Colorado Center for Astrodynamics Research The University of Colorado 1 Computation of Azimuth and Elevation George H. Born These slides describe how to.

Slides:



Advertisements
Similar presentations
MAE 5410 – Astrodynamics Lecture 5 Orbit in Space Coordinate Frames and Time.
Advertisements

ASEN 5050 SPACEFLIGHT DYNAMICS Mid-Term Review
ARO309 - Astronautics and Spacecraft Design Winter 2014 Try Lam CalPoly Pomona Aerospace Engineering.
Colorado Center for Astrodynamics Research The University of Colorado ASEN 5070 OD Accuracy Assessment OD Overlap Example Effects of eliminating parameters.
The Ellipsoid Faculty of Applied Engineering and Urban Planning
Navigation Fundamentals
Coordinate System & Time/Calendar
Based on book Datums and Map Projections for Remote Sensing, GIS and Surveying Coordinate systems for the sphere and ellipsoid Three-dimensional.
Map Projections (2/2) Francisco Olivera, Ph.D., P.E. Center for Research in Water Resources University of Texas at Austin.
Satellite geophysics. Basic concepts. I1.1a = geocentric latitude φ = geodetic latitude r = radial distance, h = ellipsoidal height a = semi-major axis,
Chapter 8 Coordinate Systems.
GTECH 201 Session 08 GPS.
Map Projections Francisco Olivera, Ph.D., P.E. Srikanth Koka
Chpt. 5: Describing Orbits By: Antonio Batiste. If you’re flying an airplane and the ground controllers call you on the radio to ask where you are and.
Modern Navigation Thomas Herring MW 10:30-12:00 Room
Satellite Communications Lecture 3
Modern Navigation Thomas Herring MW 11:00-12:30 Room
Introduction to Satellite Motion
GIS for Environmental Engineering
Geodesy, Map Projections and Coordinate Systems
AT737 Satellite Orbits and Navigation 1. AT737 Satellite Orbits and Navigation2 Newton’s Laws 1.Every body will continue in its state of rest or of uniform.
Introduction to Cartography GEOG 2016 E Lecture-3 Scale, Reference and Coordinate Systems.
Coordinate Systems in Geodesy By K.V.Ramana Murty, O. S.
Celestial Sphere. Local View On earth objects are usually viewed in flat Euclidean geometry. From the earth the stars appear to be fixed on a sphere that.
Coordinates on Earth Latitude and longitude coordinate system: Lafayette :: Lat. = 40°.5 N Long. = 87° W Greenwich, UK : Lat. = 51.5 ° N Long. = 0° W Longitudes.
ASEN 5050 SPACEFLIGHT DYNAMICS Time Systems, Conversions, f & g Prof. Jeffrey S. Parker University of Colorado – Boulder Lecture 8: Time, Conversions 1.
shops/gis/docs/projections.ppt.
Geodesy and Map Projections Geodesy - the shape of the earth and definition of earth datums Map Projection - the transformation of a curved earth to a.
Faculty of Applied Engineering and Urban Planning Civil Engineering Department Geographic Information Systems Spatial Referencing Lecture 4 Week 6 1 st.
1 Chapter 2 – Coordinate Systems Week 1.
Class 19: 3D Cartesian Coordinate Computations GISC March 2009.
University of Colorado Boulder ASEN 5070: Statistical Orbit Determination I Fall 2014 Professor Brandon A. Jones Lecture 3: Basics of Orbit Propagation.
Colorado Center for Astrodynamics Research The University of Colorado 1 STATISTICAL ORBIT DETERMINATION Error Ellipsoid B-Plane ASEN 5070 LECTURE 32 11/16/09.
MAPPING!.
Celestial Sphere. Earthly Sphere Latitude measures the number of degrees north or south of the equator. –DeKalb at 41° 55’ N Longitude measures degrees.
A Brief Introduction to Astrodynamics
Inertial Navigation System Overview – Mechanization Equation
Satellite geophysics. Basic concepts. I1.1a = geocentric latitude φ = geodetic latitude r = radial distance, h = ellipsoidal height a = semi-major axis,
Lecture 13 – Geodetic Reference Systems GISC March 2008.
ADCS Review – Attitude Determination Prof. Der-Ming Ma, Ph.D. Dept. of Aerospace Engineering Tamkang University.
ASEN 5070: Statistical Orbit Determination I Fall 2014
University of Colorado Boulder ASEN 5070: Statistical Orbit Determination I Fall 2015 Professor Brandon A. Jones Lecture 3: Time and Coordinate Systems.
EE 495 Modern Navigation Systems Navigation Mathematics Friday, January 9 EE 495 Modern Navigation Systems Slide 1 of 14.
ASEN 5050 SPACEFLIGHT DYNAMICS Two-Body Motion Prof. Jeffrey S. Parker University of Colorado – Boulder Lecture 3: The Two Body Problem 1.
AGBell -1- Build the A Train Constellation using STK Next we will use global information about the Earth to help define and understand how the A-Train.
Coordinate Transformations TM, A. Tamburro Based on Slalib docs/sun67.htx/sun67.html Tested against MACRO algorithms and.
Navigation NAU 102 Lesson 2. The Earth News Flash! It isn’t flat. But, it isn’t a perfect sphere either.
Map projections and datums
Where in the world are we? … A system for describing location on the earth What is the shape of the earth … and how earth’s shape affects the process of.
EE 495 Modern Navigation Systems Navigation Mathematics Earth Surface and Gravity Wednesday, Feb EE 495 Modern Navigation Systems Slide 1 of 14.
University of Colorado Boulder ASEN 5070: Statistical Orbit Determination I Fall 2015 Professor Brandon A. Jones Lecture 2: Basics of Orbit Propagation.
Learning from the Past, Looking to the Future James R. (Jim) Beaty, PhD - NASA Langley Research Center Vehicle Analysis Branch, Systems Analysis & Concepts.
Learning from the Past, Looking to the Future James R. (Jim) Beaty, PhD - NASA Langley Research Center Vehicle Analysis Branch, Systems Analysis & Concepts.
Celestial Mechanics III
Learning from the Past, Looking to the Future James R. (Jim) Beaty, PhD - NASA Langley Research Center Vehicle Analysis Branch, Systems Analysis & Concepts.
The Global Positioning System Rebecca C. Smyth April 17 - May 2, 2001.
Geodesy, Map Projections and Coordinate Systems Geodesy - the shape of the earth and definition of earth datums Map Projection - the transformation of.
Coordinate Systems and Map Projections
GPS Fundamentals Your location is: 37o ’ N 122o ’ W.
Spatial Referencing.
Space Mechanics.
EE 495 Modern Navigation Systems
Positional Astronomy Chapter 3 Fundamentals of Radio Interferometry
The Global Positioning System
ASEN 5050 SPACEFLIGHT DYNAMICS Intro to STK, More 2-Body
Determining Longitudes
Satellite Communications
Orbit in Space Coordinate Frames and Time
Next we will use global information about the Earth to help define and understand how the A-Train orbits the Earth.
Presentation transcript:

Colorado Center for Astrodynamics Research The University of Colorado 1 Computation of Azimuth and Elevation George H. Born These slides describe how to convert a spacecraft vector,, in ECEF or ECI coordinates to Azimuth and Elevation given geocentric latitude, east longitude, and height above the ellipsoid of a tracking station. ECEF coordinates are considered first. ECEF frame is given ECEF vector of spacecraft Station location (,, H) Geodetic latitude East longitude Height above ellipsoid

Colorado Center for Astrodynamics Research The University of Colorado 2 Computation of Azimuth and Elevation 1) Compute in the ECEF (,, ) frame and are the equatorial radius and flattening respectively of the reference ellipsoid

Colorado Center for Astrodynamics Research The University of Colorado 3 Computation of Azimuth and Elevation 2) Compute in ECEF coordinates 3) Now convert to coordinates To get replace with the coordinates of.

Colorado Center for Astrodynamics Research The University of Colorado 4 Computation of Azimuth and Elevation 4) Compute Azimuth,, and Elevation,.

Colorado Center for Astrodynamics Research The University of Colorado 5 Computation of Azimuth and Elevation 5)If the spacecraft vector is given in J2000 ECI coordinates (X, Y, Z) it is necessary to transform it into the ECEF frame. To be accurate this involves a series of five rotations to account for equatorial precession, nutation, Earth rotation, and polar motion. However, a close approximation can be obtained by only accounting for Earth rotation. This can be accomplished by computing the Greenwich sidereal time,, given by where is the rotation rate of the Earth, x rad/sec, is the angle between the ECI X-axis and the prime meridian measured in the equatorial plane, and is the value of at the reference time,. The spacecraft vector in the ECEF frame is given by Then Now proceed with step 1.

Colorado Center for Astrodynamics Research The University of Colorado 6 Computation of Azimuth and Elevation The value of at any UTC can be obtained by inserting a satellite into a scenario in STK. Set the orbit epoch and start time to the desired UTC, set the longitude of the ascending node to 0.0° and click the apply button. Then choose right ascention of the ascending node (RAAN). This will be the value of for the chosen time. Of course, one can also compute the Azimuth and Elevation in STK. For example, at universal time coordinated, UTC, JAN 1, 2008, 0 h, 0 m, 0 sec,. References: 1.Bate, Muller, and White, Fundamental of Astrodynamics, Dover, 1971, Chapter 2. 2.Curtis, H. D., Orbital Mechanics for Engineering Students, Elsevier, 2005, Chapter 5.5.