Results 71 to 80 of about 173 (112)
Ship wake-induced water column mixing and meter-scale seabed erosion in the Baltic Sea. [PDF]
Geersen J +9 more
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Reference the seabed topographic depth observations based on the national mean dynamic topography model. [PDF]
Luong TT +8 more
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STUDY ON ACHIEVING A QUASIGEOID
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Comparative analyses of quasigeoid models for the Republic of Moldova territory
В даній статті представлені результати порівняння моделей квазігеоїда для території Республіки Молдова з використанням GNSS-вимірювань для нівелювання.
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Determination of quasigeoid heights.
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LOCAL QUASIGEOID MODELLING IN IASI CITY AREA
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Mold2012 : a new gravimetric quasigeoid model over Moldova
In order to be able to use the operational Moldavian GNSS Positioning System MOLDPOS efficiently for the determination of normal heights in surveying engineering, e.g. during the construction of a road, an accurate quasigeoid model is needed. The main goal of this thesis is to present a new gravimetric quasigeoid model for Moldova (Mold2012), which has
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On the geoid–quasigeoid separation in mountain areas
Journal of Geodesy, 2009The separation between the reference surfaces for orthometric heights and normal heights—the geoid and the quasigeoid—is typically in the order of a few decimeters but can reach nearly 3 m in extreme cases. The knowledge of the geoid–quasigeoid separation with centimeter accuracy or better, is essential for the realization of national and international
Jakob Flury +2 more
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Spatial and Spectral Representations of the Geoid-to-Quasigeoid Correction
Surveys in Geophysics, 2015In geodesy, the geoid and the quasigeoid are used as a reference surface for heights. Despite some similarities between these two concepts, the differences between the geoid and the quasigeoid (i.e. the geoid-to-quasigeoid correction) have to be taken into consideration in some specific applications which require a high accuracy.
Robert Tenzer +2 more
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Quasigeoid-to-geoid determination by EGM08
Earth Science Informatics, 2012We present a method to estimate the difference between quasigeoid and geoid heights globally from the Earth Gravitational Model EGM08 and a related topographic model. The numerical computations with the standard topographic density of 2.67 g/cm3 show that the maximum and minimum of the separations are estimated to 5.47 m and −0.11 m on the Tibet ...
Lars E. Sjöberg, Mohammad Bagherbandi
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