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- Dr. Daniel R. Roman
- and Dr. Yan Ming Wang
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- Geodetic
- Ellipsoidal Height and/or Datum (h)
- Geodetic or Orthometric Height and/or Datum (H)
- Geoid Height (N)
- h = H + N
- The geoid and gravity anomalies are related mathematically:
- Oceanographic
- Global Mean Sea Level (MSL)
- Local MSL (LMSL) or Local Mean Tide
- Mean Dynamic Topography (MDT)
- MSL + MDT = LMSL
- MSL => Geodetic Datum
- LMSL => Local Vertical Datum
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- Tidal and Geodetic datums are related
- Additional gravity data are required
- Geoid modeling is best constrained with additional oceanic gravity
observations
- Some limited terrestrial observations will help fill in gapped regions
but also help to eliminate any
datum problems
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21
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- Improved terrain models already exist to help model the shortest
wavelengths
- Simultaneous lidar observations would help to model the local sea
surface and any implied datum shifts
- Impending satellite gravity missions aid in resolving global mean sea
level
- A future gravimetric geoid can be generated that will cover CONUS &
PR/VI
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