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Geometric Geodesy
GEODESY
Chapter III
Civil Engineering and Surveying
Department [CESD]
Properties of Reference Ellipsoid
Figure 1 show a schematic view of the reference ellipsoid
upon which meridians (curves of constant longitude λ) and
parallels (curves of constant latitude φ) form an orthogonal
network of reference curves on the surface. This allows a
point P in space to be coordinated via a normal to the
ellipsoid passing through P. This normal intersects the
surface at Q which has coordinates of λ, φ and P is at a
height h= QP above the ellipsoid surface. We say that P
has geodetic coordinates (λ, φ, h).
• The important thing at this stage is that the ellipsoid is a surface
of revolution created by rotating an ellipse about its minor axis,
where this minor axis is assumed to be either the Earth's
rotational axis, or a line in space close to the Earth's rotational
axis.
• Meridians of longitude are curves created by intersecting the
ellipsoid with a plane containing the minor axis and these curves
are ellipses; as are all curves on the ellipsoid created by
intersecting planes. Note here that parallels of latitude (including
the equator) are circles; since the intersecting plane is
perpendicular to the rotational axis, and circles are just special
cases of ellipses.
THE ELLIPSE
• The ellipse is one of the conic sections; a name derived
from the way they were first studied, as sections of a
cone.
• A right-circular cone is a solid whose surface is obtained
by rotation a straight line, called the generator, about a
fixed axis.
1. Cartesian equations of the ellipse
An ellipse is the locus of a point Pk that moves so that the sum of
the distances r and r' from two fixed points F and F' (the foci)
separated by a distance 2a is a constant and equal to the major
axis of the ellipse, i.e.,
r + r’ = 2a
a is the semi-major
b is the semi-minor
d = OF = OF’ is the focal distance
2. Parametric Equation of Ellipse
If auxiliary circles x2 + y2 = a2, and x2 + y2 = b2 are drawn on a common
origin O of an x, y coordinate system and radial lines are drawn at angles
from the x-axis; then the ellipse is the locus of points Pk that lie at the
intersection of lines, parallel with the coordinate axes, drawn through the
intersections of the radial lines and auxiliary circles.
This definition leads to the parametric equation of the ellipse. Consider
points A (auxiliary circle) and P (ellipse) on Figure 5. Using equation (4)
and the equation for the auxiliary circle of radius a we may write
Now the x- coordinates of A and P are the same and so the
right-hand sides of equations (5) may be equated, giving
Similarly, considering points B and P; using equation of
Cartesian and the equation for the auxiliary circle of radius
of b, derive the same parametric equations of ellipse.
Using parametric equation derive the Cartesian equation of
ellipse.
Geometric geodesy

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Geometric geodesy

  • 1. Geometric Geodesy GEODESY Chapter III Civil Engineering and Surveying Department [CESD]
  • 3. Figure 1 show a schematic view of the reference ellipsoid upon which meridians (curves of constant longitude λ) and parallels (curves of constant latitude φ) form an orthogonal network of reference curves on the surface. This allows a point P in space to be coordinated via a normal to the ellipsoid passing through P. This normal intersects the surface at Q which has coordinates of λ, φ and P is at a height h= QP above the ellipsoid surface. We say that P has geodetic coordinates (λ, φ, h).
  • 4. • The important thing at this stage is that the ellipsoid is a surface of revolution created by rotating an ellipse about its minor axis, where this minor axis is assumed to be either the Earth's rotational axis, or a line in space close to the Earth's rotational axis. • Meridians of longitude are curves created by intersecting the ellipsoid with a plane containing the minor axis and these curves are ellipses; as are all curves on the ellipsoid created by intersecting planes. Note here that parallels of latitude (including the equator) are circles; since the intersecting plane is perpendicular to the rotational axis, and circles are just special cases of ellipses.
  • 5. THE ELLIPSE • The ellipse is one of the conic sections; a name derived from the way they were first studied, as sections of a cone. • A right-circular cone is a solid whose surface is obtained by rotation a straight line, called the generator, about a fixed axis.
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  • 9. 1. Cartesian equations of the ellipse An ellipse is the locus of a point Pk that moves so that the sum of the distances r and r' from two fixed points F and F' (the foci) separated by a distance 2a is a constant and equal to the major axis of the ellipse, i.e., r + r’ = 2a a is the semi-major b is the semi-minor d = OF = OF’ is the focal distance
  • 10.
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  • 13. 2. Parametric Equation of Ellipse If auxiliary circles x2 + y2 = a2, and x2 + y2 = b2 are drawn on a common origin O of an x, y coordinate system and radial lines are drawn at angles from the x-axis; then the ellipse is the locus of points Pk that lie at the intersection of lines, parallel with the coordinate axes, drawn through the intersections of the radial lines and auxiliary circles. This definition leads to the parametric equation of the ellipse. Consider points A (auxiliary circle) and P (ellipse) on Figure 5. Using equation (4) and the equation for the auxiliary circle of radius a we may write
  • 14. Now the x- coordinates of A and P are the same and so the right-hand sides of equations (5) may be equated, giving
  • 15.
  • 16. Similarly, considering points B and P; using equation of Cartesian and the equation for the auxiliary circle of radius of b, derive the same parametric equations of ellipse. Using parametric equation derive the Cartesian equation of ellipse.