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Published byKenneth Reynard Garrett Modified over 9 years ago
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Who Needs New Datums? NGS Says… ftp://ftp.ngs.noaa.gov/pub/marti Marti Ikehara California Geodetic Advisor, Sacramento
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Outline New datums down the road GRAV-D Program New datum, epoch for CORS soon Visualizing Geodetic control VDATUM
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What IS a datum? It is NOT the same (concept) as a “projection”, which controls how maps are represented or “look” on paper or on a screen. It is a reference, a basis, for coordinates, so a datum has an origin and/or ‘zero’. “Underlying” a horizontal datum system is an ELLIPSOID, that represents the global shape of the earth; a DATUM is the ‘continental’ shape as realized with physical marks (passive or active)
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The National Geodetic Vertical Datum of 1929 was referenced to 26 tide gauges in the US and Canada
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The North American Vertical Datum of 1988 is referenced to a single tide gauge in Canada
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EQUIPOTENTIAL SURFACES
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GEOID09 compared to GEOID03 09: teal, good; yellow: State advisor-rejected; red: analysis-rejected 03 (underlying dots): dk blue, kept; orange: rejected
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From Helmer’s article in Winter 09/10 issue of California Surveyor
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2009 National Research Council Report “…uniform national standards for FEMA flood maps cannot be met until an improved orthometric height datum and geoid model exist…”
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Rationale for new Datums Terminology – Horizontal becomes GEOMETRIC – Vertical becomes GEOPOTENTIAL When?2018, if GRAV-D program is complete Why? But why?! 1.Primarily need a better vertical datum for “vertical” data(geoid, ortho ht) not obtained by traditional leveling 2.Geodetic Data collection relies upon navigation (GNSS) satellites orbiting around the mass center of the Earth – NAD83 reference frame/datum is not geocentric
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X Z Y Earth-Centered Earth-Fixed (ECEF) Coordinate System Earth Mass Center Greenwich Meridian -X-Y -Z X, Y, Z = 0 X A, Y A, Z A (not NAD83) GRS 80 Ellipsoid
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Simplified Concept of NAD 83 vs. ITRF00 (or WGS84) 2.2 meters NAD 83 Origin ITRF 00 Origin Earth’s Surface h 83 h 00 Identically shaped ellipsoids (GRS80) a = 6,378,137.000 meters (semi-major axis) 1/f = 298.25722210088 (flattening)
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Rationale for new Datums Terminology – Horizontal becomes GEOMETRIC – Vertical becomes GEOPOTENTIAL When?2018, if GRAV-D program is complete Why? But why?! 1.Primarily need a better vertical datum for “vertical” data(geoid, ortho ht) not obtained by traditional leveling 2.Geodetic Data collection relies upon navigation (GNSS) satellites orbiting around the mass center of the Earth – NAD83 reference frame/datum is not geocentric 3.Earth is not stable in all directions; reference frame must account for this to be as geodetically accurate as possible – NAD83 is not defined to include vertical velocities
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Horizontal Velocities, relative to ‘stable’ NA tectonic plate, are reflected in HTDP model
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Worldwide Tectonic Horizontal Motions
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CORS Data allows for Monitoring Vertical Crustal Motion Vertical velocities associated with Glacial Isostatic Adjustment (rebound)
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H + H t + V E + V Et 2 + 2 + 1+ 1 ITRF00 (2002.00) Evolution of Geodetic Datums: from NAD27/NGVD29 to NAD83/NAVD88 to ?/ ? H + V 2 + 1 27, 29 H + V 2 + 1 83(86), 88 H + V E + V O 2 + 1 + 1 83(92), 88 GPS +VELOCITIES (time) H + H t + V E + V O 2 + 2 + 1+ 1 83(07)+HTDP, 88 + GRAVITY (geoid model) H + H t + V E + V Et 2 + 2 + 1+ 1 GEOMETRIC (V E +G)[+V Et ] + G t 1 + 1 GEOPOTENTIAL
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The Future of Height Mod: GRAV-D Gravity for the Redefinition of the American Vertical Datum GRAV-D –Airborne gravity surveys (taking 10 years) –Coastal areas surveyed first –All USA states and territories –www.ngs.noaa.gov/GRAV-D GOAL: –Orthometric heights-”elevations” – to be good to 2 cm anywhere, anytime with an excellent ellipsoid height from GNSS technology. Currently this takes 3-4 hours at 15-second recording and dual-frequency GPS –Height changes much more easily monitored than by leveling, using new technology – GNSS heights and gravity values –Spot-checking/monitoring gravity changes with portable field units
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Hawaii Alaska “CONUS” Puerto Rico / Virgin Islands Guam / Northern Marianas American Samoa Planned GRAV-D Coverage
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NGA funded NRL plane USACE funded As of Jan 2010: 6.7% of planned areas have been flown Status of GRAV-D in early 2010
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Preliminary GRAV-D Results
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New datum, epoch for CORS Current: ITRF2000, 2002.00 Near end of year: ITRF2008, 2008.00 – NAD83 (“CORS96A”), 2010.00 No change to passive monumentation, eg, NAD83 (NSRS2007), 2007.00 About 1000 CORS nationwide – Those with >2 years of data – Changes on the order of mm, but some outliers are showing closer to decimeters – List will be prepared, showing amount of change
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http://www.dot.ca.gov/hq/row/landsurveys /geodetic/geodetic_control.html
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Datums available in VDATUM
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www.vdatum.noaa.gov
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Anything Else?! Marti.ikehara@noaa.gov 916-227-7325 ftp://ftp.ngs. ftp://ftp.ngs noaa.gov/pub/marti
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