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Height systems Rudi Gens Alaska Satellite Facility Outline y Why bother about height systems? Height systems y Relevant terms y Coordinate systems y Reference surfaces y Geopotential number y Height systems 2 Why bother about height systems? Height systems y give a meaning to a value defined for height y combination of measurements from different sources x GPS measurements vs. leveling measurements y three-dimensional calculations x SAR interferometry 3 Relevant terms y spheriod Height systems x any surface resembling a sphere x an ellipsoid of revolution y ellipsoid x defined by axes, flattening and eccentricity y flattening and eccentricity x characterize the deviation from a sphere 4 Geographical and geodetic coordinates Height systems f b a Geographic latitude Geodetic latitude 5 Geographical and geodetic coordinates y geographical coordinates Height systems x implying spherical Earth model y geodetic coordinates x implying ellipsoidal Earth model 6 Height systems Cartesian coordinates y geodetic coordinates inappropriate for satellite imagery Æ cartesian coordinates 7 Approximation vs. Reality Height systems y ellipsoid is a good approximation to the shape of the Earth but not an exact representation y Earth surface is everywhere perpendicular to the direction of gravity Æ equipotential surface y true shape of the Earth is known as geoid 8 Height systems Reference surfaces y three reference surfaces x topography x geoid x ellipsoid 9 Height systems Reference surfaces y topography represents the physical surface of the Earth 10 Height systems Reference surfaces y geoid defined as level surface of gravity field with best fit to mean sea level x maximum difference between geoid and mean sea level about 1 m 11 Height systems Reference surfaces y ellipsoid defines mathematical surface approximating the physical reality while simplifying the geometry 12 Height systems Reference surfaces y geoid undulation: vertical separation between geoid and reference ellipsoid x differences between ± 100 m x global root mean square of around 30 m 13 Height systems Reference surfaces y vertical deflection: angle between the ellipsoid normal and the plumb line x usually resolved in a north-south component ξ and an east-west component η x angles usually amount to a few arc seconds 14 Global earth model Height systems y geoid defined by a set of coefficients of a spherical harmonic expansion Æ global earth model y several models available x OSU91 x Earth Geopotential Model 1996 (EGM96) 15 Geopotential number Height systems y different height systems can be related to each other by the geopotential number C C = W0 − W = ∫ point geoid g dn x W and W0: the potentials of gravity of a point and the geoid x g: gravity value x dn: leveling increment 16 Geopotential number Height systems y different heights calculated by dividing the geopotential number by a gravity value 17 Heights Height systems y dynamic height x constant normal gravity γ0 for an arbitrary standard latitude (usually 45 degrees) x no geometrical meaning y orthometric height x natural “height above sea level” x measured along the current plumb line from the foot point on the geoid and the point on the surface x gravity value: mean gravity 18 Heights Height systems y normal height x vertical distance from terrain surface to the ellipsoid reduced by the height anomaly x measured along the ellipsoidal normal x gravity value: mean normal gravity 19 Solution y ellipsoid is convenient reference frame Height systems x mathematical figure x provides good approximation to the geoid y geoid better height reference system x reference to mean sea level allows to use tide gauges as height reference points x physical significance: ensures horizontal representation of water surfaces such lakes and seas 20 Questions Datums y datum Height systems x describes the relationship between a particular local ellipsoid and a global geodetic reference system y coordinate system x shape and size given by the ellipsoid x position given by the fixing of the origin x fixing of the origin defines a datum 22 Datums y global datums (geocentric) Height systems x Geodetic Reference System 1980 (GRS 80) x World Geodetic System 1984 (WGS 84) y local datums x North American 1927 23