Fundamentals of Geodesy

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Fundamentals of Geodesy
Presentation transcript:

Fundamentals of Geodesy Height Systems Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Orthometric Heights Discussed astronomic coordinates  and  give the position of a point on an equipotential surface To define position in 3D space a third coordinate is needed: In direction orthogonal to the level surface It gives the height of the level surface above or below the geoid The third coordinate is called orthometric height Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Orthometric Heights Orthometric height is the distance between the geoid and the level surface trough the point, measured along the plumb line. It is known that: Let dr point upward along the plumb line: Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Orthometric Heights Definition of orthometric height in terms of potential difference and gravity: The gravity cannot be measured inside the Earth’s body: Different approximations of gravity between the geoid and the Earth surface are used: Different height systems are possible Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Geopotential numbers Geopotential number C: The gravity potential difference between the geoid and the level surface of the point Orthometric height and Geopotential number Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Dynamic Heights Dynamic height : A constant gravity value is used instead of the real gravity: is normal gravity at sea level at latitude 45o Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Important Notes Points, which lie in the same level surface have: The same Geopotential numbers; W1=W2 The same Dynamic heights: Different orthometric heights!!! Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU

Is it possible? Eng. Petya Dimitrova, Dept. of Surveying and Geomatics, BAU