MARIA T. ZUBER Research Interests
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Index Abulfeda crater chain (Moon), 97 Aphrodite Terra (Venus), 142, 143, 144, 145, 146 Acheron Fossae (Mars), 165 Apohele asteroids, 353–354 Achilles asteroids, 351 Apollinaris Patera (Mars), 168 achondrite meteorites, 360 Apollo asteroids, 346, 353, 354, 361, 371 Acidalia Planitia (Mars), 164 Apollo program, 86, 96, 97, 101, 102, 108–109, 110, 361 Adams, John Couch, 298 Apollo 8, 96 Adonis, 371 Apollo 11, 94, 110 Adrastea, 238, 241 Apollo 12, 96, 110 Aegaeon, 263 Apollo 14, 93, 110 Africa, 63, 73, 143 Apollo 15, 100, 103, 104, 110 Akatsuki spacecraft (see Venus Climate Orbiter) Apollo 16, 59, 96, 102, 103, 110 Akna Montes (Venus), 142 Apollo 17, 95, 99, 100, 102, 103, 110 Alabama, 62 Apollodorus crater (Mercury), 127 Alba Patera (Mars), 167 Apollo Lunar Surface Experiments Package (ALSEP), 110 Aldrin, Edwin (Buzz), 94 Apophis, 354, 355 Alexandria, 69 Appalachian mountains (Earth), 74, 270 Alfvén, Hannes, 35 Aqua, 56 Alfvén waves, 35–36, 43, 49 Arabia Terra (Mars), 177, 191, 200 Algeria, 358 arachnoids (see Venus) ALH 84001, 201, 204–205 Archimedes crater (Moon), 93, 106 Allan Hills, 109, 201 Arctic, 62, 67, 84, 186, 229 Allende meteorite, 359, 360 Arden Corona (Miranda), 291 Allen Telescope Array, 409 Arecibo Observatory, 114, 144, 341, 379, 380, 408, 409 Alpha Regio (Venus), 144, 148, 149 Ares Vallis (Mars), 179, 180, 199 Alphonsus crater (Moon), 99, 102 Argentina, 408 Alps (Moon), 93 Argyre Basin (Mars), 161, 162, 163, 166, 186 Amalthea, 236–237, 238, 239, 241 Ariadaeus Rille (Moon), 100, 102 Amazonis Planitia (Mars), 161 COPYRIGHTED -
Sunnyvale Heritage Resources
CARIBBEAN DR 3RD AV G ST C ST BORDEAUX DR H ST 3RD AV Heritage Trees CARIBBEAN DR CASPIAN CT GENEVA DR ENTERPRISE WY 4TH AV Local Landmarks E ST CASPIAN DR BALTIC WY Heritage Resources 5TH AV JAVA DR 5TH AV MOFFETT PARK DR CROSSMAN AV 300-ft Buffer CHESAPEAKE TR GIBRALTAR CT GIBRALTAR DR ORLEANS DR MOFFETT PARK DR 7TH AV MACON RD ANVILWOOD City Boundary ENTERPRISEWY CT G ST C ST MOFFETT PARK CT 8TH AV HUMBOLDT CT PERSIAN DR FORGEWOODAV SR-237 ANVILWOODAV INNSBRUCK DR ELKO DR 9TH AV E ST FAIR OAKS WY BORREGAS AV D ST P O R P O I S ALDERWOODAV 11TH AV MOFFETT PARK DR E BA Y TR PARIA BIRCHWOODDR MATHILDA AV GLIESSEN JAEGALS RD GLIN SR-237 PLAZA DR PLENTYGLIN LA ROCHELLE TR TASMAN DR ENTERPRISE WY ENTERPRISE MONTEGO VIENNA DR KASSEL INNOVATION WAY BRADFORD DR MOLUCCA MONTEREY LEYTE MORSE AV KIHOLO LEMANS ROSS DR MUNICH LUND TASMAN CT KARLSTAD DR ESSEX AV COLTON AV FULTON AV DUNCAN AV HAMLIN CT SAGINAW FAIR OAKS AV TOYAMA DR SACO LAWRENCEEXPRESSWAY GARNER DR LYON US-101 SALERNO SAN JORGEKOSTANZ TIMOR KIEL CT SIRTE SOLOMON SUEZ LAKEBIRD DR CT DRIFTWOOD DRIFTWOOD CT CHARMWOOD CHARMWOOD CT SKYLAKE VALELAKE CT CT CLYDE AV BREEZEWOOD CT LAKECHIME DR JENNA PECOS WY AHWANEE AV LAKEDALE WY WEDDELL LOTUSLAKE CT GREENLAKE DR HIDDENLAKE DR WEDDELL DR MEADOWLAKE DR ALMANOR AV FAIRWOODAV STONYLAKE SR-237 LAKEFAIR DR CT CT LYRELAKE LYRELAKE HEM BLAZINGWOOD DR REDROCK CT LO CT CK ALTURAS AV SILVERLAKEDR AV CT CANDLEWOOD LAKEHAVEN DR BURNTWOOD CT C B LAKEHAVEN A TR U JADELAKE SAN ALESO AV R N MADRONE AV LAKEKNOLL DR N D T L PALOMAR AV SANTA CHRISTINA W CT -
Analysis of Polarimetric Mini-SAR and Mini-RF Datasets for Surface Characterization and Crater Delineation on Moon †
Proceeding Paper Analysis of Polarimetric Mini-SAR and Mini-RF Datasets for Surface Characterization and Crater Delineation on Moon † Himanshu Kumari and Ashutosh Bhardwaj * Photogrammetry and Remote Sensing Department, Indian Institute of Remote Sensing, Dehradun 248001, India; [email protected] * Correspondence: [email protected]; Tel.: +91-9410319433 † Presented at the 3rd International Electronic Conference on Atmospheric Sciences, 16–30 November 2020; Available online: https://ecas2020.sciforum.net/. Abstract: The hybrid polarimetric architecture of Mini-SAR and Mini-RF onboard Indian Chan- drayaan-1 and LRO missions were the first to acquire shadowed polar images of the Lunar surface. This study aimed to characterize the surface properties of Lunar polar and non-polar regions con- taining Haworth, Nobile, Gioja, an unnamed crater, Arago, and Moltke craters and delineate the crater boundaries using a newly emerged approach. The Terrain Mapping Camera (TMC) data of Chandrayaan-1 was found useful for the detection and extraction of precise boundaries of the cra- ters using the ArcGIS Crater tool. The Stokes child parameters estimated from radar backscatter like the degree of polarization (m), the relative phase (δ), Poincare ellipticity (χ) along with the Circular Polarization Ratio (CPR), and decomposition techniques, were used to study the surface attributes of craters. The Eigenvectors and Eigenvalues used to measure entropy and mean alpha showed distinct types of scattering, thus its comparison with m-δ, m-χ gave a profound conclusion to the lunar surface. The dominance of surface scattering confirmed the roughness of rugged material. The results showed the CPR associated with the presence of water ice as well as a dihedral reflection inside the polar craters. -
ARTICLE in PRESS EPSL-09719; No of Pages 8 Earth and Planetary Science Letters Xxx (2009) Xxx–Xxx
ARTICLE IN PRESS EPSL-09719; No of Pages 8 Earth and Planetary Science Letters xxx (2009) xxx–xxx Contents lists available at ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl 1 Regular articles 2 Could Pantheon Fossae be the result of the Apollodorus crater^-forming impact within 3 the Caloris Basin, Mercury? 4 Andrew M. Freed a,⁎, Sean C. Solomon b, Thomas R. Watters c, Roger J. Phillips d, Maria T. Zuber e 5 a Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47907, USA 6 b Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA 7 c Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC 20560, USA 8 d Planetary Science Directorate, Southwest Research Institute, Boulder, CO 80302, USA 9 e Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA 10 article info abstract OOF 11 12 Article history: 25 The ^~40^-km-diameter Apollodorus impact crater lies near the center of Pantheon Fossae, a complex of 13 Accepted 20 February 2009 radiating linear troughs itself at the approximate center of the 1500-km-diameter Caloris basin on Mercury. 26 14 Available online xxxx Here we use a series of finite element models to explore the idea that the Apollodorus crater-forming impact 27 15 induced the formation of radially oriented graben by altering a pre-existing extensional stress state. Graben 28 16 Editor: T. Spohn in the outer portions of the Caloris basin, which displayPR predominantly circumferential orientations, have 29 191718 been taken as evidence that the basin interior was in a state of horizontal extensional stress as a result of 30 20 Keywords: fi 31 21 Mercury uplift. -
Impact Melt Emplacement on Mercury
Western University Scholarship@Western Electronic Thesis and Dissertation Repository 7-24-2018 2:00 PM Impact Melt Emplacement on Mercury Jeffrey Daniels The University of Western Ontario Supervisor Neish, Catherine D. The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Jeffrey Daniels 2018 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons, Physical Processes Commons, and the The Sun and the Solar System Commons Recommended Citation Daniels, Jeffrey, "Impact Melt Emplacement on Mercury" (2018). Electronic Thesis and Dissertation Repository. 5657. https://ir.lib.uwo.ca/etd/5657 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Abstract Impact cratering is an abrupt, spectacular process that occurs on any world with a solid surface. On Earth, these craters are easily eroded or destroyed through endogenic processes. The Moon and Mercury, however, lack a significant atmosphere, meaning craters on these worlds remain intact longer, geologically. In this thesis, remote-sensing techniques were used to investigate impact melt emplacement about Mercury’s fresh, complex craters. For complex lunar craters, impact melt is preferentially ejected from the lowest rim elevation, implying topographic control. On Venus, impact melt is preferentially ejected downrange from the impact site, implying impactor-direction control. Mercury, despite its heavily-cratered surface, trends more like Venus than like the Moon. -
Ertising in Science in School · Choose Between Advertising in the Quarterly Print Journal Or on Our Website
How many schools Spring 2011 Issue 18 and teachers do you reach – worldwide? In this issue: Biomimetics: clingy as an octopus or slick as a lotus leaf? Also: News from the EIROs: Mars, snakes, robots and DNA Advertising in Science in School · Choose between advertising in the quarterly print journal or on our website. · Website: reach over 30 000 science educators worldwide – every month. · In print: target up to 15 000 European science educators every quarter, including 3000 named subscribers. · Distribute your flyers, brochures, CD-ROMs or other materials either to 3000 named subscribers or to all recipients of the print copies. For more details, see www.scienceinschool.org/advertising Published by EIROforum: I S S N : 1 Initially supported by 8 1 Subscribe (free in Europe): www.scienceinschool.org 8 the European Union: - Highlighting the best in science teaching and research 0 3 5 3 sis_18_RZ_.qxq:Layout 1 15.03.2011 18:08 Uhr Seite B About Science in School Science in School promotes inspiring science teaching by encouraging communication between Editorial teachers, scientists and everyone else involved in European science education. The journal addresses science teaching both across Europe and across disciplines: highlighting the best in teaching and cutting-edge research. It covers not only biology, physics and chemistry, but also earth sciences, engineering and medicine, Happy birthday, focusing on interdisciplinary work. The contents include teaching materials; cutting-edge science; interviews with young scientists and inspiring Science in School! teachers; reviews of books and other resources; and European events for teachers and schools. Science in School is published quarterly, both online his issue of Science in School is rather special: it’s now and in print. -
Technology Today Spring 2013
Spring 2012 TECHNOLOGY® today Southwest Research Institute® San Antonio, Texas Spring 2012 • Volume 33, No. 1 TECHNOLOGY today COVER Director of Communications Craig Witherow Editor Joe Fohn TECHNOLOGY Assistant Editor today Deborah Deffenbaugh D018005-5651 Contributing Editors Tracey Whelan Editorial Assistant Kasey Chenault Design Scott Funk Photography Larry Walther Illustrations Andrew Blanchard, Frank Tapia Circulation Southwest Research Institute San Antonio, Texas Gina Monreal About the cover Full-scale fire tests were performed on upholstered furniture Technology Today (ISSN 1528-431X) is published three times as part of a project to reduce uncertainty in determining the each year and distributed free of charge. The publication cause of fires. discusses some of the more than 1,000 research and develop- ment projects under way at Southwest Research Institute. The materials in Technology Today may be used for educational and informational purposes by the public and the media. Credit to Southwest Research Institute should be given. This authorization does not extend to property rights such as patents. Commercial and promotional use of the contents in Technology Today without the express written consent of Southwest Research Institute is prohibited. The information published in Technology Today does not necessarily reflect the position or policy of Southwest Research Institute or its clients, and no endorsements should be made or inferred. Address correspondence to the editor, Department of Communications, Southwest Research Institute, P.O. Drawer 28510, San Antonio, Texas 78228-0510, or e-mail [email protected]. To be placed on the mailing list or to make address changes, call (210) 522-2257 or fax (210) 522-3547, or visit update.swri.org. -
Geochemistry, Geophysics, Geosystems Becoming an Open Access Journal: FAQ
Geochemistry, Geophysics, Geosystems becoming an open access journal: FAQ Why is Geochemistry, Geophysics, Geosystems becoming an open access journal? AGU remains committed to open science and open data. As a part of our mission, we are focused on making science available to the widest possible audience. Since many researchers around the world have open access requirements by funders, this move to an open access model will make compliance easier. Authors will pay an open access article processing charge (APC) and retain copyright of their article which they can publish under a Creative Commons license (choose from CC-BY or CC-BY-NC-ND). There will be no excess page fees or any other additional fees for publication. In addition, there will be no subscription paywall, which means that more people will have access to your research so they can actively cite, read and share data for free. When will Geochemistry, Geophysics, Geosystems become open access? All articles in the journal will be open access as of 1 January 2022. After 8 September 2021, submissions received/accepted must agree to pay the open access article processing charge (APC), but there will be no excess page fees or any other additional fees for publication. What if I already have a paper under consideration to Geochemistry, Geophysics, Geosystems? If your paper: • is under consideration before 8 September 2021 and • publishes after 1 January 2021, then your paper will publish with copyright to the authors under a Creative Commons license for free (the fee will be waived). If your paper publishes in 2021, then the paper will publish as a subscription article (copyright AGU). -
Thomas Robert Watters
THOMAS ROBERT WATTERS Address: Center for Earth and Planetary Studies National Air and Space Museum Smithsonian Institution P. O. Box 37012, Washington, DC 20013-7012 Education: George Washington University, Ph.D., Geology (1981-1985). Bryn Mawr College, M.A., Geology (1977-1979). West Chester University, B.S. (magna cum laude), Earth Sciences (1973-1977). Experience: Senior Scientist, Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution (1998-present). Chairman, Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution (1989-1998). Research Geologist, Center for Earth and Planetary Studies, Smithsonian Institution, Planetary Geology and Tectonics, Structural Geology, Tectonophysics (1981-1989). Research Assistant, Department of Terrestrial Magnetism, Carnegie Institution of Washington, Chemical Analysis and Fission Track Studies of Meteorites (1980-1981). Research Fellowship, American Museum of Natural History, Electron Microprobe and Petrographic Study of Aubrites and Related Meteorites (1978-1980). Teaching Assistant, Bryn Mawr College (1977-1979), Physical and Historical Geology, Crystallography and Optical Crystallography. Undergraduate Assistant, West Chester University (1973-1977), Teaching Assistant in General and Advanced Astronomy, Physical and Historical Geology. Honors: William P. Phillips Memorial Scholarship (West Chester University); National Air and Space Museum Certificate of Award 1983, 1986, 1989, 1991, 1992, 2002, 2004; American Geophysical Union Editor's Citation for Excellence in Refereeing - Journal Geophysical Research-Planets, 1992; Smithsonian Exhibition Award - Earth Today: A Digital View of Our Dynamic Planet, 1999; Certificate of Appreciation, Geological Society of America, 2005, 2006; Elected to Fellowship in the Geological Society of America, 2007. The Johns Hopkins University Applied Physics Laboratory 2009 Publication Award - Outstanding Research Paper, “Return to Mercury: A Global Perspective on MESSENGER’s First Mercury Flyby (S.C. -
Latex Submission Guidelines
Latex submission guidelines The current version of the zip archive containing all components is marked April 30, 2019 The current version of the main CLS file is April 16, 2019 You are not required to use the newest template, but it is strongly recommended. Zip Contents: April‐30‐2019‐latex‐templates.zip contains these files: agujournaltemplate.tex o This is a “sample” manuscript. It contains commented out instructions and pre‐defined sections to add your work. agujournal2019.cls o This is the primary class file. It corresponds to agujournaltemplate.tex si_template_2019.tex o A “sample” supporting information readme. Like agujournaltemplate.tex, it contains a framework to fill with information about your supplemental files. agutexSI2019.cls o The class file for the supporting information readme file, si_template_2019.tex trackchanges.sty o a third‐party package that facilitates manuscript annotation, usually for tracking changes. Set package options to “inline” to show annotations, “finalnew” to compile an unmarked paper. Complete documentation is here. a directory, trackchanges‐0.7.0 o contains python scripts for automated removal of change tracking commands, if needed o also includes documentation and authorship info for the package above 1 Using agujournaltemplate.tex 1. enter the journal’s name in plain text \journalname{here} 2. enter your paper’s title \title{here} 3. List all authors \authors{here} List authors by first name or initial followed by last name and separated by commas. Use \affil{} to number affiliations, and \thanks{} for author notes. Additional author notes should be indicated with \thanks{} (current addresses, for example). Example: \authors{A. B. -
AGU Electronics Editions Package, AGU
SCHEDULE 3 Addition(s), Deletion(s) to Agreement, Licensed Materials, Subscription Period and Access Method A schedule dated 11'/11./UlfJ to the License dated 1/;-t./u;ot{ between American Geophysical Union and The California Digital Library. ADDITION(s) DELETION(s) TO THE LICENSED MATERIALS AND SUBSCRIPTION PERIOD AND ACCESS METHOD: Addition(s), Deletion(s) made by the Licensee must be approved by Publisher, agreed to, and signed by both parties. Titles(s) Period • • •• Fee AGU Electronics Editions Package* Jan 1 - Dec 31, 2011 AGU Digital Library Jan 1 - Dec 31, 2011 Purchase starting Jan 1, 2011 *Includes the journals titled: Journal of Geophysical Research - All sections Journal of Geophysical Research - Space Physics Section Journal of Geophysical Research - Solid Earth Section Journal of Geophysical Research - Oceans Section Journal of Geophysical Research - Atmospheres Section Journal of Geophysical Research - Planets Section Journal of Geophysical Research - Earth Surface Section Journal of Geophysical Research - Biogeosciences Section Water Resources Research Reviews of Geophysics Geophysical Research Letters Radio Science Tectonics Paleoceanography Global Biogeochemical Cycles Geochemistry Geophysics Geosystems Space Weather Earth Interactions (copublished with AMS and AAG) Chinese Journal of Geophysics (distributed by AGU) Nonlinear Processes in Geophysics (copublished with EGU) **Each year thereafter, a ccess fee would be charged to the Licensee. SUBSCRIBING LOCATION IP ADDRESSES UC Berkeley [Including Lawrence Berkeley Lab] -
South Pole-Aitken Basin
Feasibility Assessment of All Science Concepts within South Pole-Aitken Basin INTRODUCTION While most of the NRC 2007 Science Concepts can be investigated across the Moon, this chapter will focus on specifically how they can be addressed in the South Pole-Aitken Basin (SPA). SPA is potentially the largest impact crater in the Solar System (Stuart-Alexander, 1978), and covers most of the central southern farside (see Fig. 8.1). SPA is both topographically and compositionally distinct from the rest of the Moon, as well as potentially being the oldest identifiable structure on the surface (e.g., Jolliff et al., 2003). Determining the age of SPA was explicitly cited by the National Research Council (2007) as their second priority out of 35 goals. A major finding of our study is that nearly all science goals can be addressed within SPA. As the lunar south pole has many engineering advantages over other locations (e.g., areas with enhanced illumination and little temperature variation, hydrogen deposits), it has been proposed as a site for a future human lunar outpost. If this were to be the case, SPA would be the closest major geologic feature, and thus the primary target for long-distance traverses from the outpost. Clark et al. (2008) described four long traverses from the center of SPA going to Olivine Hill (Pieters et al., 2001), Oppenheimer Basin, Mare Ingenii, and Schrödinger Basin, with a stop at the South Pole. This chapter will identify other potential sites for future exploration across SPA, highlighting sites with both great scientific potential and proximity to the lunar South Pole.