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Gravity, Geoids, and Other Vertical Datums in the Puerto Rico/Virgin Islands Region. Dr. Daniel R. Roman and Dr. Yan Ming Wang. Geodetic Ellipsoidal Height and/or Datum (h) Geodetic or Orthometric Height and/or Datum (H) Geoid Height (N) h = H + N - PowerPoint PPT Presentation
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Gravity, Geoids, and Other Vertical Datums
in the Puerto Rico/Virgin Islands
Region
Dr. Daniel R. Roman
and Dr. Yan Ming Wang
Significant Concepts & TermsGeodetic• 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
T
N R
T
r
Tg
2
OCEAN Earth
’s
Surfa
ce
“Ellipsoid”
Geopotential Surface
Geopotential Surface
Geopotential Surface
“Geoid”
“P”
“Q”
h
N
h = H + NΔg = gP - γQ
“P”0
H
Normal to geoid
Normal toellipsoid
Deflection of Vertical
MSL
LMSL
MDT
ellipsoid
geoid
tide station/datum point
MSL + MDT = LMSL
N local geodetic datum
predicted storm surge reachactual storm
surge reach
unexpected area of storm surge
bias
From the National Geospatial-Intelligence Agency Website at:http://cddis.gsfc.nasa.gov/926/egm96/egm96.html
Statistical Comparison Between Available Geoid Height Models and 13-Point GPS on BM Profile Along NW Puerto Rico Shoreline
Geoid Height Model
Average (m) St. Dev. (m)
GEOID99 2.34 0.04
CARIB97 2.53 0.04
EGM96 2.07 0.73
No Biases Removed from GEOID99, CARIB97, or EGM96 Differences with GPSBM's
0.00
0.50
1.00
1.50
2.00
2.50
3.00
3.50
1 2 3 4 5 6 7 8 9 10 11 12 13
GPS on BM station
Res
idu
al G
eoid
Hei
gh
t (m
)
GEOID99 CARIB97 EGM96
Biases Removed for GEOID99 (2.34 m), CARIB97 (2.53 m), and EGM96 (2.07 m)
-1.00
-0.80
-0.60
-0.40
-0.20
0.00
0.20
0.40
0.60
0.80
1.00
1 2 3 4 5 6 7 8 9 10 11 12 13
GPS on BM station
(Rel
ativ
e) R
esid
ual
Geo
id H
eig
ht
(m)
GEOID99 CARIB97 EGM96
SRTM 30 m SRTM 90 m NED 1 arcsecond
Available Elevation Data Sets
Conclusions
• 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
Outlook
• 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