The effect of downward continuation of gravity anomaly to sea level in Stokes' formula

Journal of Geodesy

Volumn 74, Issue 11-12, 2001, Pages 796-804

  Sjoberg L E ^a  

^a ROYAL INSTITUTE OF TECHNOLOGY   (Sweden)

Author keywords

Analytical continuation; Geoid; Height anomaly; Stokes' formula; Topographic effects

Indexed keywords

GEOID; GRAVITY ANOMALY; SEA LEVEL; STOKES FORMULA;

EID: 0035037668     PISSN: 09497714     EISSN: None     Source Type: Journal    
DOI: 10.1007/s001900000143     Document Type: Article

References (18)

1. Stability investigations of a discrete downward continuation problem for geoid determination in the Canadian Rocky Mountains
2. Boundary-value problems for gravimetric determination of a precise geoid
3. The indirect effect of topography in the Stokes-Helmert technique for a spherical approximation of the geoid
4. Direct topographical effect of Helmert's condensation for a spherical geoid
5. 3 in gravimetric geoid determination
6. Accounting for topography in calculation of quasi-geoidal heights and plumb-line deflections from gravity anomalies
7. A new integral approach to geopotential coefficient determinations from terrestrial, gravity or satellite altimetry data
8. Refined least squares modification of Stokes formula
9. On quasi-geoid to geoid separation
10. The total terrain effect in gravimetric geoid determinations
11. The exterior Airy/Heiskanen topographic-isostatic gravity potential, anomaly and the effect of analytical continuation in Stokes' formula
12. On the topographic effects of Helmert's method of condensation
13. Topographic effects by the Stokes-Helmert method of geoid and quasi-geoid determinations
14. The indirect effect in geoid determination by Stokes-Helmert method
15. Generalized ridge regression with applications in determination of potential fields