2015
DOI: 10.1007/1345_2015_145
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Height Datum Unification by Means of the GBVP Approach Using Tide Gauges

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Cited by 8 publications
(4 citation statements)
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“…This datum is assigned a value of 0.00 metres, (0.00 metres AHD-corrected), as the mean sea level for 1966-1968 [38]. It is important to note that the mean sea-level value should be calculated from 19-year-long continuous records of water levels [46], presenting a limitation to the accuracy of the Australian datum as this was only calculated over three years. The eBTM requires a starting point for the inland inundation to be modelled.…”
Section: Input Datamentioning
confidence: 99%
See 1 more Smart Citation
“…This datum is assigned a value of 0.00 metres, (0.00 metres AHD-corrected), as the mean sea level for 1966-1968 [38]. It is important to note that the mean sea-level value should be calculated from 19-year-long continuous records of water levels [46], presenting a limitation to the accuracy of the Australian datum as this was only calculated over three years. The eBTM requires a starting point for the inland inundation to be modelled.…”
Section: Input Datamentioning
confidence: 99%
“…Consequently, it is inferable that the elevation is the variable driving the relationship between water bodies and their susceptibility to coastal inundation. As water bodies such as creeks and rivers largely feature physical characteristics of lower elevations and smaller changes in elevation (slope) than along coastlines, such areas are thus more conducive to inland coastal inundation [46]. While this is in part due to the Mackay study region being 365 km 2 , 67 times larger than the Cape Town study area of approximately 5.4 km 2 , this relationship is of note as it further affirms the strong relationship between elevation and inundation extent.…”
Section: Comparing Modelsmentioning
confidence: 99%
“…(3) The third method is estimating the anomalous potential by solving the geodetic boundary value problem (GBVP) [8]. It can provide a global solution for height unification, and the precision in well-surveyed regions reaches several centimeters [9][10][11]. However, in sparsely surveyed regions, the precision drops to the decimeter level [5].…”
Section: Introductionmentioning
confidence: 99%
“…(3) The third method is estimating the anomalous potential by solving the geodetic boundary value problem (GBVP) (Rummel and Teunissen, 1988). It can provide a global solution for height unification, and the precision in well-surveyed regions reaches several centimeters (Amjadiparvar et al, 2016;Gerlach and Rummel, 2013;Rangelova et al, 2016). But in sparsely surveyed regions the precision drops to decimeter level (Sánchez and Sideris, 2017).…”
Section: Introductionmentioning
confidence: 99%