Hubble Space Telescope Primer for Cycle 25
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Observation of the Airglow from the ISS by the IMAP Mission *Y
2013/3/13(ANGWIN workshop, Tachikawa) Observation of the airglow from the ISS by the IMAP mission *Y. Akiya [1], A. Saito [1], T. Sakanoi [2], Y. Hozumi [1], A. Yamazaki [3], Y. Otsuka [4] [1] Graduation School of Science, Kyoto University , [2] PPARC, Tohoku University, [3] ISAS/JAXA, [4] STE Laboratory, Nagoya University ----- Outline ----- Introduction of the IMAP mission Visible and near-infrared spectrographic imager Samples of airglow observation by VISI Summary “ISS-IMAP” mission Ionosphere, Mesosphere, Upper atmosphere and Plasmasphere Imagers of the ISS-IMAP mapping mission from the mission International Space Station (ISS) Observational imagers were installed on the Exposure Facility of Japanese Experimental Module: August 9th, 2012. Initial checkout: August and September, 2012 Nominal observations: October, 2012 - [Pictures: Courtesy of JAXA/NASA] [this issue]. According to characteristics of airglow emissions, wavelength range from 630 to 762 nm. Typical total intensity of such as intensity, emission height, background continuum, etc., we airglow is 100 1000 R as listed in Table 1, and 10 % variation of selected the airglow emissions which will be measured with VISI, the total intensity must be detected in order to investigate the and determined the requirements for instrumental design. The airglow variation pattern. In addition, short exposure cycle less targets and requirements are summarized in Table 1. than several seconds is necessary to measure small-scale airglow Table 1. Scientific Targets of VISI signatures (see Table 1) considering the orbital speed of ISS (~8 km/s). Airglow Required Region Scientific Typical A sectional view of VISI and its specifications are given in (waele- spatial (height) target intensity Figure 4 and Table 2, respectively. -
[OI] 5577 in the Airglow and the Aurora
Journal of Resea rch of the National Bureau of Sta ndards- D. Radio Propagation Vol. 63D, No.1, July-August 1959 Origin of [OlJ 5577 in the Airglow and the Aurora Franklin E. Roach, James W. McCaulley, and Edward Marovich (January 30, 1959) The distribution of 5577 zenith intensities at stations in the subauroral zone iB found to be unimodal with no discontinuity at the visual threshold. This is interpreted as evi dence that 5577 airglow and 5577 aurora may have a common origin. 1. Introduction origin hypothesis, their critical characteristic being the lack of any discontinuity. It i cu tomary to refer to [01] 5577 as airglow if In figure 2, a replot of the histogram of St. Amand it is invisible and as aurora if it is visible. Thus, and Ashburn is shown with a regroupillg of the data the physiological visual threshold (at approximately to correspond to class intervals of 50 R rather than the 10 R that they used. They put an approxi 1,000 myleighs 1 for extended objects) has been assumed to have a physical significance in the upper mately normal curve through the plot on the basis atmosphere with different mechanisms operative of which they were able to state that an intensity above and below the threshold. The purpose of correspondulg to a just visible aurora should occur this paper is to inquil'e into the existence of a only "once or twice in geologic time." Because physical criterion to distinguish between 5577 auroras do occur occasionally, though rarely, in southern California, the implication is that an aurora airglow and 5577 aurora. -
+ New Horizons
Media Contacts NASA Headquarters Policy/Program Management Dwayne Brown New Horizons Nuclear Safety (202) 358-1726 [email protected] The Johns Hopkins University Mission Management Applied Physics Laboratory Spacecraft Operations Michael Buckley (240) 228-7536 or (443) 778-7536 [email protected] Southwest Research Institute Principal Investigator Institution Maria Martinez (210) 522-3305 [email protected] NASA Kennedy Space Center Launch Operations George Diller (321) 867-2468 [email protected] Lockheed Martin Space Systems Launch Vehicle Julie Andrews (321) 853-1567 [email protected] International Launch Services Launch Vehicle Fran Slimmer (571) 633-7462 [email protected] NEW HORIZONS Table of Contents Media Services Information ................................................................................................ 2 Quick Facts .............................................................................................................................. 3 Pluto at a Glance ...................................................................................................................... 5 Why Pluto and the Kuiper Belt? The Science of New Horizons ............................... 7 NASA’s New Frontiers Program ........................................................................................14 The Spacecraft ........................................................................................................................15 Science Payload ...............................................................................................................16 -
Hubble Space Telescope Primer for Cycle 18
January 2010 Hubble Space Telescope Primer for Cycle 18 An Introduction to HST for Phase I Proposers Space Telescope Science Institute 3700 San Martin Drive Baltimore, Maryland 21218 [email protected] Operated by the Association of Universities for Research in Astronomy, Inc., for the National Aeronautics and Space Administration How to Get Started If you are interested in submitting an HST proposal, then proceed as follows: • Visit the Cycle 18 Announcement Web page: http://www.stsci.edu/hst/proposing/docs/cycle18announce Then continue by following the procedure outlined in the Phase I Roadmap available at: http://apst.stsci.edu/apt/external/help/roadmap1.html More technical documentation, such as that provided in the Instrument Handbooks, can be accessed from: http://www.stsci.edu/hst/HST_overview/documents Where to Get Help • Visit STScI’s Web site at: http://www.stsci.edu • Contact the STScI Help Desk. Either send e-mail to [email protected] or call 1-800-544-8125; from outside the United States and Canada, call [1] 410-338-1082. The HST Primer for Cycle 18 was edited by Francesca R. Boffi, with the technical assistance of Susan Rose and the contributions of many others from STScI, in particular Alessandra Aloisi, Daniel Apai, Todd Boroson, Brett Blacker, Stefano Casertano, Ron Downes, Rodger Doxsey, David Golimowski, Al Holm, Helmut Jenkner, Jason Kalirai, Tony Keyes, Anton Koekemoer, Jerry Kriss, Matt Lallo, Karen Levay, John MacKenty, Jennifer Mack, Aparna Maybhate, Ed Nelan, Sami-Matias Niemi, Cheryl Pavlovsky, Karla Peterson, Larry Petro, Charles Proffitt, Neill Reid, Merle Reinhart, Ken Sembach, Paula Sessa, Nancy Silbermann, Linda Smith, Dave Soderblom, Denise Taylor, Nolan Walborn, Alan Welty, Bill Workman and Jim Younger. -
REMOTE SENSING of SEISMIC ACTIVITY on VENUS USING a SMALL SPACECRAFT: INITIAL MODELING RESULTS, A. Komjathy1, A. Didion1, B. Sutin1, B
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 1731.pdf REMOTE SENSING OF SEISMIC ACTIVITY ON VENUS USING A SMALL SPACECRAFT: INITIAL MODELING RESULTS, A. Komjathy1, A. Didion1, B. Sutin1, B. Nakazono1, A. Karp1, M. Wallace1, G. Lan- toine1, S. Krishnamoorthy1, M. Rud1, J. Cutts, J. Makela2, M. Grawe2, P. Lognonné3, B. Kenda3, M. Drilleau3 and Jörn Helbert4 1Jet Propulsion Laboratory, California Institute of Technology, USA 2University of Illinois at Urbana-Champaign, USA 3Institut de Physique du Globe-Paris Sorbonne, France 4Deutsches Zentrum für Luft- und Raumfahrt e.V. (DLR), Germany Introduction: The planetary evolution and struc- other at 4.3 µm (visible on the dayside). The signifi- ture of Venus remain uncertain more than half a centu- cant advantage of observing nightglow on Venus is ry after the first visit by a robotic spacecraft. To under- that it is much brighter on Venus than on Earth [2] and stand how Venus evolved it is necessary to detect the that airglow lifetime (~4,000 sec) is significantly long- signs of seismic activity. Due to the adverse surface er than the period of seismic waves (10-30 sec). This conditions on Venus, with extremely high temperature makes it very attractive for directly detecting surface and pressure, it is infeasible with current technology, waves on Venus. This is in sharp contrast with Earth even using flagship missions, to place seismometers on where the lifetime of airglow is about one order of the surface for an extended period of time. Due to dy- magnitude smaller (~110 sec) than, e.g., the tsunami namic coupling between the solid planet and the at- waves we routinely observe on Earth with 630 nm air- mosphere, the waves generated by quakes propagate glow instruments [4]. -
Using the Tycho Catalogue for Axaf
187 USING THE TYCHO CATALOGUE FOR AXAF: GUIDING AND ASPECT RECONSTRUCTION FOR HALF-ARCSECOND X-RAY IMAGES P.J. Green, T.A. Aldcroft, M.R. Garcia, P. Slane, J. Vrtilek Smithsonian Astrophysical Observatory High resolution imaging and/or fast timing measure- ABSTRACT ments are enabled by the High Resolution Camera HRC; Kenter 1996. Advances over the high resolu- tion imagers of Einstein and ROSAT include smaller AXAF, the Advanced X-ray Astrophysics Facility will p ore size, larger micro channel plate area, lower back- b e the third satellite in the series of great observato- ground, energy resolution, and charged particle anti- ries in the NASA program, after the Hubble Space coincidence. Telescop e and the Gamma Ray Observatory. At launch in fall 1998, AXAF will carry a high reso- The AXAF CCD Imaging Sp ectrometer ACIS; lution mirror, two imaging detectors, and two sets of Garmire 1997 is a CCD array for simultaneous imag- transmission gratings Holt 1993. Imp ortant AXAF ing and sp ectroscopyE=E =2050 over almost features are: an order of magnitude improvementin the entire AXAF bandpass with high quantum e- spatial resolution, good sensitivity from 0.1{10keV, ciency and low read noise. Pictures of extended ob- and the capability for high sp ectral resolution obser- jects can b e obtained along with sp ectral information vations over most of this range. from each element of the picture. The ACIS-I array comprises 4 CCDs arranged in a square which pro- The Tycho Catalogue from the Hipparcos mission 2 vide a 16 16 arcmin eld. -
Vireo Manual.Pdf
VIREO: The Virtual Educational Observatory 1 VIREO: THE VIRTUAL EDUCATIONAL OBSERVATORY Software Reference Guide A Manual to Accompany Software Document SM 20: Circ.Version 1.0 Department of Physics Gettysburg College Gettysburg, PA 17325 Telephone: (717) 337-6028 email: [email protected] Software, and Manuals prepared by: Contemporary Laboratory Glenn Snyder and Laurence Marschall (CLEA PROJECT, Gettysburg College) Experiences in Astronomy VIREO: The Virtual Educational Observatory 2 Contents Introduction To Vireo: The Virtual Educational Observatory .................................................................................. 3 Starting Vireo ................................................................................................................................................................ 4 The Virtual Observatory Control Screen ..................................................................................................................... 4 Using an Optical Telescope ........................................................................................................................................... 5 Using the Photometer .................................................................................................................................................... 8 Using the Spectrometer ............................................................................................................................................... 11 Using the Multi-Channel Spectrometer ..................................................................................................................... -
Building a Popular Science Library Collection for High School to Adult Learners: ISSUES and RECOMMENDED RESOURCES
Building a Popular Science Library Collection for High School to Adult Learners: ISSUES AND RECOMMENDED RESOURCES Gregg Sapp GREENWOOD PRESS BUILDING A POPULAR SCIENCE LIBRARY COLLECTION FOR HIGH SCHOOL TO ADULT LEARNERS Building a Popular Science Library Collection for High School to Adult Learners ISSUES AND RECOMMENDED RESOURCES Gregg Sapp GREENWOOD PRESS Westport, Connecticut • London Library of Congress Cataloging-in-Publication Data Sapp, Gregg. Building a popular science library collection for high school to adult learners : issues and recommended resources / Gregg Sapp. p. cm. Includes bibliographical references and index. ISBN 0–313–28936–0 1. Libraries—United States—Special collections—Science. I. Title. Z688.S3S27 1995 025.2'75—dc20 94–46939 British Library Cataloguing in Publication Data is available. Copyright ᭧ 1995 by Gregg Sapp All rights reserved. No portion of this book may be reproduced, by any process or technique, without the express written consent of the publisher. Library of Congress Catalog Card Number: 94–46939 ISBN: 0–313–28936–0 First published in 1995 Greenwood Press, 88 Post Road West, Westport, CT 06881 An imprint of Greenwood Publishing Group, Inc. Printed in the United States of America TM The paper used in this book complies with the Permanent Paper Standard issued by the National Information Standards Organization (Z39.48–1984). 10987654321 To Kelsey and Keegan, with love, I hope that you never stop learning. Contents Preface ix Part I: Scientific Information, Popular Science, and Lifelong Learning 1 -
Nighttime Photochemical Model and Night Airglow on Venus
Planetary and Space Science 85 (2013) 78–88 Contents lists available at ScienceDirect Planetary and Space Science journal homepage: www.elsevier.com/locate/pss Nighttime photochemical model and night airglow on Venus Vladimir A. Krasnopolsky n a Department of Physics, Catholic University of America, Washington, DC 20064, USA b Moscow Institute of Physics and Technology, Dolgoprudnyy 141700 Russia article info abstract Article history: The photochemical model for the Venus nighttime atmosphere and night airglow (Krasnopolsky, 2010, Received 23 December 2012 Icarus 207, 17–27) has been revised to account for the SPICAV detection of the nighttime ozone layer and Received in revised form more detailed spectroscopy and morphology of the OH nightglow. Nighttime chemistry on Venus is 28 April 2013 induced by fluxes of O, N, H, and Cl with mean hemispheric values of 3 Â 1012,1.2Â 109,1010, and Accepted 31 May 2013 − − 1010 cm 2 s 1, respectively. These fluxes are proportional to column abundances of these species in the Available online 18 June 2013 daytime atmosphere above 90 km, and this favors their validity. The model includes 86 reactions of 29 Keywords: species. The calculated abundances of Cl2, ClO, and ClNO3 exceed a ppb level at 80–90 km, and Venus perspectives of their detection are briefly discussed. Properties of the ozone layer in the model agree Photochemistry with those observed by SPICAV. An alternative model without the flux of Cl agrees with the observed O Night airglow 3 peak altitude and density but predicts an increase of ozone to 4 Â 108 cm−3 at 80 km. -
A Physically-Based Night Sky Model Henrik Wann Jensen1 Fredo´ Durand2 Michael M
To appear in the SIGGRAPH conference proceedings A Physically-Based Night Sky Model Henrik Wann Jensen1 Fredo´ Durand2 Michael M. Stark3 Simon Premozeˇ 3 Julie Dorsey2 Peter Shirley3 1Stanford University 2Massachusetts Institute of Technology 3University of Utah Abstract 1 Introduction This paper presents a physically-based model of the night sky for In this paper, we present a physically-based model of the night sky realistic image synthesis. We model both the direct appearance for image synthesis, and demonstrate it in the context of a Monte of the night sky and the illumination coming from the Moon, the Carlo ray tracer. Our model includes the appearance and illumi- stars, the zodiacal light, and the atmosphere. To accurately predict nation of all significant sources of natural light in the night sky, the appearance of night scenes we use physically-based astronomi- except for rare or unpredictable phenomena such as aurora, comets, cal data, both for position and radiometry. The Moon is simulated and novas. as a geometric model illuminated by the Sun, using recently mea- The ability to render accurately the appearance of and illumi- sured elevation and albedo maps, as well as a specialized BRDF. nation from the night sky has a wide range of existing and poten- For visible stars, we include the position, magnitude, and temper- tial applications, including film, planetarium shows, drive and flight ature of the star, while for the Milky Way and other nebulae we simulators, and games. In addition, the night sky as a natural phe- use a processed photograph. Zodiacal light due to scattering in the nomenon of substantial visual interest is worthy of study simply for dust covering the solar system, galactic light, and airglow due to its intrinsic beauty. -
Optical Radiation from the Atmosphere
Utah State University DigitalCommons@USU Space Dynamics Lab Publications Space Dynamics Lab 1-1-1976 Optical Radiation from the Atmosphere Doran J. Baker Utah State University William R. Pendleton Jr. Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/sdl_pubs Recommended Citation Baker, Doran J. and Pendleton, William R. Jr., "Optical Radiation from the Atmosphere" (1976). Space Dynamics Lab Publications. Paper 2. https://digitalcommons.usu.edu/sdl_pubs/2 This Article is brought to you for free and open access by the Space Dynamics Lab at DigitalCommons@USU. It has been accepted for inclusion in Space Dynamics Lab Publications by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. cÌ E1 Baker, Doran J., and William R. Pendleton Jr. 1976. “Optical Radiation from the Atmosphere.” Proceedings of SPIE 0091: 50–62. doi:10.1117/12.955071. OPTICAL RADIATION FROM THE ATMOSPHERE Doran J. Baker and William R. Pendleton,Pendleton, Jr.Jr. Electro-Electro-Dynamics Dynamics Laboratories,Laboratories, UtahUtah StateState University Logan, Utah 84322 ABSTRACT The -interfaceinterface region which lies between the meteorological atmosphere of the Earth and "outer" space is a source ofof abundantabundant opticaloptical radiation.radiation. The purpose of thisthis paper isis toto provide the optical instrumentation engineer with a generalized understanding and a summary reference of naturally-naturally -occurring occurring aerospace radiation phenomena.phenomena. The colors of thethe radiationradiation extend over the full optical spectrum fromfrom ultravioletultraviolet throughthrough thethe infrared.infrared. The emissions, observed during both day and night times,times , areare richrich inin lineline andand bandband spectra.spectra. The parameterparameter- ization of atmosphericatmospheric light by frequency (or photonphoton energy)energy) andand byby spectral radiance is discussed. -
Modern Astronomical Optics 1
Modern Astronomical Optics 1. Fundamental of Astronomical Imaging Systems OUTLINE: A few key fundamental concepts used in this course: Light detection: Photon noise Diffraction: Diffraction by an aperture, diffraction limit Spatial sampling Earth's atmosphere: every ground-based telescope's first optical element Effects for imaging (transmission, emission, distortion and scattering) and quick overview of impact on optical design of telescopes and instruments Geometrical optics: Pupil and focal plane, Lagrange invariant Astronomical measurements & important characteristics of astronomical imaging systems: Collecting area and throughput (sensitivity) flux units in astronomy Angular resolution Field of View (FOV) Time domain astronomy Spectral resolution Polarimetric measurement Astrometry Light detection: Photon noise Poisson noise Photon detection of a source of constant flux F. Mean # of photon in a unit dt = F dt. Probability to detect a photon in a unit of time is independent of when last photon was detected→ photon arrival times follows Poisson distribution Probability of detecting n photon given expected number of detection x (= F dt): f(n,x) = xne-x/(n!) x = mean value of f = variance of f Signal to noise ration (SNR) and measurement uncertainties SNR is a measure of how good a detection is, and can be converted into probability of detection, degree of confidence Signal = # of photon detected Noise (std deviation) = Poisson noise + additional instrumental noises (+ noise(s) due to unknown nature of object observed) Simplest case (often