Title: Arizona Geographic Information Council 2002 AGIC Conference
1Arizona Geographic Information Council2002 AGIC
Conference
GIS without Geodesy is a FELONY!!
Dave Minkel, National Geodetic Survey NGS
Geodetic Advisor for Arizona Dave.Minkel_at_noaa.gov,
(602) 542-1569
2Workshop Outline
- Datums
- Earth Model (a.k.a. Ellipsoid)
- Horizontal Datums
- Vertical Datums
- Projections
- Geodetic control
- Transformations
- Public Land Survey System (PLSS)
- And (If theres time left)
- GPS Data Services from NGS
- GPS Update
- Future of the geodetic network
3The National Geodetic Survey- a brief overview -
- Formed in 1807 by President Jefferson
- Survey of the Coast (1807 - 1878)
- US Coast Geodetic Survey (1878 - 1970)
- Geodesy is the applied science that deals with
the size and shape of the earth. - Responsible for the establishment and maintenance
of the National Spatial Reference System (NSRS) - Geodetic Advisor program puts an NGS geodesist in
cooperating States
4ACRONYMS US
R
NAD 27
ITRF 97
GRS 80
WGS 84
NAVD 88
EGM 96
GEOID 99
NGVD 29
NAD 83
GEOID 96
5DATUMS
- A set of constants specifying the coordinate
system used for geodetic control, i.e., for
calculating coordinates of points on the Earth. - Specific geodetic datums are usually given
distinctive names. (e.g., North American Datum of
1983, European Datum of 1950, National Geodetic
Vertical Datum of 1929)
6HORIZONTAL DATUMS
- 8 Constants
- 3 specify the location of the origin of the
coordinate system. - 3 specify the orientation of the coordinate
system. - 2 specify the dimensions of the reference
ellipsoid
7VERTICAL DATUMS
- A set of fundamental elevations to which other
elevations are referred.
8Ellipsoid of RevolutionMathematical Model of the
Earth
N
b
a
S
a Semi major axis b Semi minor axis f
a-b Flattening a
9UNITED STATESELLIPSOID DEFINITIONS
BESSEL 1841 a 6,377,397.155 m 1/f
299.1528128
CLARKE 1866 a 6,378,206.4 m 1/f
294.97869821
GEODETIC REFERENCE SYSTEM 1980 - (GRS 80) a
6,378,137 m 1/f 298.257222101
WORLD GEODETIC SYSTEM 1984 - (WGS 84) a
6,378,137 m 1/f 298.257223563
10HORIZONTAL DATUMS
- BESSEL 1841 -------------- LOCAL ASTRO DATUMS
(1816-1879) -
NEW ENGLAND DATUM (1879-1901) -
U.S. STANDARD DATUM (1901-1913) -
NORTH AMERICAN DATUM (1913-1927) -
NORTH AMERICAN DATUM OF 1927 - OLD
HAWAIIAN DATUM - CLARKE 1866 PUERTO RICO DATUM
-
ST. GEORGE ISLAND - ALASKA -
ST. LAWRENCE ISLAND - ALASKA -
ST. PAUL ISLAND - ALASKA -
AMERICAN SAMOA 1962 -
GUAM 1963 - GRS80 ----------- NORTH AMERICAN DATUM OF
1983 -
(As of June 14, 1989)
11THE GEOID AND TWO ELLIPSOIDS
CLARKE 1866
GRS80 or WGS84
North America
Earth Mass Center
Approximately 236 meters
GEOID
123D Coordinate System (NAD 83 WGS 84)Geodetic
(Geographic) Coordinates
GRS80 or WGS84 Ellipsoid
Point (F,?)
Earth Mass Center
Latitude (F)
Semi-Minor Axis
Semi-Major Axis
Prime Meridian (Greenwich, England) 0o Longitude
Equator
Longitude (?)
133D Coordinate Systems (NAD 83, ITRF, WGS
84)Earth-Centered Earth-fixed (ECEF)
Z Axis (parallel to axis of rotation)
Point in Arizona (-X1, -Y1, Z)
GRS80-WGS84
Z1
Point (X1, Y1, Z1)
Z1
-Y1
Earth Mass Center
Y1
Y Axis (270o W)
-X1
X1
GEOID
X Axis (Prime Meridian)
14COMPARISON OF DATUM ELEMENTS
-
NAD 27 NAD 83 - ELLIPSOID CLARKE 1866 GRS80
- a 6,378,206.4 m
a 6,378,137. M - 1/f 294.9786982
1/f 298.257222101 - DATUM POINT Triangulation
Station
NONE - MEADES RANCH, KANSAS EARTH MASS
CENTER - ADJUSTMENT 25k
STATIONS 250k STATIONS - Several Hundred Base Lines
Appox. 30k EDMI Base Lines - Several Hundred Astro Azimuths
5k Astro Azimuths -
Doppler Point Positions -
VLBI Vectors - BEST FITTING North
America
World-Wide
15NAD 27 and NAD 83
Can you say Metadata?
16NAD83 is properly called NAD83 (1986) or NAD83
(86). In Arizona, NAD83 (HPGN), which is
ESRI-speak, is actually NAD83 (1992). The date
will change with the state whose data you are
looking at (e.g. UTAHs NAD83 (HPGN) is NAD83
(1994). NAD83 tells you the datum of the
coordinates, and the date tells you the year of
the adjustment (the coordinate set). Beginning
in 2005, NGS will readjust all GPS stations in
the network. At the end of that effort all
stations will be NAD83 (NSRS) or something
similar.
17ITRF
- International Terrestrial Reference Frame
- Defined by International Earth Rotation Service
(late 1980s) - Uses GRS80 Ellipsoid
- Has an epoch tag (ITRF88, ITRF03, etc.)
- 508 stations in 290 globally distributed sites
- GPS, VLBI, SLR, LLR, and DORIS
- Station velocities due to crustal motion are
included - Basis of all modern, high-accuracy networks
- Approximately (few centimeters) the same as WGS84
18WORLD GEODETIC SYSTEM 1984TR8350.2 World
Geodetic System 1984 - Its Definition
andRelationships with Local Geodetic
Systems(http//www.nima.mil/GandG/pubs.html)
DATUM WGS 84 RELEASED - SEPTEMBER 1987 BASED ON
OBSERVATIONS AT MORE THAN 1900 DOPPLER STATIONS
DATUM WGS 84(G730) 5 USAF GPS Tracking
Stations 5 DMA Evaluation Stations Datum
redefined with respect to the International
Terrestrial Reference Frame of 1992 (ITRF92) /-
20 cm in each component (Proceedings of the ION
GPS-94 pgs 285-292)
DATUM WGS 84(G873) 5 USAF GPS Tracking
Stations 7 NIMA Evaluation Stations Datum
redefined with respect to the International
Terrestrial Reference Frame of 1994 (ITRF94) /-
10 cm in each component (Proceedings of the ION
GPS-97 pgs 841-850)
19I NEED TO TRANSFORMBETWEEN WGS 84 AND NAD 83
Federal Register Notice Vol. 60, No. 157, August
15, 1995, pg. 42146 Use of NAD 83/WGS 84 Datum
Tag on Mapping Products
20MY SOFTWARE SAYS IM WORKING IN WGS-84
Unless you doing autonomous positioning (point
positioning /- 6-10 meters) youre probably NOT
in WGS-84
Project tied to WGS-84 control points obtained
from the Defense Department -- Good Luck!
Youre really working in the same reference frame
as your control points -- NAD 83?
21ELLIPSOID - GEOID RELATIONSHIP
H Orthometric Height / Elevation (NAVD 88)
h Ellipsoidal Height (NAD 83)
GPS gives you this, not elevation.
N Geoid Height (GEOID 03)
H h - N
H
TOPOGRAPHIC SURFACE
h
N
GEOID03
Geoid
Ellipsoid GRS80
22VERTICAL DATUMS
- MEAN SEA LEVEL DATUM OF 1929
- NATIONAL GEODETIC VERTICAL DATUM OF 1929
- NGVD 29
- (As of July 2, 1973)
- NORTH AMERICAN VERTICAL DATUM OF 1988
- NAVD 88
- (As of June 24, 1993)
23COMPARISON OF VERTICAL DATUM ELEMENTS
-
NGVD 29
NAVD 88 - DATUM DEFINITION 26 TIDE GAUGES
FATHERS POINT/RIMOUSKI -
IN THE U.S. CANADA
QUEBEC, CANADA -
- BENCH MARKS 100,000
450,000 - LEVELING (Km)
102,724
1,001,500 - GEOID FITTING Distorted to Fit
MSL Gauges Best Continental
Model -
24NGVD 29 and NAVD 88
Can you say Metadata?
25VERTCON (NGVD29 lt-gt NAVD 88)
- Similar to NADCON in operation
- Uses gridded data set
- Available as PC program or on-line (Geodetic Tool
Kit) - PC version allows file input
- Based on 381,833 datum differences
- Only for CONUS (48 conterminous)
- Accurate to approx. 4 cm (2 sigma)
- Does NOT replace differential leveling
26Projections
Arizona Geographic Information Council2002 AGIC
Conference
27Projections
- Geodesy is surveying when you cant pretend the
earth is flat J. Ross Mackay, NGS State Advisor,
KY - Conversely, a projection is an attempt to
represent points on the curved surface of the
Earth, as defined by a datum, on a flat sheet of
paper (or a monitor). A projections mapping
equations are used to transform the 3-D positions
(Lat., Long., Height) to 2-D positions (X,Y).
28TANGENT PLANE COORDINATE SYSTEM
Tangent Plane Single Point of Contact
29LAMBERT CONFROMAL CONICWITH 2 STANDARD PARALLELS
Grid Scale Factor
SCALE gt 1
Nn
SCALE EXACT
STANDARD PARALLELS
SCALE lt 1
Ns
SCALE EXACT
SCALE gt 1
80
CENTRAL MERIDIAN
30TRANSVERSE MERCATOR
SCALE lt 1
SCALE gt 1
SCALE EXACT
SCALE EXACT
SCALE gt 1
80
CENTRAL MERIDIAN
31PLANE COORDINATE SYSTEMS
- STATE PLANE AND UNIVERSIAL TRANSVERSE MERCATOR
GRID COORDINATES ARE A DIRECT MATHEMATICAL
CONVERSION FROM LATITUDE AND LONGITUDE TO A
CARTESIAN NORTHING AND EASTING (Y X) COORDINATE
SYSTEM, AND MUST MAINTAIN THE SAME DATUM TAG
e.g. NAD 83(1996) AS THE LATITUDE AND LONGITUDE
NATIONAL OCEAN SERVICE
32 UNIVERSAL TRANSVERSE MERCATOR (UTM)
- http//www.nima.mil/GandG/pubs.html
- The Universal Grids Universal Transverse
Mercator (UTM) and Universal
Polar Stereographic (UPS) - TM8358.2 - Transverse Mercator Projection
- Zones 6o Longitude World-Wide
- Northing Origin (0 meters- Northern Hemisphere)
at the Equator - Easting Origin (500,000 meters) at Central
Meridian of Each Zone - NAD 27 and NAD 83 both defined in meters
- NAD 27 to NAD 83 shift 200-225 meters for U.S.
NATIONAL OCEAN SERVICE
33 US National Grid (USNG)
- Grid Zone Designation - The U.S. is divided
into 6-degree longitudinal zones designated by a
number and 8-degree latitudinal bands designated
by a letter. Each area is given a unique
alpha-numeric Grid Zone Designator (GZD) (i.e.
18S). - Each GZD 6x8 degree area is covered by a
specific scheme of 100,000-meter squares where
each square is identified by two unique letters.
(i.e. 18SUJ - Identifies a specific 100,000-meter
square in the specified GZD). - A point position within the 100,000-meter
square shall be given by the UTM grid coordinates
in terms of its Easting (E) and Northing (N). An
equal number of digits shall be used for E and N
the reading shall be from left with Easting first
and then Northing. - 18SUJ2306 - Locates a point with a precision of 1
km - 18SUJ2348306479 - Locates a point with a
precision of 1 meter
NATIONAL OCEAN SERVICE
34 STATE PLANE COORDINATE SYSTEMS
- NOAA Manual NOS NGS - 5 State Plane Coordinate
System of 1983 http//www.ngs.noaa.gov/PUBS_LIB/M
anualNOSNGS5.pdf - Lambert Conformal Conic and Transverse Mercator
Projections - International, State and County Boundaries
- NAD 27 - Coordinates in U.S. Survey Feet
- NAD 83 - Coordinates Metric w/State Defined Foot
Conversion - 1 Meter 3.280833333 U.S. Survey Feet
- 1 Meter 3.280839895 International Feet
- NAD 27 to NAD 83 VERY large Positional Shifts
- (approx. 37.9 miles westerly in Arizona)
35- AZs SPC is a Transverse Mercator projection
-
- Zones defined by county lines
- Same zones as NAD 27
- Designed to maintain 110,000
- AZ W is 115,000
- NAD 83 AZ SPC uses International Foot
- NAD 27 used US Survey Foot
- Cannot tell foot unit by inspection
- Only 7 states use International Foot
- NAD 27 NAD 83 SP coordinates are
significantly different on purpose - Easting is much larger
- The relationship between all SPC systems is
rigorously defined (you can get there from here)
36111o 10' W
Origin 31o 00 N, 110o 10 W N 0.0 m, E
213,360.0 m
Central Meridian
37Central Meridian
111o 55 W
Origin 31o 00 N 111o 55 W N 0.0 m, E 213,
360.0 m
38Origin 31o 00 N 113o 45 W N 0.0 m E
213,360.0 m
Central Meridian
113o 45 W
Ramsey
39 COORDINATE CHANGES(STATE PLANE)
- STATION RAMSEY
- ARIZONA STATE PLANE COORDINATES (NAD 27/NAD 83
(92)) -
- Northing Easting
Converg Angle Scale Factor - (NAD 27) 969,877.379 ft. 423,771.616
ft. -0o 08 18.4 0.999939945 - (NAD 83) 295,628.663 m. 190,126.060 m.
-0o 08 20.0 0.99993999 - (969,908.37 ft) (623,771.92
ft) - (969,910.31 ft) (623,773.16
ft) - (1.94)
(1.24) - Converted using U.S. Survey
Foot, 1 M 3.2808333333 Ft. - Converted using International
Foot, 1 M 3.2808398501 Ft.
40STATUS OF NAD 27 AND NAD 83 STATE PLANE
COORDINATE LEGISLATION - APRIL, 2000
- NO SPCS EXISTING NAD 27
ENACTED NAD 83 SPC LEGISLATION LEGISLATION
LEGISLATION - (4) (3)
(45) - District of Columbia Alabama
Alaska Maryland (S)
Oklahoma (S) - Hawaii Arkansas Arizona
(I) Massachusetts (S) Oregon (I) - Nebraska Illinois
California (S) Michigan (I)
Pennsylvania (S) - Puerto Rico Colorado
(S) Minnesota Rhode Island -
Connecticut
(S) Mississippi (S) South Carolina
(I) - I International Feet and Meters
Delaware(S) Missouri
South Dakota - 1 m 3.280839895 feet Florida (S)
Montana (I) Tennessee (S) - S U.S. Survey Feet and Meters Georgia (S)
Nevada Texas (S) - 1 m 3.280833333 feet
Idaho (S) New
Hampshire Utah (I) - Indiana (S) New
Jersey Vermont -
Iowa New Mexico (S)
Virginia (S) -
Kansas New York (S)
Washington (S) -
Kentucky (S) North Carolina (S)
West Virginia -
Louisiana North Dakota (I)
Wisconsin (S) -
Maine Ohio
Wyoming -
41Datums Projections used in Arizona
Survey Data courtesy of Tom Elder, City of Phoenix
42GROUND LEVEL COORDINATES
- I want State Plane Coordinates at ground.
- Ground level coordinates are NOT State Plane
Coordinates!!!!! SPCs are defined on the
ellipsoid, not at ground.
43GROUND LEVEL COORDINATES
Distance (Grid) ? Distance (Ground)
Ground
Ellipsoid Height
Grid
44GROUND LEVEL COORDINATESPROBLEMS
- PROJECTS DIFFICULT TO TIE TOGETHER
- CONFUSION OF COORDINATE SYSTEMS
- LACK OF DOCUMENTATION
45Ground Level Coordinate Problem(s)
46GROUND LEVEL COORDINATESHow do I fix them?
- Surveyor (data source) must provide explicit
description of how ground coordinates were
determined METADATA !! - Divide the ground coordinates by the combined
factor - Combined factor scale factor X elevation factor
- Scale factor (combination of point scale factors)
- Elevation factor (20,906,000)/(20,906,000 H
N) - 20,960,000 m Mean earth radius
- H Orthometric Height (a.k.a. Elevation)
- N Geoid Height (Geoid 03)
- A common method to bring ground coordinates to
grid, but not necessarily the right method - Regionalized combined factor
- City of Scottsdale
- Explicitly specify the method of
projection/conversion in contracts - No Metadata No Hope (almost)
47GROUND LEVEL COORDINATESWhy would I want them?
- Flagstaff, AZ (Flagstaff NCMN)
- Elevation 2168 m, Geoid Height -23 m
- Scale factor 0.99990812
- Elevation Factor 0.999897408
- Combined Factor 0.999805537
- Distortion
- In ppm Combined factor 1 195 ppm
- Proportional 15128
- 2000 m (grid) 2000.4 (ground)
- 5280 ft (grid) 5281.03 ft (ground)
48Metadata for Positions/Coordinates
- METADATA IS DATA ABOUT DATA
- DATUM
- NAD 27, NAD 83(1986), NAD 83 (199X), NGVD29,
NAVD88 - UNITS
- Meters, U.S. Survey Feet, International Feet,
Chains, Rods, Pole - ACCURACY
- A, B, 1st, 2nd, 3rd, 3cm, Scaled
- SOURCE
- Surveyor, Engineer, Digitized, Scanned
- Who dun it?
49METADATA??
Horizontal Datum??
Plane Coordinate Zone ??
Units of Measure ??
How Accurate ??
50An example of good Metadata everything is stated
AND its clear and explicit! This information is
found in the legend for the drawings associated
with the project.
51Low DistortionProjections
Arizona Geographic Information Council2002 AGIC
Conference
52A method for reducingmap projection distortion
in areas of significant topographic
relief(Presented at 2003 ACSM Annual
Conference)
- Michael L. Dennis, P.E.
- Shephard-Wesnitzer, Inc.
-
- Western Australian Centre for Geodesy
- Curtin University of Technology
53Linear distortion at the ground
- Ratio of infinitesimal grid and ground lengths
at a point - Same in all directions for conformal projections
- Linear distortion, d, at a point on the ground
is computed here as - where
- k projection grid scale factor (w/respect to
ellipsoid) - h height of point above ellipsoid
- R ellipsoid radius
- Distortion expressed here in parts per million
(ppm)
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
54Cartoon Distortion due to curvature
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
55Horizontal distortion of grid coordinates due to
Earth curvature
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
56Cartoon Distortion due to change in ellipsoidal
height
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
57Distortion of grid coordinates due to variation
in ground height
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
58Cartoon Sloped terrain with respect reference
ellipsoid
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
59Cartoon Datum transformation to reduce
distortion due to change in height
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
60Cartoon Sloped projection with reduced linear
distortion
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
61Datum transformation and projection computation
results
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
62Verde Valley projection, revisited
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
63Sloped projection showing 20 ppm distortion area
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
64Conclusions
- Method can substantially reduce linear
distortion in areas of significant relief - Useful for areas and projects where ground
coordinates desired - But limited to areas of more-or-less uniform
topographic slope - Relatively simple to implement
- Can be used with any type of projection
- Datum transformation can be hidden inside
projection algorithm - Only 2 numbers needed to define transformation
(slopes north east) - Does not restrict transferability of data
- Fully reversible Can obtain original reference
geodetic coordinates - Can then re-project coordinates using any other
type of projection
Source Michael Dennis, PE Shepard Wesnitzer
Inc.
65Geodetic Control
Arizona Geographic Information Council2002 AGIC
Conference
66GEODETIC CONTROL
- NETWORK OF MONUMENTED POINTS
- PRECISELY MEASURED IN ACCORDANCE
- WITH STANDARD PROCEDURES
- MEET ACCURACY SPECIFICATIONS
- ADJUSTED TO FIT (or TIE) TOGETHER
- DOCUMENTED FOR MULTIPLE USE
67Stainless steel rod driven to refusal
Poured in place concrete post
68NATIONAL SPATIAL REFERENCE SYSTEM
- The National Spatial Reference System (NSRS) is
that component of the National Spatial Data
Infrastructure (NSDI) - http//www.fgdc.gov/nsdi/
nsdi.html which contains all geodetic control
contained in the National Geodetic Survey (NGS)
Data Base. This includes A, B, First, Second
and Third-Order horizontal and vertical control,
Geoid models such as GEOID 03, precise GPS orbits
and Continuously Operating Reference Stations
(CORS), and the National Shoreline as observed
by NGS as well as data submitted by other
Federal, State, and local agencies, Academic
Institutions and the private sector.
69NATIONAL SPATIAL REFERENCE SYSTEM
- ACCURATE -- cm accuracy on a global scale
- MULTIPURPOSE -- Supports Geodesy, Geophysics,
Land Surveying, Navigation, Mapping, Charting and
GIS activities - ACTIVE -- Accessible through Continuously
Operating Reference Stations (CORS) and derived
products (e.g. OPUS) - INTEGRATED -- Related to International services
and standards (e.g. International Earth Rotation
Service, International - GPS Service etc.)
70NAD 83 NETWORK PROBLEMS
POOR STATION ACCESSIBILITY
IRREGULAR STATION SPACING
POSITIONAL ACCURACY
71HIGH ACCURACY REFERENCE NETWORKS
- GPSABLE
- Clear Horizons for Satellite Signal Acquisition
- EASY ACCESSIBILITY
- Few Special Vehicle or Property Entrance
Requirements - REGULARLY SPACED
- Always within 20-100 Km
- HIGH HORIZONTAL ACCURACY
- A-Order (5 mm 110,000,000
- B-Order (8mm 11,000,000)
- HARN, HPGN, FBN
- Different acronyms for the same thing
72HIGH ACCURACY REFERENCE NETWORKS
73IMPROVING POSITIONAL ACCURACY
- TIME NETWORK
LOCAL - NETWORK SPAN ACCURACY ACCURACY
- NAD 27 1927-1986
10 Meters First-Order (1 part
in 0.1 million) -
- NAD 83 1986-1990
1 Meter First-Order(1
part in 0.1 million) - HARN 1987-1997
0.1 Meter B-Order(1
part in 1 million) -
A-Order (1 part in 10 million) - CORS 1994 -
0.02 Meter -
Horizontal -
0.04
Meter - Ellipsoid Height -
74GEODETIC CONTROL DATA SHEET
1 National Geodetic Survey, Retrieval
Date JULY 9, 2002 DV1145
DV1145 FBN - This is a Federal Base
Network Control Station. DV1145 DESIGNATION -
RAMSEY DV1145 PID - DV1145 DV1145
STATE/COUNTY- AZ/LA PAZ DV1145 USGS QUAD -
PLOMOSA PASS (1990) DV1145 DV1145
CURRENT SURVEY CONTROL DV1145
__________________________________________________
_________________ DV1145 NAD 83(1992)- 33 39
56.95619(N) 114 00 01.91029(W) ADJUSTED
DV1145 NAVD 88 - 475.040 (meters)
1558.53 (feet) ADJUSTED DV1145
__________________________________________________
_________________ DV1145 X -
-2,161,551.447 (meters) COMP
DV1145 Y - -4,854,803.033 (meters)
COMP DV1145 Z -
3,515,902.397 (meters) COMP
DV1145 LAPLACE CORR- 0.61 (seconds)
DEFLEC99 DV1145 ELLIP HEIGHT-
443.70 (meters) GPS
OBS DV1145 GEOID HEIGHT- -31.32
(meters) GEOID99 DV1145
DYNAMIC HT - 474.492 (meters) 1556.73
(feet) COMP DV1145 MODELED GRAV-
979,467.9 (mgal) NAVD 88
DV1145 DV1145 HORZ ORDER - A DV1145 VERT
ORDER - FIRST CLASS II DV1145 ELLP ORDER
- THIRD CLASS I
H h N 475.040 443.70 (-31.32) 475.040 ?
475.02
75GEODETIC CONTROL DATA SHEET
DV1145SPC AZ W - 295,628.663
190,126.060 MT 0.99993999 -0 08 20.0
DV1145SPC AZ C - 297,539.454 20,094.843
MT 1.00036036 -1 09 20.0 DV1145UTM 11
- 3,729,141.759 778,123.802 MT 1.00055373
1 39 49.7 DV1145UTM 12 - 3,729,144.619
221,777.758 MT 1.00055441 -1 39 51.9
DV1145 DV1145! - Elev Factor x
Scale Factor Combined Factor DV1145!SPC AZ W
- 0.99993035 x 0.99993999
0.99987034 DV1145!SPC AZ C - 0.99993035 x
1.00036036 1.00029068 DV1145!UTM 11
- 0.99993035 x 1.00055373 1.00048404
DV1145!UTM 12 - 0.99993035 x
1.00055441 1.00048472 DV1145
DV1145-------------------------------------------
-------------------------- DV1145 PID
Reference Object Distance
Geod. Az DV1145
dddmmss.s
DV1145 DV1143 RAMSEY RM 1
7.630 METERS 01835 DV1145 DV1147
RAMSEY AZ MK
0680936.4 DV1145 DV1974 LOS ANGELES PHOENIX
AWY BCN 25 APPROX.10.0 KM 1563949.0
DV1145 DV1144 RAMSEY RM 2
11.039 METERS 16926 DV1145--------------
--------------------------------------------------
----- DV1145 DV1145
SUPERSEDED SURVEY CONTROL DV1145 DV1145 ELLIP
H (09/30/92) 443.72 (m)
GP( ) 2 1 DV1145 NAD 83(1986)- 33 39
56.95198(N) 114 00 01.91873(W) AD( ) 2
DV1145 NAD 27 - 33 39 56.84800(N) 113
59 59.12850(W) AD( ) 2 DV1145 NAVD 88
(09/30/92) 475.04 (m) 1558.5 (f)
LEVELING 3 DV1145 NGVD 29 (??/??/92)
474.334 (m) 1556.21 (f) ADJ UNCH 1 2
76GEODETIC CONTROL DATA SHEET
- DV1145 HISTORY - Date Condition
Report By - DV1145 HISTORY - 1949 MONUMENTED
CGS - DV1145 HISTORY - 1962 GOOD
CGS - DV1145 HISTORY - 1962 GOOD
NGS - DV1145 HISTORY - 1965 GOOD
CGS - DV1145 HISTORY - 1971 GOOD
USE - DV1145 HISTORY - 1981 GOOD
NGS - DV1145 HISTORY - 1981 GOOD
NGS - DV1145 HISTORY - 1981 GOOD
NGS - DV1145 HISTORY - 1985 GOOD
AZDT - DV1145 HISTORY - 19920203 GOOD
NGS - DV1145 HISTORY - 19960306 GOOD
CHANCE - DV1145 HISTORY - 19981111 GOOD
NGS - DV1145 HISTORY - 19981117 GOOD
AZ-013 - DV1145
- DV1145 STATION
DESCRIPTION - DV1145
- DV1145'DESCRIBED BY COAST AND GEODETIC SURVEY
1949 (DHK) - DV1145'STATION LOCATED ABOUT 17 MILES AIR LINE
WEST OF HOPE, 13
77GEODETIC CONTROL DATA SOURCES
- NGS web site www.ngs.noaa.gov/datasheet.html
- on-line search for control and generates data
sheets (text search) - SDTS (Spatial Data Transfer Standard) format for
import of data into GIS software (very large
files) - Shapefiles coming soon
- State Cartographers website -
http//sco.az.gov/ngs.htm - DSWIN software data files (by county)
- used to search for control and generate data
sheets (text search) - used to generate text files for import into GIS
software - used to generate text files for import into GPS
receivers - Arizona GeoServer - sco.az.gov/website/geoserver
/ - on-line search for control and generate data
sheets with a GUI
78NEW STANDARDS FOR GEODETIC CONTROL
- Two accuracy standards
- (http//fgdc.er.usgs.gov/standards/status/swgstat.
html) - local accuracy ------------- adjacent
points - network accuracy ---------- relative to CORS
- Numeric quantities, units in cm (or mm)
- Both are relative accuracy measures
- Do not use distance dependent expression
- Horizontal accuracies are radius of 2-D 95 error
circle - Ellipsoidal/Orthometric heights are 1-D (linear)
95 error
79Datum Transformations
Arizona Geographic Information Council2002 AGIC
Conference
80DATUM TRANSFORMATIONS
- 1. WHAT DATUM ARE THE EXISTING COORDINATES ON?
- 2. WHAT DATUM DO I WANT THE NEW COORDINATES ON?
- 3. HOW LARGE A GEOGRAPHICAL AREA DO I WANT TO
CONVERT AT ONE TIME? - 4. HOW MANY POINTS ARE COMMON TO BOTH DATUMS?
- 5. WHAT IS THE DISTRIBUTION OF THE COMMON
POINTS? - 6. HOW ACCURATE ARE THE EXISTING COORDINATES?
- 0.1 Foot
- 1.0 Foot
- 10. Feet
- 7. HOW ACCURATE DO I WANT THE NEW COORDINATES?
81DATUM TRANSFORMATION IDEAL METHOD
- SATISFIES ALL USERS REQUIREMENTS
- CAPABLE OF TRANSFORMING LARGE HOLDINGS OF
COORDINATE DATA - NEAR-REAL TIME APPLICATIONS
- SIMPLE - METHOD SHOULD NOT REQUIRE AN EXPERT OR
EXPERT DECISIONS TO BE MADE - ACCURATE
82DATUM TRANSFORMATIONS
- MOLODENSKY
- Converts latitude, longitude and ellipsoidal
height to X,Y,Z Earth-Centered Coordinates. - Applies a 3-dimensional change in the origin (dX,
dY,dZ) - Applies a change in the size and shape of the
reference ellipsoid - Converts new X,Y,Z Earth-Centered Coordinates
back to latitude, longitude and ellipsoidal
height
83DATUM TRANSFORMATIONS
- MOLODENSKY
- For continental regions accuracy can be /- 8
to 10 meters - Does not model network distortions very well.
- Assumes heights in both systems are ellipsoidal
(NAD 27 did not have ellipsoidal heights).
84MOLODENSKY TRANSFORMATION
(http//www.nima.mil/GandG/pubs.html)
85NADCON
- DESIGNED TO SATISFY THE MAJORITY OF THE IDEAL
METHOD DESIGN AND IS DEFINED AS THE NATIONAL
STANDARD. - DESIGN CRITERIA
- Relies only on NGS archived data existing in both
NAD 27 and NAD 83 - Not tied to NGS Data Base
- Provides consistent results, both forward and
inverse - Fast
- Small - Fits on a PC
- Accurate
- 15 cm (1 sigma) in Conterminous U.S. NAD 27 -
NAD 83 (1986) - 5 cm (1 sigma) per State/Region NAD 83 (1986) -
HARN
Federal Register Notice Vol. 55, No. 155, August
10, 1990, pg. 32681 Notice to Adopt Standard
Method for Mathematical Horizontal Datum
Transformation
86How does NADCON work?
N 0.12344 8 -1.87842
N 0.12249 8 -1.88963
Set of gridded NAD-27 network distortion factors
Positional error due To distortion
N 0.12423 8 -1.81246
N 0.12568 8 -1.83364
N 0.12449 8 -1.88905
NSRS survey station
N 0.12640 8 -1.85407
N 0.12499 8 -1.86543
87 COORDINATE COMPARISONNAD 27 to NAD 83(1992)
- ADJUSTED vs. TRANSFORMED
- Station RAMSEY
- LATITUDE
LONGITUDE - 33-39-56.95619 114-00-01.91029
PUBLISHED (NAD83 (92)) - 33-39-57.01410
114-00-01.92238 - MOLODENSKY - 0
.05791 0.01209 -
1.784 m 0.312 m - THIS CORRESPONDS TO A POSITIONAL
- DIFFERENCE OF 1.811 m (5.94 ft)
88 COORDINATE COMPARISON NAD 27 to NAD
83(1992)
- NADCON
- http//www.ngs.noaa.gov/TOOLS/NADCON
- ADJUSTED vs. TRANSFORMED
- Station RAMSEY
-
LATITUDE LONGITUDE -
33-39-56.95619 114-00-01.91029 - PUBLISHED -
33-39-56.95626 114-00-01.90498 - NADCON -
.0007 .00531 -
0.002 m 0.137 m - THIS CORRESPONDS TO A POSITIONAL
- DIFFERENCE OF 0.137 m (0.45 ft)
89 COORDINATE COMPARISONNAD 27 to NAD 83(1996)
- ADJUSTED vs. TRANSFORMED
- Station RED STONE
- LATITUDE
LONGITUDE - 44-28-13.93221
073-11-46.77900 - PUBLISHED - 44-28-13.75032
073-11-46.60413 - MOLODENSKY -
.18189 .17487 -
5.614 m 3.865 m - THIS CORRESPONDS TO A POSITIONAL
- DIFFERENCE OF 6.816 m (22.36 ft)
90 COORDINATE COMPARISON NAD 27 to NAD
83(1996)
- NADCON
- ADJUSTED vs. TRANSFORMED
- Station RED STONE
-
LATITUDE LONGITUDE - 44-28-13.93221
073-11-46.77900 - PUBLISHED - 44-28-13.93057
073-11-46.77912 - NADCON -
.00164 .00012 -
0.051 m 0.003 m - THIS CORRESPONDS TO A POSITIONAL
- DIFFERENCE OF 0.051m (0.17 ft)
91GPS Positions What datum are they on?
- Autonomous GPS
- - WGS84 (almost ITRF)
- US Coast Guard DGPS (a.k.a. beacon)
- - NAD83
- FAA WAAS DGPS
- - ITRF (200?)
- Differentially corrected GPS
- - What Datum is the reference station on?
-
92Public Land Survey System (PLSS)
Arizona Geographic Information Council2002 AGIC
Conference
93Public Land Survey System
- A rectangular coordinate system based on a
somewhat arbitrary point (Initial Point) - Did not have geographic positions as part of the
system - A system to support land ownership or conveyance
not mapping - Depiction on USGS quads may or may not be based
on field verification - ALRIS source is digitized USGS Quads
94Public Land Survey SystemGeographic Coordinate
Data Base (GCDB)
- Maintained by BLM on a state by state basis
- Current lack of national policy
- Might be on NAD 27 or NAD 83
- NOT a legal depiction of the corner location
- Average of all available positions
- Available at www.blm.gov/gcdb/
95PLSS corner accuracy
Position comparison courtesy of Tim Smothers,
City of Peoria
96AZ/CA Boundary Project Yuma Area
97GPS Data Sources and Services from NGS
Arizona Geographic Information Council2002 AGIC
Conference
98Geodetic Tool Kit
www.ngs.noaa.gov/TOOLS/
99CONTINUOUSLY OPERATING REFERENCE STATIONS (CORS)
- Variety of Geodetic Quality Dual-Frequency
- Antennas and Receivers
- Allen-Osborne
- (SNR 8000 SNR 12 ACT)
- Ashtech
- (UZ-12, Z-XII3)
- Leica
- (SR9500 CRS1000, LEIAT5, RS500)
- Trimble
- (4000SS, 4700, 5700)
CHL1 - CAPE HENLOPEN, DE
100(No Transcript)
101CONTINUOUSLY OPERATING REFERENCE STATIONS (CORS)
- Some stations broadcast real-time correctors
- 1- 5 - 15 30 sec. post-process carrier phase
observations - Free access via Internet (RINEX-2 Format)
- More than 285 Station National Network
102CONTINUOUSLY OPERATING REFERENCE STATIONS (CORS)
- NGS PROVIDES
- Reference Site Survey Monumentation
- Horizontal and Vertical NSRS Connections
- NAD 83, ITRF94, ITRF96, ITRF97, ITRF00
Coordinates - Network Data Collection - Hourly Daily
- Daily 3D Network Integrity Adjustment
- Public Data Distribution - Internet
- (http//www.ngs.noaa.gov/CORS/cors-data.html)
- 7 Year On-Line Data Holding
103(No Transcript)
104(No Transcript)
105(No Transcript)
106CORS DATA SHEET
- ITRF 00 NAVAL STATION NEW
(NPRI), RHODE ISLAND Retrieved from NGS
DataBase on 04/06/02 at 181130.
__________________________________________________
__________________________
Antenna Reference Point(ARP)
NAVAL STATION NEW CORS ARP
--------------------------------------------------
------
PID AI3285
ITRF00 POSITION (EPOCH 1997.0)
Computed
in Aug. 2001 using every third day of data
through 2000. X 1531392.471
m latitude 41 30 35.44671 N
Y -4531474.016 m longitude
071 19 39.12747 W Z
4204982.604 m ellipsoid height -13.015 m
ITRF00 VELOCITY
Predicted with
HTDP_2.5 in Aug. 2001.
VX -0.0165 m/yr
northward 0.0044 m/yr
VY -0.0025 m/yr eastward
-0.0164 m/yr VZ
0.0033 m/yr upward 0.0000 m/yr
107CORS DATA SHEET
- NAD 83
-
NAD_83 POSITION
(EPOCH 2002.0)
Transformed from ITRF00 (epoch
1997.0) position in Mar. 2002.
X 1531393.023 m latitude 41 30
35.41588 N Y
-4531475.481 m longitude 071 19 39.12515
W Z 4204982.718 m
ellipsoid height -11.768 m
NAD_83 VELOCITY
Transformed from ITRF00 velocity in
Mar. 2002. VX
0.0005 m/yr northward -0.0014 m/yr
VY -0.0006 m/yr
eastward 0.0003 m/yr
VZ -0.0012 m/yr upward
-0.0002 m/yr
_______________________________________________
_____________________________
108OPUS WHAT IS IT?
- On-line Positioning User Service
- Provides GPS users faster easier access to the
National Spatial Reference System (NSRS)
109OPUS What Do I need?
- Dual Frequency GPS (carrier phase) data
- Resource-grade GPS unit probably NOT suitable
- Stationary antenna (no kinematic data)
- Single station no networks
- Data rates of 1, 2, 3, 5, 6, 10, 15 or 30
seconds - At least 2 hours of GPS data
- RINEX generator (software)
- Converts GPS data from manufacturers format to
industry standard format - TEQC free from UNAVCO
- http//www.unavco.ucar.edu/data_support/softwa
re/translation/translation.html
110OPUS How do I use it?
- Go to OPUS web page www.ngs.noaa.gov/OPUS
- Enter your email address
- Use browse feature to select RINEX file on your
computer - Select antenna type from menu
- Enter antenna height in meters
- Option to select State Plane Zone
- Click UPLOAD
- Check your email in a few minutes
111OPUS What do I get?
REF FRAME NAD83(CORS96)(EPOCH2002.0000)
ITRF97 (EPOCH2000.2843) X
-1933229.787(m) 0.006(m)
-1933230.343(m) 0.110(m)
Y -5043636.636(m) 0.022(m)
-5043635.169(m)
0.192(m) Z 3381904.220(m)
0.038(m)
3381904.084(m) 0.151(m) LAT 32
13 28.02620 0.023(m)
32 13 28.04274 0.011(m) E
LON 249 1 41.28058 0.012(m)
249 1 41.24070
0.040(m) W LON 110 58 18.71942
0.012(m) 110 58
18.75930 0.040(m) EL HGT
734.110(m) 0.036(m)
733.047(m) 0.265(m) ORTHO
HGT 763.270(m) 0.044(m) Geoid99
NAVD88 UTM Zone 12
SPC Zone
202(AZ) NORTHING 3565315.261(m)
NORTHING 136145.249(m)
EASTING 502650.865(m)
EASTING 302411.814(m)
112GPS Update Whats upfor the Future?
Arizona Geographic Information Council2002 AGIC
Conference
113Autonomous Positioning Before May 1, 2000
25-100 m
HORIZONTAL 100 meters
VERTICAL 156 meters
1996 Federal Radionavigation Plan Section A2-1,
Part B http//www.navcen.uscg.mil/policy/frp1996
- C/A Code on L1
- Selective Availability
114Standalone Positioning Since May 1, 2000
6-11 m
- C/A Code on L1
- No Selective Availability
115Standalone Positioning By 2011
Better resistance to interference
1-3 m
- C/A Code on L1
- C/A Code on L2
- New Code on L5
116GLOBAL POSITIONING SYSTEM
- GPS BLOCK III
- Potential Future Developments
- http//206.65.196.30/gps/issues/dotgpspressrelease
s.htm - 30 - 32 satellites
- Second and Third Civil Frequency
- (1227.60 MHZ 1176.45 MHZ)
- More Robust Signal Transmissions
- Real-Time Unaugmented 1 Meter Accuracy
- Initial Launches 2005
- Complete Replacements 2011
117GLOBAL NAVIGATION SATELLITE SYSTEMS(GNSS)
- POTENTIAL FUTURE DEVELOPMENTS
- (2005 - 2011)
- GPS MODERNIZATION - BLOCK III
- GLONASS ENHANCEMENTS (K M)
- EUROPEAN UNION - GALILEO
- 80 Satellites
- Second and Third Civil Frequency - GPS
- No Signal Encryption - GLONASS GALILEO
- More Robust Signal Transmissions
- Real-Time Unaugmented 1 Meter (or better!)
Accuracy
118The NETWORK Whats upfor the Future?
Arizona Geographic Information Council2002 AGIC
Conference
119NAD 83 READJUSTMENT
- HARN COMPLETION - SEPTEMBER 1997
- (Indiana)
- GPS HEIGHT MODERNIZATION OBSERVATIONS
- (1997 - 2003)
- (http//www.ngs.noaa.gov/initiatives/height_modern
ization.shtml - COMPLETE GPS NAD 83 3-D ADJUSTMENT
- (http//www.ngs.noaa.gov/initiatives/new_reference
.shtml) - (2004-05)
- REMOVAL OF SMALL REGIONAL DISTORTIONS
- (3 - 6 CM)
- UNIFORM COORDINATE TAG
- NAD 83 (NSRS)
120NAD 83 READJUSTMENT
121NAD 83 READJUSTMENT
- ONLY GPS DATA
- CONTINUOUSLY OPERATING REFERENCE STATIONS
- FEDERAL BASE NETWORK
- COOPERATIVE BASE NETWORK
- AIRPORT SURVEYS
- USER DENSIFICATION NETWORK
- SPECIAL SURVEYS
122GPS NETWORKS TO SUPPORT GIS CLASSICAL
123GPS NETWORKS TO SUPPORT GIS 21st CENTURY
124CLASSICAL GPS NETWORKS
- PROS
- Monumentation usually established in only 1 or 2
GPS survey campaigns - Complete coverage
- No time lag for users access to control
- CONS
- Large initial cost
- Continual network maintenance
- Monumentation destroyed or disturbed before
theyre used - System unfamiliar to non-surveyors
- Less efficient use of GPS receivers
125CONTEMPORARY GPS NETWORKS
- PROS
- Minimal permanent monumentation
- Project control established when and where needed
- Costs spread over time
- More user friendly to a wider range of spatial
data users - More efficient use of GPS receivers
- CONS
- Qualified staff to coordinate and administer user
requests - Time lag to establish project control
126GPS NETWORKS TO SUPPORT GIS
- GPS SURVEY DATA
- BLUE - BOOK SUBMISSION OF DATA FOR
- INCLUSION IN NSRS
- OR
- DATA MAINTAINED AT THE LOCAL LEVEL
127GPS NETWORKS TO SUPPORT GISBLUE-BOOK
- PROS
- DATA MAINTAINED IN NSRS IN PERPETUTITY
- UNIVERSAL DATA ACCESS VIA NGS WEB SITE
- GOOD HOUSEKEEPING SEAL OF APPROVAL
- CONS
- INCREASED INITIAL COST (15 - 20)
- SLIGHT INCREASE IN INITIAL DATA PROCESSING TIME
128GPS NETWORKS TO SUPPORT GISLOCAL MAINTENANCE
- PROS
- DECREASED INITIAL SURVEY COSTS
- LOCAL CONTROL OF ALL DATA
- CONS
- READJUSTMENTS TO FUTURE REFERENCE FRAME CHANGES
MUST BE DONE AT THE LOCAL LEVEL - DATA MAY BE DIFFICULT TO LOCATE FOR NON-LOCALS
- A.R.S. 33-137 REQUIRES PUBLISHING DATA
129NATIONAL GEODETIC SURVEY
dave.minkel_at_noaa.gov 602-542-1569
- INFORMATION CENTER
- (301) 713-3242
- info_center_at_ngs.noaa.gov
WEB SITE http//www.ngs.noaa.gov