Hydrocarbon Lakes on Titan and Their Role in the Methane Cycle Thesis by Alexander G. Hayes In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy California Institute of Technology Pasadena, California 2011 (Defended April 4th, 2011) ii © 2011 Alexander G. Hayes All Rights Reserved iii I dedicate this thesis to the next generation of professional armchair explorers. iv Acknowledgements Over the course of the past decade it has been my unbelievably good fortune to have been welcomed into the science teams of two planetary spacecraft missions and have acess to three more. As an explorer at heart, I have savored every moment of this time and recognize that is was only possible due to the generosity and intellectual guidance of a great number of people along the way. First, I would like to thank Steve Squyres and Jim Bell of Cornell University. Steve introduced me to the field of planetary science and, despite my arrogance naivety, offered me a job on his science team that ultimately made me realize my passion for planetary exploration. Jim handed over the keys to the camera instruments on the Mars Exploration Rovers (MER) and let me run wild. Similar gratitude goes out to the remainder of the MER science team, most notably Ken Herkenhoff and Phil Christensen, who provided me with access to their instruments as well. The camaraderie I experienced within the MER science team during my time at Cornell and JPL motivated my decision to pursue a career in planetary science. Upon entering the doctoral program at Caltech, I found both an intellectual mentor and friend in my advisor Oded Aharonson. Oded challenged me from day one, and I am ever grateful for his guidance and leadership. Perhaps I am most indebted to Oded for v his treatment of me as colleague, not a student, forcing me to develop the skills needed as a professional scientist. Over the course of my doctoral career, Oded ensured that every conceivable resource was at my feet before I even realized I needed it. Furthermore, Oded’s intellectual criticism help me develop the invaluable ability to strip problems down to their fundamental questions. I can only hope that he has enjoyed and benefited from our frequent intellectual debates as much as I have. I also wish to thank the remainder of my thesis committee at Caltech. Most notably, my fellowship advisor Charles Elachi. Charles provided unrestricted access to the Cassini RADAR instrument and ensured that every door I came across was not only unlocked, but held open so I could venture in and out at my leisure. John Grotzinger, my co-advisor, was an intellectual force who introduced me to the world of geology and sedimentology. George Rossman provided countless hours of intellectual discussion that transcended the field of mineral spectroscopy and reached life in general. I am honored to consider him a friend. David Stevenson excited an academic rigor in my work for which I will always be grateful. Finally, Andy Ingersoll was ever patient and vigilant in his quest to teach me the importance of simplicity. I must also thank the GPS staff, most notably Nora Oshima and Scott Dungan, for their assistance with a myriad of technical and administrative difficulties. The camaraderie and fellowship that I experience among the MER science team can only be matched by that which I felt as part of the Cassini RADAR Science Team (CRST). The members of the CRST welcomed me with open arms and provided significant support for all of the work presented in this thesis. Specifically, I would like to thank my collab- orators Steve Wall, Jonathan Lunine, Randy Kirk, Ralph Lorenz, Elizabeth Turtle, Rosaly vi Lopes, Michael Janssen, Larry Soderblom, Howard Zebker, Jason Barnes, Phil Callahan, Alice Le Gall, Lauren Wye, Karl Mitchell, and Philippe Paillou. Your contributions are directly reflected in the both the quality and style of my work. My gratitude for your sup- port is surpassed only by my regret at not having the space to adequately thank you in this document. I look forward to our future collaborations. Despite the significant support I have enjoyed from both my advisors and collaborators, my professional development would have be woefully inadequate were it not for daily interactions with fellow graduate students and friends. Kevin Lewis, Alejandro Soto, Aaron Wolf, and Margarita Maranova have acted as both technical advisors and psychological counselors. I only hope that I have helped you as much as you have helped me. I must also thank my friend, confidant, and gym partner Troy Hudson and his successor Konstantin Batygin. Jason Soderblom and Jascha Sohl-Dickstein have been with me since Cornell and I am ever-grateful for their support. I also thank Wes Watters, Antoine Lucas, Ajay Limaye, Meg Rosenburg, Megan Schwamb, and Lauren Edgar for intellectually stimulating collaborations. If we continue working together as we have, I am confident that we will take the field of planetary science by storm. Most importantly, I must thank my family for their unyielding support. My parents, Al and Mariann, have nurtured my academic pursuits since birth and always pushed me to accomplish more than I thought possible. My uncle, Joseph, acted like a second father and can be credited with invigorating my intellectual curiosity. Finally, my wife Lindsey has been my partner in all things, and I can think of no one better with whom to share both the joys of success and lessons of failure. She has been ever vii patient with me during this process and vigilant in her quest to remind me of the things that matter most; The best of example of this being our daughter, Noelle Marie. In closing, I reiterate my thanks to everyone who has supported me during this journey. I hope to emulate your support and encouragement to others during the course of my career. In this respect, I remember Steve Squyres’ response whenever I thanked him for a particular research opportunity: “Don’t thank me, just make sure you do it for someone else when you find yourself in my position.” viii Abstract Saturn’s moon Titan is the only extraterrestrial body currently known to support standing bodies of liquid on its surface and, along with Earth and Mars, is one of only three places that we know to posses or have possessed an active hydrologic cycle. Understanding the nature of Titan’s hydrologic system will teach us about the history of volatile compounds across the solar system and help define Earth’s place within it. Titan’s hydrologic cycle represents a simpler version of Earth’s water cycle, lacking an ocean as a global sink of liquid and heat, and acts as a model for the evolution of planets around other stars, as its methane-based system may be more common than Earth’s water-based system. This thesis combines several studies related to Titan’s hydrologic system, particularly focusing on the role of lacustrine deposits. Following an introduction that discusses Titan’s place in the solar system and the importance of studying its methane cycle, chapter two describes the lakes’ geographic distribution and models interaction with a porous regolith. The chapter also discusses the implications of a hemispheric asymmetry in lake distribu- tion, which has been attributed to an asymmetry in the intensity of Titan’s seasons. The evolution of the orbital parameters that generate this asymmetry provide a mechanism for transferring not only methane, but also less volatile species such as ethane, from pole to pole over tens of thousands of years. ix Chapter three discusses lake properties through an examination of Ontario Lacus, the largest lake in Titan’s southern pole. The complex dielectric properties of Ontario’s near- shore region are derived through a combined analysis of radar altimetry and backscatter. The analysis is performed within multiple regions around Ontario’s shore, producing a near-shore bathymetry map. The results of this study are then used to measure seasonal variation in chapter four. Shoreline recession at Ontario Lacus and smaller lakes which disappeared between repeat observations suggest an average meter-per-year loss rate be- tween southern summer solstice and autumnal equinox. These observations demonstrate that Titan’s surface plays an active role in its methane cycle and can be used to describe the evolution of its hydrologic system. x Contents Acknowledgements iv Abstract viii List of Figures xi List of Tables xiii List of Acronyms xv 1 Introduction: Exploring Lakes on Titan 2 2 Lake Distribution 10 2.1 Introduction . 11 2.2 Lake Distribution . 11 2.2.1 Mapping Unit Distribution . 13 2.2.2 Morphology . 18 2.2.3 Implications for Change on Orbital Timescales . 18 2.3 Shoreline Complexity . 21 2.4 Preliminary Topography . 25 2.5 Flow Through Porous Media . 27 2.6 Summary . 33 3 Lake Properties: Ontario Lacus Bathymetry and Absorptivity 35 3.1 Introduction . 36 xi 3.2 Data Reduction . 38 3.3 Model . 43 3.4 Model Validation . 50 3.5 Discussion . 62 3.6 Summary . 65 4 Seasonal Variation 67 4.1 Introduction . 68 4.2 Radar Backscatter of Lacustrine Features on Titan . 71 4.3 Observations of Change . 80 4.3.1 South Polar Region . 80 4.3.2 North Polar Region . 104 4.4 Discussion . 110 4.5 Summary . 115 5 Upcoming Observations 118 A Software for Cassini RADAR Data Manipulation 131 Bibliography 133 xii List of Figures 1.1 Images of Titan obtained by the Voyager and Cassini spacecraft . 4 1.2 Distribution of lakes on Titan poleward of 60◦. ................ 5 1.3 Comparison between radar images of lakes on Earth and Titan .