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The National Spatial Reference System Readjustment of NAD83

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The datum is the coordinate system that we use to locate ourselves on the earth ... GEOID. Earth Mass. Center. Approximately. 236 meters. Approximately. 2 meters ... – PowerPoint PPT presentation

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Title: The National Spatial Reference System Readjustment of NAD83


1
The National Spatial Reference SystemReadjustment
of NAD83
  • Chris Pearson
  • October 2005
  • Madison

2
(No Transcript)
3
Datums
Cartesian system X -2691542.5437 m Y
-4301026.4260 m Z 3851926.3688 m
  • The datum is the coordinate system that we use to
    locate ourselves on the earth
  • Involves the origin and orientation of coordinate
    axes
  • Usually the origin is near the center of mass of
    the earth
  • one axis intersects the earths surface at the
    intersection of the prime meridian and the
    equator
  • and a reference ellipsoid
  • Latitude Longitude and height

Lat Lon f 37o 23 26.38035 N l 122o 02
16.62574 W H -5.4083 m
4
WGS84, NAD83 and NAD27
NAD27
NAD83-WGS84/ITRF00

Approximately 2 meters
Earth Mass Center
GEOID
WGS84 and NAD83 share the GRS80 ellipsoid but the
origin differs by about 2m NAD27 uses the Clark
ellipsoid of 1866, the origin is 236 m from WGS84
5
Tectonic Plate Motions
6
WHAT IS ITRF AND HOW IS IT ESTABLISHED
  • ITRF stands for International Terrestrial
    Reference Frame
  • origin is at the center of mass of the whole
    Earth, including the oceans and the atmosphere
  • The datum is updated periodically. Each time
    there is a new origin, most recently with
    ITRF2000
  • Plate tectonics is accommodated by having all
    coordinates change with time.

7
Tectonic motions and NAD83
  • The earth is divided into tectonic plates in
    relative motion
  • most of the US and Canada is on one single plate
  • Allowing us to correct positions back to a stable
    North American reference frame
  • So plate motions can be ignored
  • An the advantage of NAD83

8
Adjustment tags
  • NAD83 has been readjusted periodically with most
    states having 2 or 3 adjustments
  • Each time this happens a small number of points
    are held fixed at the best values available at
    the time
  • Each readjustment will cause new coordinators for
    all points in the network.

9
Why readjust now
  • The current system with individual state
    adjustments can cause problems for projects
    crossing state lines

10
Federal Geographic Data Committee
  • The new standards require (FGDC 1998)
  • Local and network accuracy measures computed by
    random error propagation
  • This has been interpreted to mean that the local
    and network accuracies are determined by the mean
    the principal axes of the absolute and relative
    coordinate error ellipses respectively.
  • Neither of these quantities can be calculated for
    control points in the North American network
    without a full readjustment

11
Network Accuracies
  • Network accuracy of a control point
  • A value that represents the uncertainty of its
    coordinates with respect to the geodetic datum at
    the 95-percent confidence level
  • Datum is considered to be best expressed by the
    Continuous Operating Reference Stations (CORS)
  • Network accuracy values at CORS sites are
    considered to be infinitesimal (approach zero)

12
Absolute Error ellipses
  • Error ellipses area graphical representation of
    errors associated with adjusted coordinates
  • they represent the region about the computed
    position of a station where there is a particular
    probability (confidence interval) that the
    station is actually located
  • They are characterized by orientation and size of
    the principle axes
  • the size of the principle axes will increase with
    the confidence interval

13
Local Accuracies
  • Local Accuracy of a control point
  • A value that represents the uncertainty of its
    coordinates relative to other directly connected,
    adjacent control points at the 95-percent
    confidence level
  • An approximate average of the individual local
    accuracy values between this control point and
    other observed control points used to establish
    its coordinates

14
Relative error ellipses
  • Relative error ellipses show the error in point 2
    assuming that the position of point 1 is known
    precisely
  • So the only error we are considering is in the
    vector between the two points
  • Suppose we have two points

X (E2,N2)
  • Relative error ellipses represent the errors in
    the relative position between two points
  • They can be calculated regardless of whether
    observations between the points or not.

X (E1,N1)
15
National Readjustment General Comments
  • The CORS will provide the control
  • Only GPS projects will participate
  • The FBN/CBN Surveys are a key element since these
    are high accuracy (2 cm) surveys that tie the
    HARN to the CORS throughout the contiguous United
    States and provide more accurate values for the
    ellipsoid heights of most HARN stations.
  • The required free adjustment analysis of each GPS
    project that contributes to the National Spatial
    Reference System is underway.

16
  • Continuously Operating Reference Station
  • Nationwide network of GPS stations that log data
    every 30 s or better
  • Every day all data is combined and processed to
    give a independent estimate of positions
  • Can determine velocities and monitor stability by
    looking at time series
  • Control for the national readjustment

17
FBN/CBN Surveys
  • Next highest order of control
  • HARN stations
  • At least 4 hr of GPS data for each point
  • Now called B order stations

18
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19
Helmert blocking
  • developed 100 years ago by F. R. Helmert
  • a technique for breaking up a least squares
    adjustment problem into many smaller adjustments
    which can be reassembled to give the same results
    as if the adjustment was done in a single network
  • While other strategies exist for dividing a
    large survey network into manageable sized pieces
  • the method of Helmert Blocking has the crucial
    advantage of producing
  • a set of coordinates that will work together,
  • complete covariance matrix relating errors
    between all coordinates in the network

20
Helmert Blocks
  • Each state will comprise a separate block of data.

21
Time-line for National Readjustment Positions
and Ellipsoid Heights
  • All new tasks and software completed by 06/2005
  • All projects guaranteed to be included in the
    adjustment must be loaded in the database no
    later than 06/2005
  • Anticipated completion in 02/2007
  • Project Report
  • 3 months-February, 2007 through May, 2007

22
Post National Readjustment
  • A transformation model for classical non-GPS
    stations and GPS stations that were excluded from
    the National Readjustment will be needed
  • New adjustment procedures need to be developed
    that incorporate local and network accuracies
  • Areas outside the US may need to be readjusted
    (e.g. Hawaii)
  • A reference frame maintenance strategy (NAD83,
    ITRF, either or both) needs to be developed

23
Projects submitted after June 05
  • These will be added to the database using the
    current adjustment for your state
  • After the adjustment is complete,
  • These projects will be at the head of the queue
    to be added to the new adjustment
  • Using a similar procedure to that used now for
    new project submission

24
Single block adjustment of FBN
25
Estimate of coordinate shift for Illinois
  • To estimate the coordinate shift for Illinois I
    started with coordinates for the entire US FBN
  • Which were adjusted using the constraints we plan
    to use for the full adjustment
  • Compared with the existing NAD83(97) coordinates
    for Illinois

26
Implications for GIS
  • Comparing the coordinates of marks in NAD83(97)
    with the prototype national adjustment give an
    estimate of the coordinate shifts
  • Approximate shifts 0.0150.001m E and
    -0.0030.001 m N
  • Or 0.0490.002 ft E and -0.0090.003 ft N
  • 0.016 m in the vertical

  • IL HARN
    NAD83(NSRS

27
NGS Adjustment Team (1986)
NGS Adjustment Team (2005)
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