Radiation Pressure Torque and Computational Attitude Modelling of Space Debris
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AATSR Frequently Asked Questions (FAQ)
AATSR Frequently Asked Questions (FAQ) Author : IDEAS+ AATSR QC Team (Telespazio VEGA UK) IDEAS+-VEG-OQC-REP-2117 Issue 3 14 December 2016 AATSR Frequently Asked Questions (FAQ) Issue 3 AMENDMENT RECORD SHEET The Amendment Record Sheet below records the history and issue status of this document. ISSUE DATE REASON 1 20 Dec 2005 Initial Issue (as AEP_REP_001) 2 02 Oct 2013 Updated with new questions and information (issued as IDEAS- VEG-OQC-REP-0955) 3 14 Dec 2016 General updates, major edits to Q37., new questions: Q17., Q25., Q26., Q28., Q32., Q38., Q39., Q48. Now issued as IDEAS+-VEG-OQC-REP-2117 TABLE OF CONTENTS 1. INTRODUCTION ........................................................................................................................ 5 1.1 The Third AATSR Reprocessing Dataset (IPF 6.05) ............................................................ 5 1.2 References ............................................................................................................................ 6 2. GENERAL QUESTIONS ........................................................................................................... 7 Q1. What does AATSR stand for? ........................................................................................ 7 Q2. What is AATSR and what does it do? ............................................................................ 7 Q3. What is Envisat? ............................................................................................................. 7 Q4. What orbit does Envisat use? ........................................................................................ -
In Brief Modified to Increase Engine Reliability
r bulletin 102 — may 2000 3rd Space Station ESA, together with a European industrial Element to be Launched consortium headed by DaimlerChrysler (D) and including Belgian, Dutch and French NASA and the Russian Aviation and partners, was responsible for the design, Space Agency (Rosaviakosmos) plan that development and delivery of the core data the next component of the International management system, which provides Space Station (ISS) – the Zvezda service Zvezda’s main computer. module – will be launched on 12 July from the Baikonur Cosmodrome in Kazakhstan. ESA also has a contract with Rosaviakosmos and RSC-Energia for Following a Joint Programme Review and performing system and interface a General Designers’ Review in Moscow, it integration tasks required for docking with was agreed that Zvezda (Russian for Zvezda by ESA’s Automated Transfer ‘star’) will be launched by a Proton rocket Vehicle (ATV), which will be used for ISS with the second and third stage engines re-boost and logistics support missions In Brief modified to increase engine reliability. from 2003 onwards. Through its ATV industrial consortium led by Aerospatiale Zvezda will provide the early living quarters Matra Lanceurs (F), ESA is also procuring for ISS crew, together with the life sup- some Russian hardware and software for port, electrical power distribution, data use with the ATV. management, flight control, and propul- sion systems for the ISS. On the scientific side, ESA has concluded contracts with Rosaviakosmos and RSC- Energia for the conduct of scientific experiments on Zvezda, including the Global Timing System (GTS) and a radiobiology experiment (called Matroshka) to monitor and analyse radiation doses in ISS crew. -
Radiation Forces on Small Particles in the Solar System T
1CARUS 40, 1-48 (1979) Radiation Forces on Small Particles in the Solar System t JOSEPH A. BURNS Cornell University, 2 Ithaca, New York 14853 and NASA-Ames Research Center PHILIPPE L. LAMY CNRS-LAS, Marseille, France 13012 AND STEVEN SOTER Cornell University, Ithaca, New York 14853 Received May 12, 1978; revised May 2, 1979 We present a new and more accurate expression for the radiation pressure and Poynting- Robertson drag forces; it is more complete than previous ones, which considered only perfectly absorbing particles or artificial scattering laws. Using a simple heuristic derivation, the equation of motion for a particle of mass m and geometrical cross section A, moving with velocity v through a radiation field of energy flux density S, is found to be (to terms of order v/c) mi, = (SA/c)Qpr[(1 - i'/c)S - v/c], where S is a unit vector in the direction of the incident radiation,/" is the particle's radial velocity, and c is the speed of light; the radiation pressure efficiency factor Qpr ~ Qabs + Q~a(l - (cos a)), where Qabs and Q~c~ are the efficiency factors for absorption and scattering, and (cos a) accounts for the asymmetry of the scattered radiation. This result is confirmed by a new formal derivation applying special relativistic transformations for the incoming and outgoing energy and momentum as seen in the particle and solar frames of reference. Qpr is evaluated from Mie theory for small spherical particles with measured optical properties, irradiated by the actual solar spectrum. Of the eight materials studied, only for iron, magnetite, and graphite grains does the radiation pressure force exceed gravity and then just for sizes around 0. -
FAME-C: Cloud Property Retrieval Using Synergistic AATSR and MERIS Observations
Atmos. Meas. Tech., 7, 3873–3890, 2014 www.atmos-meas-tech.net/7/3873/2014/ doi:10.5194/amt-7-3873-2014 © Author(s) 2014. CC Attribution 3.0 License. FAME-C: cloud property retrieval using synergistic AATSR and MERIS observations C. K. Carbajal Henken, R. Lindstrot, R. Preusker, and J. Fischer Institute for Space Sciences, Freie Universität Berlin (FUB), Berlin, Germany Correspondence to: C. K. Carbajal Henken ([email protected]) Received: 29 April 2014 – Published in Atmos. Meas. Tech. Discuss.: 19 May 2014 Revised: 17 September 2014 – Accepted: 11 October 2014 – Published: 25 November 2014 Abstract. A newly developed daytime cloud property re- trievals. Biases are generally smallest for marine stratocu- trieval algorithm, FAME-C (Freie Universität Berlin AATSR mulus clouds: −0.28, 0.41 µm and −0.18 g m−2 for cloud MERIS Cloud), is presented. Synergistic observations from optical thickness, effective radius and cloud water path, re- the Advanced Along-Track Scanning Radiometer (AATSR) spectively. This is also true for the root-mean-square devia- and the Medium Resolution Imaging Spectrometer (MERIS), tion. Furthermore, both cloud top height products are com- both mounted on the polar-orbiting Environmental Satellite pared to cloud top heights derived from ground-based cloud (Envisat), are used for cloud screening. For cloudy pixels radars located at several Atmospheric Radiation Measure- two main steps are carried out in a sequential form. First, ment (ARM) sites. FAME-C mostly shows an underestima- a cloud optical and microphysical property retrieval is per- tion of cloud top heights when compared to radar observa- formed using an AATSR near-infrared and visible channel. -
Highlights in Space 2010
International Astronautical Federation Committee on Space Research International Institute of Space Law 94 bis, Avenue de Suffren c/o CNES 94 bis, Avenue de Suffren UNITED NATIONS 75015 Paris, France 2 place Maurice Quentin 75015 Paris, France Tel: +33 1 45 67 42 60 Fax: +33 1 42 73 21 20 Tel. + 33 1 44 76 75 10 E-mail: : [email protected] E-mail: [email protected] Fax. + 33 1 44 76 74 37 URL: www.iislweb.com OFFICE FOR OUTER SPACE AFFAIRS URL: www.iafastro.com E-mail: [email protected] URL : http://cosparhq.cnes.fr Highlights in Space 2010 Prepared in cooperation with the International Astronautical Federation, the Committee on Space Research and the International Institute of Space Law The United Nations Office for Outer Space Affairs is responsible for promoting international cooperation in the peaceful uses of outer space and assisting developing countries in using space science and technology. United Nations Office for Outer Space Affairs P. O. Box 500, 1400 Vienna, Austria Tel: (+43-1) 26060-4950 Fax: (+43-1) 26060-5830 E-mail: [email protected] URL: www.unoosa.org United Nations publication Printed in Austria USD 15 Sales No. E.11.I.3 ISBN 978-92-1-101236-1 ST/SPACE/57 *1180239* V.11-80239—January 2011—775 UNITED NATIONS OFFICE FOR OUTER SPACE AFFAIRS UNITED NATIONS OFFICE AT VIENNA Highlights in Space 2010 Prepared in cooperation with the International Astronautical Federation, the Committee on Space Research and the International Institute of Space Law Progress in space science, technology and applications, international cooperation and space law UNITED NATIONS New York, 2011 UniTEd NationS PUblication Sales no. -
Section 22-3: Energy, Momentum and Radiation Pressure
Answer to Essential Question 22.2: (a) To find the wavelength, we can combine the equation with the fact that the speed of light in air is 3.00 " 108 m/s. Thus, a frequency of 1 " 1018 Hz corresponds to a wavelength of 3 " 10-10 m, while a frequency of 90.9 MHz corresponds to a wavelength of 3.30 m. (b) Using Equation 22.2, with c = 3.00 " 108 m/s, gives an amplitude of . 22-3 Energy, Momentum and Radiation Pressure All waves carry energy, and electromagnetic waves are no exception. We often characterize the energy carried by a wave in terms of its intensity, which is the power per unit area. At a particular point in space that the wave is moving past, the intensity varies as the electric and magnetic fields at the point oscillate. It is generally most useful to focus on the average intensity, which is given by: . (Eq. 22.3: The average intensity in an EM wave) Note that Equations 22.2 and 22.3 can be combined, so the average intensity can be calculated using only the amplitude of the electric field or only the amplitude of the magnetic field. Momentum and radiation pressure As we will discuss later in the book, there is no mass associated with light, or with any EM wave. Despite this, an electromagnetic wave carries momentum. The momentum of an EM wave is the energy carried by the wave divided by the speed of light. If an EM wave is absorbed by an object, or it reflects from an object, the wave will transfer momentum to the object. -
Sentinel-1A Launch
SENTINEL-1A LAUNCH Arianespace’s seventh Soyuz launch from the Guiana Space Center will orbit Sentinel-1A, the first satellite in Europe’s Earth observation program, Copernicus. The European Space Agency (ESA) chose Thales Alenia Space to design, develop and build the satellite, as well as perform related tests. Copernicus is the new name for the European program previously known as GMES (Global Monitoring for Environment and Security), and is the European Commission’s second major space program, following Galileo. Copernicus is designed to give Europe continuous, independent and reliable access to Earth observation data. With the Soyuz, Ariane 5 and Vega launchers at the Guiana Space Center (CSG), Arianespace is the only launch services provider in the world capable of launching all types of payloads into all orbits, from the smallest to the largest geostationary satellites, from satellite clusters for constellations to cargo missions for the International Space Station (ISS). Arianespace sets the launch services standard for all operators, whether commercial or governmental, and guarantees access to space for scientific missions. Sentinel-1A is the 50th satellite with an Earth observation payload to be launched by Arianespace. Arianespace has seven more Earth observation missions in its order book, including four commercial missions (signed in 2013 and 2014). The Copernicus program is designed to give Europe complete independence in the acquisition and management of environmental data concerning our planet. ESA’s Sentinel programs comprise five satellite families: Sentinel-1, to provide continuity for radar data from ERS and Envisat. Sentinel-2 and Sentinel-3, dedicated to the observation of the Earth and its oceans. -
Sentinel-3 Product Notice
Copernicus S3 Product Notice – Altimetry Mission S3 Sensor SRAL / MWR Product LAND L2 NRT, STC and NTC Product Notice ID S3A.PN-STM-L2L.10 Issue/Rev Date 16/07/2020 Version 1.1 This Product Notice was prepared by the S3 Mission Performance Centre Preparation and ESA experts Approval ESA Mission Management Summary This is a Product Notice (PN) for the Copernicus Sentinel-3A and Sentinel-3B Surface Topography Mission (STM) Level-2 Land products at Near Real Time (NRT), Short Time Critical (STC) and Non Time Critical (NTC) timeliness. The Notice describes the STM current status, product quality and limitations, and product availability status. © ESA page 1 / 16 Processing Baseline S3A S3B Processing Baseline • Processing Baseline: 2.68 • Processing Baseline: 1.42 • • SR_1 IPF version: 06.18 SR_1 IPF version: 06.18 • MW_1 IPF version: 06.11 IPFs version • MW_1 IPF version: 06.11 • • SM_2 IPF version: 06.19 SM_2 IPF version: 06.19 Current Operational Processing Baseline IPF IPF Version In OPE since S3A SR1 06.18 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 S3A MW1 06.11 Land Centres: NRT mode : 2020-01-21 STC mode : 2020-01-21 NTC mode : 2020-01-21 S3A SM2 06.19 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 S3B SR1 06.18 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 S3B MW1 06.11 Land Centres: NRT mode : 2020-01-21 STC mode : 2020-01-21 NTC mode : 2020-01-21 S3B SM2 06.19 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 © ESA page 2 / 16 Status of the Processing Baseline S3A The Processing Baseline (PB) for Copernicus Sentinel-3A STM products associated to this PN is reported above. -
Treaties and Other International Acts Series 94-1115 ______
TREATIES AND OTHER INTERNATIONAL ACTS SERIES 94-1115 ________________________________________________________________________ SPACE Cooperation Memorandum of Understanding Between the UNITED STATES OF AMERICA and CANADA Signed at Washington November 15, 1994 with Appendix NOTE BY THE DEPARTMENT OF STATE Pursuant to Public Law 89—497, approved July 8, 1966 (80 Stat. 271; 1 U.S.C. 113)— “. .the Treaties and Other International Acts Series issued under the authority of the Secretary of State shall be competent evidence . of the treaties, international agreements other than treaties, and proclamations by the President of such treaties and international agreements other than treaties, as the case may be, therein contained, in all the courts of law and equity and of maritime jurisdiction, and in all the tribunals and public offices of the United States, and of the several States, without any further proof or authentication thereof.” CANADA Space: Cooperation Memorandum of Understanding signed at Washington November 15, 1994; Entered into force November 15, 1994. With appendix. MEMORANDUM OF UNDERSTANDING between the UNITED STATES NATIONAL AERONAUTICS AND SPACE ADMINISTRATION and the CANADIAN SPACE AGENCY concerning COOPERATION IN THE FLIGHT OF THE MEASUREMENTS OF POLLUTION IN THE TROPOSPHERE (MOPITT) INSTRUMENT ON THE NASA POLAR ORBITING PLATFORM AND RELATED SUPPORT FOR AN INTERNATIONAL EARTH OBSERVING SYSTEM 2 The United States National Aeronautics and Space Administration (hereinafter "NASA") and the Canadian Space Agency (hereinafter "CSA") -
Esa Broch Envisat 2.Xpr Ir 36
ENVISAT-1 Mission & System Summary ENVISAT-1 ENVISAT-1 Mission & System Summary Issue 2 Table of contents Table Table of contents 1 Introduction 3 Mission 4 System 8 Satellite 16 Payload Instruments 26 Products & Simulations 62 FOS 66 PDS 68 Overall Development and Verification Programme 74 Industrial Organization 78 Introduction Introduction 3 The impacts of mankind’s activities on the Earth’s environment is one of the major challenges facing the The -1 mission constists of three main elements: human race at the start of the third millennium. • the Polar Platform (); • the -1 Payload; The ecological consequences of human activities is of • the -1 Ground Segment. major concern, affecting all parts of the globe. Within less than a century, induced climate changes The development was initiated in 1989 as may be bigger than what those faced by humanity over a multimission platform; the -1 payload the last 10000 years. The ‘greenhouse effect’, acid rain, complement was approved in 1992 with the final the hole in the ozone layer, the systematic destruction decision concerning the industrial consortium being of forests are all triggering passionate debates. taken in March 1994. The -1 Ground Concept was approved in September 1994. This new awareness of the environmental and climatic changes that may be affecting our entire planet has These decisions resulted in three parallel industrial considerably increased scientific and political awareness developments, together producing the overall -1 of the need to analyse and understand the complex system. interactions between the Earth’s atmosphere, oceans, polar and land surfaces. The development, integration and test of the various elements are proceeding leading to a launch of the The perspective being able to make global observations -1 satellite planned for the end of this decade. -
Synthetic Aperture Radar in Europe: ERS, Envisat, and Beyond
SYNTHETIC APERTURE RADAR IN EUROPE Synthetic Aperture Radar in Europe: ERS, Envisat, and Beyond Evert Attema, Yves-Louis Desnos, and Guy Duchossois Following the successful Seasat project in 1978, the European Space Agency used advanced microwave radar techniques on the European Remote Sensing satellites ERS-1 (1991) and ERS-2 (1995) to provide global and repetitive observations, irrespective of cloud or sunlight conditions, for the scientific study of the Earth’s environment. The ERS synthetic aperture radars (SARs) demonstrated for the first time the feasibility of a highly stable SAR instrument in orbit and the significance of a long-term, reliable mission. The ERS program has created opportunities for scientific discovery, has revolutionized many Earth science disciplines, and has initiated commercial applica- tions. Another European SAR, the Advanced SAR (ASAR), is expected to be launched on Envisat in late 2000, thus ensuring the continuation of SAR data provision in C band but with important new capabilities. To maximize the use of the data, a new data policy for ERS and Envisat has been adopted. In addition, a new Earth observation program, The Living Planet, will follow Envisat, offering opportunities for SAR science and applications well into the future. (Keywords: European Remote Sensing satellite, Living Planet, Synthetic aperture radar.) INTRODUCTION In Europe, synthetic aperture radar (SAR) technol- Earth Watch component of the new Earth observation ogy for polar-orbiting satellites has been developed in program, The Living Planet, and possibly the scientific the framework of the Earth observation programs of Earth Explorer component will include future SAR the European Space Agency (ESA). -
MONITORING of AERODYNAMIC PRESSURES for VENUS EXPRESS in the UPPER ATMOSPHERE DURING DRAG EXPERIMENTS BASED on TELEMETRY Sylvain
MONITORING OF AERODYNAMIC PRESSURES FOR VENUS EXPRESS IN THE UPPER ATMOSPHERE DURING DRAG EXPERIMENTS BASED ON TELEMETRY Sylvain Damiani(1,2), Mathias Lauer(1), and Michael Müller(1) (1) ESA/ESOC; Robert-Bosch-Str. 5, 64293 Darmstadt, Germany; +49 6151900; [email protected] (2)GMV GmbH; Robert-Bosch-Str. 7, 64293 Darmstadt, Germany; +49 61513972970; [email protected] Abstract: The European Space Agency Venus Express spacecraft has to date successfully completed nine Aerodynamic Drag Experiment Campaigns designed in order to probe the planet's upper atmosphere over the North pole. The daily monitoring of the campaign is based on housekeeping telemetry. It consists of reducing the spacecraft dynamics in order to obtain a timely evolution of the aerodynamic torque over a pericenter passage, from which estimations of the accommodation coefficient, the dynamic pressure and the atmospheric density can be extracted. The observed surprising density fluctuations on short timescales justify the use of a conservative method to decide on the continuation of the experiments. Keywords: Venus Express, Drag Experiments, Attitude Dynamics, Aerodynamic Torque. 1. Introduction The European Space Agency's Venus Express spacecraft has been orbiting around Venus since 2006, and its mission has now been extended until 2014. During the extended mission, it has already successfully accomplished 9 Aerodynamic Drag Experiment campaigns until September 2012. Each campaign aims at probing the planet’s atmospheric density at high altitude and next to the North pole by lowering the orbit pericenter (down to 165 km of altitude), and observing its perturbations on both the orbit and the attitude of the probe.