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Financial Support for the Development of These Album Pages Provided by Mystic Stamp Company America's Leading Stamp Dealer
SPACE ON STAMPS Created for free use in the public domain American Philatelic Society ©2010 • www.stamps.org Financial support for the development of these album pages provided by Mystic Stamp Company America’s Leading Stamp Dealer and proud of its support of the American Philatelic Society www.MysticStamp.com, 800-433-7811 Space on Stamps ou might say, it all started with the dream of flight and a desire to see the world as the birds do. For tens of thousands of years mankind has watched the stars Yand wondered what they might represent. Possibly the oldest constellation identified by humans as a permanent fixture in the night sky is Ursa Major, the Great Bear, the third largest of the constellations, and best known for the seven stars that make up its rump and tail: the Big Dipper (also known as the Plough or the Wagon). The most helpful of the sky maps, a line drawn though the two outside stars on the bowl of the “dipper” points directly to the North Star. Nothing successfully got human beings above the earth on a repeatable basis, however, until the age of ballooning. The first human to go aloft was a scientist, Pilatre de Rozier, who rose 250 feet into the sky in a hot air balloon and remained suspended above the French countryside for fifteen minutes in October 1783. A month later he and the Marquis d’Arlandes traveled about 5½ miles in the first free flight, using a balloon designed by the Montgolfier brothers. The first North American flight was made January 9, 1793, from Philadelphia to Gloucester County, New Jersey. -
Geomorphology, Stratigraphy, and Paleohydrology of the Aeolis Dorsa Region, Mars, with Insights from Modern and Ancient Terrestrial Analogs
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 12-2016 Geomorphology, Stratigraphy, and Paleohydrology of the Aeolis Dorsa region, Mars, with Insights from Modern and Ancient Terrestrial Analogs Robert Eric Jacobsen II University of Tennessee, Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Geology Commons Recommended Citation Jacobsen, Robert Eric II, "Geomorphology, Stratigraphy, and Paleohydrology of the Aeolis Dorsa region, Mars, with Insights from Modern and Ancient Terrestrial Analogs. " PhD diss., University of Tennessee, 2016. https://trace.tennessee.edu/utk_graddiss/4098 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Robert Eric Jacobsen II entitled "Geomorphology, Stratigraphy, and Paleohydrology of the Aeolis Dorsa region, Mars, with Insights from Modern and Ancient Terrestrial Analogs." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Geology. Devon M. Burr, -
Oxygen Exosphere of Mars: Evidence from Pickup Ions Measured By
Oxygen Exosphere of Mars: Evidence from Pickup Ions Measured by MAVEN By Ali Rahmati Submitted to the graduate degree program in the Department of Physics and Astronomy, and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Doctor of Philosophy. ________________________________ Professor Thomas E. Cravens, Chair ________________________________ Professor Philip S. Baringer ________________________________ Professor David Braaten ________________________________ Professor Mikhail V. Medvedev ________________________________ Professor Stephen J. Sanders Date Defended: 22 January 2016 The Dissertation Committee for Ali Rahmati certifies that this is the approved version of the following dissertation: Oxygen Exosphere of Mars: Evidence from Pickup Ions Measured by MAVEN ________________________________ Professor Thomas E. Cravens, Chair Date approved: 22 January 2016 ii Abstract Mars possesses a hot oxygen exosphere that extends out to several Martian radii. The main source for populating this extended exosphere is the dissociative recombination of molecular oxygen ions with electrons in the Mars ionosphere. The dissociative recombination reaction creates two hot oxygen atoms that can gain energies above the escape energy at Mars and escape from the planet. Oxygen loss through this photochemical reaction is thought to be one of the main mechanisms of atmosphere escape at Mars, leading to the disappearance of water on the surface. In this work the hot oxygen exosphere of Mars is modeled using a two-stream/Liouville approach as well as a Monte-Carlo simulation. The modeled exosphere is used in a pickup ion simulation to predict the flux of energetic oxygen pickup ions at Mars. The pickup ions are created via ionization of neutral exospheric oxygen atoms through photo-ionization, charge exchange with solar wind protons, and electron impact ionization. -
ROSS T. SHINYAMA #8830-0 SUMMER II. Kaiawtr I+9599-O First L-Lawaiian Center 999 Bishop Street, 23Rd Floor
WATANABI] ING I-LP A Limited Liability [,aw Parrnership ":r : , 1 I ' I J. DOUGLAS ING #1538-0 i.,,i l i t I i '.tì ROSS T. SHINYAMA #8830-0 SUMMER II. KAIAWtr I+9599-O First l-lawaiian Center 999 Bishop Street, 23rd Floor Honolulu, Ilawaii 968 1 3 Telephone No.: (808) 544-8300 Facsimile No.: (808) 544-8399 E-mails : [email protected] Attorneys for TMT INTBRNATIONAL OBSBRVATORY, I,LC BOARD OF LAND AND NATURAL RESOURCES FOR THE STATE OF I]AWAI'I IN THE MATTER OF Case No. BLNR-CC -16-002 TMT INTERNATIONAL A Contested Case l{earing Re Conservation OBSBRVATORY, LLC'S PRE-HEARING District Use Permit (CDUP) I{A-3568 for the STATEMENT; EXHIBIT ..1,'; Thirty Meter Telescope at the Mauna Kea CERTIFICATE OF SERVICE Science Reserve, I(a'ohe Mauka, Hãmakua District, Island of Hawai'i, TMK (3) 4-4- 0l 5:009 TABLtr OF CONTBNTS IN'IRODUC]'ION II DI]SCRIPI'ION OF THE PROJECT AND ITS PROCI]DURAL HISTORY A. Description ofthe Project.................. 3 B. Procedulal Llistory 3 l. General Lease and the MI(SR 3 2. T'he Project 5 III. BURDEN OF PROOF I IV. ISSUES TO BE DECIDED AND TIO'S STATEMENT OF POSI'|iON.. A. The Project, Including the Plans Incorporatcd in the Application, is Consistent with Chapter 183C of the Hawai'i Revised Statutes, the Criteria in HAR $ 13-5- 30(c), and Other Applicable Conservation District Rules......... ..........9 i. The Project is consistent with the purpose of the Conservation District.. 10 2. The Project is consistent with the objectives of the sub2one................... -
Deep Space 2: the Mars Microprobe Project and Beyond
First International Conference on Mars Polar Science 3039.pdf DEEP SPACE 2: THE MARS MICROPROBE PROJECT AND BEYOND. S. E. Smrekar and S. A. Gavit, Mail Stop 183-501, Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasa- dena CA 91109, USA ([email protected]). Mission Overview: The Mars Microprobe Proj- System Design, Technologies, and Instruments: ect, or Deep Space 2 (DS2), is the second of the New Telecommunications. The DS2 telecom system, Millennium Program planetary missions and is de- which is mounted on the aftbody electronics plate, signed to enable future space science network mis- relays data back to earth via the Mars Global Surveyor sions through flight validation of new technologies. A spacecraft which passes overhead approximately once secondary goal is the collection of meaningful science every 2 hours. The receiver and transmitter operate in data. Two micropenetrators will be deployed to carry the Ultraviolet Frequency Range (UHF) and data is out surface and subsurface science. returned at a rate of 7 Kbits/second. The penetrators are being carried as a piggyback Ultra-low-temperature lithium primary battery. payload on the Mars Polar Lander cruise ring and will One challenging aspect of the microprobe design is be launched in January of 1999. The Microprobe has the thermal environment. The batteries are likely to no active control, attitude determination, or propulsive stay no warmer than -78° C. A lithium-thionyl pri- systems. It is a single stage from separation until mary battery was developed to survive the extreme landing and will passively orient itself due to its aero- temperature, with a 6 to 14 V range and a 3-year shelf dynamic design (Fig. -
Aerothermodynamic Design of the Mars Science Laboratory Heatshield
Aerothermodynamic Design of the Mars Science Laboratory Heatshield Karl T. Edquist∗ and Artem A. Dyakonovy NASA Langley Research Center, Hampton, Virginia, 23681 Michael J. Wrightz and Chun Y. Tangx NASA Ames Research Center, Moffett Field, California, 94035 Aerothermodynamic design environments are presented for the Mars Science Labora- tory entry capsule heatshield. The design conditions are based on Navier-Stokes flowfield simulations on shallow (maximum total heat load) and steep (maximum heat flux, shear stress, and pressure) entry trajectories from a 2009 launch. Boundary layer transition is expected prior to peak heat flux, a first for Mars entry, and the heatshield environments were defined for a fully-turbulent heat pulse. The effects of distributed surface roughness on turbulent heat flux and shear stress peaks are included using empirical correlations. Additional biases and uncertainties are based on computational model comparisons with experimental data and sensitivity studies. The peak design conditions are 197 W=cm2 for heat flux, 471 P a for shear stress, 0.371 Earth atm for pressure, and 5477 J=cm2 for total heat load. Time-varying conditions at fixed heatshield locations were generated for thermal protection system analysis and flight instrumentation development. Finally, the aerother- modynamic effects of delaying launch until 2011 are previewed. Nomenclature 1 2 2 A reference area, 4 πD (m ) CD drag coefficient, D=q1A D aeroshell diameter (m) 2 Dim multi-component diffusion coefficient (m =s) ci species mass fraction H total enthalpy -
Aerocapture FS-Pdf.Indd
NASA Facts National Aeronautics and Space Administration Marshall Space Flight Center Huntsville, Alabama 35812 FS-2004-09-127-MSFC July 2004 Aerocapture Technology NASA technologists are working to develop ways to place robotic space vehicles into long-duration, scientific orbits around distant Solar System destinations without the need for the heavy, on-board fuel loads that have historically inhibited vehicle performance, mission dura- tion and available mass for science payloads. Aerocapture -- a flight maneuver that inserts a space- craft into its proper orbit once it arrives at a planet -- is part of a unique family of “aeroassist” technologies under consideration to achieve these goals and enable robust science missions to any planetary body with an appreciable atmosphere. Aerocapture technology is just one of many propulsion technologies being developed by NASA technologists and their partners in industry and academia, led by NASA’s In-Space Propulsion Technology Office at the Marshall Space Flight Center in Huntsville, Ala. The Center implements the In-Space Propulsion Technolo- gies Program on behalf of NASA’s Science Mission Directorate in Washington. Aerocapture uses a planet’s or moon’s atmosphere to accomplish a quick, near-propellantless orbit capture to place a space vehicle in its proper orbit. The atmo- sphere is used as a brake to slow down a spacecraft, transferring the energy associated with the vehicle’s high speed into thermal energy. Aerocapture entering Mars Orbit. The aerocapture maneuver starts with an approach trajectory into the atmosphere of the target body. The dense atmosphere creates friction, slowing the craft and placing it into an elliptical orbit -- an oval shaped orbit. -
“Mining” Water Ice on Mars an Assessment of ISRU Options in Support of Future Human Missions
National Aeronautics and Space Administration “Mining” Water Ice on Mars An Assessment of ISRU Options in Support of Future Human Missions Stephen Hoffman, Alida Andrews, Kevin Watts July 2016 Agenda • Introduction • What kind of water ice are we talking about • Options for accessing the water ice • Drilling Options • “Mining” Options • EMC scenario and requirements • Recommendations and future work Acknowledgement • The authors of this report learned much during the process of researching the technologies and operations associated with drilling into icy deposits and extract water from those deposits. We would like to acknowledge the support and advice provided by the following individuals and their organizations: – Brian Glass, PhD, NASA Ames Research Center – Robert Haehnel, PhD, U.S. Army Corps of Engineers/Cold Regions Research and Engineering Laboratory – Patrick Haggerty, National Science Foundation/Geosciences/Polar Programs – Jennifer Mercer, PhD, National Science Foundation/Geosciences/Polar Programs – Frank Rack, PhD, University of Nebraska-Lincoln – Jason Weale, U.S. Army Corps of Engineers/Cold Regions Research and Engineering Laboratory Mining Water Ice on Mars INTRODUCTION Background • Addendum to M-WIP study, addressing one of the areas not fully covered in this report: accessing and mining water ice if it is present in certain glacier-like forms – The M-WIP report is available at http://mepag.nasa.gov/reports.cfm • The First Landing Site/Exploration Zone Workshop for Human Missions to Mars (October 2015) set the target -
A Tracer of CO2 Density Variations in the Martian Lower CO2 Density Provided by the Mars Climate Database Is Scaled Down by a Factor Between 0.50 and 0.66
Journal of Geophysical Research: Planets 1 RESEARCH ARTICLE The O( S) 297.2-nm Dayglow Emission: A Tracer of CO2 Density 10.1029/2018JE005709 Variations in the Martian Lower Thermosphere Key Points: L. Gkouvelis1 , J.-C. Gérard1 , B. Ritter1,2 , B. Hubert1 , N. M. Schneider3 , and S. K. Jain3 • Limb observations of the O(1S-3P) fi dayglow by MAVEN con rm 1LPAP, STAR Institute, Université de Liège, Liege, Belgium, 2Royal Observatory of Belgium, Brussels, Belgium, 3LASP, existence of previously predicted emission peak near 80 km University of Colorado Boulder, Boulder, CO, USA • We successfully model the lower peak emission profile and show that 1 it only depends on the vertical CO2 Abstract The O( S) metastable atoms can radiatively relax by emitting airglow at 557.7 and 297.2 nm. The distribution and solar Ly-alpha latter one has been observed with the Imaging Ultraviolet Spectrograph onboard the Mars Atmosphere • Combination of model and fi observations enable to constrain the and Volatile Evolution Mars orbiter since 2014. Limb pro les of the 297.2-nm dayglow have been collected slant CO2 column over the peak and near periapsis with a spatial resolution of 5 km or less. They show a double-peak structure that was previously the corresponding atmospheric predicted but never observed during earlier Mars missions. The production of both 297.2-nm layers is pressure dominated by photodissociation of CO2. Their altitude and brightness is variable with season and latitude, reflecting changes in the total column of CO2 present in the lower thermosphere. Since the lower emission peak near 85 km is solely produced by photodissociation, its peak is an indicator of the unit optical depth Correspondence to: pressure level and the overlying CO2 column density. -
ROSS T. SHTNYAMA #8830-0 Li;Ij
s23820 WATANABE ING LLP A Limited Liability Law Partnership li;ij ,ji,,'ì j-1 ir i J. DOUGLAS ING #1.538-0 BRIAN A. KANG #6495.0 ROSS T. SHTNYAMA #8830-0 SUMMER H. KAIAWE #9599-0 First Hawaiian Center 999 Bishop Street, 23rd Floor Honolulu, Hawaii96813 Telephone No.: (808) 544-8300 Facsimile No.: (S08) 544-8399 E-mails: [email protected] Attorneys for TMT I NTERNATIONAL OBSERVATORY, LLC BOARD OF LAND AND NATURAL RESOURCES FOR TI-IE STATE OF HAWAI'I IN THE MATTER OF , Case No. BLNR-CC-16-002 TMT INTERNATIONAL OBSERVATORY, LLC'S A Contested Case Hearing Re Csnservation IFOU'RT|{ AMENDED EXHIBIT LIST and Distríct Use Permit (CDUP) HA-3568 forthe ADDITIONAL EXHIBIT C-40; CERTIFICATE OF Thirty Meter Telescope at the Mauna Kea SERVICE Science Reserve, Kaohe Mauka, Hamaku Distrrict, lsland of Hawaii, TMK (3) 4-4'OL5 PARTY: TMT INTERNATIONAL OBSERVATORY, LLC Received Exhibit No Description lnto Evidence c-1 Testimony of Ed Stone c-2 Testimony of Gary Sanders Received Exhibit No. Description lnto Evidence Graphic showing Mitigation Measures Reduce Size and Visibility of c-3 TMT c-4 Testimony of Mike Bolte New York Times article: From Hawaii's Mauna Kea, A Universe of ' c-5 Discoveries (October 3, 2016) c-6 Testimony of David M. Callies c-7 Testimony of James Hallstrom, including Curriculum Vitae c-8 Testimony of Dr. Heather Kaluna c-9 Testimony of Naea Stevens c-1_0 Direct Testimony of Amber lmai-Hong c-1L Testimony of Robert B. Rechtman Thirty Meter Telescope Archaeological Report, prepared by c-12 Genevieve Glennon and Robert Rechtman (October -
Insight Spacecraft Launch for Mission to Interior of Mars
InSight Spacecraft Launch for Mission to Interior of Mars InSight is a robotic scientific explorer to investigate the deep interior of Mars set to launch May 5, 2018. It is scheduled to land on Mars November 26, 2018. It will allow us to better understand the origin of Mars. First Launch of Project Orion Project Orion took its first unmanned mission Exploration flight Test-1 (EFT-1) on December 5, 2014. It made two orbits in four hours before splashing down in the Pacific. The flight tested many subsystems, including its heat shield, electronics and parachutes. Orion will play an important role in NASA's journey to Mars. Orion will eventually carry astronauts to an asteroid and to Mars on the Space Launch System. Mars Rover Curiosity Lands After a nine month trip, Curiosity landed on August 6, 2012. The rover carries the biggest, most advanced suite of instruments for scientific studies ever sent to the martian surface. Curiosity analyzes samples scooped from the soil and drilled from rocks to record of the planet's climate and geology. Mars Reconnaissance Orbiter Begins Mission at Mars NASA's Mars Reconnaissance Orbiter launched from Cape Canaveral August 12. 2005, to find evidence that water persisted on the surface of Mars. The instruments zoom in for photography of the Martian surface, analyze minerals, look for subsurface water, trace how much dust and water are distributed in the atmosphere, and monitor daily global weather. Spirit and Opportunity Land on Mars January 2004, NASA landed two Mars Exploration Rovers, Spirit and Opportunity, on opposite sides of Mars. -
Apollo Over the Moon: a View from Orbit (Nasa Sp-362)
chl APOLLO OVER THE MOON: A VIEW FROM ORBIT (NASA SP-362) Chapter 1 - Introduction Harold Masursky, Farouk El-Baz, Frederick J. Doyle, and Leon J. Kosofsky [For a high resolution picture- click here] Objectives [1] Photography of the lunar surface was considered an important goal of the Apollo program by the National Aeronautics and Space Administration. The important objectives of Apollo photography were (1) to gather data pertaining to the topography and specific landmarks along the approach paths to the early Apollo landing sites; (2) to obtain high-resolution photographs of the landing sites and surrounding areas to plan lunar surface exploration, and to provide a basis for extrapolating the concentrated observations at the landing sites to nearby areas; and (3) to obtain photographs suitable for regional studies of the lunar geologic environment and the processes that act upon it. Through study of the photographs and all other arrays of information gathered by the Apollo and earlier lunar programs, we may develop an understanding of the evolution of the lunar crust. In this introductory chapter we describe how the Apollo photographic systems were selected and used; how the photographic mission plans were formulated and conducted; how part of the great mass of data is being analyzed and published; and, finally, we describe some of the scientific results. Historically most lunar atlases have used photointerpretive techniques to discuss the possible origins of the Moon's crust and its surface features. The ideas presented in this volume also rely on photointerpretation. However, many ideas are substantiated or expanded by information obtained from the huge arrays of supporting data gathered by Earth-based and orbital sensors, from experiments deployed on the lunar surface, and from studies made of the returned samples.