Coordinate Systems ig g
Earth Ellipsoid, ellipsoidal coordinates, satellite coordinate systems
(Part I)
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MSc Geodetic Engineering
Module Coordinate Systems 1st Semester, 2020/21
Jürgen Kusche Coordinate Systems ig g
Today • Earth as a flattened body, Earth ellipsoid • Ellipsoidal coordinates and transformations • Earth’s rotation and inertial coordinate system • Kepler angles and satellite coordinate systems 2
References • Kusche J, Lecture Notes -> ecampus • Jekeli C., Geometric Reference Systems in Geodesy, Ohio State University (-> https://kb.osu.edu/handle/1811/77986) Coordinate Systems ig g
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Earth as a flattened body Coordinate Systems ig g
Some observations • Earth is not a perfect sphere. • In first approximation, it resembles a sphere flattened at the poles • Best-fitting polar radius 20 km less than equatorial radius (~ 6380km) • Therefore, in geodesy we use an ellipsoid of revolution as a reference surface → latitude, longitude and height 4
How do we know this? • History of geodesy: arc measurements, 17th and 18th century • World-wide geodetic networks, geodetic datums • Satellite observations of the (dynamical) flattening of the Earth: precession of satellite orbital plane observed already with Sputnik-1 Coordinate Systems ig g
History of geodesy: arc measurements, 17th Cassini’s Ellipsoid and 18th century
Semimajor axis
Rotation axis 5
Eccentricity parameter
Modern geodesy: Huygens’s Ellipsoid precession of satellite orbital plane Coordinate Systems ig g
Geodetic measurements enable to determine 3D positions with mm – accuracy
GPS installation for monitoring potential volcanic deformation (Japan, Photo: J. Kusche)
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Reference surfaces in geodesy require a definition precise at mm-level. → ellipsoid of revolution with • semi-major axis a • semi-minor axis b < a 7 a, b defined at sub-mm-level. Coordinate Systems ig g
Ellipsoid of revolution
Parametric description
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For an ellipsoid of revolution it is sufficient to consider the meridional ellipse, with the p-coordinate Coordinate Systems ig g
Ellipsoid of revolution
Use of other ellipsoid parameters
9 Linear eccentricity
2nd numerical eccentricity Geometrical flattening 1st numerical eccentricity Coordinate Systems ig g
Ellipsoid parameters in practice (+ derived from other parameters)
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There are several relations between the parameters, e.g. Coordinate Systems ig g
Important
• For a given ellipsoid only two parameters are independent 11 • All others are “derived” and can (and must) be computed from the two given ones with maximum precision • “Maximum precision” means all parameters must be given or computed with sufficient precision (digits) that allow transformation of coordinates with 0.1 mm accuracy. • This must be considered in particular for numerical eccentricy or flattening parameters Coordinate Systems ig g
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Earth ellipsoid
(introducing the ellipsoidal latitude) Coordinate Systems ig g
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Ellipsoidal latitude and the slope of the tangent Coordinate Systems ig g
(all derivations can be found
in lecture notes J. Kusche) 14
→ p, z
(“radius equation”) → r Coordinate Systems ig g
Ellipsoidal longitude and latitude
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N: transverse radius of curvature (radius of prime vertical)
p b 16
a Sphere
N R N = p cos B
R Coordinate Systems ig g
K N: transverse radius of curvature (radius of prime vertical) e3
Surface normal
P 17
N N
K e2
K e1 Coordinate Systems ig g
K N: transverse radius of curvature (radius of prime vertical) e 3 M: meridional radius of curvature
P 18
N M
K e2
K e1 Coordinate Systems ig g
M: meridional radius of curvature
19 Coordinate Systems ig g
6400000 m c
6380000 m N
6360000 m 20 K e3 6340000 m
6320000 m 0 45 90 P
M N Equator North Pole N = semi-major axis a N = maximum
K e1 Coordinate Systems ig g
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Ellipsoidal coordinates Coordinate Systems ig g
Ellipsoidal (also called geographical) longitude and latitude
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Exterior to the ellipsoid: Ellipsoidal longitude, latitude, and height
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Ellipsoidal longitude, latitude, and height
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Ellipsoidal longitude and latitude (“GPS-coordinates”) (e.g. ITRF)
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Always need to know • Ellipsoid parameter • Location & orientation of ellipsoid w.r.t. solid Earth = reference frame (e.g. ITRF) → lecture MGE-05 Google maps Coordinate Systems ig g
Ellipsoidal heights (GNSS) and physical heights
Ellipsoidal heights Physical heights - Geometrical reference surface - Reference surface = Geoid - GNSS-determined (i.e. from x,y,z) - Spirit levelling (+ gravity) 26
Geoid
Ellipsoid Coordinate Systems ig g
Ellipsoidal heights (GNSS) and physical heights: Geoid undulations
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Ellipsoid
Geoid Coordinate Systems ig g
Geoid (Geoid undulations = height of the Geoid above the Ellipsoid)
GFZ Potsdam
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Coordinate transformations
(for given ellipsoid parameters) Coordinate Systems ig g
Ellipsoidal coordinates → Cartesian coordinates
1. Compute N
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2. Compute x, y, z
or √ Coordinate Systems ig g
Cartesian coordinates → Ellipsoidal coordinates (I)
1. compute
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2. Since N depends on , computing latitude and height…
…requires iterative solution.
E.g. start values: Coordinate Systems ig g
Cartesian coordinates → Ellipsoidal coordinates (II)
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Terminate e.g. when |h[k+1]-h[k]|<
and R|[k+1]-[k]|<
(e.g. for =0.1 mm)
Typically 4-5 iterations sufficient. √