The high-degree ellipsoidal Stokes integral (Ardestani and Martinec, 2003a) is used to compute the geoidal heights over a territory in Iran. To compute the low-degree part of the geoidal heights a global geopotential model (EGM96) is used and for the high-degree part, the solution of the ellipsoidal Stokes boundary-value problem (BVP) in the form of surface integral is applied.
Therefore the geoidal heights con be calculated for a part of Iranian territory where the data is available.
E. Ardestani, V. (2006). The Iranian geoid by high-degree ellipsoidal Stokes integral. Journal of the Earth and Space Physics, 32(1), 1-5. doi: 10.22059/jesphys.2006.80070
MLA
Vahid E. Ardestani. "The Iranian geoid by high-degree ellipsoidal Stokes integral", Journal of the Earth and Space Physics, 32, 1, 2006, 1-5. doi: 10.22059/jesphys.2006.80070
HARVARD
E. Ardestani, V. (2006). 'The Iranian geoid by high-degree ellipsoidal Stokes integral', Journal of the Earth and Space Physics, 32(1), pp. 1-5. doi: 10.22059/jesphys.2006.80070
VANCOUVER
E. Ardestani, V. The Iranian geoid by high-degree ellipsoidal Stokes integral. Journal of the Earth and Space Physics, 2006; 32(1): 1-5. doi: 10.22059/jesphys.2006.80070
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