1982
DOI: 10.1007/bf02525730
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An evaluation of orthometric height accuracy using bore hole gravimetry

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Cited by 13 publications
(10 citation statements)
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“…However, a true orthometric height cannot be computed exactly (e.g., Jekeli 2000), becauseḡ is inside the topography and cannot be measured (cf. Strange 1982;Tenzer et al 2005). There are a number of different methods of approximatingḡ, resulting in several variants of orthometric heights (e.g., Helmert 1890;Neithammer 1932;Mader 1954; Strang van Hees 1992; Kao et al 2000;Hwang and Hsiao 2003;Tenzer et al 2005).…”
mentioning
confidence: 99%
“…However, a true orthometric height cannot be computed exactly (e.g., Jekeli 2000), becauseḡ is inside the topography and cannot be measured (cf. Strange 1982;Tenzer et al 2005). There are a number of different methods of approximatingḡ, resulting in several variants of orthometric heights (e.g., Helmert 1890;Neithammer 1932;Mader 1954; Strang van Hees 1992; Kao et al 2000;Hwang and Hsiao 2003;Tenzer et al 2005).…”
mentioning
confidence: 99%
“…This requires knowledge of gravity variations (cf. Strange, 1982) or mass-density distribution (cf. Sünkel, 1986;Allister and Featherstone, 2001) inside the topography.…”
Section: Height Systems Related To Gravity: Natural or Physical Heightsmentioning
confidence: 99%
“…where g is the mean gravity along the plumb line (inside the Earth). As g cannot be observed directly (besides some stations with borehole gravity data; Strange 1982), hypotheses about the interior gravity field are necessary, which is one of the main drawbacks of the orthometric heights. Assuming a constant density of the topographic masses (2670 kg m -3 ) as well as a flat topography (so-called Poincaré-Prey reduction) leads to…”
Section: The Geoid and Heightsmentioning
confidence: 99%