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Geoid Modeling at noaa dru A. Smith, Ph. D
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tarix | 11.04.2018 | ölçüsü | 460 b. | | #37270 |
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Dru A. Smith, Ph.D. National Geodetic Survey National Ocean Service, NOAA November 13, 2000
Topics of Discussion The many definitions of “height” Why does anyone need a geoid model? NOAA resources and partnerships Geoid modeling 101 Current status and future directions
The many definitions of “height” Orthometric Height (H) - Height from the geoid to the Earth’s surface
- Frequently (informally) called “height above mean sea level”
- On most topographic maps
- e.g. “The Height of Mount Everest is 8848 meters”
The many definitions of “height” Ellipsoidal Height (h) - Height from the ellipsoid to the Earth’s surface
- Usually derived from GPS measurements
- Easy to obtain through GPS
- Has few physical applications
- e.g. water does not necessarily run ‘downhill’ in ellipsoid heights
The many definitions of “height” Geoid Height (N) - Height from ellipsoid up to geoid
- Also called “geoid undulation”
- N = h - H
- “N” determined from gravity measurements
Why do we need a geoid model? It saves money It saves time (but time = money) Additional scientific and economic uses:
The geographic community needs orthometric heights, H Old way: H = H0 + H (spirit leveling) - Time consuming, 4 person team. Expensive!
New way: H = h - N (GPS & geoid) - Fast, accurate, 1 person team. Cheap!
Part of NOAA’s “Height Modernization” program
Saving money with a geoid model Baltimore County GPS project, Phase III - Installed new vertical control benchmarks
- 290 square miles (1/3 of Baltimore county)
- Traditional leveling: 7 1/2 months / $174,000
- GPS and geoid: 3 weeks / $ 49,000
Savings: $125,000 = 72% !!
Saving money with a geoid model Baltimore county GPS project, Phase III - 1/3 of 1 county out of 3142 counties
- Informal extrapolation:
- The geoid could save 150-1500 million dollars for this application alone
- Depends on achieving an accurate geoid not just in Baltimore, but everywhere
NOAA is uniquely qualified to undertake this research Geoid research is cross-disciplinary
Within NOAA: Within NOAA: - NOS : NGS -- gravity database, GPS on leveled benchmarks and research on high resolution geoid modeling
- NESDIS : NGDC -- Gravity and topography data
- NESDIS : ORA : ORAD -- Satellite altimetry and oceanic gravity
Partner groups: Partner groups: - NIMA -- Significant gravity and DEM data
- USGS -- DEM data
- NASA -- Global gravity field with NIMA
- NTIA -- DEM data
- Universities -- Data and research
- States -- GPS cooperative surveys
- Other countries (Canada, Mexico, Caribbean, Denmark) -- Data and tech transfers
Geoid modeling 101 Gravity measurements every 5-10 km Digital elevation models (30-100 m) Global gravity field models GPS heights on leveled benchmarks
GEOID99 accuracy: GEOID99 accuracy: Absolute - +/- 2.5 cm about North American Vertical Datum of 1988 (NAVD 88)
Differential - +/- 0.2 to 3.5 cm between points 1 to 40+ km apart
Today: Surveyors can do sub-cm spirit leveling over lines up to 10 km long Today: Surveyors can do sub-cm spirit leveling over lines up to 10 km long Tomorrow: Surveyors expect to do 100+ km lines at similar accuracy with GPS and geoid (“GPS leveling”)
1 cm error budget (absolute and differential) 1 cm error budget (absolute and differential) Supercomputers? - Occasional, one shot, massive computations
- Maui supercomputer: Fall 2000 (UNM/USAFRL)
The geoid is the bridge between historical data sets and new cost-saving GPS technology The geoid is the bridge between historical data sets and new cost-saving GPS technology Geoid modeling is an integral part of Height Modernization The “1 cm geoid” is achievable in the USA within 10 years
Dr. Dru A. Smith 301-713-3202 x 149 Fax: 301-713-4172 Dru.Smith@noaa.gov www.ngs.noaa.gov/GEOID
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