Earth and Planetary Remote Sensing Instruments/Sensors
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Articles Upon the Hox Family by Comparing Averages of Days Impacted by These Events with Averages of Non-Impacted 3945–3977, Doi:10.5194/Acp-13-3945-2013, 2013
Atmos. Chem. Phys., 15, 2889–2902, 2015 www.atmos-chem-phys.net/15/2889/2015/ doi:10.5194/acp-15-2889-2015 © Author(s) 2015. CC Attribution 3.0 License. Stratospheric and mesospheric HO2 observations from the Aura Microwave Limb Sounder L. Millán1,2, S. Wang2, N. Livesey2, D. Kinnison3, H. Sagawa4, and Y. Kasai4 1Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, California, USA 2Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA 3National Center for Atmospheric Research, Boulder, Colorado, USA 4National Institute of Information and Communications Technology, Koganei, Tokyo, Japan Correspondence to: L. Millán ([email protected]) Received: 18 June 2014 – Published in Atmos. Chem. Phys. Discuss.: 8 September 2014 Revised: 17 February 2015 – Accepted: 24 February 2015 – Published: 13 March 2015 Abstract. This study introduces stratospheric and meso- sphere where O3 chemistry is controlled by catalytic cycles spheric hydroperoxyl radical (HO2) estimates from the Aura involving the HOx (HO2, OH and H) family (Brasseur and Microwave Limb Sounder (MLS) using an offline retrieval Solomon, 2005): (i.e. run separately from the standard MLS algorithm). This new data set provides two daily zonal averages, one during X C O3 ! XO C O2 (R1) daytime from 10 to 0.0032 hPa (using day-minus-night dif- O C XO ! O2 C X; (R2) ferences between 10 and 1 hPa to ameliorate systematic bi- ases) and one during nighttime from 1 to 0.0032 hPa. The where the net effect of these two reactions is simply vertical resolution of this new data set varies from about 4 km O C O ! 2O (R3) at 10 hPa to around 14 km at 0.0032 hPa. -
+ 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 -
SWIFTS and SWIFTS-LA: Two Concepts for High Spectral Resolution Static Micro-Imaging Spectrometers
EPSC Abstracts Vol. 9, EPSC2014-439-1, 2014 European Planetary Science Congress 2014 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2014 SWIFTS and SWIFTS-LA: two concepts for high spectral resolution static micro-imaging spectrometers E. Le Coarer(1), B. Schmitt(1), N. Guerineau (2), G. Martin (1) S. Rommeluere (2), Y. Ferrec (2) F. Simon (1) F. Thomas (1) (1) Univ. UGA ,CNRS, Lab. IPAG, Grenoble, France. (2) ONERA/DOTA Palaiseau France ([email protected] grenoble.fr). Abstract All these instruments use either optical gratings, Fourier transform or AOTF spectrometers. The two SWIFTS (Stationary-Wave Integrated Fourier first types need moving mirrors to scan spectrally Transform Spectrometer) represents a family of very thus adding complexity and failure risk in space. The compact spectrometers based on detection of interesting solution of AOTF, without moving part standing waves for which detectors play itself a role (only piezo) is however limited in resolution to a few in the interferential detection mechanism. The aim of cm-1 due to limitation in monocrystal size (fragile). this paper is to illustrate how these spectrometers can Strong limitations of these instruments in terms of be used to build efficient imaging spectrometers for performances (spectral & spatial resolution and range, planetary exploration inside dm3 instrumental volume. S/N ratio) come from their already large mass, The first mode (SWIFTS) is devoted to high spectral volume, and power consumption. Further increasing resolving power imaging (R~10000-50000) for one of these characteristics will be at the cost of even 40x40 pixels field of view. The second mode bigger instruments. -
The Space-Based Global Observing System in 2010 (GOS-2010)
WMO Space Programme SP-7 The Space-based Global Observing For more information, please contact: System in 2010 (GOS-2010) World Meteorological Organization 7 bis, avenue de la Paix – P.O. Box 2300 – CH 1211 Geneva 2 – Switzerland www.wmo.int WMO Space Programme Office Tel.: +41 (0) 22 730 85 19 – Fax: +41 (0) 22 730 84 74 E-mail: [email protected] Website: www.wmo.int/pages/prog/sat/ WMO-TD No. 1513 WMO Space Programme SP-7 The Space-based Global Observing System in 2010 (GOS-2010) WMO/TD-No. 1513 2010 © World Meteorological Organization, 2010 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate these publication in part or in whole should be addressed to: Chairperson, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0)22 730 84 03 P.O. Box No. 2300 Fax: +41 (0)22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] FOREWORD The launching of the world's first artificial satellite on 4 October 1957 ushered a new era of unprecedented scientific and technological achievements. And it was indeed a fortunate coincidence that the ninth session of the WMO Executive Committee – known today as the WMO Executive Council (EC) – was in progress precisely at this moment, for the EC members were very quick to realize that satellite technology held the promise to expand the volume of meteorological data and to fill the notable gaps where land-based observations were not readily available. -
The Cassini Ultraviolet Imaging Spectrograph Investigation
THE CASSINI ULTRAVIOLET IMAGING SPECTROGRAPH INVESTIGATION 1, 1 1 LARRY W. ESPOSITO ∗, CHARLES A. BARTH , JOSHUA E. COLWELL , GEORGE M. LAWRENCE1, WILLIAM E. McCLINTOCK1,A. IAN F. STEWART1, H. UWE KELLER2, AXEL KORTH2, HANS LAUCHE2, MICHEL C. FESTOU3,ARTHUR L. LANE4, CANDICE J. HANSEN4, JUSTIN N. MAKI4,ROBERT A. WEST4, HERBERT JAHN5, RALF REULKE5, KERSTIN WARLICH5, DONALD E. SHEMANSKY6 and YUK L. YUNG7 1University of Colorado, Laboratory for Atmospheric and Space Physics, 1234 Innovation Drive, Boulder, CO 80303, U.S.A. 2Max-Planck-Institut fur¨ Aeronomie, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany 3Observatoire Midi-Pyren´ ees,´ 14 avenue E. Belin, F31400 Toulouse, France 4JetPropulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, U.S.A. 5Deutsches Zentrum fur¨ Luft und Raumfahrt, Institut fur¨ Weltraumsensorik und Planetenerkundung, Rutherford Strasse 2, 12489 Berlin, Germany 6University of Southern California, Department of Aerospace Engineering, 854 W. 36th Place, Los Angeles, CA 90089, U.S.A. 7California Institute of Technology, Division of Geological and Planetary Sciences, MS 150-21, Pasadena, CA 91125, U.S.A. (∗Author for correspondence: E-mail: [email protected]) (Received 8 July 1999; Accepted in final form 18 October 2000) Abstract. The Cassini Ultraviolet Imaging Spectrograph (UVIS) is part of the remote sensing payload of the Cassini orbiter spacecraft. UVIS has two spectrographic channels that provide images and spectra covering the ranges from 56 to 118 nm and 110 to 190 nm. A third optical path with a solar blind CsI photocathode is used for high signal-to-noise-ratio stellar occultations by rings and atmospheres. A separate Hydrogen Deuterium Absorption Cell measures the relative abundance of deuterium and hydrogen from their Lyman-α emission. -
Version 2.2 Level 2 Data Quality and Description Document
JPL D-33509 Earth Observing System (EOS) Aura Microwave Limb Sounder (MLS) Version 2.2 Level 2 data quality and description document. 0 70 N FWHM / km FWHM / km -2 0 2 4 6 8 10 12 0 100 200 300 400 500 600 0.1 1.0 10.0 Pressure / hPa 100.0 1000.0 -0.2 0.0 0.2 0.4 0.6 0.8 1.0 1.2 -2 -1 0 1 2 Kernel, Integrated kernel Profile number Equator FWHM / km FWHM / km -2 0 2 4 6 8 10 12 0 100 200 300 400 500 600 0.1 1.0 10.0 Pressure / hPa 100.0 1000.0 -0.2 0.0 0.2 0.4 0.6 0.8 1.0 1.2 -2 -1 0 1 2 Kernel, Integrated kernel Profile number Nathaniel J. Livesey, William G. Read, Alyn Lambert, Richard E. Cofield, David T. Cuddy, Lucien Froidevaux, Ryan A Fuller, Robert F. Jarnot, Jonathan H. Jiang, Yibo B. Jiang, Brian W. Knosp, Laurie J. Kovalenko, Herbert M. Pickett, Hugh C. Pumphrey, Michelle L. Santee, Michael J. Schwartz, Paul C. Stek, Paul A. Wagner, Joe W. Waters, and Dong L. Wu. Version 2.2x-1.0a May 22, 2007 Jet Propulsion Laboratory California Institute of Technology Pasadena, California, 91109-8099 Where to find answers to key questions This document serves two purposes. Firstly, to Do not use data for any profile where the field • summarize the quality of version 2.2 (v2.2) EOS MLS Status is an odd number. Level 2 data. -
Chapter 7 Instrument Packages
Chapter 7 Instrument Packages Richard E. Cofield, William A. Imbriale, and Richard E. Hodges This chapter describes antennas used on various instrument packages for science spacecraft. The instruments have been primarily used for the Earth Observing System (EOS), a series of spacecraft to observe Earth from the unique vantage point of space. This chapter includes radiometers (7.1–7.3), scatterometers (7.4), radars (7.5), and altimeters (7.6). 7.1 Radiometers Richard E. Cofield Radiometry is the measurement of electromagnetic radiation using highly sensitive receivers. The blackbody radiation spectrum given by Planck’s radiation law provides a reference against which the radiation spectra of real bodies at the same physical temperature are compared. The spectral, polarization, and angular variations of a scene of interest are dictated by the geometrical configuration and physical properties (dielectric and thermal) of surfaces and interior regions of (1) the materials under study, and (2) the medium (atmosphere or space) through which we make observations. Radiometer parameters (such as frequency, viewing angle, and polarization) can be chosen to relate the radiometer’s output signal strength to properties of the observed scenes. This section describes passive microwave radiometry from spaceborne instruments developed at Jet Propulsion Laboratory (JPL): passive in contrast to active (radio detection and ranging [radar] or laser induced differential absorption radar [lidar]) systems such as altimeters and the scatterometers discussed below, and microwave as a consequence of Planck’s law at the 341 342 Chapter 7 temperature ranges of natural emitters. Hence, it is convenient to express radiometric signals (radiant power per unit bandwidth) as radiances having units of temperature (kelvin, or K). -
VIRTIS/Venus Express Summary
VIRTIS for Venus Express Pierre Drossart# and Giuseppe Piccioni&, December 2002 #LESIA, Obs. Paris and &IASF,Rome VIRTIS (Visible and Infrared Thermal Imaging Spectrometer) is a complex instrument initially devoted to the remote sensing study of comet Wirtanen on the Rosetta mission, at wavelengths between 0.3 and 5 mm. The focal planes, with state of the art CCD and infrared detectors achieve high sensitivity for low emissivity sources. Due to the high flexibility of the operational modes of VIRTIS, these performances are also ideally adapted for the study of Venus atmosphere, both on night and day sides. VIRTIS is therefore aimed to provide a 4- dimensional study of Venus atmosphere (2D imaging + spectral dimension + temporal variations), the spectral variations permitting a sounding at different levels of the atmosphere, from the ground up to the thermosphere. The infrared capability of VIRTIS is especially well fitted to the thermal sounding of the night side atmosphere (Taylor et al, 1997), which give a tomography of the atmosphere down to the surface. Precursors: First attempts of imaging spectrometry on the Venus night side from space in the near infrared were made by NIMS/Galileo (Figure 1) in 1990 (Carlson et al, 1990) and VIMS/Cassini in 1999 (Baines et al, 2000). These fast fly-bys gave an idea of how powerful this method of investigation could be at Venus. Unfortunately, the limited duration of the fly- bys allowed only limited investigations, in particular on the meteorological evolution of the clouds. Observation of Venus with a new generation imaging spectrometer like VIRTIS would provide a unique opportunity to continue these investigations on an extended basis. -
The Science Return from Venus Express the Science Return From
The Science Return from Venus Express Venus Express Science Håkan Svedhem & Olivier Witasse Research and Scientific Support Department, ESA Directorate of Scientific Programmes, ESTEC, Noordwijk, The Netherlands Dmitri V. Titov Max Planck Institute for Solar System Studies, Katlenburg-Lindau, Germany (on leave from IKI, Moscow) ince the beginning of the space era, Venus has been an attractive target for Splanetary scientists. Our nearest planetary neighbour and, in size at least, the Earth’s twin sister, Venus was expected to be very similar to our planet. However, the first phase of Venus spacecraft exploration (1962-1985) discovered an entirely different, exotic world hidden behind a curtain of dense cloud. The earlier exploration of Venus included a set of Soviet orbiters and descent probes, the Veneras 4 to14, the US Pioneer Venus mission, the Soviet Vega balloons and the Venera 15, 16 and Magellan radar-mapping orbiters, the Galileo and Cassini flybys, and a variety of ground-based observations. But despite all of this exploration by more than 20 spacecraft, the so-called ‘morning star’ remains a mysterious world! Introduction All of these earlier studies of Venus have given us a basic knowledge of the conditions prevailing on the planet, but have generated many more questions than they have answered concerning its atmospheric composition, chemistry, structure, dynamics, surface-atmosphere interactions, atmospheric and geological evolution, and plasma environment. It is now high time that we proceed from the discovery phase to a thorough -
VIRTIS on Venus Express: Retrieval of Real Surface Emissivity on Global Scales
VIRTIS on Venus Express: retrieval of real surface emissivity on global scales Gabriele E. Arnold*a, David Kappela, Rainer Hausb, Laura Telléz Pedrozaa, c, Giuseppe Piccionid, and Pierre Drossarte aDeutsches Zentrum für Luft- und Raumfahrt e.V. (DLR), Institute of Planetary Research, Rutherfordstrasse 2, 12489 Berlin, Germany; bWestfälische Wilhelms-Universität, Institute of Planetology, Wilhelm-Klemm-Str. 10, 48149 Münster, Germany; cUniversity Potsdam, Institute of Earth and Environmental Science, Karl-Liebknecht-Str. 24-25, 14476 Potsdam, Germany; dIstituto di Astrofisica e Planetologia Spaziali (IAPS), INAF, Via Fosso del Cavaliere 100, 00133, Roma, Italy; eLaboratoire d’Études Spatiales et d’Instrumentation en Astrophysique (LESIA), Observatoire de Paris, 5 Place Jules Janssen, 92195, Meudon, France. *[email protected]; phone +49-3067055370; fax + 49-3067055303 ABSTRACT The extraction of surface emissivity data provides the data base for surface composition analyses and enables to evaluate Venus’ geology. The Visible and InfraRed Thermal Imaging Spectrometer (VIRTIS) aboard ESA’s Venus Express mission measured, inter alia, the nightside thermal emission of Venus in the near infrared atmospheric windows between 1.0 and 1.2 µm. These data can be used to determine information about surface properties on global scales. This requires a sophisticated approach to understand and consider the effects and interferences of different atmospheric and surface parameters influencing the retrieved values. In the present work, results of a new technique for retrieval of the 1.0 – 1.2 µm – surface emissivity are summarized. It includes a Multi-Window Retrieval Technique, a Multi-Spectrum Retrieval technique (MSR), and a detailed reliability analysis. The MWT bases on a detailed radiative transfer model making simultaneous use of information from different atmospheric windows of an individual spectrum. -
Laser Video Demo on Space Station Aims to Vastly Improve Downlink Rates by Mark Whalen
Jet FEBRUARY Propulsion 2014 Laboratory VOLUME 44 NUMBER 2 Breaking the bottleneck Laser video demo on Space Station aims to vastly improve downlink rates By Mark Whalen Technicians at Kennedy Space Center unload and inspect the Optical Payload for Lasercomm Science payload after its arrival last summer. It’s scheduled to launch no earlier than March 1. Sometime in the near future, a group of young The 90-day mission is JPL’s first payload to be JPL engineers could look back on 2014 not only as mounted on the outside of the space station (two the early days of their careers but also as the time others have gone inside), and the first to launch on they were part of critical research that’s one of the a SpaceX vehicle. When the Dragon capsule docks keys to NASA’s future success. with the station, OPALS will be robotically extracted A group of about 20 JPLers in the lab’s Phaeton from the trunk of the Dragon, then manipulated by a early-career-hire program contributed to the Optical robotic arm for positioning. Payload for Lasercomm Science, or OPALS, which is The JPL experiment won’t be serviceable from its preparing for a March 1 launch from Kennedy Space outpost. OPALS could operate for up to two years, Center to the International Space Station. The goal? noted Oaida. To lay the foundation that could boost the rate at What next? If OPALS is successful, the next step which spacecraft send data to Earth by more than a would be to try to miniaturize the technology for factor of 10. -
Sources of Biases in Microwave Radiative Transfer Modelling Peter
Sources of Biases in Microwave Radiative Transfer Modelling Peter Bauer ECMWF Shinfield Park, Reading, RG2 9AX, UK [email protected] 1. Introduction Microwave satellite observations represent the most important information source for atmospheric temperature and temperature distributions in most current operational numerical weather prediction systems. At ECMWF, most data from the Advanced Microwave Sounding Unit (AMSU) instruments A and B are assimilated from four different satellites of the National Oceanic and Atmospheric Administration (NOAA) polar orbiting series (NOAA-15, 16, (17,) 18) as well as from National Aeronautic and Space NASA’s Aqua satellite. Microwave imager measurements are sensitive to integrated atmospheric moisture, surface properties as well as clouds and precipitation. While advanced infrared sounders offer better vertical resolution for sounding applications, microwave data is less affected by cloud contamination and therefore provides better data coverage. At ECMWF, microwave sounder data is operationally assimilated since 1992 (Eyre et al. 1993) and imager data (Special Sensor Microwave / Imager, SSM/I) since 1999 (Phalippou 1996, Gérard and Saunders 1999). Initially, the assimilation was performed through a 1D-Var retrieval of geophysical variables such as temperature profile or integrated moisture that were then assimilated in the global system as pseudo- observations. This procedure was later replaced by the direct assimilation of radiances in the 4D-Var system (McNally et al. 2000, Bauer et al. 2002). The radiative transfer (RT) modeling was aimed at the Tiros Operational Vertical Sounder (TOVS) data modeling (RTTOV, Eyre 1991) that developed into a general RT modeling tool-kit applicable to most available satellite sensors (Saunders et al.