Pages that link to "Item:Q704994"
From MaRDI portal
The following pages link to A solution to the downward continuation effect on the geoid determined by Stokes' formula (Q704994):
Displaying 13 items.
- Downward continuation of Helmert's gravity (Q697119) (← links)
- On the solvability of the Stokes pseudo-boundary-value problem for geoid determination (Q697126) (← links)
- On some problems of the downward continuation of the \(5'\times 5'\) mean Helmert gravity disturbance (Q697216) (← links)
- The exterior Airy/Heiskanen topographic-isostatic gravity potential, anomaly and the effect of analytical continuation in Stokes' formula (Q697236) (← links)
- Performance of three types of Stokes's kernel in the combined solution for the geoid (Q697238) (← links)
- A computation scheme to model the geoid by the modified Stokes formula without gravity reductions (Q705010) (← links)
- A general model for modifying Stokes' formula and its least-squares solution (Q705013) (← links)
- High-resolution regional geoid computation without applying Stokes's formula: a case study of the Iranian geoid (Q1013475) (← links)
- The effect of downward continuation of gravity anomaly to sea level in Stokes' formula. (Q1862581) (← links)
- Two different views of topographical and downward-continuation corrections in the Stokes-Helmert approach to geoid computation. (Q1862582) (← links)
- Downward continuation and geoid determination based on band-limited airborne gravity data. (Q1862636) (← links)
- The topographic bias by analytical continuation in physical geodesy (Q2477780) (← links)
- Polyhedral approximations in physical geodesy (Q5941603) (← links)