Orientation of Quickbird, Ikonos and Eros a Stereopairs by an Original Rigorous Model
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Seismic Wavefield Polarization
E3S Web of Conferences 12, 06001 (2016) DOI: 10.1051/e3sconf/20161206001 i-DUST 2016 Seismic wavefield polarization – Part I: Describing an elliptical polarized motion, a review of motivations and methods Claire Labonne1,2, a , Olivier Sèbe1, and Stéphane Gaffet2,3 1 CEA, DAM, DIF, 91297 Arpajon, France 2 Univ. Nice Sophia Antipolis, CNRS, IRD, Observatoire de la côte d’Azur, Géoazur UMR 7329, Valbonne, France 3 LSBB UMS 3538, Rustrel, France Abstract. The seismic wavefield can be approximated by a sum of elliptical polarized motions in 3D space, including the extreme linear and circular motions. Each elliptical motion need to be described: the characterization of the ellipse flattening, the orientation of the ellipse, circle or line in the 3D space, and the direction of rotation in case of non-purely linear motion. Numerous fields of study share the need of describing an elliptical motion. A review of advantages and drawbacks of each convention from electromagnetism, astrophysics and focal mechanism is done in order to thereafter define a set of parameters to fully characterize the seismic wavefield polarization. 1. Introduction The seismic wavefield is a combination of polarized waves in the three-dimensional (3D) space. The polarization is a characteristic of the wave related to the particle motion. The displacement of particles effected by elastic waves shows a particular polarization shape and a preferred direction of polarization depending on the source properties (location and characteristics) and the Earth structure. P-waves, for example, generate linear particle motion in the direction of propagation; the polarization is thus called linear. Rayleigh waves, on the other hand, generate, at the surface of the Earth, retrograde elliptical particle motion. -
Chapter 7 Mapping The
BASICS OF RADIO ASTRONOMY Chapter 7 Mapping the Sky Objectives: When you have completed this chapter, you will be able to describe the terrestrial coordinate system; define and describe the relationship among the terms com- monly used in the “horizon” coordinate system, the “equatorial” coordinate system, the “ecliptic” coordinate system, and the “galactic” coordinate system; and describe the difference between an azimuth-elevation antenna and hour angle-declination antenna. In order to explore the universe, coordinates must be developed to consistently identify the locations of the observer and of the objects being observed in the sky. Because space is observed from Earth, Earth’s coordinate system must be established before space can be mapped. Earth rotates on its axis daily and revolves around the sun annually. These two facts have greatly complicated the history of observing space. However, once known, accu- rate maps of Earth could be made using stars as reference points, since most of the stars’ angular movements in relationship to each other are not readily noticeable during a human lifetime. Although the stars do move with respect to each other, this movement is observable for only a few close stars, using instruments and techniques of great precision and sensitivity. Earth’s Coordinate System A great circle is an imaginary circle on the surface of a sphere whose center is at the center of the sphere. The equator is a great circle. Great circles that pass through both the north and south poles are called meridians, or lines of longitude. For any point on the surface of Earth a meridian can be defined. -
Chisinau,Moldova,17-21 May 2010
Chisinau,Moldova,17-21 May 2010 Azerbaijan is an independent country located at the west coast of the Caspian Sea with a population of about 9 million and a territory of 86.6 thousand square kilometers. Azerbaijan is a country of rich mineral resources, including oil and gas and is known as a miraculous country with centuries-old history and ancient culture. As its well known space activities are the priority of as so called super power countries. National Aerospace Agency (NASA) of Azerbaijan was established in 1974. NASA of Azerbaijan is the main organization among the state organizations, which officially deals with aerospace researches in the Republic. NASA of Azerbaijan carries out works in different scientific fields, including Remote Sensing, astrophysics, development of space and air borne apparatus and equipments, designing of scientific devices. NASA of Azerbaijan was established to coordinate and establish scientific and industrial base for conducting fundamental and applied investigations in space researches of the Earth and application of results in the national economy of the country. NASA’s scientific and industrial activities related with the development of theoretical principles and design works and production of the system for gathering, processing, distribution and application of remote sensing data in order to investigate natural resources, land usage, environmental monitoring and forecasting of disaster events. Chisinau,Moldova,17-21 May 2010 InstituteInstitute for for Space Space ResearchResearch Institute Institute -
Remote Sensing for Drought Monitoring & Impact Assessment
1 Remote Sensing for Drought Monitoring & Impact Assessment: Progress, Past 2 Challenges and Future Opportunities 3 4 Harry West, Nevil Quinn & Michael Horswell 5 Centre for Water, Communities & Resilience; Department of Geography & Environmental 6 Management; University of the West of EnglanD, Bristol 7 8 CorresponDing Author: Harry West ([email protected]) 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 1 24 Remote Sensing for Drought Monitoring & Impact Assessment: Progress, Past 25 Challenges and Future Opportunities 26 27 Abstract 28 Drought is a common hydrometeorological phenomenon anD a pervasive global hazarD. As 29 our climate changes, it is likely that Drought events will become more intense anD frequent. 30 Effective Drought monitoring is therefore critical, both to the research community in 31 Developing an unDerstanDing of Drought, anD to those responsible for Drought management 32 anD mitigation. Over the past 50 years remote sensing has shifteD the fielD away from 33 reliance on traditional site-baseD measurements anD enableD observations anD estimates of 34 key drought-relateD variables over larger spatial anD temporal scales than was previously 35 possible. This has proven especially important in Data poor regions with limiteD in-situ 36 monitoring stations. Available remotely senseD Data proDucts now represent almost all 37 aspects of Drought propagation anD have contributeD to our unDerstanDing of the 38 phenomena. In this review we chart the rise of remote sensing for Drought monitoring, 39 examining key milestones anD technologies for assessing meteorological, agricultural anD 40 hyDrological Drought events. We reflect on challenges the research community has faceD to 41 Date, such as limitations associateD with Data recorD length anD spatial, temporal anD 42 spectral resolution. -
A Study of Trajectory Models for Satellite Image Triangulation
265-276_07-096.qxd 2/16/10 3:36 PM Page 265 A Study of Trajectory Models for Satellite Image Triangulation In-seong Jeong and James Bethel Abstract metric camera. In common use, it generally encompasses Many Spaceborne imagery products are provided with both the internal camera geometry as well as any relevant metadata or support data having diverse types, representa- platform motions. For exploitation of a particular image, the tions, frequencies, and conventions. According to the vari- variables and parameters of that model must be assigned ability of metadata, a compatible physical sensor model numerical values, either from calibration, acquisition time approach must be constructed. Among the three components auxiliary sensors, triangulation, or some combination thereof. of the sensor model, i.e., trajectory model, projection equa- Generally, sensor models fall into two categories: models tions, and parameter subset selection, the construction of the based on the explicit physical characteristics of the system, position and attitude trajectory is closely linked with the and replacement models with generic, polynomial form availability and type of support data. In this paper, we show (RPCs), whose numerical values are obtained by means of a how trajectory models can be implemented based on support physical model. For the purposes of this paper, we will data from six satellite image types: QuickBird, Hyperion, exclude from consideration any polynomial based models SPOT-3, ASTER, PRISM, and EROS-A. Triangulation for each (rubber sheet warping) for which numerical parameters are image is implemented to investigate the feasibility and assigned without reference to a physical model. A physi- suitability of the different trajectory models. -
PVO Spinning Spacecraft Coordinates (PVO SSCC)
PVO Spinning Spacecraft coordinates (PVO_SSCC): Spacecraft coordinates (Xs, Ys, Zs) are used to describe the physical mounting locations of the Sun sensors, the star sensor, and the experiment sensors. The spacecraft coordinate system is centered at the spacecraft center of mass and rotates with the spacecraft. The Xs-Ys plane is parallel to the plane of the spacecraft equipment shelf. The positive Zs axis points out the top of the spacecraft. The positive Ys axis coincides with the split line of the equipment shelf. With no spacecraft wobble or nutation, the spacecraft positive Zs axis will coincide with the spin axis and the equipment shelf will thus be perpendicular to the spin axis. PVO Inertial Spacecraft Coordinates (PVO_ISCC): The inertial spacecraft coordinate system for the PVO spacecraft is same coordinate system as the spinning spacecraft coordinate system (SSCC) except that it does not spin with the spacecraft. Thus the Spin axis or positive Z axis direction is the same in both systems and it points out the top (toward the BAFTA assembly) of the spacecraft. The axes in the spin plane are defined as follows: The X-Z plane is defined to contain the spacecraft-Sun vector with the positive X direction being sunward, and the coordinate system is defined to be right-handed. The transformation from SSCC to ISCC is: _ _ | cos(p) -sin(p) 0 | | sin(p) cos(p) 0 | | 0 0 1 | _ _ where p is the spin phase angle measured in ISSC coordinates. Venus Solar Orbital Coordinates (VSO): The VSO coordinate system is a Cartesian coordinate system centered on Venus. -
Maximizing the Utility of Satellite Remote Sensing for the Management of Global Challenges
UN-GGIM Exchange Forum Maximizing the Utility of Satellite Remote Sensing for the Management of Global Challenges Paulo Bezerra Managing Director MDA Geospatial Services Inc. paulo@mdacorporation . com RESTRICTION ON USE, PUBLICATION OR DISCLOSURE OF PROPRIETARY INFORMATION This document contains information proprietary to MacDonald, Dettwiler and Associates Ltd., to its subsidiaries, or to a third party to which MacDonald, Dettwiler and Associates Ltd. may have a legal obligation to protect such information from unauthorized disclosure, use or duplication. Any disclosure, use or duplication of this document or of any of the information contained herein for other thanUse, the duplication,specific pur orpose disclosure for which of this it wasdocument disclosed or any is ofexpressly the information prohibited, contained except herein as MacDonald, is subject to theDettwiler restrictions and Assoon thciatese title page Ltd. ofmay this agr document.ee to in writing. 1 MDA Geospatial Services Inc. (GSI) Providing Essential Geospatial Products and Services to a global base of customers. SATELLITE DATA DISTRIBUTION DERIVED INFORMATION SERVICES Copyright © MDA ISI GeoCover Regional Mosaic. Generated Top Image - Copyright © 2002 DigitialGlobe from LANDSAT™ data. Bottom Image - RADARSAT-1 Data © CSA (()2001). Received by the Canada Centre for Remote Sensing. Processed and distributed by MDA Geospatial Services Inc. Use, duplication, or disclosure of this document or any of the information contained herein is subject to the restrictions on the title page of this document. MDA GSI - Satellite Data Distribution Worldwide distributor of radar and optical satellite data RADARSAT-2 GeoEye WorldView RapidEye USA Canada Brazil Chile RADARSAT-2 Data and Products © MACDONALD DETTWILER AND Copyright © 2011 GeoEye ASSOCIATES LTD. -
Satellite Remote Sensing and GIS Applications in Agricultural Meteorology
Satellite Remote Sensing and GIS Applications in Agricultural Meteorology Proceedings of the Training Workshop 7-11 July, 2003, Dehra Dun, India Editors M.V.K. Sivakumar P.S. Roy K. Harmsen S.K. Saha Sponsors World Meteorological Organization (WMO) India Meteorological Department (IMD) Centre for Space Science and Technology Education in Asia and the Pacific (CSSTEAP) Indian Institute of Remote Sensing (IIRS) National Remote Sensing Agency (NRSA) and Space Application Centre (SAC) AGM-8 WMO/TD No. 1182 World Meteorological Organisation 7bis, Avenue de la Paix 1211 Geneva 2 Switzerland 2004 Published by World Meteorological Organisation 7bis, Avenue de la Paix 1211 Geneva 2, Switzerland World Meteorological Organisation All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior written consent of the copyright owner. Typesetting and Printing : M/s Bishen Singh Mahendra Pal Singh 23-A New Connaught Place, P.O. Box 137, Dehra Dun -248001 (Uttaranchal), INDIA Ph.: 91-135-2715748 Fax- 91-135-2715107 E.mail: [email protected] Website: http://www.bishensinghbooks.com FOREWORD CONTENTS Satellite Remote Sensing and GIS Applications in Agricultural .... 1 Meteorology and WMO Satellite Activities – M.V.K. Sivakumar and Donald E. Hinsman Principles of Remote Sensing ......... 23 Shefali Aggarwal Earth Resource Satellites ......... 39 – Shefali Aggarwal Meteorological Satellites ......... 67 – C.M. Kishtawal Digital Image Processing ......... 81 – Minakshi Kumar Fundamentals of Geographical Information System ......... 103 – P.L.N. Raju Fundamentals of GPS ......... 121 – P.L.N. Raju Spatial Data Analysis ........ -
Users, Uses, and Value of Landsat Satellite Imagery— Results from the 2012 Survey of Users
Users, Uses, and Value of Landsat Satellite Imagery— Results from the 2012 Survey of Users By Holly M. Miller, Leslie Richardson, Stephen R. Koontz, John Loomis, and Lynne Koontz Open-File Report 2013–1269 U.S. Department of the Interior U.S. Geological Survey i U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette Kimball, Acting Director U.S. Geological Survey, Reston, Virginia 2013 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Miller, H.M., Richardson, Leslie, Koontz, S.R., Loomis, John, and Koontz, Lynne, 2013, Users, uses, and value of Landsat satellite imagery—Results from the 2012 survey of users: U.S. Geological Survey Open-File Report 2013–1269, 51 p., http://dx.doi.org/10.3133/ofr20131269. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Contents Contents ......................................................................................................................................................... ii Acronyms and Initialisms ............................................................................................................................... -
Operational Aspects of Orbit Determination with GPS for Small Satellites with SAR Payloads Sergio De Florio, Tino Zehetbauer, Dr
Deutsches Zentrum Microwave and Radar Institute für Luft und Raumfahrt e.V. Department Reconnaissance and Security Operational Aspects of Orbit Determination with GPS for Small Satellites with SAR Payloads Sergio De Florio, Tino Zehetbauer, Dr. Thomas Neff Phone: +498153282357, [email protected] Abstract Requirements Scientific small satellite missions for remote sensing with Synthetic Taylor expansion of the phase Φ of the radar signal as a Aperture Radar (SAR) payloads or high accuracy optical sensors, pose very function of time varying position, velocity and acceleration: strict requirements on the accuracy of the reconstructed satellite positions, velocities and accelerations. Today usual GPS receivers can fulfill the 4π 233 Φ==++++()t Rtap ()()01kk apttaptt ()(-) 02030 ()(-) k aptt ()(-) k ο () t accuracy requirements of this missions in most cases, but for low-cost- λ missions the decision for a appropriate satellite hardware has to take into Typical requirements, for 0.5 to 1.0 m image resolution, on account not only the reachable quality of data but also the costs. An spacecraft position vector x: analysis is carried out in order to assess which on board and ground equipment, which type of GPS data and processing methods are most −−242 appropriate to minimize mission costs and full satisfying mission payload x≤≤⋅≤⋅ 15 mmsms x 1.5 10 / x 6.0 10 / (3σ ) requirements focusing the attention on a SAR payload. These are requirements on the measurements, not on the real motion of the satellite Required Hardware Typical Position -
Platforms & Sensors
PLATFORMS & SENSORS Platform: the vehicle carrying the remote sensing device Sensor: the remote sensing device recording wavelengths of energy e.g. Aerial photography - the plane and the camera Satellite image example: Platform: Landsat (1, 5, 7 etc..) Sensor: Multispectral Sensor (MSS) or Thematic Mapper (TM) Selected satellite remote sensing systems NASA Visible Earth: long list Wim Bakker's website http://members.home.nl/wim.h.bakker http://earthobservatory.nasa.gov/IOTD/view.php?id=52174 1. Satellite orbits “Sun-synchronous” “Geostationary” Land monitoring Weather satellites ~ 700 km altitude ~ 30,000 km altitude Satellite orbits Geostationary / geosynchronous : 36,000 km above the equator, stays vertically above the same spot, rotates with earth - weather images, e.g. GOES (Geostat. Operational Env. Satellite) Sun-synchronous satellites: 700-900 km altitude, rotates at circa 81-82 degree angle to equator: captures imagery approx the same time each day (10am +/- 30 minutes) - Landsat path: earthnow Sun-synchronous Graphic: http://ccrs.nrcan.gc.ca/resource/tutor/datarecept/c1p2_e.php 700-900 km altitude rotates at ~ 81-82 ° angle to the equator (near polar): captures imagery the same time each day (10.30am +/- 30 minutes) - for earth mapping Orbit every 90-100 minutes produces similar daytime lighting Geostationary satellites capture a (rectangular) scene, sun-synchronous satellites capture a continuous swath, … which is broken into rectangular scenes. 2. Scanner types Whiskbroom (mirror/ cross-track): a small number of sensitive diodes for each band sweep perpendicular to the path or swath, centred directly under the platform, i.e. at 'nadir' e.g. LANDSAT MSS /TM Pushbroom (along-track): an array of diodes (one for each column of pixels) is 'pointed' in a selected direction, nadir or off-nadir, on request, usually 0-30 degrees (max.), e.g. -
Argentine Space Program and Regional Cooperation
Argentine Space Program and Regional Cooperation Felix Menicocci Secretary General, CONAE United Nations/Turquey/European Space Agency Workshop on “Space Technology Applications for Socio-Economic Benefits” 14 – 17 September 2010, Istambul, Turkey CONAE-National Commission on Space Activities • CONAE is a specialized agency created in May 1991 to be in charge of national space activities • It is under the authority of the Ministry of Foreign Affairs, International Trade and Worship It has a Strategic Plan: the National Space Program, issued in 1995 and revised periodically, the latest version is 2008-2015. The National Space Program The Space Program particularly emphasizes the use and scope of the concept of “Space Information Cycle ” The concept comprises the set of information from space which together with information from other sources, will have a relevant impact on certain socioeconomic activities within the country. The National Space Program Six information cycles have been defined in topics such as: agricultural, fishing and forest activities climate, hydrology and oceanography disaster management monitoring of environment and natural resources cartography, geology and mining production health applications Courses of Action Satellite Access to Missions Space CONAE Ground Information Infrastructure Systems Institutional Development Ground Infrastructure : Córdoba Space Center Ground Infrastructure : Córdoba Space Center Córdoba Space Center Córdoba Ground Station and planned antenae footprints Satellite Systems The National