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Page 1: Geoid Modeling at NOAA

Geoid Modeling at NOAA

Dru A. Smith, Ph.D.National Geodetic SurveyNational Ocean Service, NOAA

November 13, 2000

Page 2: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

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

Page 3: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

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”

Page 4: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Page 5: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

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

Page 6: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

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

Page 7: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Page 8: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Why do we need a geoid model?

• It saves money

• It saves time (but time = money)

• Additional scientific and economic uses:– Geophysical: Oil and other subsurface features– Oceanographic: Sea level rise and current

modeling

Page 9: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Saving money with a geoid model

• 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

Page 10: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

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% !!

Page 11: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

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

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November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

NOAA resources / partnerships

• NOAA is uniquely qualified to undertake this research

• Geoid research is cross-disciplinary

Page 13: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

NOAA resources

• 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

Page 14: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

NOAA partnerships

• 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

Page 15: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Geoid modeling 101

• Gravity measurements every 5-10 km

• Digital elevation models (30-100 m)

• Global gravity field models

• GPS heights on leveled benchmarks

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November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Page 17: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Page 18: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Current Status

• 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

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November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Positioning for the Future

• 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”)

Page 20: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Achieving Higher Accuracies

• 1 cm error budget (absolute and differential)– Better theory– More data (Terabytes, USA; Petabytes, Globe)– More computational power

• Supercomputers?– Occasional, one shot, massive computations– Maui supercomputer: Fall 2000 (UNM/USAFRL)

Page 21: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Conclusions

• 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

Page 22: Geoid Modeling at NOAA

November 13, 2000Geoid Modeling at NOAA

Dr. Dru A. Smith

Contact Information

• Dr. Dru A. Smith

• 301-713-3202 x 149

• Fax: 301-713-4172

[email protected]

• www.ngs.noaa.gov/GEOID


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