Coordinate
Systems
•   Required readings:
    • Coordinate systems:19-1 to 19-6.
    • State plane coordinate systems: 20-1 to 20-5, 20-7, 20-
      10, and 20-12.
•   Required figures:
    • Coordinate systems: 19-1, 19-2, 19-6, 19-7 and 19-8.
    • State plane coordinate systems: 20-1 to 20-3, 20-10.
    • Recommended, not required, readings: 19-7 to 19-11,
      20-11, and 20-13.
           Coordinate Systems
•   Geoid and Ellipsoid, what for?
                  Ellipsoid Parameters
•   Ellipsoid parameters (equations not required):
    •   semi-major axes (a), semi-minor axes (b)
    •   e = a 2  b 2 = first eccentricity
                  b2
                                    a
    •                              2
        N = normal length =   1 e    sin 2 
•   Great circles and meridians
•   Two main ellipsoids in North America:
    •  Clarke ellipsoid of 1866, on which NAD27 is based
     • Geodetic Reference System of 1980 (GRS80): on
       which NAD83 is based.
•   For lines up to 50 km, a sphere of equal volume can be
    used
         Geodetic Coordinate System
•   System components, coordinates
        Geodetic System Coordinates
•   Definitions :
    – Geodetic latitude (f): the angle in the meridian
        plane of the point between the equator and the normal
        to the ellipsoid through that point.
    –   Geodetic longitude (l): the angle along the equator
        between the Greenwich and the point meridians
    –   Height above the ellipsoid (h)
    Universal Space Rectangular System
              •   System definition, X, Y, Z
              •   Advantage and disadvantage
              •   X, Y, Z from geodetic coordinates
     Z
                        X = (N+h) cosf cosl
                        Y = (N+h) cosf sinl
                  Y
                        Z = ( N(1-e2) +h) sinf
X
    State Plane Coordinate Systems
•   Plane rectangular systems, why use them?
•   How to construct them: Project the earth’s
    surface onto a developable surface.
•   Two major projections: Lambert Conformal
    Conic, and Transverse Mercator.
                      Coneann.gif
      Secants, Scales, and Distortions
•   Scale is exact along the secants, smaller than
    true in between.
•   Distortions are larger away from the secants
             Choosing a Projection
•   States extending East-west: Lambert Conical
•   States extending North-South: Mercator
    Cylindrical.
•   A single surface will provide a single zone.
    Maximum zone width is 158 miles to limit
    distortions to 1:10,000. States longer than 158 mi,
    use more than one zone (projection).
     Standard Parallels & Central
              Meridians
•   Standard Parallels: the secants, no distortion
    along them. At 1/6 of zone width from zone edges
•   Central Meridians: a meridian at the middle of
    the zone, defines the direction of the Y axis.
•   The Y axis points to the grid north, which is the
    geodetic north only at the central meridian
•   To compute the grid azimuth ( from grid north)
    from geodetic azimuth ( from geodetic north):
          grid azimuth = geodetic azimuth - q
                Geodetic and SPCS
•   Control points in
    SPCS are initially
    computed from
    Geodetic
    coordinates (direct
    problem). If
    NAD27 is used the
    result is SPCS27. If
    NAD83 is used, the
    result is SPCS83.
•   Define: q, R, Rb, C,
    and how to get
    them.
    Direct and Inverse Problems
• Direct (Forward):
   • given: f, l     get X, Y?
   • Solution: X = R sin q + C
   •                Y = Rb - R cos q
   • Whenever q is used, it is -ve west (left) of the central
     meridian.
•               q = geodetic azimuth - grid azimuth
• Indirect (Inverse): Solve the above mentioned equations
  to compute R, and q. Use tables to compute f, l .
• In both cases, use a computer program whenever
  is available. Wolfpack can do it, see next slide.
  q = geodetic azimuth - grid azimuth
                 Grid N                    Grid N
        B
                      Geodetic N Geodetic N
                                               Grid Az
                                     Geodetic Az      A
                  Geodetic Az               Central Meridian of
                                            the zone
Central Meridian of Grid Az
the zone
q   : NEGATIVE at point A
    West of the CM
                                  q   POSITIVE at point A
                                      East of the CM
• Forward Computations: given (f,   l)       get (X, Y).
• Inverse Computations: given (X, Y)     get (f, l)
     Surveys Extending from one
          Zone to Another
•   There is always an overlap area between the
    zones.
•   When in the transition zone, compute the geodetic
    coordinates of two points from their X, Y in first
    zone (direct problem).
•   Compute X, Y of the same points in the second
    zone system from their geodetic coordinates
    (inverse problem)
•   Compute the azimuth of the line, use the azimuth
    and new coordinates to proceed.
Review of Project 2
    PI (V)
C
         T
    PC
                     Two vertical
             BVC 1   curves can be set-
        20
BVC 2                out at the same
                     time from either
                     BVC 1 or BVC 2.
                     The direction of
                     each of the
                     Centerlines curves
                     is shown to the
                     left. Assume that
                     the BM for
                     elevation is BVC
                     and IS NOT 20
                     Last tree
Yellow-to post