Nimbus-7 Earth Radiation Budget Calibration History--Part I: the Solar Channels
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TIROS 8 12/21/63 Delta-22 TIROS-H (A-53) 17B S National Aeronautics and TIROS 9 1/22/65 Delta-28 TIROS-I (A-54) 17A S Space Administration TIROS Operational 2TIROS 10 7/1/65 Delta-32 OT-1 17B S John F. Kennedy Space Center 2ESSA 1 2/3/66 Delta-36 OT-3 (TOS) 17A S Information Summaries 2 2 ESSA 2 2/28/66 Delta-37 OT-2 (TOS) 17B S 2ESSA 3 10/2/66 2Delta-41 TOS-A 1SLC-2E S PMS 031 (KSC) OSO (Orbiting Solar Observatories) Lunar and Planetary 2ESSA 4 1/26/67 2Delta-45 TOS-B 1SLC-2E S June 1999 OSO 1 3/7/62 Delta-8 OSO-A (S-16) 17A S 2ESSA 5 4/20/67 2Delta-48 TOS-C 1SLC-2E S OSO 2 2/3/65 Delta-29 OSO-B2 (S-17) 17B S Mission Launch Launch Payload Launch 2ESSA 6 11/10/67 2Delta-54 TOS-D 1SLC-2E S OSO 8/25/65 Delta-33 OSO-C 17B U Name Date Vehicle Code Pad Results 2ESSA 7 8/16/68 2Delta-58 TOS-E 1SLC-2E S OSO 3 3/8/67 Delta-46 OSO-E1 17A S 2ESSA 8 12/15/68 2Delta-62 TOS-F 1SLC-2E S OSO 4 10/18/67 Delta-53 OSO-D 17B S PIONEER (Lunar) 2ESSA 9 2/26/69 2Delta-67 TOS-G 17B S OSO 5 1/22/69 Delta-64 OSO-F 17B S Pioneer 1 10/11/58 Thor-Able-1 –– 17A U Major NASA 2 1 OSO 6/PAC 8/9/69 Delta-72 OSO-G/PAC 17A S Pioneer 2 11/8/58 Thor-Able-2 –– 17A U IMPROVED TIROS OPERATIONAL 2 1 OSO 7/TETR 3 9/29/71 Delta-85 OSO-H/TETR-D 17A S Pioneer 3 12/6/58 Juno II AM-11 –– 5 U 3ITOS 1/OSCAR 5 1/23/70 2Delta-76 1TIROS-M/OSCAR 1SLC-2W S 2 OSO 8 6/21/75 Delta-112 OSO-1 17B S Pioneer 4 3/3/59 Juno II AM-14 –– 5 S 3NOAA 1 12/11/70 2Delta-81 ITOS-A 1SLC-2W S Launches Pioneer 11/26/59 Atlas-Able-1 –– 14 U 3ITOS 10/21/71 2Delta-86 ITOS-B 1SLC-2E U OGO (Orbiting Geophysical -
Disrupted Solar Transit at 140 Mhz Over the Mexican Array Radio Telescope Due Space Weather Events
URSI AP-RASC 2019, New Delhi, India; 09 - 15 March 2019 Disrupted Solar Transit at 140 MHz over the Mexican Array Radio Telescope due Space Weather Events *Victor De la Luz(1)(2), Julio Mejia-Ambriz(1)(2), and Americo Gonzalez(2) (1) Conacyt, Servicio de Clima Espacial Mexico, Morelia, Mexico. 58190. http://www.sciesmex.unam.mx (2) Instituto de Geofisica, Unidad Michoacan, UNAM, Morelia, Mexico. 58190. Abstract Figure 2 show two solar transits centered at peak, for 22 (green line, quiet) and 26 (blue line, close to the solar flare) In this work we present the records of the disrupted so- June, 2015. We observed clearly the changes of amplitude lar transits at 140 MHz at Mexican Array Radio Telescope of the signal. (MEXART) related with active regionsand a solar flare dur- ing the week of June 20 - 26, 2015. 4 Conclusions 1 Introduction We show that space weather, in particular solar flares, mod- ifies the antenna pattern related with solar transit in the MEXART at 140 MHz. The increase in the flux saturated The transit instrument Mexican Array Radio Telescope the instrument at June 22. For this reasson, we used the 5Th (MEXART) is located in Coeneo, Mexico. Their main pro- lateral left lobe to characterize the increase of the flux. We pose is record extra-galactic radio source to observe the observed that at peak, the flux increases 16 mV in the max- interplanetary scintillation (IPS) [3]. The radio telescope imum level at June 22, 2015 compared against the baseline have central frequency of 139.65 MHz and bandwidth of 2 of the transit in quiet conditions. -
1 Comparison of Solar Evaluation Tools
COMPARISON OF SOLAR EVALUATION TOOLS: FROM LEARNING TO PRACTICE Sophia Duluk Heather Nelson Department of Architecture Department of Architecture University of Oregon University of Oregon Eugene, OR 97403 Eugene, OR 97403 Email: [email protected] Email: [email protected] Alison Kwok Department of Architecture University of Oregon Eugene, OR 97403 Email: [email protected] ABSTRACT obstacles to the use of software and a number of misunderstandings about principles and concepts of solar Solar tools and software have evolved in the last ten years to radiation. These can cause under- or overestimations, assist designers in evaluating a site for shading, solar access, leading to heavy energy consequences when handling daylighting design, photovoltaic placement, and passive building loads and thermal comfort. solar heating potential. This paper presents a comparative evaluation of solar site analysis tools as base cases for This study focuses on comparing six tools readily available evaluation. We present the results from on site to design professionals: Solar Transit (1), Solar Pathfinder measurements, software predictions, output accuracy, ease (http://www.solarpathfinder.com/index), Solmetric Suneye of use, design inputs needed for Passive House Planning (http://www.solmetric.com), HORIcatcher+Meteonorm Protocol (PHPP), and other criteria to discuss the (http://www.meteotest.ch/en/footernavi/solar_energy/horicat capabilities of the tools in education and in architectural cher/) and two iPhone applications. Additionally, the study design practice. We compare six tools: Solar Transit, Solar will examine shading protocols used for the Passive House Pathfinder + Solar Pathfinder Assistant software, Solmetric Planning Package (PHPP) to see how the tools compare to Suneye + Thermal Assistant Software, HORIcatcher + the PHPP shading assumptions, and determine the Meteonorm, and two iPhone applications. -
Satellite Data Communications Link Requirements for a Proposed Flight Simulation System
Theses - Daytona Beach Dissertations and Theses 4-1994 Satellite Data Communications Link Requirements for a Proposed Flight Simulation System Gerald M. Kowalski Embry-Riddle Aeronautical University - Daytona Beach Follow this and additional works at: https://commons.erau.edu/db-theses Part of the Aviation Commons Scholarly Commons Citation Kowalski, Gerald M., "Satellite Data Communications Link Requirements for a Proposed Flight Simulation System" (1994). Theses - Daytona Beach. 266. https://commons.erau.edu/db-theses/266 This thesis is brought to you for free and open access by Embry-Riddle Aeronautical University – Daytona Beach at ERAU Scholarly Commons. It has been accepted for inclusion in the Theses - Daytona Beach collection by an authorized administrator of ERAU Scholarly Commons. For more information, please contact [email protected]. Gerald M. Kowalski A Thesis Submitted to the Office of Graduate Programs in Partial Fulfillment of the Requirements for the Degree of Master of Aeronautical Science Embry-Riddle Aeronautical University Daytona Beach, Florida April 1994 UMI Number: EP31963 INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. UMI® UMI Microform EP31963 Copyright 2011 by ProQuest LLC All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. -
I Technical Memorandum 80704
NASA-TM-80704 19800019413 N/ A i TechnicalMemorandum 80704 Meteorological Satellites- LIBRAR, YcOPY- ._, : 3'JMm ..... HAMPVATON, L. J. Allison (Editor), A. Schnapf, B. C. Diesen, III, P. S. Martin, A. Schwalb, and W. R. Bandeen JUNE 1980 NationalAeronauticsand S0aceAdministration GoddardSpace FlightCenter Greenbelt.Maryland20771 METEOROLOGICALSATELLITES LewisJ. Allison (Editor) Goddard Space Flight Center Greenbelt, Maryland Contributing Authors: Abraham Schnapf, Bernard C. Diesen, III, Philip S. Martin, Arthur Schwalb, and WilliamR. Bandeen ABSTRACT This paper presents an overviewof the meteorologicalsatellite programs that havebeen evolvingfrom 1958 to the present and reviews plans for the future meteorological and environmental satellite systems that are scheduled to be placed into servicein the early 1980's. The development of the TIROS family of weather satellites, including TIROS, ESSA, ITOS/NOAA,and the present TIROS-N (the third-generation operational system) is summarized. The contribution of the Nimbus and ATS technology satellites to the development of the operational polar- orbiting and geostationary satellites is discussed. Included are descriptions of both the TIROS-N and the DMSPpayloadscurrently under developmentto assurea continued and orderly growth of these systemsinto the 1980's. iii CONTENTS ABSTRACT ............................................... iii EVOLUTION OF THE U.S. METEOROLOGICAL SATELLITE PROGRAMS ....... 1 TIROS ............................................... 1 ESSA ............................................... -
Using the SFA Star Charts and Understanding the Equatorial Coordinate System
Using the SFA Star Charts and Understanding the Equatorial Coordinate System SFA Star Charts created by Dan Bruton of Stephen F. Austin State University Notes written by Don Carona of Texas A&M University Last Updated: August 17, 2020 The SFA Star Charts are four separate charts. Chart 1 is for the north celestial region and chart 4 is for the south celestial region. These notes refer to the equatorial charts, which are charts 2 & 3 combined to form one long chart. The star charts are based on the Equatorial Coordinate System, which consists of right ascension (RA), declination (DEC) and hour angle (HA). From the northern hemisphere, the equatorial charts can be used when facing south, east or west. At the bottom of the chart, you’ll notice a series of twenty-four numbers followed by the letter “h”, representing “hours”. These hour marks are right ascension (RA), which is the equivalent of celestial longitude. The same point on the 360 degree celestial sphere passes overhead every 24 hours, making each hour of right ascension equal to 1/24th of a circle, or 15 degrees. Each degree of sky, therefore, moves past a stationary point in four minutes. Each hour of right ascension moves past a stationary point in one hour. Every tick mark between the hour marks on the equatorial charts is equal to 5 minutes. Right ascension is noted in ( h ) hours, ( m ) minutes, and ( s ) seconds. The bright star, Antares, in the constellation Scorpius. is located at RA 16h 29m 30s. At the left and right edges of the chart, you will find numbers marked in degrees (°) and being either positive (+) or negative(-). -
A Microwave Sounder for GOES-R: a Geostar Progress Report
A Microwave Sounder for GOES-R: A GeoSTAR Progress Report B. H. Lambrigtsen, P. P. Kangaslahti, A. B. Tanner, W. J. Wilson Jet Propulsion Laboratory – California Institute of Technology Pasadena, CA Abstract The Geostationary Synthetic Thinned Aperture Radiometer (GeoSTAR) is a new concept for a microwave sounder, intended to be deployed on NOAA’s next generation of geostationary weather satellites, GOES-R. A ground based prototype has been developed at the Jet Propulsion Laboratory, under NASA Instrument Incubator Program sponsorship, and is now undergoing tests and perform- ance characterization. The initial space version of GeoSTAR will have performance characteristics equal to those of the AMSU system currently operating on polar orbiting environmental satellites, but subsequent versions will significantly outperform AMSU. In addition to all-weather temperature and humidity soundings, GeoSTAR will also provide continuous rain mapping, tropospheric wind profiling and real time storm tracking. In particular, with the aperture synthesis approach used by GeoSTAR it is possible to achieve very high spatial resolutions even in the crucial 50-GHz tempera- ture sounding band without having to deploy the impractically large parabolic reflector antenna that is required with the conventional approach. GeoSTAR therefore represents both a feasible way of getting a microwave sounder in GEO as well as offers a clear upgrade path to meet future require- ments. GeoSTAR has a number of other advantages relative to real-aperture systems as well, such as 2D spatial coverage without mechanical scanning, system robustness and fault tolerance, operational flexibility, high quality beam formation, and open ended performance expandability. The technology and system design required for GeoSTAR are rapidly maturing, and it is expected that a space demonstration mission can be developed before the first GOES-R launch. -
What Is Sun Outage? One Problem That Can Occur with Satellite Systems
What is Sun Outage? One problem that can occur with satellite systems is what is termed a "Satellite Solar Outage" or "Sun Outage". During a solar outage it may not be possible to receive the signal from the satellite, or alternatively the signal will be degraded. Solar outages affect all satellite systems, and they are quite predictable and they arise from the basic physics behind the operation of a satellite system, and indeed any radio communications link. Satellite solar outage basics Satellite solar outages occur because the Sun (which is a powerful broadband microwave noise source) passes directly behind the satellite (when viewed from Earth) and the receiver with the beam directed towards the satellite picks up both the satellite signal and the noise from the Sun. The degree of interference caused by a satellite solar outage varies from slight signal degradation to complete loss of signal as the downlink is swamped by the noise from the Sun. For geostationary satellites, the solar outage can typically cause disruption to the received signal for a few minutes each day for a few days. The exact date, time and duration of such events depends on a variety of factors including: Receiver location Location of the particular satellite Size, or more specifically the beam width of the antenna The apparent radius of the Sun as seen from the earth (about 0.25 ). Accuracy of alignment of the antenna direction towards the satellite Parameters such as the antenna directivity can make large differences to the amount of time of the solar outage. Antennas with a very wide beam width could be affected for as much as half an hour, whereas antennas with higher gain and directivity levels as are more commonly used for satellite reception will be affected for much shorter periods of time. -
Appendix a Missions and Sensors
Appendix A Missions and Sensors This appendix contains descriptive and technical information on satellite and aircraft missions and the characteristics of their sensors. It commences by looking briefly at those programs intended principally for gathering weather information, and proceeds to missions for earth observational remote sensing, including hyperspectral and radar platforms and sensors. Sufficient detail is given on data characteristics so that implications for image processing and analysis can be understood. In most cases mechanical and signal handling properties are not given, except for a few historical and illustrative cases. A.1 Weather Satellite Sensors A.1.1 Polar Orbiting and Geosynchronous Satellites Two broad types of weather satellite are in common use. One is of the polar orbiting, or more generally low earth orbit, variety whereas the other is at geosynchronous altitudes. The former typically have orbits at altitudes of about 700 to 1500 km whereas the geostationary altitude is approximately 36,000 km (see Appendix B). Typical of the low orbit satellites are the current NOAA series (also referred to as Advanced TIROS-N, ATN), and their forerunners the TIROS, TOS and ITOS satellites. The principal sensor of interest from this book’s viewpoint is the NOAA AVHRR. This is described in Sect. A.1.2 following. The Nimbus satellites, while strictly test bed vehicles for a range of meteoro- logical and remote sensing sensors, also orbited at altitudes of around 1000 km. Nimbus sensors of interest include the Coastal Zone Colour Scanner (CZCS) and the Scanning Multichannel Microwave Radiometer (SMMR). Only the former is treated below. 390 A Missions and Sensors Geostationary meteorological satellites have been launched by the United States, Russia, India, China, ESA and Japan. -
Table of Artificial Satellites Launched in 1978
This electronic version (PDF) was scanned by the International Telecommunication Union (ITU) Library & Archives Service from an original paper document in the ITU Library & Archives collections. La présente version électronique (PDF) a été numérisée par le Service de la bibliothèque et des archives de l'Union internationale des télécommunications (UIT) à partir d'un document papier original des collections de ce service. Esta versión electrónica (PDF) ha sido escaneada por el Servicio de Biblioteca y Archivos de la Unión Internacional de Telecomunicaciones (UIT) a partir de un documento impreso original de las colecciones del Servicio de Biblioteca y Archivos de la UIT. (ITU) ﻟﻼﺗﺼﺎﻻﺕ ﺍﻟﺪﻭﻟﻲ ﺍﻻﺗﺤﺎﺩ ﻓﻲ ﻭﺍﻟﻤﺤﻔﻮﻇﺎﺕ ﺍﻟﻤﻜﺘﺒﺔ ﻗﺴﻢ ﺃﺟﺮﺍﻩ ﺍﻟﻀﻮﺋﻲ ﺑﺎﻟﻤﺴﺢ ﺗﺼﻮﻳﺮ ﻧﺘﺎﺝ (PDF) ﺍﻹﻟﻜﺘﺮﻭﻧﻴﺔ ﺍﻟﻨﺴﺨﺔ ﻫﺬﻩ .ﻭﺍﻟﻤﺤﻔﻮﻇﺎﺕ ﺍﻟﻤﻜﺘﺒﺔ ﻗﺴﻢ ﻓﻲ ﺍﻟﻤﺘﻮﻓﺮﺓ ﺍﻟﻮﺛﺎﺋﻖ ﺿﻤﻦ ﺃﺻﻠﻴﺔ ﻭﺭﻗﻴﺔ ﻭﺛﻴﻘﺔ ﻣﻦ ﻧﻘﻼ ً◌ 此电子版(PDF版本)由国际电信联盟(ITU)图书馆和档案室利用存于该处的纸质文件扫描提供。 Настоящий электронный вариант (PDF) был подготовлен в библиотечно-архивной службе Международного союза электросвязи путем сканирования исходного документа в бумажной форме из библиотечно-архивной службы МСЭ. © International Telecommunication Union Table of artificial satellites launched in 1978 COSMOS-1 012 1978 54A C0SM0S-1064 1978 119A MOLNYA-1 (40 ) 1978 55A A C0SM0S-1013 1978 56A C0SM0S-1065 1978 120A MOLNYA-1 (41) 1978 72 A COSMOS-1066 1 21A MOLNYA-1 (42) 1978 80A AMSAT-OSCAR-8 1978 26B C0SM0S-1014 1978 56B 1978 MOLNYA-3 (9) 1 978 9A ANIK-B1 1978 116A C0SM0S-1015 1978 56 C COSMOS-1067 1978 122A C0SM0S-1016 1978 56D COSMOS-1 068 1978 -
MASER: a Science Ready Toolbox for Low Frequency Radio Astronomy
MASER: A Science Ready Toolbox for Low Frequency Radio Astronomy Baptiste Cecconi1,2, Alan Loh1, Pierre Le Sidaner3, Renaud Savalle3, Xavier Bonnin1, Quynh Nhu Nguyen1, Sonny Lion1, Albert Shih3. Stéphane Aicardi3, Philippe Zarka1,2, Corentin Louis1,4, Andrée Coffre2, Laurent Lamy1,2, Laurent Denis2, Jean-Mathias Grießmeier5, Jeremy Faden6, Chris Piker6, Nicolas André4, Vincent Génot4, Stéphane Erard1, Joseph N Mafi7, Todd A King7, Jim Sky8, Markus Demleitner9 1LESIA, Observatoire de Paris, CNRS, PSL, Meudon, France, 2Station de Radioastronomie de Nançay, Observatoire de Paris, CNRS, PSL, Université d’Orléans, Nançay, France, 3DIO, Observatoire de Paris, CNRS, PSL, Paris, France. 4IRAP, CNRS, Université Paul Sabatier, CNES, Toulouse, France. 5LPC2E, CNRS, Université d’Orléans, Orléans, France. 6Dep. Physics and Astronomy, University of Iowa, Iowa City, Iowa, USA. 7IGPP, UCLA, Los Angeles, California, USA. 8Radio Sky Publishing, USA. 9Heidelberg Universität, Heidelberg, Germany. Corresponding author: Baptiste Cecconi ([email protected]) MASER (Measurements, Analysis, and Simulation of Emission in the Radio range) is a comprehensive infrastructure dedicated to time-dependent low frequency radio astronomy (up to about 50 MHz). The main radio sources observed in this spectral range are the Sun, the magnetized planets (Earth, Jupiter, Saturn), and our Galaxy, which are observed either from ground or space. Ground observatories can capture high resolution data streams with a high sensitivity. Conversely, space-borne instruments can observe below the ionospheric cut-off (at about 10 MHz) and can be placed closer to the studied object. Several tools have been developed in the last decade for sharing space physics data. Data visualization tools developed by various institutes are available to share, display and analyse space physics time series and spectrograms. -
Multilayer Modeling of the Aureole Photometry During the Venus Transit: Comparison Between SDO/HMI and Vex/SOIR Data C
A&A 595, A115 (2016) Astronomy DOI: 10.1051/0004-6361/201628528 & c ESO 2016 Astrophysics Multilayer modeling of the aureole photometry during the Venus transit: comparison between SDO/HMI and VEx/SOIR data C. Pere1,2,?, P. Tanga1, Th. Widemann2,3, Ph. Bendjoya1, A. Mahieux4,5, V. Wilquet4, and A. C. Vandaele4 1 Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS, Laboratoire Lagrange, Bvd de l’Observatoire, CS 34229, 06304 Nice Cedex 4, France e-mail: [email protected] 2 LESIA, UMR CNRS 8109, Paris Observatory, France 3 DYPAC, EA 2449, Université de Versailles-Saint-Quentin-en-Yvelines, Guyancourt, France 4 Belgian Institute for Space Aeronomy, 3 Av. Circulaire, 1180 Brussels, Belgium 5 Fonds National de la Recherche Scientifique, Brussels, Belgium Received 16 March 2016 / Accepted 12 July 2016 ABSTRACT Context. The mesosphere of Venus is a critical range of altitudes in which complex temperature variability has been extensively studied by the space mission Venus Express (VEx) during its eight-year mission (2006−2014). In particular, the Solar Occultation in the InfraRed (SOIR) instrument probed the morning and evening terminator in the 70−170 km altitude region, at latitudes extending from pole to pole, using spectroscopic multiband observations collected during occultations of the Sun at the limb. Data collected at different epochs and latitudes show evidence of short and medium timescale variability as well as latitudinal differences. Spatial and temporal variability is also predicted in mesospheric and thermospheric terminator models with lower boundary conditions at 70 km near cloud tops. Aims. The Venus transit on June 5−6, 2012 was the first to occur with a spacecraft in orbit around Venus.