained in the atmosphere, increasing and amplifying the warming. • The greenhouse effect is counter-acted by an anti-greenhouse effect that cools the atmosphere. • This is mainly due to stratospheric haze particles that are transparent to infrared but absorb visible light. • The net effect of the positive (+23 K) and negative (-11 K) greenhouse effects is +12 K, raising the surface temperature from 84 K to 94 K. • Compare to the Earth (+30 K), Venus (+500 K) and Mars (+5 K). • Titan experiences a ~30 yr seasonal cycle due its orbital inclination. • Imaging in 1992 showed a ‘smile’: a bright up-turned arc in the southern hemisphere at red wavelengths. Blue images showed the opposite: a bright northern hemisphere. • In 2002 the trend was reversed, with a ‘frowning’ bright (red) north. • We now know that this effect is due to the seasonal ‘migration’ of haze from south to north and back, caused by a summer-pole-to-winter-pole circulation in the stratosphere. At least 12 haze layers are seen on this Cassini ISS image at 10°S. (NASA/JPL/SSI) Titan Atmosphere Schematic. Credit: ESA Image: R. Lorenz/STScI For more information, including electronic downloads of this poster and the full white paper, please visit: http://www.astro.umd.edu/~nixon/titanclimate.html